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Sample records for fase solida granitoides

  1. Estudio del comportamiento de una sustancia de cambio de fase con condición de borde convectiva

    OpenAIRE

    Lozano, Ricardo; Villa Saravia, Luis Tadeo; Bouciguez, Angélica Carmen

    2016-01-01

    El proceso de fusión - solidificación, ha sido abordado con anterioridad, procurando soluciones a problemas de difusión con cambio de fase, cuando estando inicialmente solidas a la temperatura de fusión son sometidas a un flujo de calor por uno de sus laterales. Un flujo interesante es el convectivo, pues es la forma más realista de entrada o extracción de calor a la sustancia de cambio de fase. Dada esta condición de borde resulta interesante observar el comportamiento de la sustancia, cuand...

  2. Solida: A Blockchain Protocol Based on Reconfigurable Byzantine Consensus

    OpenAIRE

    Abraham, Ittai; Malkhi, Dahlia; Nayak, Kartik; Ren, Ling; Spiegelman, Alexander

    2018-01-01

    The decentralized cryptocurrency Bitcoin has experienced great success but also encountered many challenges. One of the challenges has been the long confirmation time. Another chal- lenge is the lack of incentives at certain steps of the protocol, raising concerns for transaction withholding, selfish mining, etc. To address these challenges, we propose Solida, a decentralized blockchain protocol based on reconfigurable Byzantine consensus augmented by proof-of-work. Solida improves on Bitcoin...

  3. Solida: A Blockchain Protocol Based on Reconfigurable Byzantine Consensus

    OpenAIRE

    Abraham, Ittai; Malkhi, Dahlia; Nayak, Kartik; Ren, Ling; Spiegelman, Alexander

    2016-01-01

    The decentralized cryptocurrency Bitcoin has experienced great success but also encountered many challenges. One of the challenges has been the long confirmation time. Another challenge is the lack of incentives at certain steps of the protocol, raising concerns for transaction withholding, selfish mining, etc. To address these challenges, we propose Solida, a decentralized blockchain protocol based on reconfigurable Byzantine consensus augmented by proof-of-work. Solida improves on Bitcoin i...

  4. Petrological mineralogical and geochemical characterization of the granitoids and fracture fillings developed in Ratones Mines (Spain); Caracterizacion petrologica, mineralogica, geoquimica y evaluacion del comportamiento geoquimico de las REE en la fase solida (granitoides y rellenos fisurales) del sistema de interaccion agua-roca delentorno de la Mina Ratones

    Energy Technology Data Exchange (ETDEWEB)

    Buil Gutierrez, B [Ciemat. Madrid (Spain)

    2002-07-01

    The petrological, mineralogical and geochemical characterisation of the granitoids and fracture fillings developed in the Ratones Mine (Caceres, Spain) has been done in order to understand rock-water interaction processes which control water geochemical parameters. Special interest has been devoted to the analysis and interpretation of REE patterns in the solid phase (granitoids and fracture fillings) because they constitute geochemical tracers in water-rock interaction process. Moreover, REE are considered as actinide analogues. In order to characterise the solid phase (granitoids and fracture fillings) several investigation scales (system, outcrop, whole rock, mineral and geochemical components) have been considered and different types of samples have been analysed. These factors control the methodological approach used in this investigation. The analytical methods we have used in this investigation are microscope, qualitative and semi-quantitative methods (XRD, SEM,EDAX) and quantitative methods (ICP-MS, XRF, EM, LAM-IC-MS). The bulk of the granitoids located around the Ratones Mine Belongs to the alkaline feldspar granite-sienogranite lihotype and they show a peraluminous and subalkaline pattern. From the mineralogical point of view, they are composed by quartz, K-feldspar (Or>90%), showing sericitation, moscovitization and turmolinization altherations, alkaline plagioclase (An-=-3%), usually altered to sericite, saussirite and less frequently affected by moscovitization processes, Fe-Al biotite, frequently affected by chloritization processes and sometimes replaced by muscovite, and finally muscovite (>2% celadonite and <4% paragonite) both of primary and secondary origin. The differences observed between the different lithotypes are related with the modal proportion of the principal minerals,with the presence or absence of certain accessory minerals ( turmaline, cordierite), with specific textural patterns, grain size and also with the richness in specific

  5. Desarrollo embrionario y larval temprano de Gari solida (Gray, 1828 (Bivalvia: Psammobiidae

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    Ramiro Contreras

    2014-03-01

    Full Text Available Se describe el desarrollo temprano del culengue (Gari solida (Gray, 1828 hasta el estado inicial de larva velígera, a partir de dos desoves efectuados en el verano de 2009. El desove se indujo a 80 ejemplares maduros, entre 50-60 mm de longitud valvar, mediante desecación a temperatura ambiente por aproximadamente media hora y posterior choque térmico (12-14°C y 23-25°C. Los reproductores fueron previamente acondicionados durante 90 días a 14°C en promedio, alimentados con Isochrysis aff galbana (T-Iso, Chaetoceros calcitrans y Tetraselmis suecica en proporción 1:1:1, a una concentración de 300.000 cel mL-1. Los ovocitos se fertilizaron en proporción de 10:1 espermatozoide/ovocito y se incubaron en estanques de 50 L, a 15 ± 0,8°C, sin aireación, con agua de mar filtrada a 1 μm e irradiada con luz ultravioleta. Se efectuaron observaciones y mediciones de los estados de embriogénesis y larva velígera tipo D, registrándose el tiempo de duración de cada fase. La embriogénesis se completó entre 23-24 h post- fecundación (pf y el estado de larva velígera tipo D se alcanzó en 36-37 h pf, midiendo 78 ± 4,7 μm de longitud. Una cubierta gelatinosa rodea al ovocito y se mantiene hasta que se desarrolla completamente la larva D libre nadadora, en 50-52 h pf. Este trabajo constituye un primer reporte sobre el desarrollo temprano de G. solida. Para profundizar en este conocimiento sería deseable incluir técnicas de microscopía electrónica en futuros estudios.

  6. Geología de la parte sur de la Sierra de San Luis y granitoides asociados, Argentina

    Directory of Open Access Journals (Sweden)

    Llambías, E. J.

    1992-12-01

    , cuarcitas y filitas. El grado metamórfico intermedio está representado por esquistos biotíticos cuarzo oligoclásicos con abundantes venas pegmatoideas. El más alto grado metamórfico está representado por gneises, anfibolitas y migmatitas y al mismo están asociados los cuerpos máficos a ultramáficos. Se han reconocido tres fases de deformación, siendo la última (D3, ordovícica, la que imprime la estructura más marcada.Los granitoides se han agrupado respecto de D3 en pre-, sin- y post-cinemáticos. Los primeros se encuentran en las fajas de bajo grado metamórfico y están compuestos por tonalitas, granodioritas y monzogranitos, fuertemente deformados. Su edad se desconoce. Los cuerpos sin-cinemáticos son predominantemente leucogranodioritas con granate y muscovita. Muestran bajo contraste reológico y térmico con respecto a la caja. Su edad es de 454 ± 21 m.a. Los granitoides post-cinemáticos son comúnmente monzogranitos con megacristales de feldespato potásico, ricos en titanita. Son discordantes, subcirculares y están asociados a una fase distensiva. Su edad está comprendida entre 423 y 320 m.a. y marca la finalización del ciclo Famatiniano.

  7. Rb-Sr isochronous age of Vepor pluton granitoids

    International Nuclear Information System (INIS)

    Bagdasaryan, G.P.; Gykasyan, R.Kh.; Cambel, B.

    1986-01-01

    The result are presented of geochronological investigations of the Vepor pluton granitoids by the Rb-Sr isochronous method. The results prove the Variscan age of granodiorite magmatism of the Sihla type (387±27 m.y.) and the Early Variscan age of leucocratic granitoids of the Vepor and the Ipel types (284±22 m.y.). Since the initial ratio of 87 Sr/ 86 Sr in granitoids of the Sihla type is 0.7054 and of the Vepor type 0.7060, it can be assumed that during the formation of the granitoids of veporides there was an increased supply of matter from the main source affecting genesis of granitoids. The results prove a polyphase character of the Variscan granitoids of Veporicum. (author)

  8. Petrotectonic framework of granitoids and associated granulites at ...

    Indian Academy of Sciences (India)

    tion that wraps around the feldspar augen. The sheared granitoid ..... 1987) has been used to classify the granitoids ... The data for all the analyses used in the diagrams are given in table 1. ..... Different stages of crystal-plastic deformation are.

  9. Histopathological survey of the mussel Mytilus chilensis (Mytilidae and the clam Gari solida (Psammobiidae from southern Chile

    Directory of Open Access Journals (Sweden)

    Florencia Cremonte

    2015-03-01

    Full Text Available A total of 175 specimens of mussels, Mytilus chilensis (Mytilidae, and 56 specimens of clams, Gari solida (Psammobiidae, were collected in natural beds and culture sites of southern Chile. Juvenile mussel specimens (3 cm of maximum length were free of parasites and diseases, whilst the commercial sized populations was parasitized by intracellular inclusions of bacteria-like organisms in the digestive gland epithelium and in the gills, by ciliates in the gills, turbellarians similar to Paravortex (Rhabocoela in the intestine lumen and copepods attached to the gills. In addition, the disseminated neoplasia disease was also present although in low prevalences. In the clam, G. solida, prokariotic inclusions were found in the digestive gland epithelium and bacteria-like organisms in the gills, often encapsulated by haemocytes; oocysts containing up to 8 sporozoites similar to Nematopsis (Apicomplexa in the connective tissue, causing haemocytic infiltration when the intensity of infection was high; ciliates belonging to two different species (one of them similar to Trichodina inhabiting the gills; and a turbellarian similar to Paravortex in the lumen of digestive system without apparent host reaction. The populations of the bivalve species here studied were devoid of serious pathogens.

  10. Potassium-argon ages of two granitoids northwest of Kumasi, Ghana

    International Nuclear Information System (INIS)

    Agyei, E.K.

    1989-01-01

    Four granitic samples from two granitoids northwest of Kumasi,Ghana, have been dated using the conventional K-Ar method. Two samples NB1 NB2 from a road-cutting at Nyamebekyere village, located about 60 km from Kumasi on the Kumasi-Sunyani road gave biotite ages of 2144+/= 11 Ma and 2144+/=7 Ma, respectively. The biotite ages for two samples NTN1 and NTN2 from Kassardjan quarry, located about 3 km south of the Kumasi-Sunyani road at Ntensere village some 20 km northwest of Kumasi were 2070+/= 10 Ma and 2099+/=14 Ma, respectively. A hornblende age of 2169+/=26 Ma was obtained for NTN2 which suggests a slow cooling during the uplift of the granitoid. Although the biotite ages obtained here for the two G2 granitoids are older than most of the reported biotite ages which happen to be for G1 granites, it is too premature to generalize that G2 granitoids are older than G1 granitoids. (author). 21 refs. 1 fig. 1 tab

  11. Distribution of natural radioactive elements in Western Carpathians granitoids

    International Nuclear Information System (INIS)

    Katlovsky, V.

    1979-01-01

    The content of natural radioactive elements was determined using the 1024-channel analyser NTA-512 B with NaI(Tl) scintillators or with a Ge(Li) detector. The following groups of samples were processed: 1. granitoids, pegmatites and weathered rocks in the Small Carpathians; 2. acid magmatites of exotic rocks of the klippen zone; 3. granitoids of the Western Carpathians. The results of the measurements are summed up. (Ha)

  12. The age of Male Karpaty Mts. granitoid rocks determined by Rb-Sr isochrone method

    International Nuclear Information System (INIS)

    Badgasaryan, G.P.; Gukasyan, R.Kh.; Veselsky, J.

    1982-01-01

    The results are presented of nuclear geochronological datings of Male Karpaty Mts. granitoids by Rb-Sr isochrone method. Using the method the age of Bratislava massif granitoids was established to be 347+-4 mil. y. at ( 87 Sr/ 86 Sr)=0.7076+-0.0013 and the age of Modra massif granitoids to be 324+-18 mil. y. at ( 87 Sr/ 86 Sr)=0.7075+-0.00032 (2σ). The relative agreement of age of both massifs as well as the agreement of the primary ratio ( 87 Sr/ 86 Sr) 0 not only testifies to their continuity in age but also in genesis. The same relations also confirm the genetic dependence of pegmatites and leucocratic granitoids on fundamental types of granitoids building up the Bratislava and Modra massifs. (author)

  13. DURATION OF GRANITOID MAGMATISM IN PERIPHERAL PARTS OF LARGE IGNEOUS PROVINCES (BASED ON 40AR/39AR ISOTOPIC STUDIES OF ALTAI PERMIAN-TRIASSIC GRANITOIDS

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    O. A. Gavryushkina

    2017-01-01

    Full Text Available In large igneous provinces (LIP of fold areas, granitoid rocks are dominant, while mantle-derivated rocks play a subordinate role in rock formation. If magma emissions are impulsive, it may take 25–30 million years for a LIP to form and take shape. In this paper, we present the results of 40Ar/39Ar isotopic studies of Permian-Triassic grani­toids in the Altai region, Russia, and clarify the evolution of this region located at the periphery of the Siberian LIP. These granitoids are very diverse and differ not only in their rock set, but also in the composition features. In the study region, the granodiorite-granite and granite-leucogranite association with the characteristics of I- and S-types as well rare metal ore-bearing leucogranites are observed along with gabbro- and syenite-granite series, including mafic and intermediate rocks with the A2-type geochemical features. The 40Ar/39Ar data obtained in our study suggest that most of the studied granitoids intruded within a short period of time, 254–247 Ma. This timeline is closely related to the formation of granitoids in theKuznetsk basin and dolerite dikes in the Terekta complex (251–248 and 255±5 Ma, respectively, as well as intrusions of lamproite and lamprophyre dikes of the Chuya complex (245–242 and 237–235 Ma. Thus, we conclude that the Altai Permian-Triassic granitoids are varied mainly due to the evolution of mafic magmatism.

  14. Condición somática de la almeja Polymesoda solida (Veneroidea: Corbiculidae durante el periodo lluvioso, enel Parque Natural Isla de Salamanca, Caribe colombiano

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    María Virginia De La Hoz Aristizábal

    2010-03-01

    Full Text Available Se evaluó la condición somática de la almeja Polymesoda solida en tres lagunas del Parque Isla de Salamanca (abril a noviembre de 2004, durante el periodo lluvioso. En 60 individuos por laguna, se analizaron mensualmente índices de condición, rendimiento, relación talla-peso y madurez gonadal en fresco. También se midió salinidad, temperatura, pH, oxígeno disuelto, transparencia y profundidad del agua. Los mayores índices de condición coincidieron con descensos en el nivel del río Magdalena, especialmente en Poza Verde y El Torno. Estos índices fueron más altos en tallas entre 27mm y 33mm, donde también se ubicó la talla media de madurez sexual. En Poza Verde, laguna con mayor influencia del río, se presentaron los mayores índices de condición, rendimiento, peso húmedo y frecuencia de madurez, revelando una mejor condición de los organismos. El índice de condición (peso cuerpo/ peso concha presentó mayor coeficiente de regresión múltiple con la salinidad, pH y transparencia, sugiriendo la importancia del régimen hidrológico en su regulación. Las diferencias espaciales en las variables evaluadas, resaltan la necesidad de tener en cuenta la heterogeneidad de este tipo de estuarios para la conservación y manejo adecuado de la pesquería de P. solida.Somatic condition of the clam Polymesoda solida (Veneroidea: Corbiculidae in the rainy season of the Salamanca Island Natural Park, Colombian Caribbean. The estuarine clam Polymesoda solida is the main fishery resource in the Salamanca Island Natural Park. I sampled the clam in three interconnected lagoons (Poza Verde, El Torno and Atascosa during the rainy period (April to November 2004. Sixty individuals were monthly collected by hand on each lagoon; 30 to analyze two condition indexes (relationship between body and shell weight and between soft dry and wet weight, yield (meat percentage and length-weight relationships. Maturity of female gonad smears was assessed on the

  15. Radiation Polymerization in the Solid Phase; Polymerisation radiochimique en phase solide; Radiatsionnaya polimerizatsiya v tverdoj faze; Radiopolimerizacion en fase solida

    Energy Technology Data Exchange (ETDEWEB)

    Barkalov, I. M.; Gol' danskij, V. I.; Enikolopov, N. S.; Terekhova, S. F.; Trofimova, G. M.

    1963-11-15

    u otra sustancia adecuada. Por ejemplo, en la radiopolimerizacion de una serie de monomeros orientados en complejos clatraticos de urea y tiourea, se obtienen polimeros cristalinos de estructura espacial regular. Sin embargo, el procedimiento mas sencillo consiste en orientar el monomero en el propio reticulado cristalino. Aunque todavia quedan por dilucidar numerosos aspectos teoricos de esta cuestion, la aplicacion practica del metodo parece sumamente promisoria. Asi, en la radiopolimerizacion del trioxietileno cristalino, se obtiene un polioximetileno altamente cristalizado. Con todo, es necesario proseguir el estudio teorico de esta cuestion. Para cada monomero resulta indispensable determinar en que medida los distintos tipos de reacciones que se desarrollan durante la irradiacion y la fusion consecutiva de los monomeros solidos (reaccion radioquimica especifica, postpolimerizacion y polimerizacion en los puntos de transicion de las fases) contribuyen al conjunto del proceso. El estudio detallado de la radiopolimerizacion de una serie de monomeros, mediante el metodo calorimetrico y la observacion de la resonancia paramagnetica de los electrones llevada a cabo recientemente en el Instituto de fisicoquimica de Moscu, ha demostrado que la reaccion radioquimica especifica desempefia el papel fundamental en el curso de la irradiacion. Una vez concluida esta, los procesos de polimerizacion del acrilnitrilo (entre -196{sup o}C y -140{sup o}C) y del acetato de vinilo (entre -196{sup o}C y -100{sup o}C) se detienen por mas que las senales de resonancia paramagnetica de los electrones conserven la misma forma e intensidad u por prolongada que sea la duracion de los iones generados por la irradiacion. Los resultados de estos experimentos atestiguan la probable importancia del papel que desempenan los estados excitados de breve duracion en la radiopolimerizacion de una serie de monomeros en fase solida. Esa polimerizacion ''bajo el haz'' se desarrolla practicamente sin

  16. Rb-Sr isochrone dating of granitoids from Tribec Mts

    International Nuclear Information System (INIS)

    Bagdasaryan, G.P.; Gukasyan, R.Kh.; Cambel, B.; Broska, I.

    1990-01-01

    The results of Rb-Sr isochrone dating of granitoids from the Tribec-Zobor crystalline complex region are presented. Whole-rock Rb-Sr isochrone indicates an age of 352±5 m.y., the initial ratio being ( 87 Sr/ 86 Sr) 0 =0.70582±0.00008, which approaches the hitherto published initial ratios from the Tatric-Veporide part of the crystalline complex. This indicates a common source of granitoid rocks over the entire region studied. (author). 2 figs., 1 tab., 15 refs

  17. Petrography, geochemistry and tectonic setting of Rigi granitoid body (east of Lut Block, Central Iran)

    International Nuclear Information System (INIS)

    Ghonjalipour, R.; Biabangard, H.; Ahmadi, A.

    2016-01-01

    The Rigi Granitoid Mountain is located in 5 Km West of Dehsalm and 85 Km West of Nehbandan city, southeast of Birjand province and east of Lut Block. This granitoid with Eocene-Oligocene age was penetrated into sedimentary rocks (shale, limestone and sandstone) and changes theses rocks to skarn, hornfels and calcsilicate rocks. This granitoid consist of granodiorite, quartz monzonite and syenogranite with plagioclase, orthose, biotite, hornblende and quartz minerals. Sericite, chlorite, and Magnetite are secondary mineral in these rocks. Geochemical properties this pluton showes that it subalkaline and has metaluminous. Geochemical diagrams and presence of hornblende mineral in this pluton shows that belong to I-type granite. The rocks in granitoid pluton are enrichment LREE compare to HREE, high contents of LILE relative to HFSE and negative anomalies of Nb, Ti and P show it granitoid related to subduction zone. Also, tectonomagmatic diagrams improve that this pluton has belong to active continental margin.

  18. Petrogenesis of shoshonitic granitoids, eastern India: Implications for the late Grenvillian post-collisional magmatism

    Directory of Open Access Journals (Sweden)

    B. Goswami

    2014-11-01

    Full Text Available Many elongated, lenticular plutons of porphyritic granitoids are distributed mainly near the southern and northern margin of the Chhotanagpur Gneissic Complex (CGC which belongs to the EW to ENE–WSW tending 1500 km long Proterozoic orogenic belt amalgamating the North and South Indian cratonic blocks. The late Grenvillian (1071 ± 64 Ma Raghunathpur porphyritic granitoid gneiss (PGG batholith comprising alkali feldspar granite, granite, granodiorite, tonalite, quartz syenite and quartz monzonite intruded into the granitoid gneisses of southeastern part of CGC in the Purulia district, West Bengal and is aligned with ENE–WSW trending North Purulia shear zone. Mineral chemistry, geochemistry, physical condition of crystallization and petrogenetic model of Raghunathpur PGG have been discussed for the first time. The petrographic and geochemical features (including major and trace-elements, mineral chemistry and 87Sr/86Sr ratio suggest these granitoids to be classified as the shoshonitic type. Raghunathpur batholith was emplaced at around 800 °C and at 6 kbar pressure tectonic discrimination diagrams reveal a post-collision tectonic setting while structural studies reveal its emplacement in the extensional fissure of North Purulia shear zone. The Raghunathpur granitoid is compared with some similar granitoids of Europe and China to draw its petrogenetic model. Hybridization of mantle-generated enriched mafic magma and crustal magma at lower crust and later fractional crystallization is proposed for the petrogenesis of this PGG. Mafic magma generated in a post-collisional extension possibly because of delamination of subducting slab. Raghunathpur batholith had emplaced in the CGC during the final amalgamation (∼1.0 Ga of the North and South Indian cratonic blocks. Granitoid magma, after its generation at depth, was transported to its present level along megadyke channel, ways within shear zones.

  19. A-type and I-type granitoids and mylonitic granites of Hassan Salaran area of SE Saqqez, Kurdistan, Iran

    Science.gov (United States)

    Abdullah, Fakhraddin Mohammad; Saeed Ahmad, Sheler

    2014-05-01

    The Hassan Salarn area is located 20km to southeast of Saqqez city in Kurdistan Province, western Iran. In this area there are two distinct granitic rock suites consisting A-type and I-type granites and also mylonitic granites. These A-type and I-type granites have various petrological and geochemical characteristics. They also have different origins and petrogenesis. A-type granitoids comprise alkali feldspar granite, syenogranite and quartz alkali feldspar syenite, whereas I-type granitoids are composed of monzogranite, granodiorite and tonalite. Geochemically, A-type granitoids are peralkaline and acmite-normative but I-type granitoids are subalkaline (calc-alkaline), metaluminous and diopside-normative. A-type granitoids are also ferroan alkali and ferroan alkali-calcic whereas I-type granitoids are magnesian and calcic. A-type granitoids resemble to within plate granites and post-orogenic granites whereas I-type granitoids resemble to volcanic arc granites. A-type granitoids contain higher concentrations of alkalies, Zr, Rb, Nb, Y, Th, Ce, high FeO/MgO ratios and lower concentrations of Mg, Ca and Sr, resembling post-orogenic A-type granites. It is possible that heat from a mantle-derived magma which intruded into the lower crust, and/or rapid crustal extension have been essential generation of approriate melts producing A-type granitoids. Thus we can conclude that A-type granitoids were generated from a mixed mantle-crust source. Negative Nb anomalies and low contents of Ti and P probably indicate a subduction-related origin for protolith of I-type granitoids. Negative Nb anomalies and enrichment in Ce relative to its adjacent elements can be related to involvement of continental crust in magmatic processes. I-type granitoids are also enriched in Rb, Ba, K, Th, Ce and depleted in Nb, Zr and Y, indicating that they have had interacted with crust. I-type granitoids may result from contamination of mantle-derived magmas by continental crust during a subduction

  20. Interaction between felsic granitoids and basic dykes in ...

    Indian Academy of Sciences (India)

    37

    Many workers gave detailed petrographical and geochemical data of the ... greenstone complex (Malviya et al., 2006; Kumar et al., 2013; Singh and ...... Mafic rock shows lobate shape pointing towards granitoids (marked by the white arrows);.

  1. SHRIMP zircon dating of granitoids from Myanmar: constraints on the tectonic evolution of Southeast Asia

    International Nuclear Information System (INIS)

    Barley, M.E.; Pickard, A.L.; Zaw, K.; University of Tasmania, Hobart, TAS

    1999-01-01

    Full text: Situated south of the eastern syntaxis of the Himalayas, Myanmar occupies a key position in the tectonic evolution of Southeast Asia. However, there is almost no modern geochronology for this region. In this contribution we present new SHRIMP zircon dates for granitoids from the Shan Scarp (Mogok Metamorphic Belt), Taninthayi (Tenasserim) Region in the Myeik (Mergui) Archipelago and Central Valley (Western Myanmar) regions of Myanmar. The oldest ages obtained were from Jurassic granitoids, gneisses and amphibolites interlayered with marbles that were metamorphosed and deformed during the Eocene-Oligiocene and Miocene in the Mogok Metamorphic Belt. The occurrence of mid-Jurassic metamorphosed igneous rocks in the Mogok Metamorphic Belt is similar to that in the Hunza Karakoram and confirms interpretations that the southern margin of Asia became an Andean-type convergent margin at that time. Ages between 120 and 80 Ma for l-type granitoids intruding the Mogok Metamorphic Belt, Myeik Archipelago and Western Myanmar confirm that an up to 200km wide mid Cretaceous magmatic belt extended along the Eurasian margin from Tibet to Sumatra. Fractionated l-Type granitoids, that locally host Sn-W mineralisation, were emplaced in the Myeik Archipelago (and adjacent Thailand) in the latest Cretaceous to Early Eocene (80 to 50 Ma). These granitoids formed a wide convergent margin magmatic belt as the Indian plate rapidly approached Eurasia. Deformation and high-grade metamorphism occurred in the Mogok Metamorphic Belt during the Eocene-Oligiocene as the collision between India and Eurasia initiated crustal thickening prior to extrusion, or rotation, of Indochina and northward movement of Western Myanmar. Arc magmatism continued in Western Myanmar with emplacement of granitoids in the Central Valley. Deformation, extensional uplift and further granitoid magmatism occurred in the Mogok Metamorphic Belt during the Early Miocene northward movement of Western Myanmar

  2. Granitoids of South Korea and Southwest Japan. Trace element evidence regarding their differentiation

    International Nuclear Information System (INIS)

    Tsusue, Akio; Mizuta, Toshio; Tamai, Tadaharu.

    1994-01-01

    Although we have already published our trace element data for granitoids of South Korea and Southwest Japan, and we have interpreted REE patterns and Ba, Rb and Sr relationships of the granitoids (Tsusue et al., 1986, 1987a, 1987b, 1988), we intend to review briefly the trace element data of South Korea and Southwest Japan in this report. (J.P.N.)

  3. Gold contents of sulfide minerals in granitoids from southwestern New Brunswick, Canada

    Science.gov (United States)

    Yang, Xue-Ming; Lentz, David R.; Sylvester, Paul J.

    2006-07-01

    The abundance of gold and selected trace elements in magmatic sulfide and rock-forming minerals from Silurian-Devonian granitoids in southwestern New Brunswick were quantitatively analyzed by laser-ablation inductively coupled plasma mass-spectrometry. Gold is mainly hosted in sulfide minerals (i.e., chalcopyrite, pyrrhotite, and pyrite), in some cases perhaps as submicron inclusions (nanonuggets). Gold is below detection (caca % qGTbGaaeyzaiaabYgacaqG0baaaOGaeyypa0JaaGymaiaaiwdacaaI % WaGaeyySaeRaaGioaiaaiodacaGGSaGaaeiiaiaabggacaqGUbGaae % izaiaabccacaWGebWaa0baaSqaaiaabgeacaqG1baabaGaaeiCaiaa % bMhacaqGVaGaaeyBaiaabwgacaqGSbGaaeiDaaaakiabg2da9iaaio % dacaaI2aGaaGOmaiabgglaXkaaiMdacaaI2aaaaa!6E8F! D^{{{text{cpy/melt}}}}_{{{text{Au}}}}= 948 ± 269,{text{ }}D^{{{text{po/melt}}}}_{{{text{Au}}}} = 150 ± 83,{text{ and }}D^{{{text{py/melt}}}}_{{{text{Au}}}} = 362 ± 96. This result suggests that gold behavior in the granitoid systems is controlled by the conditions of sulfur saturation during magmatic evolution; the threshold of physiochemical conditions for sulfur saturation in the melts is a key factor affecting gold activity. Gold behaves incompatibly prior to the formation of sulfide liquids or minerals, but it becomes compatible at their appearance. Gold would be enriched in sulfur-undersaturated granitoid magmas during fractionation, partitioning into evolved magmatic fluids and favoring the formation of intrusion-related gold deposits. However, gold becomes depleted in residual melts if these melts become sulfur-saturated during differentiation, leading to gold precipitation in the early sulfide phases of a granitoid suite. Late-stage Cl-bearing magmatic-hydrothermal fluids with low pH and relatively high oxidation state derived from either progressively cooling magmas at depth or convective circulation of meteoric water buffered by reduced carbon-bearing sediments, may scavenge gold from early sulfide minerals. If a significant amount of gold produced in this

  4. Cyclic formation and stabilization of Archean lithosphere by accretionary orogenesis: Constraints from TTG and potassic granitoids, North China Craton

    Science.gov (United States)

    Wang, Wei; Cawood, Peter A.; Liu, Shuwen; Guo, Rongrong; Bai, Xiang; Wang, Kang

    2017-09-01

    Accretionary orogens are major sites of modern continental growth, yet their role in the development of Archean continental crust remains enigmatic. Diverse granitoid suites from tonalite-trondhjemite-granodiorite (TTG) to potassic granitoids appeared during late Archean, representing a period of major continental formation and stabilization. In this study, whole-rock geochemical and zircon U-Pb and Lu-Hf isotopic data are reported for Neoarchean granitoid gneisses from the Northern Liaoning Terrane, northeastern North China Craton (NCC). Older granitoid gneisses ( 2592-2537 Ma) define three magmatic zones migrating from southeast to northwest, each showing a common magmatic evolution from high-pressure TTGs to medium-/low-pressure TTGs and potassic granitoids. They have depleted zircon ƐHf(t) of +0.5 to +8.7. Younger 2529-2503 Ma potassic granitoids and TTGs occur throughout the terrane, which are marked by variable zircon ƐHf(t) of -4.7 to +8.1, and are coeval with regional high-grade metamorphism. Petrogenetic modeling and changing Sr/Y and (La/Yb)N of the granitoids suggest that the crust experienced episodic thickening and thinning and became progressively evolved through development of potassic granitoids and sedimentary successions. The metavolcanic basement to the granitoids display tholeiitic to calc-alkaline affinities, together with the top-to-the-northwest thrusting and associated volcanogenic massive sulfide-type Cu-Zn deposits, suggesting cyclic crustal formation of Northern Liaoning within an accretionary orogen with a SE-dipping subduction polarity. Cyclic crustal thickening and thinning is related to tectonic switching from advancing to retreating relations between the downgoing and overriding plate. After 2530 Ma, this accretionary system accreted to the ancient continental nucleus of NCC (Anshan-Benxi Terrane), signifying final lithosphere stabilization.

  5. Oxygen isotope regional pattern in granitoids from the Cachoeirinha Belt, northeast Brazil

    International Nuclear Information System (INIS)

    Sial, A.N.

    1984-01-01

    Four groups of granitoids are present within the Cachoeirinha belt and in the adjacent migmatitic basement, between 37 0 and 40 0 W long. and 7 0 and 8 0 15' S lat., States of Pernambuco and Paraiba: a) K 2 O - enriched, very porphyritic; b) a calc-alkalic slightly porphyritic group; c) group with trondjemitic affinities; and d) peralkalic group. Petrology and oxygen isotope geochemistry for over 100 samples from these groups were studied. Almost all plutons for which 5 or more samples were analyzed, exhibit a total range of gamma 18 O less than 2% o. A broad range of mean oxygen isotope composition is observed, varying from 6.93 to 12.79% o. There is a systematic regional trend in which the calc-alkalic granitoids (conceicao-type) found within the Cachoeirinha space are the most 18 O - enriched rocks (10.6 to 12.9% o) while the lowest mean gamma 18 O values (4.5 to 9.7% o) are found in the K 2 O - enriched granitoids (Itaporanga-type). Intermediate gamma 18 O values were recorded in the bodies with trondhjemitic affinities (8.9 to 9.8% o) which intruded metasediments of the Salgueiro Group and in the peralkalic granitoids of Catingueira (8.1 to 9.8% o) which intruded Cachoeirinha metamorphics. Among the potassic granitoids, mean gamma 18 O increases from Bodoco to Itaporanga (from west to east). As a whole, the W.R. gamma 18 O of these plutons correlate with the type of grade of metamorphism of the host rocks and, therefore, with the tectonic framework, increasing from those which intruded the gneiss-migmatites to those which intruded the low-grade metamorphics of the Cachoeirinha Group. The possible origin of each rock group is discussed in light of the oxygen isotope geochemistry. (Author) [pt

  6. Fases fluoradas como sorventes para extração em fase sólida de pesticidas e compostos perfluorados

    OpenAIRE

    Cristiane Vidal

    2015-01-01

    Resumo: Fases sólidas fluoradas apresentam características oriundas das propriedades da ligação C-F, como o alto momento de dipolo e a baixa polarizabilidade e isto confere seletividades peculiares a elas. Existem diversas fases estacionárias alquilperfluoradas e fenilperfluoradas comerciais para cromatografia líquida, entretanto, a oferta de fases sólidas fluoradas para extração em fase sólida (SPE) é menor. Assim, este trabalho descreve um novo método de SPE utilizando uma fase fluorada pre...

  7. Geological, petrogical and geochemical characteristics of granitoid rocks in Burma: with special reference to the associated WSn mineralization and their tectonic setting

    Science.gov (United States)

    Zaw, Khin

    The granitoid rocks in Burma extend over a distance of 1450 km from Putao, Kachin State in the north, through Mogok, Kyaukse, Yamethin and Pyinmana in the Mandalay Division, to Tavoy and Mergui areas, Tenasserim Division, in the south. The Burmese granitoids can be subdivided into three N-S trending, major belts viz. western granitoid belt, central graniotoid belt and eastern granitoid belt. The Upper Cretaceous-Lower Eocene western belt granitoids are characterized by high-level intrusions associated with porphyry Cu(Au) related, younger volcanics; these plutonic and volcanic rocks are thought to have been emplaced as a magmatic-volcanic arc (inner magmatic-volcanic arc) above an east-dipping, but westwardly migrating, subduction zone related to the prolonged plate convergence which occurred during Upper Mesozoic and Cenozoic. The central granitoid belt is characterized by mesozonal, Mostly Upper Cretaceous to Lower Eocene plutons associated with abundant pegmalites and aplites, numerous vein-type W-Sn deposits and rare co-magmatic volcanics. The country rocks are structurally deformed, metamorphic rocks of greenschist to upper amphibolite facies ranging in age as early as Upper Precambrian to Upper Paleozoic and locally of fossiliferous, metaclastic rocks (Mid Jurassic to Lower Cretaceous). Available K/Ar radiometric data indicate significant and possibly widespread thermal disturbances in the central granitoid belt during the Tertiary (mostly Miocence). In this study, the distribution, lithological, textural and structural characteristics of the central belt granitoids are reviewed, and their mineralogical, petrological, and geochemical features are presented. A brief description of W-Sn ore veins associated with these granitoid plutons is also reported. Present geological, petrological and geochemical evidences demonstrate that the W-Sn related, central belt granitoids are mostly granodiorite and granite which are commonly transformed into granitoid gneisses

  8. Age of granitoids from the Kohut Veporic zone according to Rb-Sr isochrone analysis

    International Nuclear Information System (INIS)

    Cambel, B.; Bagdasaryan, G.P.; Gukasyan, R.K.; Dupej, J.

    1988-01-01

    Rb-Sr isochrone analyses of granitoid rocks from the southern part of the Veporic zone - the so-called Kohut zone - are presented. In this region, the Sinec (Rimavica) type of granitoids formerly considered to be Late Palaeozoic to Neoide, is found. The present isochrone research determines them as equivalents of granitoids of the Sihla type (387±27 m.y.). The Sinec (Rimavica) granite reaches an age of 392±5 m.y. This extended age must partly be attributed to additional processes which took place in the stage of retrograde alterations. The conclusions are of considerable importance in clarifying the metamorphic age and stratigraphy of the crystalline complex in the region of the southern Veporic zone. (author). 9 figs., 4 tabs., 38 refs

  9. 222Rn activity concentration differences in groundwaters of three Variscan granitoid massifs in the Sudetes (NE Bohemian Massif, SW Poland)

    International Nuclear Information System (INIS)

    Przylibski, Tadeusz A.; Gorecka, Joanna

    2014-01-01

    Based on research conducted in three Variscan granitoid massifs located within the crystalline Bohemian Massif, the authors confirmed that the higher the degree of their erosional dissection, the smaller the concentration of 222 Rn in groundwaters circulating in these massifs. This notion implies that radon waters and high-radon waters, from which at least some of the dissolved radon should be removed before feeding them as drinking water to the water-supply system, could be expected in granitoid massifs which have been poorly exposed by erosion. At the same time, such massifs must be taken into account as the areas of possible occurrence of radon medicinal waters, which in some countries can be used for balneotherapy in health resorts. Slightly eroded granitoid massifs should be also regarded as very probable radon prone areas or areas of high radon potential. - Highlights: • The concentration of 222 Rn in groundwater depends on the zone of the granitoid massif which is exposed on the ground surface. • The highest 222 Rn concentrations occur in the least eroded granitoid massifs, the lowest in massifs with exposed root parts. • The stronger the erosional dissection of a granitoid massif, the lower 222 Rn concentration in groundwaters in this massif. • Not all granitoid massifs are areas with groundwaters containing high concentrations of 222 Rn. • The least eroded granitoid massifs are radon prone areas with the occurrence of high-radon and radon groundwaters

  10. The Rb/Sr ages for granitoids of the Middle Chukotka: a new approach to the geological history of the region

    International Nuclear Information System (INIS)

    Efremov, S.V.; Kozlov, V.D.; Sandimirova, G.P.

    2000-01-01

    For studying the history of geological evolution of the Middle Chukotka in the Mesozoic by the method of Rb-Sr dating the age of granitoids in the region was determined. It was ascertained that the granitoids have different genetic nature, their formation involving the most intensive tectonic restructuring. Magmatism was manifested in two stages. Formation of the first stage granitoids (126-144 mln. years) relates to orogenesis, while that of the second stage granitoids (∼ 80 mln. years) - to the process of the Chukotka folded region activation [ru

  11. Study of rare earth elements for the characterization and metalogenetic evaluation of granitoids of the paranaense shield

    International Nuclear Information System (INIS)

    Chiodi Filho, C.; Santos, J.F. dos; Moretzsohn, J.S.

    1989-01-01

    REE geochemistry combined with major and trace elements data, provide some diagnostic criteria regarding the origin, the geotectonic setting and the metallogenesis of granitoid intrusions in the Parana Shield. The intrusions were grouped as mantle (Sintexis Series) and crustal (Transformation Series) origins. The two lineages include six suites, with pre, syn, tardi-to-post and post-collisional emplacement. From the metallogenetic standpoint, the 'Sintexis' granitoids can be labelled as ''0Mo-W-Cu-Au porphyry-granites''and the 'Transformation' granitoids as Sn-W greisengranites. (author) [pt

  12. The W (Sn-Mo)-specialized catinga suite and other granitoids of the Brusque Group, neo proterozoic of the state of Santa Catarina, Southern Brazil

    International Nuclear Information System (INIS)

    Castro, Neivaldo Araujo de; Crosta, Alvaro Penteado; Basei, Miguel Angelo Stipp

    1999-01-01

    The petrographic, geochemical and isotopic data on the granitoids intrusive in the Brusque Group, State of Santa Catarina, southern Brazil, are presented in this paper. These are late-to post-tectonic rocks, being the most evolved ones those that constitute the Catinga Suite. The granitoids intrusive in the southern domain of the Brusque Group are grayish rocks, in which biotite (when present) is practically the only mafic mineral. They are rather reduced, slightly alkalic, transitional between meta-and peraluminous. An acid subvolcanic pluton, the Ribeirao da Velha pluton, has similar petrographic and geochemical characteristics, and seems to be genetically related to these granitoids. LREE fractionation relative to HREE is incipient for the Catinga suite, and the REE patterns showing strong negative Eu anomaly. Initial 87 Sr/ 86 Sr ratios, from the literature for these granitoids are around 0.721 (Sao Joao Batista granitoid) and the only available t DM model age (Valsungana granitoid) points to a genesis from a continental crust of ca. 2020 Ma old. Gneiss-migmatitic rocks such as those that occur in the eastern portion of Brusque Group domain and as enclaves in the Nova Italia granitoid are strong candidates for protoliths of these granitoids. Little available information on the granitoids intrusive in the northern domain of the Brusque Group reports the presence of pink K-feldspar hornblende granitoids (Faxinal pluton) and light pink K-feldspar biotite granitoid (Guabiruba pluton). These granitoids are more enriched in K and more oxidized than those in the southern domain, and the LREE fractionation relative to HREE is strong, with the REE patterns showing incipient negative Eu anomaly. It is suggested that part of the Au concentrations found in the northern domain may be genetically associated with the granitoids, since they present characteristics favorable to promote Au mineralizations than the granitoids in the southern domain. Distinct protoliths and

  13. Geochemistry and petrogenesis of the Kolah-Ghazi granitoid assemblage, south of Esfahan

    Directory of Open Access Journals (Sweden)

    Jamshid Ahmadian

    2018-04-01

    Full Text Available Introduction The Kolah-Ghazi granitoid assemblage is located in the south of Esfahan and in the Sanandaj-Sirjan magmatic-metamorphic zone. The Sanandaj-Sirjan zone is extended for 1500 km from Sirjan in the southeast to Sanandaj in the northwest of Iran and is situated in the west of Central Iranian terrane. The Sanandaj-Sirjan zone represents the metamorphic belt of the Zagros orogeny which is part of the Alpine- Himalayan orogenic belt. The Kolah-Ghazi granitoid assemblage consists of granodiorite, granites, quartz-rich granitoid and minor tonalite. The aim of this paper is to represent the mineralogy, geochemistry, petrogenesis and tectonic setting of this plutonic assemblage. Materials and methods More than 60 samples representing all of the rock units in the study area were chosen for microscopic studies. Then, 22 samples were selected for geochemical studies. The major elements were determined with XRF in the Naruto University, Japan. The trace and rare earth elements were analyzed by ICP-MS in the Acmelab, Canada. The geochemical results are presented in Table 1. Results and Discussion The Kolah-Ghazi granitoid assemblage intruded into the Jurassic sedimentary units and overlaid by lower Cretaceous sandstone and conglomerate which suggest Upper Jurassic as the possible age of the Kolah-Ghazi intrusion. Based on the modal studies, this granitoid assemblage is comprised of granite, granodiorite, quartz-rock granitoid and tonalite with different igneous textures including symplectic, myrmekitic, rapakivi, poikilitic and porphyroid. There are some xenoliths, microgranular enclaves and sur micaceous enclaves in the Kolah-Ghazi granitoid assemblage. Xenoliths are mostly derived from Jurassic shale and sandstones which have been trapped in the magma. The sur micaceousenclaves have tonalite composition. The sur micaceous enclaves are biotite-rich rock fragments which display metamorphic texture. The sur micaceous enclaves are classified as

  14. Ams Fabric and Deformation of The Jawornik Granitoids In The Zloty Stok - Skrzynka Deformation Zone (sudetes, SW Poland)- Preliminary Interpretations.

    Science.gov (United States)

    Werner, T.; Bialek, D.

    Jawornik granitoids comprise the NE-SW trending sequences of the 1cm up to 1 km thick granitoid veins surrounded by schists and gneisses of the Zloty Stok - Skrzynka deformation zone in Eastern Sudetes (SW Poland). According to conflicting theories granitoids are of magmatic origin or were formed from blastomylonitic rocks that underwent multiphase deformation. AMS studies were performed for the 53 sites lo- calized within granitoid veins and within the surrounding gneisses. AMS foliations for granitoid veins of various thickness as well as for gneisses dip at moderate to steep an- gles to N-NW. AMS lineations in the surrounding gneisses plunge subhorizontally to NE-SW that reflects the regional NE-SW shearing components. Magnetic lineations for sites within wider veins of granitoids plunge at low angles (mostly from S to W) but with more varying trends between sites. Mezoscopic tectonic foliations are record- able only in 50% of sites. They show good correlation with AMS planar fabric on the site scale. The uniformity of AMS fabric on the site scale and high AMS anisotropy within all sites (P of 1.05-1.30, T of 0.3-0.6 on average) suggest syntectonic gener- ation of granitoids. Further interpretations of the AMS and tectonic fabrics will be performed when microtectonic studies and chemical analyses results are available.

  15. The Pedregal granite (Portugal: petrographic and geochemical characterization of a peculiar granitoid

    Directory of Open Access Journals (Sweden)

    Ferreira, J. A.

    2014-12-01

    Full Text Available The Pedregal granite outcrops in the Central Iberian Zone, northern Portugal, in the eastern border of a synorogenic variscan granite-migmatite complex sub-concordant with the regional metamorphic structures. It is a granitoid (ca. 3 km2 with an elongated NW-SE shape intruded in staurolite-micaschist and banded gneiss-migmatite rocks, with local igneous breccias in the contact. The country rocks belong to a metapelitic and metasammitic sequence of Edicarian-Cambrian age, known as the “Complexo Xisto-Grauváquico” (CXG which shows a main regional foliation with a NW-SE to NNW-SSE direction. The Pedregal granite is peraluminous (its A/CNK parameter ranges from 1.18 to 1.62, with a magnesian and alkali to alkali-calcic signature. The peculiar features of the granite are high contents of Zr (389 to 435 ppm and a LREE flat pattern, which are uncommon characteristics for granitic rocks, as well as the corroded shape of the biotite, and the large amount of secondary muscovite. These peculiar features distinguish it from the adjacent synorogenic granites. The field, petrographical and chemical features of the Pedregal granite are in accordance with a second phase of partial melting of a residuum, depleted by melt segregation during a first melting episode with the involvement of peritectic garnet and abundant residual biotite with LREE- and Zr-bearing accessory minerals. Besides, the intrusive character of the granite, and the presence of metasedimentary xenoliths point out to a secondary diatexite.El granito de Pedregal aflora en la Zona Centro-Ibérica, en el norte de Portugal, en el borde oriental de un complejo granito-migmatítico sinorogénico varisco, subconcordante con las estructuras metamórficas regionales. Es un granitoide (ca. 3 km2 de forma elongada NW-SE, que intruye en micaesquistos estaurolíticos y en rocas gneissico- migmatíticas bandeadas, con brechas ígneas locales en el contacto. Las rocas encajantes pertenecen a una

  16. Petrology, geochronology, geochemistry and petrogenesis of Bajestan granitoids, North of Ferdows, Khorasan Razvi Province

    Directory of Open Access Journals (Sweden)

    Reyhaneh Ahmadirouhani

    2017-02-01

    Full Text Available Introduction The investigated area is situated in the south west of the Khorasan Razavi Province along the North West of the Lut Block. Different types of metal ore bodies along with non-metal deposits have already been documented in the Lut Block (Karimpour et al., 2008. Most of the study area is covered with granitoid rocks. Metamorphic rocks with unknown age are present in the north of the area. Skarns are observed in contact with fault zones and intrusive bodies. Eocene volcanic rocks with andesite and andesibasalt composition are located in the east and north east of the area (Ahmadirouhani et al., 2015. The study area that is a part of the Lut Block has a high potentials for Cu, Fe, Au, and Barite mineralization along the observed alteration zones. In the present study, the petrography, petrogenesis, Sr–Nd isotopes, and U–Pb zircon age of acidic granitoids in the east of Bajestan were investigated. Materials and methods In the current study, 400 rock samples were collected from the field and 170 thin sections were prepared for petrography studies. Thirty samples of volcanic rocks, intrusions, and dykes were analyzed using XRF at the Geological Survey of Iran. Twenty-five samples were selected for the elemental analysis using ICP-MS by the Acme Lab Company (Canada, 16 samples of them were related to acidic intrusive bodies and dykes. In addition, zircon crystals from four samples of the granitoids bodies were collected for U–Pb dating. Approximately 50 zircon grains (i.e. euhedral, clear, uncracked crystals with no visible heritage cores and no inclusions were hand-picked from each sample. Through cathodoluminescence imaging, the internal structure and the origin of zircon grains were examined at the Geological Survey of Vienna, Austria. Moreover, zircons were dated using the (LA-ICP-MS method at the Laboratory of Geochronology, the University of Vienna, Austria using the methodology outlined in Klötzli et al., (2009. Sr and Nd

  17. INTERACTIONS BETWEEN GABBROID AND GRANITOID MAGMAS DURING FORMATION OF THE PREOBRAZHENSKY INTRUSION, EAST KAZAKHSTAN

    Directory of Open Access Journals (Sweden)

    S. V. Khromykh

    2017-01-01

    Full Text Available The paper reports on studies of the Preobrazhensky gabbro‐granitoid intrusion, East Kazakhstan, com‐ posed of the rocks that belong to four phases of intrusion, from quartz monzonites and gabbroids to granite‐ leucogranites. Specific relationships between basite and granitoid rocks are usually classified as the result of interac‐ tions and mixing of liquid magmas, i.e. magma mingling and mixing. Basite rocks are represented by a series from biotite gabbros to monzodiorites. Granitoids rocks are biotite‐amphibole granites. Porphyric granosyenites, com‐ bining the features of both granites and monzodiorites, are also involved in mingling. It is established that the primary granitoid magmas contained granosyenite/quartz‐monzonite and occurred in the lower‐medium‐crust conditions in equilibrium with the garnet‐rich restite enriched with plagioclase. Monzodiorites formed during fractionation of the parent gabbroid magma that originated from the enriched mantle source. We propose a magma interaction model describing penetration of the basite magma into the lower horizons of the granitoid source, which ceased below the viscoplastic horizon of granitoids. The initial interaction assumes the thermal effect of basites on the almost crystal‐ lized granitic magma and saturation of the boundary horizons of the basite magma with volatile elements, which can change the composition of the crystallizing melt from gabbroid to monzodiorite. A ‘boundary’ layer of monzodiorite melt is formed at the boundary of the gabbroid and granitoid magmas, and interacts with granitoids. Due to chemical interactions, hybrid rocks – porphyric granosyenites – are formed. The heterogeneous mixture of monzodiorites and granosyenites is more mobile in comparison with the overlying almost crystallized granites. Due to contraction frac‐ turing in the crystallized granites, the heterogeneous mixture of monzodiorites and granosyenites penetrate into the

  18. Rare earth element lithogeochemistry of granitoid mineral deposits

    Energy Technology Data Exchange (ETDEWEB)

    Taylor, R.P.; Fryer, B.J. (Memorial Univ. of Newfoundland, St. John' s (Canada). Dept. of Earth Sciences)

    1983-12-01

    As a monitor of the processes involved in the formation of granitoid mineral deposits the coherent group behaviour of the rare earth elements (REE) actively reflects changing fluid characteristics. For example, in the porphyry environment, magmatic-hydrothermal fluids produce potassic alteration with strong enrichment in the light rare earth elements, reflecting their high pH, low fluid/rock ratios, and the dominant role of Cl/sup -/ complexing in metal (i.e. Cu, Au) transport. With increasing fluid/rock ratios and decreasing pH accompanying the progressive involvement of meteoric fluids (and the production of propylitic, argillic, and phyllic alteration) anionic species such as F/sup -/ and CO/sub 3//sup 2 -/ become important in metal (e.g. Mo, W) transport through complexing, and their activity in the hydrothermal fluids is illustrated by mobilization of the heavy rare earth elements. The relative involvement of Cl/sup -/ versus F/sup -/ versus CO/sub 3//sup 2 -/ in metal transport in other granite-related systems can also be monitored through REE behaviour. Hence granitoid tin-tungsten mineralization and associated greisenization typically exhibit heavy rare earth enrichment and evidence the importance of F/sup -/ and CO/sub 3//sup 2 -/ in metal transport. Similarly, heavy rare earth element enrichment in hydrothermal uranium deposits can be related to the transport of uranium as carbonate complexes. REE are widely accepted as powerful tools in the study of rock petrogenesis, but their use has been neglected in the investigation of mineral deposits. The recognition of the systematic variation of REE distributions in granitoid mineral deposits suggests that the application of REE geochemistry, particularly when integrated with fluid inclusion and isotope studies, can provide l) an effective method for identifying the physiochemical controls of metal transport and 2) a useful criterion of elucidating metal distribution.

  19. Rare earth element lithogeochemistry of granitoid mineral deposits

    International Nuclear Information System (INIS)

    Taylor, R.P.; Fryer, B.J.

    1983-01-01

    As a monitor of the processes involved in the formation of granitoid mineral deposits the coherent group behaviour of the rare earth elements (REE) actively reflects changing fluid characteristics. For example, in the porphyry environment, magmatic-hydrothermal fluids produce potassic alteration with strong enrichment in the light rare earth elements, reflecting their high pH, low fluid/rock ratios, and the dominant role of Cl - complexing in metal (i.e. Cu, Au) transport. With increasing fluid/rock ratios and decreasing pH accompanying the progressive involvement of meteoric fluids (and the production of propylitic, argillic, and phyllic alteration) anionic species such as F - and CO 3 2- become important in metal (e.g. Mo, W) transport through complexing, and their activity in the hydrothermal fluids is illustrated by mobilization of the heavy rare earth elements. The relative involvement of Cl - versus F - versus CO 3 2- in metal transport in other granite-related systems can also be monitored through REE behaviour. Hence granitoid tin-tungsten mineralization and associated greisenization typically exhibit heavy rare earth enrichment and evidence the importance of F - and CO 3 2- in metal transport. Similarly, heavy rare earth element enrichment in hydrothermal uranium deposits can be related to the transport of uranium as carbonate complexes. REE are widely accepted as powerful tools in the study of rock petrogenesis, but their use has been neglected in the investigation of mineral deposits. The recognition of the systematic variation of REE distributions in granitoid mineral deposits suggests that the application of REE geochemistry, particularly when integrated with fluid inclusion and isotope studies, can provide l) an effective method for identifying the physiochemical controls of metal transport and 2) a useful criterion of elucidating metal distribution

  20. U-Pb SHRIMP data and geochemical characterization of granitoids intruded along the Coxixola shear zone, Provincia Borborema, NE Brazil

    Energy Technology Data Exchange (ETDEWEB)

    Guimaraes, Ignez de Pinho; Silva Filho, Adejardo Francisco da; Silva, Francis M.J.V. da, E-mail: ignez@ufpe.br [Universidade Federal de Pernanmbuco (UFPE), Recife, PE (Brazil). Dept. de Geologia; Armstrong, Richard [Australian National University (Australia)

    2011-07-01

    A large volume of granitic magmatism associated with large scale shear zone and metamorphism under high-T amphibolite facies conditions characterize the Brasiliano Orogeny in the Borborema Province, NE Brazil. Granitoids from two plutons and later dykes intruded along the Coxixola shear zone show distinct crystallization ages and geochemical signature. The oldest granitoids (618 ± 5 Ma), Serra de Inacio Pereira Pluton are coeval with the peak of regional metamorphism and they were probably originated by melting of a paleoproterozoic source. The granitoids from the Serra do Marinho Pluton show crystallization age of 563 ± 4 Ma and geochemical signature of post-collisional A-type granites. The later dykes have crystallization age of 526 ± 7 Ma, geochemical signature of A-type granitoids. (author)

  1. Indoor radon related to uranium in granitoids of the Central Bohemian plutonic complex

    International Nuclear Information System (INIS)

    Barnet, I.; Fojtikova, I.

    2004-01-01

    The study is based on the indoor radon data (one year measurements, Kodak LR 115 track etch detectors), vectorized geological maps 1:50000, vectorized coordinates of dwellings and uranium data for granitoid types of the Central Bohemian Plutonic Complex (CBPC). Using ArcGis 8.2 programme, the position of 16145 dwellings was linked to a geological database covering the CBPC (approx. 3200 km 2 ), and the type of underlying rock type was specified for each house. The resulting databases enabled us to calculate the mean EEC indoor Rn data for particular granitoid types and to study the relationship between the indoor Rn and the U concentrations. The petrogenetically variable CBPC was emplaced during Variscan orogenesis (330-350 Ma) and is among the most radioactive rock types within the Bohemian Massif. A long-term process of CBPC genesis resulted in more than 20 granitoid types, differing by their petrogenetic characteristics as well as mineralogical and chemical composition, including uranium concentration. The relation between the mean indoor radon values and uranium concentrations in particular rock types was examined. A positive regression between indoor Rn and uranium as the source of Rn soil gas clearly demonstrates how regional geology influences the indoor radon activity concentration in dwellings. The highest indoor Rn concentrations were observed in the Sedlcany granodiorite and Certovo bremeno syenite, where also the highest gamma dose rates (150-210 nGy.h -1 ) within all granitoid types in the Czech Republic were observed. The two rock types differ from other granitoids by a relatively high zircon concentration, which is the main source of U and subsequently of soil gas Rn being released from the bedrock. The lower indoor Rn values of Certovo bremeno syenite which do not correspond with the high U concentrations can be explained by a relatively low permeability of its clayey weathering crust. This feature was also observed for soil gas radon concentration

  2. Emplacement, petrological and magnetic susceptibility characteristics of diverse magmatic epidote-bearing granitoid rocks in Brazil, Argentina and Chile

    Science.gov (United States)

    Sial, A. N.; Toselli, A. J.; Saavedra, J.; Parada, M. A.; Ferreira, V. P.

    1999-03-01

    Magmatic epidote (mEp)-bearing granitoids from five Neoproterozoic tectonostratigraphic terranes in Northeastern (NE) Brazil, Early Palaeozoic calc-alkalic granitoids in Northwestern (NW) Argentina and from three batholiths in Chile have been studied. The elongated shape of some of these plutons suggests that magmas filled fractures and that dyking was probably the major mechanism of emplacement. Textures reveal that, in many cases, epidote underwent partial dissolution by host magma and, in these cases, may have survived dissolution by relatively rapid upward transport by the host magma. In plutons where such a mechanism is not evident, unevenly distributed epidote at outcrop scale is armoured by biotite or near-solidus K-feldspar aggregates, which probably grew much faster than epidote dissolution, preventing complete resorption of epidote by the melt. Al-in-hornblende barometry indicates that, in most cases, amphibole crystallized at P≥5 kbar. Kyanite-bearing thermal aureoles surrounding plutons that intruded low-grade metamorphic rocks in NE Brazil support pluton emplacement at intermediate to high pressure. mEp show overall chemical variation from 20 to 30 mol% (mole percent) pistacite (Ps) and can be grouped into two compositional ranges: Ps 20-24 and Ps 27-30. The highest Ps contents are in epidotes of plutons in which hornblende solidified under Pcorrosion of individual epidote crystals included in plagioclase in high-K calc-alkalic granitoids in NE Brazil, emplaced at 5-7 kbar pressure, yielded estimates of magma transport rate from 70 to 350 m year -1. Most of these plutons lack Fe-Ti oxide minerals and Fe +3 is mostly associated with the epidote structure. Consequently, magnetic susceptibility (MS) in the Neoproterozoic granitoids in NE Brazil, as well as Early Palaeozoic plutons in Argentina and Late Palaeozoic plutons in Chile, is usually low (3.0×10 -3 SI, typical of magnetite-series granitoids crystallized under higher oxygen fugacity. In NE

  3. Tectonic implications of U-Pb (zircon) Geochronology of Chor Granitoids of the Lesser Himalaya, Himachal Pradesh, NW Himalaya

    Science.gov (United States)

    Singh, P.; Bhakuni, S. S.

    2017-12-01

    Granitoids of various ages ranging from Proterozoic to Tertiary occur throughout the Himalayan fold-thrust belt. The occurrence of the Neoproterozoic granitoids are very less in the Himalayan orogen. One of the best example of Neoproterozoic granitoids is Chor granitoids, which are the intrusive granite bodies in the Paleoproterozoic of the Lesser Himalayan Crystallines of the Jutogh Group. In the central part these granites are non-foliated homogeneous that are porphyritic and peraluminous in nature (Singh et al., 2002; Bhargava et al., 2014, 2016), whereas in the peripheral part these are foliated showing south directed shear sense of movement. In this work we present the U-Pb (zircon) geochronology of two different granites samples of the Chor granitoids of Himachal Pradesh, NW Himalaya. The Jutogh Group of rocks is thrust over the Lesser Himalayan Sequence along the Jutogh Thrust or MCT. The geochronology of the Chor Granitoids and Lesser Himalayan Crystallines and their relationship with each other, including with the Indian shield are sparsely obscure. U-Pb zircon geochrnological age populations from these granitoids yield ages between 780 and 980 Ma. One sample gives the prominent age spectra for 206Pb/238U with weighted mean age of 908.3 ± 6.7 Ma (2σ) MSWD = 2.4 (n = 18). Similarly another sample gives the age of crystallization with weight mean age of 917 ± 17 Ma (2σ) MSWD = 3 (n = 11) and Th/U ratios of both samples are >0.1, indicating their magmatic origin. As a result of ductile shearing of granites along the MCT during the Cenozoic Himalayan Orogeny, the age has reduced to 780 Ma. The Neoproterozoic age of Chor granite matches with the Neoproterozoic detrital zircon age (800 to 1000 Ma by Parrish and Hodges 1996, Decelles et al., 2000) of the HHC. On the basis of U-Pb (zircon) geochronological ages, it is revealed that the source of zircons of the Chor granite and HHC rocks was the northern margin of the Pan-African orogen. The Chor granitoids was

  4. Petrography and geochronology of the Sao Jose dos Quatro Marcos granitoids, southwestern Mato Grosso, Brazil

    International Nuclear Information System (INIS)

    Carneiro, M.A.; Ulbrich, H.H.G.J.; Kawashita, K.

    1989-01-01

    An area of about 400Km 2 was mapped in the region of Sao Jose dos Quatro Marcos, southwestern State of Mato Grosso, western Brazil. Various granitoid rocks were recognized, intrusive into basement gneisses, and mapped as two distinct units, one of massive late granitoids (mostly 3a and 3b granites) and one of foliated granitoids, with oriented mafic minerals, consisting mainly of tonalites and, to a lesser degree, of granodiorites. The sequence of intrusion is from tonalites to granodiorites to late granites. Magmatic textures are usually preserved in the rocks, with the exception of some clearly recrystallized samples. Field aspects, as well as petrography and mineralogy, suggest a genetic relationship between the various granitoid types, showing overall features commonly cited as typical of 'I' lineages. A Rb/Sr whole-rock isochron obtained from 3b granites (six points) shows an age of 1,472 +- 19 Ma, and Sr 87 86 initial ratio of 0.7037 +- 0.0004; a nine point isochron (adding two tonalites and one granodiorite) yelds similar results (age of 1,505 +- 20 Ma, initial ratio of 0.7029+- 0.0003). The obtained ages confirm the existence of a thermal-magmatic event at about 1,500 Ma at the southern border of the Amazon Craton. (author) [pt

  5. A petrochemical investigation of a group of granitoids in the Cnydas area, West of Upington

    International Nuclear Information System (INIS)

    Jankowitz, J.A.C.

    1981-01-01

    Detailed mapping in the eastern Namaqualand Metamorphic Complex west of Upington, indicates that the Cnydas batholith can be divided into ten different granitoidal phases. The classification is based on the intrusive field relationships supported by variation in mineralogy, texture, petrography and geochemistry. A differentiation sequence from granodiorite through mesocratic granite to leucogranite is proposed on the basis of geochemical evidence. The chemistry and petrography suggests an I-type origin for these granitoids

  6. Lithogeochemistry of rare-earth elements in the characterization of granitoids from the Cachoeirinha belt, Northeast Brazil

    International Nuclear Information System (INIS)

    Sial, A.N.

    1984-01-01

    Detailed rare-earth element study on about 40 samples from 14 granitic bodies distributed within and in adjacent areas of the Cachoeirinha belt, states of Pernambuco and Paraiba, between 37 0 and 40 0 W long. and 7 0 and 8 0 15' lat., was performed. These bodies include potassic, calc-alkalic, and peralkalic granitic associations, besides one with trondhjemitic affinities. The REE patterns for the potassic granitoids (Bodoco, Serra da Lagoinha and Itaporanga) which pierced basement migmatites, are strongly fractionated, mutually similar, LREE-enriched, and lack En anomaly. The calc-alkalic granitoids (Conceicao-type) intruded the low-grade metamorphics, and display strongly fractionated REE patterns, LREE-enriched relative to HREE, and exhibit a discrete, yet significative negative Eu anomaly. The granitoids with trondhjemitic affinities (Serrita-type) which intruded the Salgueiro schists, exhibit Σ REE much lower than in the previously mentioned granituids - REE patterns are strongly fractionated, LREE - enriched in relation to HREE, with discrete positive Eu anomaly and HREE approaching chondrite abundances. REE patterns of the peralkalic granitoids (Catingueira-type) ressemble those of rocks with trondhjemitic affinities and show a discrete positive Eu anomaly. The REE geochemistry agrees essentially with the major chemistry of the 4 granitoid associations, and is consistent with the 18 O/ 1 6O behavior which of ten varies sympathetically with Σ REE and S;O 2 . The presence of magmatic epidote, a high pressure phase, in three of these associations suggests that these rocks crystallized at a relatively great depth. (D.M.) [pt

  7. Petrology and Geochemistry of Shakh Sefid Granitoid and related skarn in the North of Rayen (southeastern of Kerman

    Directory of Open Access Journals (Sweden)

    Habib biabangard

    2017-11-01

    Full Text Available The Shakh Sefid Granitoid pluton and related Skarn are located 80 Km in the southeastern of Kerman and 20 Km north of Rayen. This area   is geologically located in the southeastern of the Lut block in the Central Iran. The Shakh Sefid Granitoid with Eocene-Oligocene age cuts the Cretaceous sedimentary rocks and led to the formation of Skarn. The granitoids are granite and granodiorite in composition composing of quartz, plagioclase, orthoclase, as primary minerals, biotite as minor and chlorite and sericite as secondary minerals. The sedimentary rocks are shale, sandstone, siltstone and limestone. Metamorphic rocks are marble and Skarns. The Skarn is calcic type. Garnet (grossular-andradite, tremolite and magnetite are the main minerals that are often accompanied with hematite, goethite and limonite. Pyrite, chalcopyrite and copper carbonate (malachite and azurite are the other minerals in Skarn. Geochemical studies show that the amount of major and minor elements of granitoid with increasing SiO2 content do not change due to the uniform mass, low dispersion of elements which result from heterogeneous textures and low alteration zone. Spider diagrams from minor elements normalized to Chondrite and primitive mantle show enrichment of all elements except for Ti, positive anomalies of Th, Pb and negative anomalies of Ti, P and Sr for the Sakh Sefid granitoids are probably due to crustal contamination. They are enriched in light rare earth elements (LREE between 10 to 100 times and heavy elements (HREE enrichment between 1 to 10 times compared to the reference (chondrite and regular pattern with approximately the same slope , the parallel trends indicate that the granitoid rocks share  a common source rock . The Shakh Sefid granitoid is I-type, metaluminous to peraluminous belonging to an active continental margin. Mineral and Mineralization in Kuh Shakh Sefid skarn is remarkably similar to iron skarn deposits. Minerals such as garnet and

  8. the origin of late archaean granitoids in the sukumaland greenstone

    African Journals Online (AJOL)

    Mgina

    melting at the base of a late Archaean thickened sub-arc basaltic crust. Melting to form the Suite 1 granitoids occurred in the eclogite stability field whereas Suite 2 formed by melting at shallower ... of TTG in terms of slab melting processes.

  9. Melting of subducted continental crust: Geochemical evidence from Mesozoic granitoids in the Dabie-Sulu orogenic belt, east-central China

    Science.gov (United States)

    Zhao, Zi-Fu; Liu, Zhi-Bin; Chen, Qi

    2017-09-01

    Syn-collisional and postcollisional granitoids are common in collisional orogens, and they were primarily produced by partial melting of subducted continental crust. This is exemplified by Mesozoic granitoids from the Dabie-Sulu orogenic belt in east-central China. These granitoids were emplaced in small volumes in the Late Triassic (200-206 Ma) and the Late Jurassic (146-167 Ma) but massively in the Early Cretaceous (111-143 Ma). Nevertheless, all of them exhibit arc-like trace element distribution patterns and are enriched in Sr-Nd-Hf isotope compositions, indicating their origination from the ancient continental crust. They commonly contain relict zircons with Neoproterozoic and Triassic U-Pb ages, respectively, consistent with the protolith and metamorphic ages for ultrahigh-pressure (UHP) metaigneous rocks in the Dabie-Sulu orogenic belt. Some granitoids show low zircon δ18O values, and SIMS in-situ O isotope analysis reveals that the relict zircons with Neoproterozoic and Triassic U-Pb ages also commonly exhibit low δ18O values. Neoproterozoic U-Pb ages and low δ18O values are the two diagnostic features that distinguish the subducted South China Block from the obducted North China Block. Thus, the magma source of these Mesozoic granitoids has a genetic link to the subducted continental crust of the South China Block. On the other hand, these granitoids contain relict zircons with Paleoproterozoic and Archean U-Pb ages, which are present in both the South and North China Blocks. Taken together, the Mesozoic granitoids in the Dabie-Sulu orogenic belt and its hanging wall have their magma sources that are predominated by the continental crust of the South China Block with minor contributions from the continental crust of the North China Block. The Triassic continental collision between the South and North China Blocks brought the continental crust into the thickened orogen, where they underwent the three episodes of partial melting in the Late Triassic, Late

  10. Genesis of Neoproterozoic granitoid magmatism in the Eastern Aracuai Fold Belt, eastern Brazil: field, geochemical and Sr-Nd isotopic evidence

    International Nuclear Information System (INIS)

    Celino, Joil Jose; Botelho, Nilson Francisquini; Pimentel, Marcio Martins

    2000-01-01

    The Neoproterozoic granitoid magmatism of the Aracuai Fold Belt (AFB) is an important element for the discussion of the evolution of this belt and its relationships with the African counterpart, the West Congo Belt. In the eastern part of the AFB, four different granitoid suites were recognized. The Nanuque Suite (NQS) comprises syn-tectonic peraluminous cordierite-bearing monzogranites. The Sao Paulinho Suite (SPS) consists of Th-rich peraluminous two mica or biotite-only granitoids. Calc-alkalic granitoids with magmatic epidote were grouped into the Itagimirim Suite (ITS) and post-tectonic charnockitic rocks were grouped into the Salomao Suite (SLS). Sm-Nd mineral isochron and Rb- isochron yielded ages of yielded ages of respectively 761 Ma and 714 Ma for the Nanuque and Sao Paulino suites. The general Sr-Nd isotopic characteristics of the granitoid suites and some country rocks indicate that the parental magmas were mostly the product of melting of the Paraiba do Sul metasediments. The chronological and genetic evolution the Neoproterozoic plutonism can be envisaged in a model of est-dipping subduction zone, followed by a continental collision between the Brasiliano/Pan-African (Brazil) and Congo (Africa cratons and final episodes of uplift and collapse. (author)

  11. On the metamorphic history of an Archaean granitoid greenstone terrane, East Pilbara, Western Australia, using the 40Ar/39Ar age spectrum technique

    International Nuclear Information System (INIS)

    Wijbrans, J.R.; McDougall, I.

    1987-01-01

    Age spectrum analyses of blue-green hornblendes from amphibolites from the Western Shaw Belt, East Pilbara, Western Australia, indicate an age of at least 3200 Ma for early regional metamorphism. Ages on hornblende and muscovite from the narrow contact zone with the adjacent Yule Batholith probably data updoming of the granitoid gneiss terranes at 2950 Ma. Hornblendes from within the Shaw Batholith and from a contact zone of a post-tectonic granitoid yield ages of 2840-2900 Ma, indicating either prolonged high temperatures within the granitoid gneiss terranes or a separate thermal pulse associated with the intrusion of post-tectonic granitoids. The preservation of very old hornblendes in a narrow greenstone belt surrounded by massive granitoid gneiss domes indicates that remarkable contrasts in metamorphic geotherms existed over short distances during the Late Archaean, suggesting that updoming occurred during a period of rapid tectonism. (orig.)

  12. Ar-Ar dating and petrogenesis of the Early Miocene Taşkapı-Mecitli (Erciş-Van) granitoid, Eastern Anatolia Collisional Zone, Turkey

    Science.gov (United States)

    Oyan, Vural

    2018-06-01

    The Early Miocene Taşkapı-Mecitli granitoid that is located in the northern section of the Eastern Anatolia Collision Zone has typical I-type, metaluminous and calk-alkaline characteristics. It also contains mafic microgranular / magmatic enclaves (MMEs). New Ar-Ar dating results show that the age of the Taşkapı-Mecitli granitoid is ∼23 Ma and it crystallised in the Early Miocene, in contrast to its previously known Cretaceous age. Identical crystallisation ages (∼23 Ma), similar mineral assemblages and geochemical compositions, and indistinguishable isotopic compositions of MMEs and host rocks imply that the MMEs are most consistent with a cumulate origin formed at earlier stages of the same magmatic system that produced the Taşkapı-Mecitli granitoid. MELTS modelling suggests that magma of the Taşkapı-Mecitli granitoid was the result of fractionation under a crustal pressure of 4 kbar, with a H2O content of 1.5%. EC-AFC model calculation reveals that the Taşkapı-Mecitli granitoid includes from 0.5% to 2% crustal assimilation rates. These rates indicate that crustal contamination can be negligible when compared to fractional crystallisation in the evolution of the magma beneath the Taşkapı-Mecitli granitoid. The partial melting model calculations and MORB-normalised trace element concentrations of the least evolved samples of the Taşkapı-Mecitli granitoid are consistent with those of mafic melts obtained from partial melting of interacting mantle- lower crust with a melting degree of 18%. The age (23 Ma) of the post- or syn-collisional Taşkapı-Mecitli granitoid suggests that the collision between Arabian and Eurasian plates could be before/around ∼23 Ma (Late Oligocene to Early Miocene).

  13. Granitoides paleozoicos de la Sierra de Narváez, Sistema de Famatina, Argentina: Hibridización de magmas en un margen continental activo

    Directory of Open Access Journals (Sweden)

    Cisterna, C. E.

    1992-12-01

    Full Text Available The granitoids from the Sierra de Narváez were investigated for their geochemical and petrographical characteristics. They are composed of calc-alkaline granites, granodiorites and tonalites, similar to the other paleozoic granitoids of the Famatina System. These rocks are intrusive in the Las Planchadas (volcanic rocks and Suri (sedimentary rocks Formations, which are probably cogenetic with the granitoids within the same magmatic cycle.The study of the granitoids reveals the close relationship between their composition and the abundance of the enclosed magmatic inclusions. The latter represent rocks and granodioritic tonalitic and diorite composition, and have a great number of mineralogical characteristic that suggest the presence of two magmas, mafic and felsic for the origin of such enclaves.The close chemical relationship existing between the inclusions and their host rocks shows that the mafic and felsic components are compositionally modified and that the granitoids are more or less hybridized.Trace elements discrimination diagrams have been used as a tools for fingerprinting the tectonic setting of the Sierra de Narváez granitoids. The geochemistry as well as the geologic relations of the granitoids with the roughly coeval ordovician vulcanism indicate a volcanic arc environment.Las rocas que afloran en el extremo septentrional de la Sierra de Narváez están representadas por una asociación de monzogranitos, granodioritas y tonalitas que definen una serie calcoalcalina, de características similares a las de otros intrusivos del Paleozoico del Sistema de Famatina. Estos granitoides se hallan intruyendo las Formaciones Las Planchadas y Suri, representadas por vulcanitas y metasedimentitas, respectivamente, y corresponderían a un mismo evento magmático del Paleozoico Inferior.Los granitoides estudiados presentan abundantes inclusiones ígneas de composición granodiorítica o tonalítica y diorítica. La estrecha relación que

  14. Electron probe micro analyser chemical zircon ages of the Khetri granitoids, Rajasthan, India: records of widespread late palaeoproterozoic extension-related magmatism

    International Nuclear Information System (INIS)

    Kaur, Parampreet; Chaudhri, Naveen; Biju-Sekhar, S.; Yokoyama, K.

    2006-01-01

    A number of granitoid plutons were emplaced in the northernmost entity of the Aravalli craton, the Khetri Copper Belt (KCB). We report here Th-U-Pb electron probe micro analyser chemical ages for zircon and monazite from two granitoid plutons of the north KCB, the Biharipur and Dabla. Zircons occurring in the granitoids depict well-developed magmatic zoning and are chronologically unzoned. Both the plutons and their diverse granitoid facies are coeval and provide ages around 1765-1710 Ma. Geochemical attributes of the studied plutons are typical of A-type within-plate granites and consistent with an extensional tectonic environment. Our new age data are comparable to the petrologically similar A-type granitoids of the Alwar region, which have provided zircon chemical ages around 1780-1710 Ma. These analogous ages imply a widespread late palaeoproterozoic extension-related plutonism in the northern part of the Aravalli craton. The monazites, which were recovered only from the mafic magmatic rocks of the Biharipur pluton, yielded an isochron age of 910 ±10 Ma, signifying an over- print of a younger neoproterozoic thermal event in the region. (author)

  15. Direct evidence for the origin of low-18O silicic magmas: Quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake, Oregon

    International Nuclear Information System (INIS)

    Bacon, C.R.; Adami, L.H.; Lanphere, M.A.

    1989-01-01

    Partially fused granitoid blocks were ejected in the climactic eruption of Mount Mazama, which was accompanied by collapse of Crater Lake caldera. Quartz, plagioclase, and glass in the granitoids have much lower δ 18 O values (-3.4 to +4.9per mille) than any fresh lavas of Mount Mazama and the surrounding region (+5.8 to +7.0per mille). Oxygen isotope fractionation between phases in granitoids is consistent with equilibrium at T≥900deg C following subsolidus exchange with hydrothermal fluids of meteoric origin. Assimilation of ≅ 10-20% of material similar to these granitoids can account for the O and Sr isotopic compositions of lavas and juvenile pyroclasts derived from the climactic magma chamber, many of which have δ 18 O values ≅ 0.5per mille or more lower than comparable lavas of Mount Mazama. The O isotope data provide the only clear evidence for such assimilation because the mineralogy and chemical and radiogenic isotopic compositions of the granitoids (dominantly granodiorite) are similar to those of erupted juvenile magmas. The granitoid blocks from Crater Lake serve as direct evidence for the origin of 18 O depletion in large, shallow silicic magma bodies. (orig.)

  16. Petrogenesis of Luchuba and Wuchaba granitoids in western Qinling: geochronological and geochemical evidence

    Science.gov (United States)

    Kong, Juanjuan; Niu, Yaoling; Duan, Meng; Zhang, Yu; Hu, Yan; Li, Jiyong; Chen, Shuo

    2017-12-01

    The West Qinling Orogenic Belt (WQOB) is a major portion of the Qinling-Dabie-Sulu Orogen and holds essential information for understanding the prolonged evolution of the northeastern branch of the Paleo-Tethys in East Asia. This study focuses on the petrogenesis of granitoids from Luchuba and Wuchaba plutons in the WQOB. We obtained zircon U-Pb ages of 211 ± 1.4 Ma for the Luchuba pluton and 218.7 ± 1.3 Ma for the Wuchaba pluton, which are the same as the proposed timing of continental collision at ˜220 Ma. We thus interpret the granitoids to represent a magmatic response to the collision between the North China Craton (NCC) and the Yangtze Block (YB). The two plutons are metaluminous to weakly peraluminous I-type granitoids. Samples from the two plutons show strong light rare earth element (REEs) enrichment and weak heavy REE depletion, with varying negative Eu anomalies, which is most consistent with significant plagioclase fractionation although the possible effect of plagioclase as residual phase in the magma source region cannot be ruled out. In primitive mantle normalized multi-element variation diagrams, nearly all the samples show negative Nb, Ta, P and Ti anomalies and relative enrichment in Rb, Pb, U and K. These characteristics resemble those of the average continental crust. The Luchuba pluton has lower (87Sr/86Sr)i (0.7051 to 0.7104), higher ɛNd(t) (-8.11 to -5.73) and ɛHf(t) (-6.70 to -1.65) than mature continental crust ([87Sr/86Sr] i > 0.72, ɛNd(t) pluton also has lower (87Sr/86Sr)i (0.7069 to 0.7080), higher ɛNd(t) (-9.86 to -3.34) and ɛHf(t) (-5.69 to 1.58) than mature continental crust. We conclude that the Luchuba and Wuchaba granitoids in the WQOB are best explained as resulting from fractional crystallization with crustal assimilation of parental magmas derived from melting of Mianlue oceanic crust under amphibolite facies conditions during the initial stage of continental collision between the North China Craton and the Yangtze Block

  17. Aprovechamiento del cambio de fase en la construcción

    OpenAIRE

    Domínguez Alonso, Manuel

    2011-01-01

    Nociones de transmisión de calor y de masa. Desfase y amortiguamiento. Los materiales de cambio de fase. Los materiales de cambio de fase en la construcción. Los materiales de cambio de fase en la climatización.

  18. On the metamorphic history of an Archaean granitoid greenstone terrane, East Pilbara, Western Australia, using the /sup 40/Ar//sup 39/Ar age spectrum technique

    Energy Technology Data Exchange (ETDEWEB)

    Wijbrans, J.R.; McDougall, I.

    1987-07-01

    Age spectrum analyses of blue-green hornblendes from amphibolites from the Western Shaw Belt, East Pilbara, Western Australia, indicate an age of at least 3200 Ma for early regional metamorphism. Ages on hornblende and muscovite from the narrow contact zone with the adjacent Yule Batholith probably data updoming of the granitoid gneiss terranes at 2950 Ma. Hornblendes from within the Shaw Batholith and from a contact zone of a post-tectonic granitoid yield ages of 2840-2900 Ma, indicating either prolonged high temperatures within the granitoid gneiss terranes or a separate thermal pulse associated with the intrusion of post-tectonic granitoids. The preservation of very old hornblendes in a narrow greenstone belt surrounded by massive granitoid gneiss domes indicates that remarkable contrasts in metamorphic geotherms existed over short distances during the Late Archaean, suggesting that updoming occurred during a period of rapid tectonism.

  19. The mechanics of granitoid systems and maximum entropy production rates.

    Science.gov (United States)

    Hobbs, Bruce E; Ord, Alison

    2010-01-13

    A model for the formation of granitoid systems is developed involving melt production spatially below a rising isotherm that defines melt initiation. Production of the melt volumes necessary to form granitoid complexes within 10(4)-10(7) years demands control of the isotherm velocity by melt advection. This velocity is one control on the melt flux generated spatially just above the melt isotherm, which is the control valve for the behaviour of the complete granitoid system. Melt transport occurs in conduits initiated as sheets or tubes comprising melt inclusions arising from Gurson-Tvergaard constitutive behaviour. Such conduits appear as leucosomes parallel to lineations and foliations, and ductile and brittle dykes. The melt flux generated at the melt isotherm controls the position of the melt solidus isotherm and hence the physical height of the Transport/Emplacement Zone. A conduit width-selection process, driven by changes in melt viscosity and constitutive behaviour, operates within the Transport Zone to progressively increase the width of apertures upwards. Melt can also be driven horizontally by gradients in topography; these horizontal fluxes can be similar in magnitude to vertical fluxes. Fluxes induced by deformation can compete with both buoyancy and topographic-driven flow over all length scales and results locally in transient 'ponds' of melt. Pluton emplacement is controlled by the transition in constitutive behaviour of the melt/magma from elastic-viscous at high temperatures to elastic-plastic-viscous approaching the melt solidus enabling finite thickness plutons to develop. The system involves coupled feedback processes that grow at the expense of heat supplied to the system and compete with melt advection. The result is that limits are placed on the size and time scale of the system. Optimal characteristics of the system coincide with a state of maximum entropy production rate. This journal is © 2010 The Royal Society

  20. FRACCIONAMIENTO DE CONTAMINANTES ORGÁNICOS PERSISTENTES EN AIRE URBANO DE MADRID: FASE GAS Y FASE PARTICULADA

    Directory of Open Access Journals (Sweden)

    Beatriz Barbas

    2014-01-01

    Full Text Available En el presente trabajo se evaluó la presencia de algunos Contaminantes Orgánicos Persistentes (COP en muestras de aire de la ciudad de Madrid (España, discriminando entre la fase gas (FG y la materia particulada en suspensión (MPS. Para ello se utilizaron captadores activos de alto volumen (CAV equipados con espumas de poliuretano y filtros de microfibra de vidrio. Los policlorobifenilos resultaron los contaminantes mayoritarios (104.6 ± 86.6 pg/Nm3, media ± desviación estándar, seguidos de polibromodifenil éteres (20.4 ± 11.6 pg/Nm3, declorane plus (0.8 ± 0.5 pg/Nm3 y finalmente policlorodibenzo-p-dioxinas y policlorodibenzofuranos (0.3 ± 0.1 pg/Nm3. Los resultados, en concordancia con los obtenidos en otras ciudades, no sólo confirman la presencia de COP en el aire de Madrid, sino que evidencian diferencias importantes en cuanto al fraccionamiento (presencia mayoritaria en la fase gas o en la fase particulada entre los distintos analitos y congéneres evaluados.

  1. Transformation of juvenile Izu-Bonin-Mariana oceanic arc into mature continental crust: An example from the Neogene Izu collision zone granitoid plutons, Central Japan

    Science.gov (United States)

    Saito, Satoshi; Tani, Kenichiro

    2017-04-01

    Granitic rocks (sensulato) are major constituents of upper continental crust. Recent reviews reveal that the average composition of Phanerozoic upper continental crust is granodioritic. Although oceanic arcs are regarded as a site producing continental crust material in an oceanic setting, intermediate to felsic igneous rocks occurring in modern oceanic arcs are dominantly tonalitic to trondhjemitic in composition and have lower incompatible element contents than the average upper continental crust. Therefore, juvenile oceanic arcs require additional processes in order to get transformed into mature continental crust enriched in incompatible elements. Neogene granitoid plutons are widely exposed in the Izu Collision Zone in central Japan, where the northern end of the Izu-Bonin-Mariana (IBM) arc (juvenile oceanic arc) has been colliding with the Honshu arc (mature island arc) since Middle Miocene. The plutons in this area are composed of various types of granitoids ranging from tonalite to trondhjemite, granodiorite, monzogranite and granite. Three main granitoid plutons are distributed in this area: Tanzawa plutonic complex, Kofu granitic complex, and Kaikomagatake granitoid pluton. Tanzawa plutonic complex is dominantly composed of tonalite and trondhjemite and characterized by low concentration of incompatible elements and shows geochemical similarity with modern juvenile oceanic arcs. In contrast, Kofu granitic complex and Kaikomagatake granitoid pluton consists mainly of granodiorite, monzogranite and granite and their incompatible element abundances are comparable to the average upper continental crust. Previous petrogenetic studies on these plutons suggested that (1) the Tanzawa plutonic complex formed by lower crustal anatexis of juvenile basaltic rocks occurring in the IBM arc, (2) the Kofu granitic complex formed by anatexis of 'hybrid lower crust' comprising of both basaltic rocks of the IBM arc and metasedimentary rocks of the Honshu arc, and (3) the

  2. Granites and granitoids of the southern region - Granite molybdenite system

    International Nuclear Information System (INIS)

    Issler, R.S.

    1987-01-01

    Economic concentrations of molybdenum are genetically closely associated with acidic and moderately acid granitoids-granites, granodiorites, monzonites and diorites, and are located in two geotectonic settings: subduction-related and rift-related. The aim of this paper is twofold, first succinctly approach the geology, tectonic setting and chemical parameters of the 'granite molybdenite system' as defined by Mutschler and/or alcali granite porphyry bodies emplaced in the North American continent for occasion of a Mesozoic-Fanerozoic extensile event; second to relate the computer-assisted evaluation of 422 major element chemical analysis of granites and granitoids of southern region of Brazil, using chemical fingerprints (SiO 2 ≥ 74. Owt%, Na 2 O ≤ 3.6wt%, K 2 O ≥ 4.5wt%), and K 2 O/Na 2 O ratio > 1.5 developed and testified from North American and Finnish occurrences, may locate molybdenite-bearing granite bodies with high exploration potential. These techniques suggest that some late Precambrian to early Paleozoic granite-rhyolite assemblages inserted at domains of the SG. 22/23 Curitiba/Iguape, SH. 21/22 Uruguaiana/Porto Alegre and SI.22 Lagoa Mirim Sheets, have exploration potential for molybdenum. (author) [pt

  3. Petrology of Oligocene Ghaleh Yaghmesh granitoids in the west of Yazd province

    Directory of Open Access Journals (Sweden)

    Bahareh Fazeli

    2017-02-01

    Full Text Available Introduction The generation and evolution of granitic magmas has been a hot debated subject among petrologists. The diversity of their origin has led different authors to propose that these rocks are not simple in their origin and might be generated in more ways than one. In the past several decades, many petrologists used a variety characteristics to subdivide the granitoid rocks. Such proposals have of course been forward by Chappell and White (1974 for the granitoids of Eastern Australia. They divided these granitoids into two distinct types (I-and S-type granitic rocks, which they interpreted as being derived from igneous and sedimentary source rocks, respectively. The Ghaleh Yaghmesh plutonic massif is located in the most western part of Yazd and it forms a part of the Urumieh-Dokhtar magmatic belt. The belt is response to subduction of Neo-Tethyan oceanic crust beneath central Iran (Alavi, 1994. During Cretaceous-Late Tertiary, numerous granitoid bodies were exposed in this belt, many of which have been studied by a number of workers (e.g. Sepahi and Malvandi, 2008; Honarmand et al., 2013; Kananian et al., 2014. The massif composed of diorite, quartzdiorite, tonalite, granodiorite and granite (Oligocene intruded into the Eocene volcanic and pyroclastic rocks including rhyolite, rhyodacite, andesitic, rhyodacitic and rhyolitic tuff. The main purpose of the present paper is to describe the petrography, and whole rock geochemistry of the Ghaleh Yaghmish granitoids as well as discussing their petrogenetic and tectonic significance in the light of the regional geological framework of the study area. Materials and methods After field studies and sampling, fifty thin sections were prepared for petrographic study. Twenty-one fresh samples were selected for XRF chemical analysis performed at the Southern Methodist University (Dallas - USA. Thin polished sections of granodiorite rocks were prepared for composition determining and structure formula

  4. Pre- and syn-Ross orogenic granitoids at Drake Head and Kartografov Island, Oates Coast, northern Victoria Land, East Antarctica

    International Nuclear Information System (INIS)

    Adams, C.J.; Roland, N.W.

    2002-01-01

    The majority of the Oates Coast, northern Victoria Land granitoids, typified by those at Drake Head and Kartografov Island (Harald Bay), are monzogranites with lesser granodiorites and minor quartz-monzodiorite and syenogranite. All are plagioclase-K-feldspar-biotite granitoids with additional muscovite, garnet and/or hornblende, and are subalkaline and peraluminous. Berg Granite typifies the early Ordovician, Granite Harbour Instrusive (GHI) suite of the Ross Orogen at the Oates Coast. Granitoids from Kartografov Island have higher amounts of Fe+Mg+Ti and an ambiguous Rb-Sr geochronology: they could be either pre-Ross Orogeny in age, or syn-Ross Orogeny and representing a lower structural level of GHI. The Drake Head granite gneiss has a fractionated leuco-granite composition similar to Berg Granite, and is intruded by granite and granodiorite. Rb-Sr ages indicate that all are Neoproterozoic, although the granite gneiss result is probably an errorchron age, reflecting its less uniform nature (granodiorite:649 ± 30 Ma, initial ratio 0.7065 +/- 6; granite gneiss: 682 ± 140 Ma, initial ratio 0.7107 ± 50). These late Neoproterozoic granitoids provide a source for distinctive detrital zircon age components in extensive early Paleozoic turbidites of Australia-New Zealand-Antarctica. (author). 24 refs., 5 figs., 1 tab

  5. An isotopic study of granitoids in the Litchfield Block, Northern Territory

    International Nuclear Information System (INIS)

    Page, R.W.; Bower, M.J.; Guy, D.B.

    1984-01-01

    The Litchfield Block contains a variety of granitoids, gneissic rocks, and migmatites that are intrusive into metasediments of probable Early Proterozoic age at the western margin of the Pine Creek Inlier. Isotopic data, which include U-Pb measurements on cogenetic zircon and xenotime and Rb-Sr total-rock measurements on the least metamorphosed granodiorites, show that these rocks crystallised from mantle-derived melts between 1840 Ma and 1850 Ma ago. Radiogenic Pb was lost from zircon in the early Palaeozoic (about 435 Ma), but xenotime remained a closed system until recent time. Many granitoids in the Litchfield Block have a gneissic fabric imposed during greenschist to amphibolite-grade regional metamorphism. This disturbance allowed partial isotopic re-equilibration of Rb-Sr total-rock systems, at about 1770 +- 16 Ma. As this igneous and metamorphic evolution is mirrored in other parts of the Pine Creek Inlier, the Halls Creek Inlier, and many other orogenic belts in northern Australia, its recognition and isotopic definition in the Litchfield Block further emphasise the magnitude and chronological integrity of this early Proterozoic tectonic event

  6. Chemical Zoning of Feldspars in Lunar Granitoids: Implications for the Origins of Lunar Silicic Magmas

    Science.gov (United States)

    Mills, R. D; Simon, J. I.; Alexander, C.M. O'D.; Wang, J.; Christoffersen, R.; Rahman, Z..

    2014-01-01

    Fine-scale chemical and textural measurements of alkali and plagioclase feldspars in the Apollo granitoids (ex. Fig. 1) can be used to address their petrologic origin(s). Recent findings suggest that these granitoids may hold clues of global importance, rather than of only local significance for small-scale fractionation. Observations of morphological features that resemble silicic domes on the unsampled portion of the Moon suggest that local, sizable net-works of high-silica melt (>65 wt % SiO2) were present during crust-formation. Remote sensing data from these regions suggest high concentrations of Si and heat-producing elements (K, U, and Th). To help under-stand the role of high-silica melts in the chemical differentiation of the Moon, three questions must be answered: (1) when were these magmas generated?, (2) what was the source material?, and (3) were these magmas produced from internal differentiation. or impact melting and crystallization? Here we focus on #3. It is difficult to produce high-silica melts solely by fractional crystallization. Partial melting of preexisting crust may therefore also have been important and pos-sibly the primary mechanism that produced the silicic magmas on the Moon. Experimental studies demonstrate that partial melting of gabbroic rock under mildly hydrated conditions can produce high-silica compositions and it has been suggested by that partial melting by basaltic underplating is the mechanism by which high-silica melts were produced on the Moon. TEM and SIMS analyses, coordinated with isotopic dating and tracer studies, can help test whether the minerals in the Apollo granitoids formed in a plutonic setting or were the result of impact-induced partial melting. We analyzed granitoid clasts from 3 Apollo samples: polymict breccia 12013,141, crystalline-matrix breccia 14303,353, and breccia 15405,78

  7. Some genetic aspects of hydrothermal uranium deposits in the Bakulja granitoide (Serbia)

    International Nuclear Information System (INIS)

    Jelenkovic, Rade

    1998-01-01

    This paper discusses the influence of temperature and the way of hydrothermal fluids flow in function of both the degree of tectonized granitoid and the origin of solutions, and partly the processes accompanying mineralization expressed through physico-chemical, mineralogical and mechanical alterations of the mother rock. It has been concluded that heat energy exchange is in function of: 1) petrochemical characteristic of a rock the hydrothermal fluids flow through; 2) degree of tectonization of the surrounding mineralized rocks; 3) volume and morphology of the fissured-porous space; 4) form of uranium bonding in mineral carriers; 5) degree of uranium leaching in hydrothermal solutions; 6) the way of hydrothermal fluids flow, and 7) coefficient of heat exchange expressed by distribution of heat energy within a fluid-rock system. It has also been established that contraction of granite volume results from physico-chemical processes that take place within a granitoid-hydrothermal fluid system and its quantification has been carried out. (Author)

  8. Mafic microgranular enclave swarms in the Chenar granitoid stock, NW of Kerman, Iran: evidence for magma mingling

    Science.gov (United States)

    Arvin, M.; Dargahi, S.; Babaei, A. A.

    2004-10-01

    Mafic microgranular enclaves (MME) are common in the Early to Middle Miocene Chenar granitoid stock, northwest of Kerman, which is a part of Central Iranian Eocene volcanic belt. They occur individually and in homogeneous or heterogeneous swarms. The MME form a number of two-dimensional structural arrangements, such as dykes, small rafts, vortices, folded lens-shapes and late swarms. The enclaves are elongated, rounded to non-elongated and subrounded in shape and often show some size-sorting parallel to direction of flow. Variation in the elongation of enclaves could reflect variations in the viscosity of the enclave, the time available for enclave deformation and differential strain during flow of the host granitoid magma. The most effective mechanism in the formation of enclave swarms in the Chenar granitoid stock was velocity gradient-related convection currents in the granitoid magma chamber. Gravitational sorting and the break-up of heterogeneous dykes also form MME swarms. The MME (mainly diorite to diorite gabbro) have igneous mineralogy and texture, and are marked by sharp contacts next to their host granitoid rocks. The contact is often marked by a chilled margin with no sign of solid state deformation. Evidence of disequilibrium is manifested in feldspars by oscillatory zoning, resorbed rims, mantling and punctuated growth, together with overgrowth of clinopyroxene/amphibole on quartz crystals, the acicular habit of apatites and the development of Fe-Ti oxides along clinopyroxene cleavages. These observations suggest that the MMEs are derived from a hybrid-magma formed as a result of the intrusion of a mafic magma into the base of a felsic magma chamber. The density contrast between hybrid-magma and the overlying felsic magma was reduced by the release of dissolved fluids and the ascent of exsolved gas bubbles from the mafic magma into the hybrid zone. Further convection in the magma chamber dispersed the hybridized magma as globules in the upper parts of

  9. Resultados de la fase de engorde en invernaderos

    OpenAIRE

    Sonnenholzner, Stanislaus

    2002-01-01

    Resultados de la fase de engorde en invernaderos Continuando con la serie de experimentos que se están desarrollando en la estación experimental Pesglasa para evaluar el efecto del tratamiento térmico en la supervivencia del camarón, se realizó la fase de engorde en invernaderos.

  10. Granitoid magmatism of Alarmaut granite-metamorphic dome, West Chukotka, NE Russia

    Science.gov (United States)

    Luchitskaya, M. V.; Sokolov, S. D.; Bondarenko, G. E.; Katkov, S. M.

    2009-04-01

    Main tectonic elements of West Chukotka are Alazey-Oloy, South-Anyui and Anyui-Chukotka fold systems, formed as a result of collision between structures of North-Asian continent active margin and Chukotka microcontinent [1-3]. South-Anyui fold system, separating Alazey-Oloy and Anyui-Chukotka systems, is considered as suture zon, formed as a result of oceanic basin closing [4-6]. Continent-microcontinent collision resulted in formation of large orogen with of northern and southern vergent structures, complicated by strike-slip deformations [7, 8]. Within Anyui-Chukotka fold system several rises, where most ancient deposits (crystalline basement and Paleozoic cover of Chukotka microcontinent) are exposed, were distinguished [2, 9-11]. Later they were considered as granite-metamorphic domes [12-14]. Alarmaut dome is located at West Chukotka to the north from Bilibino city and is traced from south to north in more than 120 km. General direction of structure is discordant to prevailing NW extensions of tectonic elements of the region. Paleozoic-Triassic deposits are exposed within the Alarmaut dome: 1) D3-C1 - crystalline schists, quartz-feldspar metasandstones, quartzites, marbles (700 m) [11]; 2) C1 - marblized limestones, quartz-feldspar metasandstones, quartzites, amphibole-pyroxene crystalline schists. Limestones contain corals, indicating Visean age of deposits [11]. Metamorphism reaches amphibolite facies, maximum P-T conditions are 660°С and 5 kbar. Migmatites, indicating in situ partial melting, are observed. Intensity of deformations of Paleozoic rocks increases at the boundary with Triassic deposits [11]; in the western part of dome slices of Pz rocks are separated by blastomylonite horizons [14]. Within Alramaut dome granitoids of Lupveem batholith (central part of dome), Bystrinsky pluton (southeastern part), and small Koyvel' and Kelil'vun plutons were studied. New U-Pb SHRIMP zircon data indicate Early Cretaceous (117-112 m.a.) age of granitoids [15

  11. Petrological mineralogical and geochemical characterization of the granitoids and fracture fillings developed in Ratones Mines (Spain)

    International Nuclear Information System (INIS)

    Buil Gutierrez, B.

    2002-01-01

    The petrological, mineralogical and geochemical characterisation of the granitoids and fracture fillings developed in the Ratones Mine (Caceres, Spain) has been done in order to understand rock-water interaction processes which control water geochemical parameters. Special interest has been devoted to the analysis and interpretation of REE patterns in the solid phase (granitoids and fracture fillings) because they constitute geochemical tracers in water-rock interaction process. Moreover, REE are considered as actinide analogues. In order to characterise the solid phase (granitoids and fracture fillings) several investigation scales (system, outcrop, whole rock, mineral and geochemical components) have been considered and different types of samples have been analysed. These factors control the methodological approach used in this investigation. The analytical methods we have used in this investigation are microscope, qualitative and semi-quantitative methods (XRD, SEM,EDAX) and quantitative methods (ICP-MS, XRF, EM, LAM-IC-MS). The bulk of the granitoids located around the Ratones Mine Belongs to the alkaline feldspar granite-sienogranite lihotype and they show a peraluminous and subalkaline pattern. From the mineralogical point of view, they are composed by quartz, K-feldspar (Or>90%), showing sericitation, moscovitization and turmolinization altherations, alkaline plagioclase (An-=-3%), usually altered to sericite, saussirite and less frequently affected by moscovitization processes, Fe-Al biotite, frequently affected by chloritization processes and sometimes replaced by muscovite, and finally muscovite (>2% celadonite and <4% paragonite) both of primary and secondary origin. The differences observed between the different lithotypes are related with the modal proportion of the principal minerals,with the presence or absence of certain accessory minerals ( turmaline, cordierite), with specific textural patterns, grain size and also with the richness in specific

  12. Crustal evolution of granitoids and gneisses from the Cambaizinho belt, southern Brazil: Review zircon Pb-Pb evaporation ages and Pb-Nd-Sr isotopes

    International Nuclear Information System (INIS)

    Remus, M.V.D; Macambira, M.B; Hartmann, L.A.; Beilfuss, M

    2001-01-01

    Deformed granitoids and gneisses from the Cambai Complex (900-700 Ma) along Cambaizinho Creek and in the Vila Nova do Sul region, state of Rio Grande do Sul, Brazil, were formed in a remarkably short time, about 10 m.y., between 704±13 and 697±3 Ma. The data base of this work includes eighteen zircon Pb/Pb evaporation analyses, five Pb isotope in feldspar and whole rock. The oldest known rocks in the region are polydeformed dioritic gneisses dated by conventional U-Pb zircon at 704±13 Ma. New Pb-Pb zircon evaporation data on the late transcurrent, less deformed and more evolved granitoids (Sanga do Jobim Granitoids) yield a 697± Ma age and indicates that the evolution of the plutonic magmatism in the area was nearly contemporaneous. These data contrast with previous interpretations based on Rb-Sr data which considered that these rock associations were formed during a longer time period (700-640 Ma). All these granitoids intruded the supracrustal sequence. These granitoids yield a minimum age of about 700 Ma for the formation of the supracrustal sequence and its regional dynamothermal metamorphism. Lead isotope composition of K-feldspar from Sanga do Jobim Granitoids plot close to, but slightly below the lead isotope evolution curve of orogeny in the Zartmann and Doe model (1981). This indicates that the setting for these granitoids was that of a juvenile magmatic arc. These new data plus previous data in the region also corroborate that the crustal evolution involved juvenile crust accreted between 760-700 Ma. In contrast, the Cacapava and Sao Sepe Granites intruded the supracrustal sequences along the eastern side of the Sao Gabriel Block at 562 Ma and 550 Ma, respectively, and show Pb and Nd isotope signatures from an old basement. This evidence suggests that the juvenile terrane was thrusted over the older basement situated along the eastern part of the shield during the Dom Feliciano collisional orogeny at about 620-590 Ma (au)

  13. New monazite U-Pb age constraints on the evolution of the Paleoproterozoic Vaasa granitoid batholith, western Finland

    Directory of Open Access Journals (Sweden)

    A.K. Kotilainen

    2016-09-01

    Full Text Available The Vaasa batholith, western Finland, is a large, peraluminous granitoid pluton that crystallized at 1.88–1.87 Ga during the culmination of the Svecofennian orogeny. The batholith has gradual contacts, through metatexites and diatexites, with the enveloping metasedimentary rocks of the Bothnian Belt. We present ID-TIMS U-Pb age data on monazite from granitoids and xenoliths of the Vaasa batholith and combine these with published U–Pb zircon ages in order to shed further light on the evolution of the Vaasa batholith. The apparent monazite ages for seven of the examined samples are 1870–1863 Ma, and 1855±3 Ma for one further sample from the southern part of the batholith. Combined with pre-existing data, the monazite ages of the granitoids are 9 to 18 Ma (face values or 3 to 9 Ma (external errors considered younger than the U–Pb zircon crystallization ages from respective samples. Our new data suggest slow cooling for the Vaasa batholith – the closure/saturation temperature of the monazite U–Pb system was probably reached in ~10 m.y. after the crystallization of magmatic zircon in the examined rocks.

  14. FASCODE for the environment (FASE)

    Energy Technology Data Exchange (ETDEWEB)

    Snell, H.E.; Moncet, J.L. [Atmospheric and Environmental Research, Inc., Cambridge, MA (United States); Anderson, G.P.; Chetwynd, J.H. [Phillips Lab., Hanscom AFM, MD (United States)] [and others

    1996-04-01

    The Optical Physics Division of the Phillips Laboratory, with support from the U.S. Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) Program, is developing a state-of-the-art line-by-line atmospheric radiative transfer model as the successor to FASCODE. The goal of this project is to create a computationally efficient model which contains the most up-to-date atmospheric physics. The new model, known as FASCODE for the Environment, or {open_quotes}FASE{close_quotes}, will combine the best features of FASCODE and LBLRTM, the DOE`s standard radiative transfer model. FASE will also contain new features such as new cross-sections for heavy molecules, and improved solar irradiance model, and improvements to the Schumann-Runge bands and continuum. The code will be optimized for vectorized and/or parallel processing. put under configuration control for easy maintenance, and structured into separate modules for each function: atmospheric profiles, layer optical properties, radiative transfer, multiple-scattering, etc. This modular structure will allow for increased flexibility and easy customization of the code for specialized applications, such as a forward model for iterative inversion algorithms. Ease-of-use will be enhanced with improved input control structures and documentation to accommodate the needs of novice and advanced users. This paper addresses changes which have been made to FASCODE and LBLRTM to create FASE, and gives an overview of the modular structure and its capabilities.

  15. Ordovician A-type granitoid magmatism on the Ceará Central Domain, Borborema Province, NE-Brazil

    Science.gov (United States)

    Castro, Neivaldo A.; Ganade de Araujo, Carlos E.; Basei, Miguel A. S.; Osako, Liliane S.; Nutman, Alan A.; Liu, Dunyi

    2012-07-01

    We present field relationships, major and trace element geochemistry and U-Pb SHRIMP and ID-TIMS geochronology of the A-type Ordovician Quintas pluton located in the Ceará Central Domain of the Borborema Province, in northeastern Brazil. This pluton presents a concentric geometry and is composed mainly of syenogranite, monzogranite, quartz syenite to quartz monzodiorite, monzogabbro and diorite. Its geochemical characteristics [SiO2 (52-70%), Na2O/K2O (1.55-0.65), Fe2O3/MgO (2.2-7.3), metaluminous to sligthly alkaline affinity, post-collisional type in (Y + Nb) × Rb diagram, and A-type affinity (Ga > 22 ppm, Nb > 20 ppm, Zn > 60 ppm), REE fractioned pattern with negative Eu anomaly] are coherent with post-collisional A2-type granitoids. However, the emplacement of this pluton is to some extent temporally associated with the deposition of the first strata of the Parnaíba intracratonic basin, attesting also to a purely anorogenic character (A1-type granitoid). The emplacement of this pluton is preceded by one of the largest known orogenesis of the planet (Neoproterozoic Pan-African/Brasiliano) and, if it is classified as an A2-type granitoid, it provides interesting constraints about how long can last A2-type magmatic activity after a major collisional episode, arguably triggered by disturbance of the underlying mantle, a topic extensively debated in the geoscience community.

  16. Review of the geochemistry and metallogeny of approximately 1.4 Ga granitoid intrusions of the conterminous United States

    Science.gov (United States)

    du Bray, Edward A.; Holm-Denoma, Christopher S.; Lund, Karen; Premo, Wayne R.

    2018-03-27

    The conterminous United States hosts numerous volumetrically significant and geographically dispersed granitoid intrusions that range in age from 1.50 to 1.32 billion years before present (Ga). Although previously referred to as A-type granites, most are better described as ferroan granites. These granitoid intrusions are distributed in the northern and central Rocky Mountains, the Southwest, the northern midcontinent, and a swath largely buried beneath Phanerozoic cover across the Great Plains and into the southern midcontinent. These intrusions, with ages that are bimodally distributed between about 1.455–1.405 Ga and 1.405–1.320 Ga, are dispersed nonsystematically with respect to age across their spatial extents. Globally, although A-type or ferroan granites are genetically associated with rare-metal deposits, most U.S. 1.4 Ga granitoid intrusions do not contain significant deposits. Exceptions are the light rare-earth element deposit at Mountain Pass, California, and the iron oxide-apatite and iron oxide-copper-gold deposits in southeast Missouri.Most of the U.S. 1.4 Ga granitoid intrusions are composed of hornblende ± biotite or biotite ± muscovite monzogranite, commonly with prominent alkali feldspar megacrysts; however, modal compositions vary widely. These intrusions include six of the eight commonly identified subtypes of ferroan granite: alkali-calcic and calc-alkalic peraluminous subtypes; alkalic, alkali-calcic, and calc-alkalic metaluminous subtypes; and the alkalic peralkaline subtype. The U.S. 1.4 Ga granitoid intrusions also include variants of these subtypes that have weakly magnesian compositions. Extreme large-ion lithophile element enrichments typical of ferroan granites elsewhere are absent among these intrusions. Chondrite-normalized rare-earth element patterns for these intrusions have modest negative slopes and moderately developed negative europium anomalies. Their radiogenic isotopic compositions are consistent with mixing involving

  17. Abundances of chemical elements in granitoids of different geological ages and their characteristics in China

    Directory of Open Access Journals (Sweden)

    Changyi Shi

    2011-04-01

    Full Text Available Actual granitoid analytical data of 767 composited samples are presented here. The data source is 6080 samples collected mainly from 750 large- to middle-sized granitoid bodies across China. Data from the composited samples, which includes that of 70 elements, is analyzed according to geological age — Archeozoic (Ar, Proterozoic (Pt, Eopaleozoic (Pz1, Neopaleozoic (Pz2, Mesozoic (Mz, and Cenozoic (Cz — and three major compositional varieties, e.g. alkali-feldspar granite, syenogranite and adamellite. Petrochemical parameters, trace-element content and rare-earth element (REE distributions of the different rock types and geological ages are characterized, and change tendencies through Archean to Cenozoic time are recorded. The comprehensive analytical data presented here has not been previously published. This significant data set can be used as fundamental information in studies of basic China geology, magma petrogenesis, ore exploration and geochemistry.

  18. Diversity, origin and tectonic significance of the Mesoarchean granitoids of Ourilândia do Norte, Carajás province (Brazil)

    Science.gov (United States)

    da Silva, Luciano Ribeiro; de Oliveira, Davis Carvalho; dos Santos, Maria Nattânia Sampaio

    2018-03-01

    This study investigates the diversity, origin and tectonic significance of the Ourilândia do Norte Mesoarchean granitoids, emplaced near Rio Maria-Carajás domains boundary, southeastern Amazonian Craton (Brazil). In this area, previous works has identified sanukitoids (∼2.87 Ga), (quartz) diorites of BADR affinity and undifferentiated leucogranites, with charnockites cross-cutting the other granitoids. New geological mapping data allowed to differentiate three new groups of granitoids: (i) biotite monzogranites (BMzG); (ii) epidote-biotite granodiorites (EBGd); and (iii) porphyritic granitoids (pGrt). Thus, this paper aims to define their classification, nature, formation processes and deformation aspects, and discuss the relations between plutonism and deformation for the Ourilandia do Norte granitoids. The petrographic data showed that each one of these groups can be subdivided into two facies. The BMzG is differentiated into equigranular (eBMzG) and heterogranular (hBMzG) and the EBGd into heterogranular (hEBGd) and sparsely porphyritic (spTEBGd). These granitoids constitute two batholiths separated by a rock strip of sanukitoid and BADR affinities. Both are largely dominated by BMzG rocks, with less abundant EBGd lenses. The pGrt is individualized in porphyritic granodiorites (pBHGd) and trondhjemites (pEBTd), which occur as smaller bodies. Structurally, the central portions these plutons represent lower strain domains, while their borders are marked by large-scale shear zones, where occur submagmatic and mylonitic fabrics of ENE-WSW main direction and subvertical dip, respectively. The meso- and microstructural data indicate that the rocks studied are syn-to late-tectonic and were affected by high temperature deformation (>500 °C) and low differential stress, in a sinistral transpression regime, indicating that both fabrics are related to the a same deformational event. Geochemically, except the pEBTd facies that has sodic affinity, the Ourilândia do

  19. Estudio de separación de fases en sistemas líquido-líquido usando LIX 984N en fase orgánica

    Directory of Open Access Journals (Sweden)

    Castillo-Segura, J.

    2012-04-01

    Full Text Available In this work we studied the sedimentation and coalescence phenomena in liquid-liquid dispersion without chemical reaction, the aqueous electrolyte consisted of 0.25 M sodium sulfate and an organic phase characteristic organic extractant for copper (LIX 984N diluted in a commercial solvent (Shellsol 24 AR. The phenomena that dominate the phase separation have been studied by several researchers, which proposed a number of models to predict sedimentation and coalescence profiles. In this work we applied a semi-empirical model to describe the phenomena involved, varying the following experimental conditions: percentage of extractant in organic phase (5 - 30 % v / v, continuous phase (aqueous and organic, time and stirring speed (30 - 1800 s and 400 - 1200 rpm respectively. The main results show that from the 800 rpm of agitation this variable has no influence on primary breakup time, in the same way for 180 seconds of stirring produces the same effect. The fraction of dispersed phase in the packing zone found was 0.74. For higher levels of percentage of extractant in organic phase increased the phase separation time as when the organic phase was used as the continuous phase relative to the aqueous phase. We found a partial adjustment of the experimental data in relation to the simulated values , which is attributable to two factors: the initial inertia of the system once the agitation stopped and the existence of different times of inflection points of the curves of sedimentation and coalescence. In the different articles found in literature assume that the above phenomena occur simultaneously.

    En este trabajo se estudiaron los fenómenos de sedimentación y coalescencia en una dispersión líquido-líquido sin reacción química, la fase acuosa consistió en electrolito de sulfato de sodio 0,25 M y una fase orgánica de extractante característico para el cobre (LIX 984N diluido en un solvente comercial (shellsol 24 AR. Los fenómenos que

  20. Devonian granitoids and their hosted mafic enclaves in the Gorny Altai terrane, northwestern Central Asian Orogenic Belt: crust-mantle interaction in a continental arc setting

    Science.gov (United States)

    Chen, Ming; Sun, Min

    2016-04-01

    Granitoids are a major component in the upper continental crust and hold key information on how did the continental crust grow and differentiate. This study focuses on the Yaloman intrusive complex from the Gorny Altai terrane, northwestern Central Asian Orogenic Belt (CAOB). The association of granitoids and mafic enclaves can provide important clues on the source nature, petrogenetic processes and geodynamic setting of the Yaloman intrusive complex, which in turn will shed light on the crustal evolution in the northwestern CAOB. Zircon U-Pb dating shows that the granitoids, including quartz diorites and granodiorites, were emplaced in ca. 389-387 Ma. The moderate Na2O + K2O contents and low A/CNK values indicate that these rocks belong to the sub-alkaline series with metaluminous to weakly peraluminous compositions. The granitoids yield two-stage zircon Hf model ages of ca. 0.79-1.07 Ga and whole-rock Nd model ages of ca. 0.90-0.99 Ga, respectively, implying that they were mainly sourced from Neoproterozoic juvenile crustal materials. The mafic enclaves show an almost identical crystallization age of ca. 389 Ma. The identification of coarse-grained xenocrysts and acicular apatites, together with the fine-grained texture, makes us infer that these enclaves are likely to represent magmatic globules commingled with the host magmas. The low SiO2 and high MgO contents of the mafic enclaves further suggest that substantial mantle-derived mafic melts were probably involved in their formation. Importantly, the SiO2 contents of the granitoids and mafic enclaves are well correlated with other major elements and most of the trace elements. Also a broadly negative correlation exists between the SiO2 contents and whole-rock epsilon Nd (390 Ma) values of the granitoids. Given the observation of reversely zoned plagioclases within the granitoids and the common occurrence of igneous mafic enclaves, we propose that magma mixing probably played an important role in the formation

  1. Les granitoïdes hercyniens post-collisionnels du Maroc oriental : une province magmatique calco-alcaline à shoshonitiqueThe post-collisional Hercynian granitoids from eastern Morocco: a calc-alkaline to shoshonitic magmatic province

    Science.gov (United States)

    El Hadi, Hassan; Tahiri, Abdelfatah; Reddad, Aicha

    2003-11-01

    The post-collisional Hercynian granitoids crop out in the easternmost part of the Moroccan Hercynian belt. Petrographical and geochemical studies show a composition similarity in the various granitoids. The granitoids belong to per-aluminous and metaluminous magmatic associations. They have evolved according to a scheme similar to high-K calc-alkaline to shoshonitic associations. To cite this article: H. El Hadi et al., C. R. Geoscience 335 (2003).

  2. A-type granitoid in Hasansalaran complex, northwestern Iran: Evidence for extensional tectonic regime in northern Gondwana in the Late Paleozoic

    Science.gov (United States)

    Azizi, Hossein; Kazemi, Tahmineh; Asahara, Yoshihiro

    2017-07-01

    The Hasansalaran plutonic complex is one of the main intrusive bodies with a wide range of granite, monzonite, diorite and syenite that crop out in northwest Iran. This body includes Paleozoic granitoids that are surrounded and cut by Cretaceous granitoids. Zircon U-Pb age dating shows that the crystallization of this body occurred at 360 Ma ago in the Early Carboniferous. Whole rock compositions of the investigated intrusive body, show high contents of Ga (11.1-76.3 ppm), Zr (73.5-1280 ppm), Zn (43.7-358 ppm), Y(17.9-177 ppm), enrichment of rare earth elements (REEs) together with high Ga/Al ratios and a strong Eu negative anomaly, fairly consistent with typical A-type signature. The low εNd(t = 360 Ma) value (model for evolution of northwest Iran in the Late Paleozoic. Based on our model, the upwelling of a mantle plume, probably due to the proto-Tethys oceanic rollback activity beneath northern Gondwana, had a crucial role in the uplifting of the continental crust and resulted in the crystallization of A-type granitoids with some gabbroic rocks in northwest Iran.

  3. From steep feeders to tabular plutons - Emplacement controls of syntectonic granitoid plutons in the Damara Belt, Namibia

    Science.gov (United States)

    Hall, Duncan; Kisters, Alexander

    2016-01-01

    Granitoid plutons in the deeply eroded south Central Zone of the Damara Belt in Namibia commonly show tabular geometries and pronounced stratigraphic controls on their emplacement. Subhorizontal, sheet-like pluton geometries record emplacement during regional subhorizontal shortening, but the intrusion of spatially and temporally closely-related granitoid plutons at different structural levels and in distinct structural settings suggests independent controls on their levels of emplacement. We describe and evaluate the controls on the loci of the dyke-to-sill transition that initiated the emplacement of three syntectonic (560-530 Ma) plutons in the basement-cover stratigraphy of the Erongo region. Intrusive relationships highlight the significance of (1) rigidity anisotropies associated with competent sedimentary packages or pre-existing subhorizontal granite sheets and (2) rheological anisotropies associated with the presence of thick ductile marble horizons. These mechanical anisotropies may lead to the initial deflection of steep feeder conduits as well as subsequent pluton assembly by the repeated underaccretion of later magma batches. The upward displacement of regional isotherms due to the heat advection associated with granite emplacement is likely to have a profound effect on the mechanical stratification of the upper crust and, consequently, on the level at which granitoid pluton emplacement is initiated. In this way, pluton emplacement at progressively shallower crustal depths may have resulted in the unusually high apparent geothermal gradients recorded in the upper crustal levels of the Damara Belt during its later evolution.

  4. Geochemical characteristics of granitoids and related mafic granulites from the Pan-African Dahomeyide belt, southeastern Ghana

    International Nuclear Information System (INIS)

    Aidoo, F.

    2012-07-01

    The Dahorneyide orogenic belt marks the southeastern limit of the West Africa craton (WAC). The belt consists of three structural units which include the deformed eastern edge of the WAC with its cover rocks made up of the Togo and the Buern Structural Units (external nappes), a suture zone assemblage of mafic and ultramafic rocks, and granitoid gneiss-rnigmatite assemblages (east of the suture zone). Geochemical and petrographic characteristics of the granitoids from the external nappes and mafic and ultramafic granulites roeks from the suture zone have been studied with the objective of inferring their petrogenesis and tectonic setting in which they were formed. Twenty five (25) representative samples were selected for petrographic studies and fifteen samples for major and trace elements composition using ICP-AES and ICP-MS respectively. The granitoids gneisses are mainly biotite muscovite gneisses, migmatites and granodiorites made up of quartz (25-68%), biotite (7-30%), plagioclase (8-40%), muscovite (4-20%) with some few pyroxene, sericite and calcite observed in some oF the samples. Within these rocks is an amphibole rich gneiss composed of about 45% amphiboles. The granitoid gneisses contain SiO 2 content of 40.60-68.90 wt. % with low Mg# of 36-46. Geochernically, they are classified as I-type, mctaluminous to peraluminous, magnessian to ferroan, calcic to calc alkali granitoids. They exhibit fractionated REE patterns with (La/Sm) N = 1.80-5.85 and (La/Yb) N = 3.76-76.30, and negative to positive Eu anomalies (Eu/Eu*'' = 0.68-2.10. The primitive mantle-normalised, trace element patterns show that the granitoid gneisses are characterised by enrichment in LILE relative to HFSE and in LREE relative HREE. They display subduction-related trace element characteristics of positive Ba and negative Ti, Ta, Nb and Hf anomalies. The mafic granulites are composed of quartz (16-43%), hornblende (12-45%), plagioclase (13-23%), pyroxene (13-17%), garnet (4

  5. Multiple sources of magmatism. granitoids from southeast Kohistan, NW Himalayas, Pakistan

    International Nuclear Information System (INIS)

    Khan, M. A.; Qazi, M. S.

    2005-01-01

    The Kohistan island arc terrane in the northwestern Himalayas of N. Pakistan is sandwiched between the Indian and Karakoram plated. The base of the arc is occupied by a major stratiform ultramafic-gabbroic complex (the Sapat-Babusar complex), which overrides the crust of the Indian plate along the Indus suture (i.e., the Main Mantle Thrust; MMT). It was intruded into the base of a thick pile of metavolcanics (the Kamila belt), which comprise a tectonic collage of MORB-type tholeiitic basalts, island-arc tholeiites and calc-alkaline andesites. The Chilas complex, comprising ultramafic and gabbronorite rocks, is also intrusive into the Kamila belt, it is emplaced onto the top rather than the base of the Kamila belt. A sizeable proportion of granitoid rocks are present in the south-eastern part of Kohistan, which intruded the Kamila amphibolites. These are predominantly dioritic in composition, but include gabbros, granodiorites, granites and trondhjemites. The granitoids occur in two types. (1) large sheet-like lenticular masses, and (2) minor intrusives in the form of veints, sills or dykes. Three large sheets like bodies are mapped. All these bodies are composite, comprising gabbros, diorite/tonalite, granodiorite and granite. The minor intrusion of granitic and trondhjemitic composition are abundantly present in the form of veins, sills and dykes; and are characterized by variation in distribution. Strong shearing transformed the rocks into blastomylonite gneisses. The mineral assemblage consists of quartz, plagioclase, emphibole, epidote, chlorite, biotite, muscovite, sphene, magnetite and apatite. (author)

  6. Multiple sources of magmatism: granitoids from southeast kohistan, nw himalayas Pakistan

    International Nuclear Information System (INIS)

    Sayab, M.; Qazi, M.S.

    2005-01-01

    The Kohistan island arc terrane in the northwestern Himalayas of N. Pakistan is sandwiched between the Indian and Karakoram plates. The base of the arc is occupied by a major stratiform ultramafic-gabbroic complex (the Sapat-Babusar complex). which overrides the crust of the Indian plate along the Indus suture (i. e., the Main Mantle Thrust; MMT). It was intruded into the base of a thick pile of metavolcanics (the Kamila belt), which comprise a tectonic collage of MORB-type tholeiitic basalts, island-arc tholeiites and calc-alkaline andesites. The Chilas complex, comprising ultramafic and gabbronorite rocks, is also intrusive into the Kamila belt. It is emplaced onto the top rather than the base of the Kamila belt. A sizeable proportion of granitoid rocks are present in the south-eastern part of Kohistan. Which intruded the Kamila amphibolites. These are predominantly dioritic in composition but include gabbros, granodiorites, granites and trondhjemites. The granitoids occur in two types: (I) large sheet-like lenticular masses, and (2) minor intrusives in the form of veins sills or dykes. Three large sheets like bodies are mapped. All these bodies are composite, comprising gabbros, diorite/tonalite. granodiorite and granite. The minor intrusions of granitic and trondhjemitic composition are abundantly present in the form of veins, sills and dykes and are characterized by variation in distribution. Strong shearing transformed the rocks into blastomylonite gneisses. The mineral assemblage consists of quartz, plagioclase, Amphibole, epidote, chlorite, biotite, muscovite, sphene, magnetite and apatite. (author)

  7. Oxygen and U-Th isotopes and the timescales of hydrothermal exchange and melting in granitoid wall rocks at Mount Mazama, Crater Lake, Oregon

    Science.gov (United States)

    Ankney, Meagan E.; Bacon, Charles R.; Valley, John W.; Beard, Brian L.; Johnson, Clark M.

    2017-01-01

    We report new whole rock U-Th and in-situ oxygen isotope compositions for partially melted (0–50 vol% melt), low-δ18O Pleistocene granitoid blocks ejected during the ∼7.7 ka caldera-forming eruption of Mt. Mazama (Crater Lake, Oregon). The blocks are interpreted to represent wall rocks of the climactic magma chamber that, prior to eruption, experienced variable amounts of exchange with meteoric hydrothermal fluids and subsequent partial melting. U-Th and oxygen isotope results allow us to examine the timescales of hydrothermal circulation and partial melting, and provide an “outside in” perspective on the buildup to the climactic eruption of Mt. Mazama. Oxygen isotope compositions measured in the cores and rims of individual quartz (n = 126) and plagioclase (n = 91) crystals, and for transects across ten quartz crystals, document zonation in quartz (Δ18OCore-Rim ≤ 0.1–5.5‰), but show homogeneity in plagioclase (Δ18OCore-Rim ≤ ±0.8‰). We propose that oxygen isotope zonation in quartz records hydrothermal exchange followed by high-temperature exchange in response to partial melting caused by injection of basaltic to andesitic recharge magma into the deeper portions of the chamber. Results of modeling of oxygen diffusion in quartz indicates that hydrothermal exchange in quartz occurred over a period of ∼1000–63,000 years. Models also suggest that the onset of melting of the granitoids occurred a minimum of ∼10–200 years prior to the Mazama climactic eruption, an inference which is broadly consistent with results for magnetite homogenization and for Zr diffusion in melt previously reported by others.Uranium-thorium isotope compositions of most granitoid blocks are in 238U excess, and are in agreement with a 238U enriched array previously measured for volcanic rocks at Mt. Mazama. Uranium excess in the granitoids is likely due to enrichment via hydrothermal circulation, given their low δ18O values. The sample with the

  8. Unusual Rb-Sr data on the age of two typical peralkaline granitoid plutons in West Transbeikalia

    International Nuclear Information System (INIS)

    Litvinovskij, B.A.; Posokhov, V.F.; Zanvilevich, A.N.

    1995-01-01

    Rb-Sr isotope study of two typical plutons in West Transbaikalia (Bryansk and Kharitonov) has been carried out. For alkaline and peralkaline suits of the Bryansk pluton the obtained data are 287 ± m.y., I Sx =0.7054 ± 3 and 285 ± 1 m.y., I Sr =0.7037 ± 3 respectively. Rb-Sr age of peralkaline syenites and granites from the Kharitonov pluton are in more or less consistency with those on the Malokunal pluton (233 ± 5 m.y.) and much less than the age of the Khorinsk pluton (253 ± 3 m.y.). Taking into account the K-Ar data on amphibole from the peralkaline granitoids it is concluded that probable age of these rocks span the interval 250-220 m.y. However results obtained from the Bryansk pluton suggest that within the Mongolia-Transbaikalia belt one more stage of peralkaline granitoid generation i.e. the Early Permian stage could be manifested as well. 20 refs.; 5 figs.; 3 tabs

  9. U-Th-Pb systematics of some granitoids from the northeastern Yilgarn Block, Western Australia and implications for uranium source rock potential

    Energy Technology Data Exchange (ETDEWEB)

    Stuckless, J S; Nkomo, I T [Geological Survey, Denver, CO (USA); Bunting, J A [Geological Survey of Western Australia, Perth

    1981-11-01

    The Mount Boreas-type granite and spatially associated syenitic granitoid of Western Australia yield Pb-Pb ages of 2370 +- 100 Ma and 2760 +- 210 Ma, respectively. Th-Pb ages, although less precise, are concordant with these ages, and therefore the apparent ages are interpreted to be the crystallisation ages for these two units. U-Pb ages are variable and for the most part anomalously old, which suggests a Cainozoic uranium loss. However, this loss is generally small (3..mu..g/g); therefore, neither granitoid in its fresh state provides a good source for nearby calcrete-hosted uranium deposits. The possibility remains that the Mount Boreas-type granite that has been completely weathered during the Tertiary could have been a source for the calcrete-type uranium deposits in W.A. Although the Mount Boreas-type granite is highly fractionated, it does not bear a strong geochemical imprint of a sedimentary precursor. This feature contrasts it with apparently fresh granitoids from other parts of the world that have lost large amounts of uranium (approx. 20..mu..g/g) and are associated with large roll-type and other low temperature-type uranium deposits.

  10. Geochemistry and petrogenesis of Mesoproterozoic A-type granitoids from the Danish island of Bornholm, southern Fennoscandia

    DEFF Research Database (Denmark)

    Johansson, Åke; Waight, Tod Earle; Andersen, Tom

    2016-01-01

    Granitoids and gneisses from the Danish island of Bornholm have been investigated using whole rock geochemistry, Sr and Nd isotope geochemistry and Hf isotopes in zircon. Recent U–Pb dating shows that the rocks were formed during a short time interval at 1.45 to 1.46 Ga, penecontemporaneous...

  11. Granitoids of the Dry Valleys area, southern Victoria Land, Antarctica : plutons, field relationships, and isotopic dating

    International Nuclear Information System (INIS)

    Allibone, A.H.; Cox, S.C.; Johnstone, R.D.

    1993-01-01

    Detailed mapping throughout much of the Dry Valleys area indicates the region is underlain by 15 major granitoid plutons and numerous smaller plugs and dikes. Intrusive relationships of these plutons and dikes indicate repeated intrusion of superficially similar granitoids at different times. Sufficient internal lithologic variation occurs within individual plutons, to allow correlation with several of the previously defined granitoid units based on lithologic character. Consequently, previous subdivision schemes based on lithology are no longer tenable and are here replaced with a subdivision scheme based on the identification of individual plutons. The elongate, concordant Bonney, Denton, Cavendish, and Wheeler Plutons, which range in composition between monzodiorite and granodiorite, are the oldest relatively undeformed plutons in the Dry Valleys area. Each pluton is characterised by flow alignment of K-feldspar megacrysts, hornblende, biotite, and mafic enclaves. Field relationships and radiometric dating indicate these are deep-level plutons, emplaced synchronous with upper amphibolite facies metamorphism of the adjacent Koettlitz Group between 589 and 490 Ma ago. Elongate, discordant plutons of equigranular homogeneous biotite granodiorite and granite (Hedley, Valhalla, St Johns, Suess) were subsequently emplaced by stoping at a relatively high crustal level at 490 Ma. These eight plutons are cut by numerous swarms of Vanda mafic and felsic porphyry dikes. The ovoid, discordant, high level Pearse, Nibelungen, Orestes, Brownworth, Swinford, and Harker Plutons, emplaced between c. 486 and 477 Ma, display mutually crosscutting relationships with the youngest of the Vanda dikes. These younger plutons range in composition between monzonite and granite. Some are characterised by K-feldspar megacrystic textures superficially similar to some of the oldest concordant plutons. (author). 57 refs.; 2 tabs.; 4 figs

  12. The tardi-Pan-African granitoids of South-Westerner Anti-Atlas (Morocco: Evolution from magnesian to ferroan type. Example of the Ifni inlier

    Directory of Open Access Journals (Sweden)

    El Aouli, E. H.

    2007-06-01

    Full Text Available The study of the neoproterozoic granitoids in the Ifni Inlier and those of the other inliers in south-westerner Anti-Atlas shows that this magmatism evolves from magnesian to ferroan type. In the Ifni inlier, these granitoids outcrop within the sedimentary and volcanogenic formations of the Ouarzazate Super- Group SGO (615 to 540 My. They belong to two distinct magmatic episodes (i an early one composed of magnesian granitoids with alkali-calcic and metaluminous to slightly aluminous character (quartz bearing diorite, granodiorite and monzogranite intrusive in the lower formations of the SGO, and (ii a late episode associated to the summit of the SGO volcanites, which includes granites and sub-volcanic syenogranites of iron-bearing type and alkali-calcic to alkaline affinity. These magmatisms resulting from the partial melting of mixed material mark the end of the last Panafrican episode and would be set up in a transition from orogenic to anorogenic settings which announce the Paleozoic cycle. They would be contemporary to posterior with the exhumation of the extensive metamorphic domes of the Western Anti-Atlas.El estudio de los granitoides neoproterozoicos de la “boutonnière” (complejo plutono-metamórfico profundo con geometría subcircular de Ifni y de los de otras “boutonnières” del dominio suroccidental del Anti-Atlas, demuestra que este magmatismo evoluciona desde un tipo magnésico hacia un tipo férrico. En la “boutonnière” de Ifni, estos granitoides afloran en el interior de formaciones sedimentarias y volcano-sedimentarias del Supergrupo de Ouarzazate SGO (615 a 540 Ma. Pertenecen a dos episodios magmáticos diferentes (i un episodio precoz compuesto de granitoides magnésicos, calcoalcalinos y metaluminosos a poco aluminosos (dioritas con cuarzo, granodioritas y monzogranitos que intruyen en las formaciones inferiores del SGO, (ii un episodio tardío asociado con un vulcanismo terminal a techo del

  13. PROFIL PROTEIN HIPOFISA SAPI PERAH PERANAKAN FRIES HOLLAND (PFH BETINA FASE FOLIKULER DAN LUTEA

    Directory of Open Access Journals (Sweden)

    Nurul Isnaini

    2012-04-01

    Full Text Available ABSTRAK   Penelitian dilakukan dengan tujuan untuk mengetahui profil protein hipofisa sapi perah PFH betina fase folikuler dan fase luteal dengan menggunakan metode SDS-PAGE. Hasil penelitian ini diharapkan dapat digunakan sebagai acuan untuk melaksanakan pengujian jenis protein tertentu yang terdapat dalam hipofisa sapi perah PFH.Materi yang digunakan dalam penelitian ini adalah hipofisa sapi perah PFH betina Fase Folikuler dan Fase Luteal. Sampel hipofisa didapatkan dari Rumah Potong Hewan (RPH Singosari Malang. Metode penelitian yang digunakan dalam penelitian ini adalah metode observasi. Dimana sampel hipofisa sapi perah PFH fase folikuler dan fase luteal dilakukan isolasi protein, dan ditentukan Berat Molekul (BM proteinnya. Data yang diperoleh dianalisis dengan menggunakan analisis diskriptif. Hasil penelitian menunjukkan bahwa profil protein hipofisa fase folikuler dan fase luteal sapi perah PFH memiliki perbedaan. Pada hipofisa fase folikuler memiliki 12 pita protein, yaitu 163; 112,3; 101,3; 85,8; 80,6; 71,2; 53,3; 45,2; 39,9; 32,4; 29,8; dan 24,8 kDa. Pada hipofisa fase luteal memiliki 12 pita protein, yaitu 163; 112,3; 101,3; 85,8; 71,2; 60,3; 53,3; 45,2; 39,9; 32,4; 29,8; dan 24,8 kDa. Pita protein yang membedakan adalah pita dengan berat molekul 80,6 kDa hanya terdapat pada hipofisa fase folikuler, dan pita dengan berat molekul 60,3 kDa hanya terdapat pada hipofisa fase luteal. Kesimpulan yang diperoleh dari penelitian ini adalah terdapat perbedaan profil protein yang dihasilkan pada hipofisa fase folikuler dengan hipofisa fase luteal. Saran yang diberikan adalah perlu dilakukan penelitian lanjutan yaitu uji immunoblothing atau westernblothing (WB untuk memastikan keberadaan  protein-protein tertentu.   Kata kunci: Hipofisa, folikuler, luteal, berat molekul protein. HIPOPHISIS PROTEIN PROFILE OF CROSSBREED FRIESH HOLLAND DAIRY CATTLE IN FOLLICULAR AND LUTEAL PHASE   ABSTRACT   The aim of this research was to identification of

  14. Termodinámica y diagramas de fase.

    Directory of Open Access Journals (Sweden)

    ANDRÉS FELIPE AGUDELO SANTAMARÍA

    2005-01-01

    Full Text Available Los diagramas de fase son la representación del equilibrio termodinámico de un sistema y permiten predecir las fases presentes y sus proporciones para unas condiciones determinadas. En este trabajo se plantea su fundamento termodinámico y se usa el modelo de solución ideal para obtener los diagramas de equilibrio líquido-sólido de algunos sistemas binarios, utilizando datos termodinámicos existentes en la literatura. Este modelo, aunque simple, permite una buena aproximación a algunos sistemas, y en general es una herramienta útil cuando se carece de datos experimentales. Aunque los diagramas de equilibrio son de gran utilidad en la práctica ingenieril, en la práctica pocos sistemas exhiben comportamiento ideal, ya que esto requiere mucha semejanza entre los componentes.

  15. Granitoids of the Dry Valleys area, southern Victoria Land : geochemistry and evolution along the early Paleozoic Antarctic Craton margin

    International Nuclear Information System (INIS)

    Allibone, A.H.; Cox, S.C.; Smillie, R.W.

    1993-01-01

    Field relationships and geochemistry indicate granitoid plutons of the Dry Valleys area comprise at least three petrogenetically distinct suites. The older Dry Valleys 1a (DV1a) suite, comprising the Bonney, Catspaw, Denton, Cavendish, and Wheeler Plutons and hornblende-biotite orthogneisses, and Dry Valleys 1b (DV1b) suite, comprising the Hedley, Valhalla, St Johns, Dun, Calkin, and Suess Plutons, biotite granitoid dikes and biotite orthogneisses, were emplaced before prominent swarms of Vanda mafic and felsic dikes. Both the DV1a and DV1b suites are time transgressive, with older intrusions in each suite being emplaced during the later stages of deformation of the Koettlitz Group. Younger granitoids that postdate the majority of the Vanda dikes include: the Dry Valleys 2 (DV2) suite, comprising the Pearse and Nibelungen Plutons plus several smaller, unnamed plugs; and the Harker, Swinford, Orestes, and Brownworth Plutons with identical field relationships and enclaves but distinct chemistries. Chemical characteristics and limited Rb-Sr isotopic dating indicate plutonism before c. 500 Ma was dominated by the Cordilleran I-type DV1a suite, inferred to have developed during melting above a west-dipping subduction zone along the Antarctic Craton margin. The chemical characteristics of the DV1b suite indicate large-scale melting of a quartzo-feldspathic protolith lacking residual plagioclase, but containing refractory garnet. Potential DV1b suite source rocks include metamorphosed immature sediments, possibly underplated along the subduction zone associated with DV1a magmatism, or older granitoid orthogneisses. Major DV1b plutonism at 490 Ma marks the end of subduction-related plutonism in southern Victoria Land. Younger DV2 alkali-calcic, Caledonian I-type plutonism is inferred to have formed in response to uplift and extension between 480 and 455 Ma. Lack of DV2 suite correlatives and Vanda mafic and felsic dikes in northern Victoria Land suggests significantly

  16. Permian alkali granitoids of the transbaikal region (new Rb-Sr dates)

    Energy Technology Data Exchange (ETDEWEB)

    Sukhanov, M K; Ryakhovskij, V M; Abramov, A V

    1984-01-01

    Rubidium-strontium isotopic investigations of granitoids from Khorinsk and Middle Oninsk massifs were conducted. Isochrones for two chief-modifications of rocks - subalkaline syenites and alkaline granites-were constructed. The age of syenites is determined to be (293 + 20) x 10/sup 6/ at (/sup 87/Sr//sup 86/Sr)/sub 0/=0.7044 +- 0.0106 that of alkaline granites - (253 +- 3) x 10/sup 6/ at (/sup 87/Sr//sup 86/Sr)/sub 0/=0.7077 +- 0.0033. Analytical data for determination of rubidium-strontium age of rocks of the mentioned massits are presented as well.

  17. Petrochemical and Tectonogenesis of Granitoids in the Wuyo-Gubrunde Horst, Northeastern Nigeria: Implication for Uranium Enrichment

    Energy Technology Data Exchange (ETDEWEB)

    Bolarinwa, Anthony Temidayo, E-mail: atbola@yahoo.com; Bute, Saleh Ibrahim [University of Ibadan, Department of Geology (Nigeria)

    2016-06-15

    The Wuyo-Gubrunde Horst in the northeastern Nigeria consists of migmatite gneiss, unaltered, altered, and sheared porphyritic granites, pegmatites, aplites, basalts, and sandstone. Uranium has been reported in rhyolite, sheared rocks, and sandstone within the area. The petrogenesis of the granitoids and associated rocks in the area was evaluated in the light of new geochemical data, which showed that the U content of altered porphyritic granite is highest and hydrothermal-related. The granitoids are metaluminous, sub-alkaline, and S-type granite, and have evolved by partial melting of crustal material emplaced at moderate depth of 20–30 km in a syn-to late-collisional within-plate tectonic setting. The negative Eu/Eu* anomaly and high (La/Yb){sub N} ratio of the granitoids indicate magma fractionation. The low SiO{sub 2} (<53%) and high Fe{sub 2}O{sub 3} (10%) of the altered porphyritic granite compared to other similar rock units suggest pervasive alteration. The associated basalts are tholeiitic, emplaced within continental plate tectonic setting, and enriched in Ni, V, Nb, Sr, and light rare earth elements, and they have SiO{sub 2}, Fe{sub 2}O{sub 3}, V, Th, and Co contents that are similar to those of the altered porphyritic granites. The U occurrence in the Wuyo-Gubrunde Horst is believed to be sourced from the adjoining Bima sandstone in the Benue Trough, which locally contains carbonaceous zones with anomalously high concentrations of U. The Fe{sup 2+}/Fe{sup 3+} redox fronts formed by alteration of the iron-rich basalts provided the requisite geochemical barrier for U-bearing hydrothermal fluid, causing enrichment of U leached and mobilized from the sandstone through fractures in the rocks.

  18. Surface and bulk modifications of 1.5 mole % Sr/La{sub 2}O{sub 3} catalyst with different Co, Ni, and Cu amounts

    Energy Technology Data Exchange (ETDEWEB)

    Gonzalez Cortes, Sergio; Fontal, Bernardo [Universidad de los Andes, Merida (Venezuela); Moronta, Delfin [Universidad Central de Venezuela, Caracas (Venezuela)

    2001-08-01

    The effects of Co, Ni and Cu oxide content on the surface and bulk of the 1.5 mole % Sr/La{sub 2}O{sub 3} catalysts were studied. Series of M/Sr-La catalysts (MCo, Ni, Cu) were prepared by successive immersion impregnation. The solids were characterized by X-ray diffraction (XRD), infrared spectroscopy (FTIR), temperature-programmed reduction (TPR), electron paramagnetic resonance (EPR), specific surface area measurements (BET) and thermogravimetric analysis (TGA). The Sr/La{sub 2}O{sub 3} modified with different Co, Ni, and Cu loading shows a strong metal oxide interaction with La{sub 2}O{sub 3}. This probably begin over anionic vacancies or structure defects favoring LaSrMO{sub x} solid solution formation with island-like structures according to a Volmer-Weber growth. It is proposed that the growth mode of La-Co, La-Ni and La-Cu stoichiometric phases occur from solid solutions. The formation of only a La-M single phase, probably non-stoichiometric, increases the material porosity while different phases favor the agglomeration or sintering of the particles. [Spanish] En este trabajo se estudia el efecto de la cantidad de cobalto, niquel y cobre sobre las estructuras superficial y masica del sistema 1.5% molar Sr/La{sub 2}O{sub 3}. Los catalizadores M/Sr-La (M = Co, Ni, Cu) fueron preparados por el metodo de impregnacion con exceso de solucion. Los solidos se caracterizaron por difraccion de rayos-X, espectroscopia infrarroja con transformada de Fourier, reduccion a temperatura programada, resonancia paramagnetica del electron, medidas del area superficial especifica por el metodo de BET y analisis termogravimetrico. El catalizador Sr/La{sub 2}O{sub 3} modificado con diferentes cantidades de Co, Ni y Cu muestra una interaccion fuerte con el oxido del metal de transicion, probablemente sobre las vacancias anionicas o defectos estructurales que favorecen la formacion de la solucion solida LaSrMox en forma de isla, segun el mecanismo de crecimiento de fase de Volmer

  19. A review of the ascent and emplacement of granitoid bodies into the crust

    Directory of Open Access Journals (Sweden)

    Katarína Bónová

    2005-03-01

    Full Text Available This paper relates to basic information (i.e. mechanical aspects of ascent, indicators faciliting the discriminability of various ascent styles about the models of ascent and emplacement of granitoid bodies, since the purely mechanical aspect of intrusion of magmas is a fascinating subject and it has generated a considerable controversy over many years. Individual models are demonstrated by world-known occurrences and examples from Western Carpathian’s region. The conditions of magma migration are demonstrated as well.

  20. Age, geochemical affinity and geodynamic setting of granitoids and felsic volcanics in the basement of Wrangel Island

    Science.gov (United States)

    Luchitskaya, Marina; Moiseev, Artem; Sokolov, Sergey; Tuchkova, Marianna; Sergeev, Sergey

    2016-04-01

    Granitoids and basic rocks of Wrangel Island are the components of Precambrian metamorphic basement, exposed in the anticlinorium in the central part of the island and named as Wrangel complex (Kameneva, 1970; Ageev, 1979; Til'man et al., 1964, 1970; Ganelin, 1989; Kos'ko et al., 1993, 2003). The latter is composed of volcanic, volcaniclastic and clastic rocks metamorphosed in greenshist to locally lower amphibolite facies (Kos'ko et al., 2003; Cecile et al., 1991). Obtained earlier datings of granitoids and basic rocks from Wrangel complex display a wide scatter: 609-700 Ma, U-Pb zircon (Cecile et al., 1991; Kos'ko et al., 1993); 590 Ma, Pb-Pb zircon; 574, 575 Ma, K-Ar whole rock; 475 Ma, Rb-Sr muscovite (Kos'ko et al., 2003). Our previous U-Pb SHRIMP datings indicate the episode of granitoid activity in 681-707 Ma (Luchitskaya et al., 2014). Here we present new results from zircon SIMS and LA-ICP-MS U-Pb dating and geochemical data for granites and felsic volcanics of Wrangel complex. Granites of Wrangel complex in the area of Khishchnikov River form small tabular bodies less than 30 meters in thickness. They range from slightly recrystallized muscovite granites to gneissic and mylonitic ones. Felsic and basic volcanics are exposed in the central part of Wrangel Island (rivers Neizvestnaya and Krasnyy Flag). Their interrelations are unknown and earlier they were considered as single bymodal assemblage of C1 sequence (Kos'ko et. al., 1993, 2003). Samples were collected in the area of Pervaya Mountain, visible thickness of volcanics ~100 meters. Basalts are overlain by conglomerates with detrite zircons no younger than 550 Ma (Moiseev et al., 2009, 2015). Wheited mean ages of zircons from muscovite granites and mylonitic ones are 592.9±6.7 Ma (n=10) and 692.9±5.0 Ma (n=30); in two samples we suppose the age of crystallization ~700 Ma. Wheited mean ages of zircons from felsic volcanics are 594.4±7.1 Ma (n=10) and 598.6±7.5 Ma (n=10). Granites and felsic

  1. REFORMA TRIBUTARIA EN FASES

    Directory of Open Access Journals (Sweden)

    Ricardo Chávez

    2016-01-01

    Full Text Available En este artículo el principal objetivo es analizar tanto cualitativa como cuantitati- vamente el impacto del momento de una reforma tributaria, es decir, el aumento progresivo y avisado (en fases de los impuestos en contraposición con una reforma de una sola vez. Los resultados indican que una reforma en fase debiera producir dos efectos: un efecto sustitución que impulsa a las empresas a adelantar inversión y con ello debiera aumentar el Producto Interno Bruto ( PIB y la inflación. La reacción del banco central debiera ser subir la tasa de interés. El otro efecto es negativo y consiste en un efecto riqueza que reduce el precio de las acciones y aumenta el tipo de cambio, Tomando como ejemplo el caso de Chile, que realizó una reforma en base recientemente (2014: se tiene que un aumento de 1% de los impuestos debería producir, producto de la distorsión intertemporal, un aumento de 0.17% en el PIB dentro del primer año del anuncio. No obstante, pueden existir otros elementos de naturaleza muy heterogénea que pueden influenciar negativamente la implemen- tación de la reforma y, por tanto, cancelar por completo este efecto de sustitución intertemporal. Entre estos elementos negativos se tiene la falta de claridad de la re- forma por parte del gobierno, al grado de virulencia de las discusiones en el Congre- so y su influencia en las expectativas de los empresarios, la falta de credibilidad, por ejemplo, la incertidumbre de nuevas alzas de impuestos, etcétera.

  2. Rock strength measurements on Archaean basement granitoids recovered from scientific drilling in the active Koyna seismogenic zone, western India

    Science.gov (United States)

    Goswami, Deepjyoti; Akkiraju, Vyasulu V.; Misra, Surajit; Roy, Sukanta; Singh, Santosh K.; Sinha, Amalendu; Gupta, Harsh; Bansal, B. K.; Nayak, Shailesh

    2017-08-01

    Reservoir triggered earthquakes have been occurring in the Koyna area, western India for the past five decades. Triaxial tests carried out on 181 core samples of Archaean granitoids underlying the Deccan Traps provide valuable constraints on rock strength properties in the Koyna seismogenic zone for the first time. The data include measurements on granite gneiss, granite, migmatitic gneiss and mylonitised granite gneiss obtained from boreholes KBH-3, KBH-4A, KBH-5 and KBH-7 located in the western and eastern margins of the seismic zone. Salient results are as follows. (i) Increase of rock strength with increasing confining pressure allow determination of the linearized failure envelopes from which the cohesive strength and angle of internal friction are calculated. (ii) Variable differential stresses at different depths are the manifestations of deformation partitioning in close association of fault zone(s) or localized fracture zones. (iii) Fractures controlled by naturally developed weak planes such as cleavage and fabric directly affect the rock strength properties, but the majority of failure planes developed during triaxial tests is not consistent with the orientations of pre-existing weak planes. The failure planes may, therefore, represent other planes of weakness induced by ongoing seismic activity. (iv) Stress-strain curves confirm that axial deformation is controlled by the varying intensity of pre-existing shear in the granitoids, viz., mylonite, granite gneiss and migmatitic gneiss. (v) Frequent occurrences of low magnitude earthquakes may be attributed to low and variable rock strength of the granitoids, which, in turn, is modified by successive seismic events.

  3. ANSIEDAD–ESTADO A LO LARGO DE LAS FASES DE COMPETENCIA DEPORTIVA

    Directory of Open Access Journals (Sweden)

    Jaime Alberto Arenas Granada

    2014-11-01

    Full Text Available Con el objetivo de conocer el comportamiento de la ansiedad–estado en tres fases de competencia deportiva (clasificatoria, semifinal y final e identificar diferencias entre el género, delegaciones y experiencia deportiva, fue empleada la escala de ansiedad–estado del Inventario de Ansiedad Estado y Rasgo (IDARE/STAI, para lo cual se obtuvo un total de 173 datos (clasificatoria, n= 98; semifinal, n=43; final n= 32 en una muestra intencional de hombres y mujeres voleibolistas representantes de seis instituciones universitarias. Estudio empírico cuantitativo, de alcance longitudinal y análisis estadístico no paramétrico. Los resultados permitieron establecer la correlación positiva y significativa entre las fases de competencia y los niveles de ansiedad–estado, se observaron diferencias significativas en el género, en función al promedio general y la fase clasificatoria; con mayores puntajes de ansiedad–estado por parte de las mujeres. Los promedios de las fases no establecieron diferencias estadísticamente significativas, como tampoco se observó en las delegaciones, ni en la experiencia deportiva. Sin embargo, se destaca la importancia de la experiencia deportiva como variable a considerar en las demandas de la competencia deportiva. Los resultados son discutidos y direccionados a la instauración de programas de entrenamiento psicológico, así como el desarrollo de nuevos trabajos en esta línea.

  4. Plantas indicadoras de clomazone na fase vapor

    Directory of Open Access Journals (Sweden)

    Fábio Schreiber

    2013-10-01

    Full Text Available A volatilização representa um processo importante no deslocamento de agrotóxicos para o ambiente. As características físico-químicas da molécula do clomazone indicam que este possui potencial de volatilização. Em vista do exposto, para a realização deste estudo, foram conduzidos dois experimentos com o objetivo de avaliar a suscetibilidade das espécies: pepino, melão, milho, sorgo e arroz a diferentes formulações do herbicida clomazone na fase vapor. Para isso, foram utilizadas caixas de vidro hermeticamente fechadas, com a presença de diferentes formulações de clomazone e as espécies vegetais. As formulações utilizadas foram Gamit 360 CS®, Gamit 500 EC® e Gamit Star®. Com os resultados obtidos, foi possível concluir que, dentre as espécies avaliadas, independente da formulação utilizada, a de menor tolerância ao herbicida clomazone na fase vapor foi o sorgo, seguido do milho e do arroz.

  5. Una técnica para obtener la fase icosahédrica en peliculas delgadas multicapas de AICr

    Directory of Open Access Journals (Sweden)

    D. Chaverri

    2016-03-01

    Full Text Available Se describe el procedimiento empleado para producir películas delgadas de multicapas de AlCr con fase icosahédrica utilizando un sistema de alto vacío con cañón de electrones. Las muestras con fase icosahédrica experimentan reconocimiento in situ al condensar las capas sobre sustratos calientes (aproximadamente360°C. Para identificarla fase icosahédrica se utiliza microscopía electrónica de transmisión en el modo de difracción. Se comparan las muestras con fase con otras formadas simultáneamente sobre sustratos a aproximadamente 100°C.

  6. Geochronology, petrogenesis and metallogeny of Piaotang granitoids in the tungsten deposit region of South China

    International Nuclear Information System (INIS)

    He Zhenyu; Xu Xisheng; Wang Xudong; Yu Yao; Zou Haibo

    2010-01-01

    The tungsten deposit region of South China is well known as the world's leading tungsten (W) producer. The Piaotang tungsten deposit in the region is such a representative large-scale quartz vein type tungsten polymetallic deposit that is closely associated with granitoids. In the present study we present precise LA-ICP-MS zircon U-Pb dating and LA-MC-ICPMS zircon Hf isotopic data for the samples from exposed quartz diorite body and buried granite stock in the Piaotang tungsten deposit area. Zircon U-Pb dating results indicate that the quartz diorite body was formed in Early Paleozoic time at 439±2 Ma, whereas the granite body was emplaced in EarlyYanshanian time at 158±3 Ma. Both the quartz diorite and granite have negative ε Hf (t) values, with similar two-stage zircon Hf model ages ranging from 1.8 to 2.1 Ga. Through integration of our new data with the isotope data of Precambrian basement rocks in western Cathaysia, we suggest that the Paleoproterozoic Hf model ages (1.8-2.1 Ga) might be an average age which resulted from mixing of continental materials of different ages. Both the Piaotang Early Paleozoic quartz diorite and Early Yanshanian granite are produced by reworking of the heterogeneous Neoproterozoic crust. Our zircon ages, together with the geochemical data and geological features and ore-forming ages of this tungsten deposit, indicate that the buried Early Yanshanian granite, rather than the exposed quartz diorite, is genetically associated with tungsten mineralization. The distinct metallogeny difference between the Piaotang Early Paleozoic quartz diorite and Early Yanshanian granite can be ascribed to the different degrees of magma differentiation. The Early Yanshanian granite is highly differentiated rock and similar to the other W-Sn deposits generating granitoids in South China. The extents of magma differentiation depend on the tectonic setting and the mechanism of magma generation. On the basis of the relationship between two different

  7. Behaviour of {sup 238}U, {sup 234}U, {sup 228}Ra and {sup 226}Ra in rock alterations: study of Morungaba granitoids, SP-Brazil and ground water in its fractures; Comportamento de {sup 238}U, {sup 234}U, {sup 228}Ra e {sup 226}Ra na alteracao de rochas: estudo dos granitoides de Morungaba (SP) e aguas subterraneas de suas fraturas

    Energy Technology Data Exchange (ETDEWEB)

    Santos, Rosana N. dos [Pontificia Univ. Catolica de Sao Paulo, SP (Brazil). Dept. de Fisica]. E-mail: rosana@pucsp.br; Marques, Leila S. [Sao Paulo Univ., SP (Brazil). Inst. de Astronomia, Geofisica e Ciencias Atmosfericas. Dept. de Geofisica]. E-mail: leila@iag.usp.br

    2005-07-01

    This work presents the first results obtained on the investigation of the behavior of uranium and radium radioisotopes in the processes of weathering and rock-water interaction of Morungaba granitoids belonging to Meridional Pluton (Valinhos Town-SP-Brazil). Specific activities of {sup 238}U, {sup 234}U, {sup 228}Ra and {sup 226}Ra were determined in non altered granitoids (Group A), as well as in those affected by different degrees of weathering (Groups B, C and D). The uranium specific activities were determined by alpha spectrometry method, whereas for the determination of radium isotopes high resolution gamma-ray spectrometry technique was employed. The data indicate that {sup 238}U and {sup 234}U are in radioactive equilibrium in the fresh analyzed granitoids, but show a slight depletion of {sup 234}U in relation to {sup 238}U in the weathered rocks. The ({sup 226}Ra/{sup 238}U) and ({sup 226}Ra/{sup 234}U) activity ratios of all investigated rocks are similar, showing a significant {sup 226}Ra depletion, which is probably caused by its preferential leaching. These results indicate that even samples macroscopically classified as fresh rocks, their systems have been opened for some geochemical changes. The high ({sup 234}U/{sup 238}U) activity ratios of groundwaters which are found in the fractures of these granitoids suggest their prolonged residence times in the aquifer and/or their percolation by other rocks presenting different geochemical properties. (author)

  8. Al CERN prima fase sistema gestione dati LHC

    CERN Multimedia

    2003-01-01

    "Al via la prima fase per la realizzazione del sistema Lhc computing Grid (LCG), progettato per elaborare le quantita' di dati senza precedenti che, a partire dal 2007, saranno prodotte dagli esperimenti eseguiti con il nuovo grande acceleratore Large Hadron Collider (LHC), presso il Cern di Ginevra" 1 page

  9. Visualization of cranial nerves by MR cisternography using 3D FASE. Comparison with 2D FSE

    Energy Technology Data Exchange (ETDEWEB)

    Asakura, Hirofumi; Nakano, Satoru; Togami, Taro [Kagawa Medical School, Miki (Japan)] (and others)

    2001-03-01

    MR cisternography using 3D FASE was compared with that of 2D FSE in regard to visualization of normal cranial nerves. In a phantom study, contrast-to-noise ratio (C/N) of fine structures was better in 3D FASE images than in 2D FSE. In clinical cases, visualization of trigeminal nerve, abducent nerve, and facial/vestibulo-cochlear nerve were evaluated. Each cranial nerve was visualized better in 3D FASE images than in 2D FSE, with a significant difference (p<0.05). (author)

  10. Visualization of cranial nerves by MR cisternography using 3D FASE. Comparison with 2D FSE

    International Nuclear Information System (INIS)

    Asakura, Hirofumi; Nakano, Satoru; Togami, Taro

    2001-01-01

    MR cisternography using 3D FASE was compared with that of 2D FSE in regard to visualization of normal cranial nerves. In a phantom study, contrast-to-noise ratio (C/N) of fine structures was better in 3D FASE images than in 2D FSE. In clinical cases, visualization of trigeminal nerve, abducent nerve, and facial/vestibulo-cochlear nerve were evaluated. Each cranial nerve was visualized better in 3D FASE images than in 2D FSE, with a significant difference (p<0.05). (author)

  11. Impacto de "El Niño 1997-98" sobre el asentamiento larval de algunos invertebrados marinos bentónicos de bahía Independencia, Pisco -Perú

    Directory of Open Access Journals (Sweden)

    Elmer Ramos

    2014-06-01

    Full Text Available Se evaluó mensualmente los cambios y la magnitud del impacto de "El Niño" (EN, sobre el mecanismo del asentamiento larval de algunos invertebrados marinos bentónicos, en sustratos artificiales filamentosos (fibra nylon, entre enero 1996 y julio 1998, en una estación fija, a 10m de profundidad, situada en el lado oriental de la Isla Independencia, en Bahía Independencia, Durante 1996, en la fase fría "La Niña" (LN, el número de especies presentó un pico en abril y la densidad en junio. En la fase cálida EN 199798, la densidad total y el número de especies, presentaron un primer pico en marzo de 1997, luego, un segundo pico, en febrero y julio de 1998, respectivamente. Un primer grupo de especies que intensificó su asentamiento durante la fase fría LN 1996, estuvo constituido por el bivalvo Hiatella solida, el turbelario Notoplana sp. y el gastrópodo Caecum chilense. El segundo grupo intensificó su asentamiento en la etapa temprana de la fase cálida EN 1997-98, Y lo formaron el braquiópodo Discinisca lamel/osa, el equinodermo Ophíactís kr6yerí y bivalvos de la Familia Mytllidae, Un tercer grupo, mostró una intensificación del asentamiento larval, en la etapa tardía de la fase cálida EN 1997-98, a inicios de 1998, y fue formado por el bivalvo Argopecten purpuratus y un gastrópodo turriforme. La aparición de larvas recién asentadas de especies tropicales, como el bivalvo Ptería stema y el gastrópodo Epitoníum sp., tuvo lugar en la etapa tardía de la fase cálida EN 1997-98.

  12. Geology and geochemistry of Massangana Granitoid Complex, Brazil, and its relation with tin mineralization

    International Nuclear Information System (INIS)

    Romanini, S.J.

    1982-01-01

    The geochemical and petroLogical characteristics of the Massangana Granitoid Complex, situated in the Rondonia Federal Territory, Brazil, aiming to discriminate the tin mineralized granitic rocks from the no mineralized ones. The collected samples consists of examples in tin mineralized and sterile phases. The elements traces were determined by x-ray fluorescence analysis, emission spectrography, molecular absorption spectrophotometry and atomic absorption spectrophotometry. The complex edifying evolved in four sucessive episodes called Massangana Phase, Bom Jardim Phase, Sao domingos Phase and Taboca Phase ordered stratigraphycally in this sequence. (author/M.C.K.) [pt

  13. Fases de cultivo: Establecimiento y crecimiento rapido

    Science.gov (United States)

    R. Kasten Dumroese; Douglass F. Jacobs; Kim M. Wilkinson

    2012-01-01

    En este capítulo y en el siguiente, se analizan en detalle las fases de crecimiento por las cuales pasa todo cultivo. Cabe recordar que para llegar a esta instancia se deben haber realizado varios pasos previos en forma adecuada, como el tratamiento de las semillas, la limpieza de contenedores y su llenado con medio de crecimiento de buena calidad. Estos temas se han...

  14. Petrogenesis of Jurassic granitoids at the northeastern margin of the North China Craton: New geochemical and geochronological constraints on subduction of the Paleo-Pacific Plate

    Science.gov (United States)

    Liu, Jin; Zhang, Jian; Liu, Zhenghong; Yin, Changqing; Zhao, Chen; Peng, Youbo

    2018-06-01

    At the junction between the North China Craton (NCC) and the Central Asian Orogenic Belt (CAOB), northern Liaoning province, NE China, there are widespread Jurassic igneous rocks. The tectonic setting and petrogenesis of these rocks are unresolved. Zircon U-Pb dating, whole-rock geochemistry, and Hf isotopic compositions of Jurassic granitoids were investigated to constrain their ages and petrogenesis in order to understand the tectonic evolution of the Paleo-Pacific Ocean along the northeastern margin of the NCC. Geochronological data indicate that magmatism occurred between the early and late Jurassic (180-156 Ma). Despite the wide range in ages of the intrusions, Jurassic granitoids were likely derived from a similar or common source, as inferred from their geochemical and Hf isotopic characteristics. Compared to the island arc andesite-dacite-rhyolite series, the Jurassic granitoids are characterized by higher SiO2, Al2O3, and Sr contents, and lower MgO, FeOT, Y, and Yb contents, indicating that the primary magmas show typical characteristics of adakitic magmas derived from partial melting of thickened lower crust. These findings, combined with their εHf(t) values (+1.4 to +5.4) and two-stage model ages (1515-1165 Ma), indicate the primary magmas originated from partial melting of juvenile crustal material accreted during the Mesoproterozoic. They are enriched in large-ion lithophile elements (e.g., Rb, K, Th, Ba, and U) and light rare-earth elements (REE), and depleted in high-field-strength elements (e.g., Nb, Ta, Ti, and P) and heavy REE. Based on these findings and previous studies, we suggest that the Jurassic adakitic granitoids (180-156 Ma) were formed in an active continental margin and compressive tectonic setting, related to subduction of the Paleo-Pacific Plate.

  15. Field, geochemistry and Sr-Nd isotopes of the Pan-African granitoids from the Tifnoute Valley (Sirwa, Anti-Atlas, Morocco): a post-collisional event in a metacratonic setting

    Science.gov (United States)

    Toummite, A.; Liegeois, J. P.; Gasquet, D.; Bruguier, O.; Beraaouz, E. H.; Ikenne, M.

    2013-10-01

    In the Tifnoute Valley, three plutonic units have been defined: the Askaoun intrusion, the Imourkhssen intrusion and the Ougougane group of small intrusions. They are made of quartz diorite, granodiorite and granite and all contain abundant mafic microgranular enclaves (MME). The Askaoun granodiorite and the Imourkhssen granite have been dated by LA-ICP-MS on zircon at 558 ± 2 Ma and 561 ± 3 Ma, respectively. These granitic intrusions are subcontemporaneous to the widespread volcanic and volcano-detrital rocks from the Ouarzazate Group (580-545 Ma), marking the post-collisional transtensional period in the Anti-Atlas and which evolved towards alkaline and tholeiitic lavas in minor volume at the beginning of the Cambrian anorogenic intraplate extensional period. Geochemically, the Tifnoute Valley granitoids belong to an alkali-calcic series (high-K calc-alkaline) with typical Nb-Ta negative anomalies and no alkaline affinities. Granitoids and enclaves display positive ɛNd-560Ma (+0.8 to +3.5) with young Nd-TDM between 800 and 1200 Ma and relatively low 87Sr/86Sr initial ratios (Sri: 0.7034 and 0.7065). These values indicate a mainly juvenile source corresponding to a Pan-African metasomatized lithospheric mantle partly mixed with an old crustal component from the underlying West African Craton (WAC). Preservation in the Anti-Atlas of pre-Pan-African lithologies (c. 2.03 Ga basement, c. 800 Ma passive margin greenschist-facies sediments, allochthonous 750-700 Ma ophiolitic sequences) indicates that the Anti-Atlas lithosphere has not been thickened and was never an active margin during the Neoproterozoic. After a transpressive period, the late Ediacaran period (580-545 Ma) is marked by movement on near vertical transtensional faults, synchronous with the emplacement of the huge Ouarzazate Group and the Tifnoute Valley granitoids. We propose here a geodynamical model where the Tifnoute Valley granitoids as well as the Ouarzazate Group were generated during the post

  16. Old inherited zircons in two synkinematic variscan granitoids: the 'granite du Pinet' and the 'Orthogneiss de Marvejols' (Southern French Massif Central)

    International Nuclear Information System (INIS)

    Pin, C.

    1981-01-01

    Two granitic bodies outcropping in the metamorphic basement of the Southern French Massif Central have been studied with the zircon U-Pb method: the Pinet granite (Rouergue area) and the Marvejols orthogneisses (Serie du Lot). It is shown that neither of them are pre-Variscan intrusions but that they were emplaced synkinematically, during the early stages of the Hercynian tectonometamorphic event. As numerous other S-type granitoids, both formations are characterized by an important inherited zircon component, whose apparent age is 1800 +- 200 m.y. Lower intersections with the Concordia curve allow to settle an emplacement age around 350-360 m.y., although the Pinet zircons display a complex pattern, owing both to heterogeneity of the inherited component and to late isotopic disturbances. Regional consequences of the synkinematic character of these S-type granitoids are outlined. It is shown that inherited zircons occurences often hinder accurate dating and the possible petrogenetic significance of the old proterozoic component is discussed. (orig.)

  17. TransiÃÃes de fase induzidas por altas pressÃes no molibdato de Ãtrio.

    OpenAIRE

    AbraÃo Cefas Torres Dias

    2011-01-01

    Neste trabalho investigamos as propriedades vibracionais do molibidato de Ãtrio hidratado e anidro em funÃÃo da pressÃo hidrostÃtica. A anÃlise dos modos vibracionais mostra que esse material experimenta uma transiÃÃo de fase da estrutura ortorrÃmbica para uma fase de mais baixa simetria para valores de pressÃo em torno de 0,3 GPa, provavelmente monoclÃnica, antes de se transformar em uma estrutura com alto grau de desordem a partir de 2,4 GPa. A transiÃÃo estrutural da fase ordenada para a f...

  18. Studies of the Solid and Liquid Phases of HF, HCl and HBr by Slow-Neutron Inelastic Scattering; Etude des Phases Solide et Liquide de HF, HCl Et HBr par la Diffusion Inelastique des Neutrons Lents; 0418 0417 0423 0427 0415 041d 0418 0415 0422 0412 0415 0420 0414 042b 0425 0418 0416 0418 0414 041a 0418 0425 0424 0410 0417 HF, HCl I HBr 0421 041f 041e 041c 041e 0429 042c 042e 041d 0415 0423 041f 0420 0423 0413 041e 0413 041e 0420 0410 0421 0421 0415 042f 041d 0418 042f 041c 0415 0414 041b 0415 041d 041d 042b 0425 041d 0415 0419 0422 0420 041e 041d 041e 0412 ; Estudio de las Fases Solida y Liquida del HF, HCl Y HBr por Dispersion Inelastica de Neutrones Lentos

    Energy Technology Data Exchange (ETDEWEB)

    Boutin, H. [Picatinny Arsenal, Dover, NJ (United States); Brookhaven National Laboratory, Upton, NY (United States); Safford, G. J. [Brookhaven National Laboratory, Upton, NY (United States)

    1965-06-15

    l'hydrogene facilite dans une grande mesure l'explication des spectres correspondant aux phases solides de HCl et de HBr. Cependant, ces donnees ne concordent pas avec les theories qui rendent compte des phases solides de ces composes uniquement en fonction d'arrangements dipolaires simples ou d'interactions a grande distance faisant intervenir le moment dipolaire d'un seul element de reseau en interaction avec un champ electrique moyen. (author) [Spanish] Los autores han estudiado las fases liquida y solida del HF, HCI y HBr, entre 30 y 1200 cm{sup 1}, recurriendo a la dispersion inelastica de neutrones frios (0,005 eV). Estas mediciones se realizaron a fin de examinar sistematicamente la influencia que ejerce el aumento del grado de electronegatividad y del tamano de los aniones sobre los movimientos moleculares de baja frecuencia, tanto en fase solida como liquida. Se estudio en primer lugar el HF por saberse -segun datos obtenidos en experimentos de difraccion realizados con rayos X- que en el estado solido forma largas cadenas enlazadas en zigzag por el hidrogeno. El espectro de los neutrones inelasticamente dispersos en las fases liquida y solida del HF pone de relieve el alto grado de asociacion que existe en el estado solido como consecuencia del enlace hidrogeno. Los autores han comparado, con fines de interpretacion, los datos correspondientes al HF con datos analogos sobre la dispersion en el caso de los iones HF{sub 2}{sup -} y H{sub 2}F{sub 3}{sup -}, que presentan estructuras semejantes a las de las unidades que comprenden, en el HF, las cadenas enlazadas en zigzag por el hidrogeno. Tambien compararon esos datos con los resultados de las mediciones Raman y del espectro infrarrojo en los iones HFJ. Estas comparaciones permitieron distinguir entre las caracteristicas de frecuencia de una sola unidad, y de las caracteristicas de la cadena entera y de los modos reticulares de baja frecuencia. La raya observada a 0, 067 eV ha podido asociarse a la

  19. Geochronology of granitoids and gnaisses from the Rio Maria, Mata Geral farm and Itacaiunas river regions, southern Para, Brazil

    International Nuclear Information System (INIS)

    Montalvao, R.M.G. de; Tassinari, C.C.G.; Bezerra, P.E.L.; Prado, P.

    1984-01-01

    Granitoids and gneisses occurring at Rio Maria, Mata Geral farm and Itacaiunas river regions, southern Para, underwent radiometric age determinations by Rb/Sr method using conventional isochrons. Results obtained from the Rio Maria and Mata Geral farm regions allowed te establishment of a reference 2,600 my Rb/Sr isochron with an initial Sr 87 /Sr 86 ratio of 0.7009. This result resembles the one obtained for granitoids and gneisses hosting rocks of the Serra do Inaja greenstone belt, located some what south of this area, which yielded, in Rb/Sr isochron, a radiometric age of 2,696 + - 79 my with an initial Sr 87 /Sr 86 ratio of 0.701. Results obtained from the Itacaiunas river region allowed for the establishment of a Rb/Sr referential isochron of 2,480 + - 40 my wth an initial Sr 87 /.Sr 86 ratio of 0.7072. Due to low initial ratios, it is suggested that the rocks from the Rio Maria, Mata Geral farm and Serra do Inaja regions formed from Mafic crust or superior mantle reworking, while those from the Itacaiunas river region, due to a high initial ratio, result from reworking at high crustal levels. (Author) [pt

  20. The geochemistry and geochronology of some proterozoic granitoid rocks from the Natal structural and metamorphic province, Southeastern Africa

    International Nuclear Information System (INIS)

    Kerr, A.; Milne, G.C.; Eglington, B.M.

    1987-01-01

    The Natal Structural and Metamorphic Province is thought to be an eastern extension of the Namaqua Metamorphic Province. Until recently few geochemical and isotopic data have been available on many of the rocks of this mobile belt. This paper presentes initial geochemical and geochronological information on the granitoids and associated rocks from three areas NSMP. Together, these areas provide a traverse through central and southern parts of the Mapumulo Group. Supracrustal gneisses, of uncertain age, are the oldest rocks in all areas, while the granitic intrusives range from 1,200-850 Ma, with a tendency for younger dates towards dates towards the south. Low initial 87 Sr/ 86 Sr ratios for these plutonic units suggest that the rocks were the products of partial melting of a relatively juvenile (circa 1,400 Ma) protolith. A type granites are common within the NSMP and give a range of ages, indicating that conditions suitable for their formation persited in this part of the African continent for an extended period of time. Economic deposits are lacking in eastern (Natal) sector of the mobile belt. Reconnaissance studies, however indicate that syn-tolate-Kinematic granitoids, intruded circa 1,000 Ma, are enriched in uranium and thorium irrespective of bulk chemistry, textural nature,mineralogy,structural setting, and isotopic characteristics. (author) [pt

  1. INFLUENCIA DE LAS FASES LUNARES SOBRE EL RENDIMIENTO DEL MAÍZ (Zea mays variedad NB6

    Directory of Open Access Journals (Sweden)

    Larry Flores Martínez

    2012-10-01

    Full Text Available La observación de las fases lunares para realizar actividades agrícolas, es una costumbre de muchas culturas alrededor del mundo. Sin embargo, existen pocos estudios científicos relacionados con este tema. El objeto  de esta investigación fue determinar la influencia de las fases lunares sobre el rendimiento del maíz. Para ello se consultó a 45 productores de 19 comunidades de la Región Autónoma Atlántico Sur (RAAS, sobre el uso de las fases lunares para la siembra. Además, se estableció un experimento utilizando un diseño de bloques completamente al azar con cuatro repeticiones por cada fase lunar (16 parcelas en total. Se midió el porcentaje de germinación, el crecimiento y rendimiento del cultivo.  Los datos fueron analizados utilizando el programa InfoStat versión 2010. Los resultados reflejan que la germinación de las semillas presentó diferencias estadísticas significativas, siendo mayores en parcelas sembradas en las fases de cuarto creciente y luna nueva. La variable altura, largo y peso de mazorca, no presentaron diferencias significativas según fase lunar. En la variable diámetro del tallo se encontró diferencia significativa; las plantas sembradas en luna nueva presentaron el mayor diámetro. El daño causado por enfermedades y herbívoros presentó un resultado variable para las cuatro fases lunares. El peso promedio del maíz sembrado en la fase de luna nueva fue mayor que en las otras fases, contrario a la creencia popular de los productores de la región.SUMMARYObservation of the moon phases for agricultural activities is a custom in many cultures around the world. However, there are few scientific studies related to this topic. The purpose of this research was to determine the influence of moon phases on corn yields. In order to achieve this goal, 45 producers were consulted from 19 communities in the South Atlantic Autonomous Region (RAAS, regarding the use of the moon phases for sowing. Besides, an

  2. The possibility of use of Kremicj granitoid (Serbia) as an architectural stone

    International Nuclear Information System (INIS)

    Kureshevicj, Lidja

    2010-01-01

    The stone from the granitoid pluton of Kremić in southern Serbia has been examined in order to evaluate the possibility of its use as an architectural stone. Both field observations and laboratory testing of specimens have been performed. Although the specimens were collected from the field surface level, their physicomechanical lab test results have shown that the rock mass itself fulfils all the requirements for use as an architectural stone set by the State through Serbian standards. Also, the stone quality is higher in deeper ground levels, where the weathering agents have less intense effects. This stone does not have high ornamental properties, but it has a finegrained texture and low mica content which has a positive effect on its technical characteristics and susceptibility to processing. (Author)

  3. Metasedimentary, granitoid, and gabbroic rocks from central Stewart Island, New Zealand

    International Nuclear Information System (INIS)

    Allibone, A.H.; Tulloch, A.J.

    1997-01-01

    A NNE-NE trending strip, 3-8 km wide, extending from the Freshwater valley across Mt Rakeahua Table Hill, and Mt Allen to the northern end or the Tin Range was mapped at a scale of 1:12,500 to locate and investigate the boundary between the Median Tectonic Zone (MTZ) and Western Province on Stewart Island. A NNE-trending fault, herein termed the Escarpment Fault, separates predominantly ductily deformed rocks on its south side from essentially undeformed rocks to the north. North of the Escarpment Fault, a small (2-3 km 2 ) pluton of alkali-feldspar granite (Freds Camp) intruded gabbroic rocks tentatively considered to be associated with gabbro/anorthosite/diorite of the Rakeahua pluton, centred on Mt Rakeahua. Both units were subsequently intruded by I-type biotite granite of the South West Arm pluton. South of the Escarpment Fault the oldest intrusions are biotite tonalite-granite orthogneisses (Ridge and Table Hill plutons) intercalated with the sillimanite-cordierite-bearing Pegasus Group metasedimentary rocks, considered to represent the Western Province. They contain titanite, allanite, and magmatic epidote-bearing assemblages, implying affinities with I-type granitoids. These older granitoids have been affected by at least three phases of ductile deformation. Immediately south of the Escarpment Fault, the Escarpment pluton (hornblende, biotite, quartz, monzonite-quartz monzodiorite) only exhibit effects of the third phase of deformation. Minor gabbroic intrusives concordant with the S 3 fabric intrude the Pegasus Group and intercalated orthogneisses. Plutons of two-mica, garnet ±cordierite granite (Blaikies and Knob) and younger biotite-titanite-magmatic epidote granite (Campsite) cut fabrics associated with the third phase of ductile deformation. Preliminary U-Pb dating indicate Devonian-Carboniferous, Jurassic, and Early Cretaceous emplacement ages for Ridge Orthogneiss, Freds Camp pluton, South West Arm pluton, and Blaikies pluton, respectively. South

  4. Mecanismos de deformación plástica en policristales cerámicos con fases secundarias vítreas

    Directory of Open Access Journals (Sweden)

    Meléndez Martínez, J. J.

    2005-10-01

    Full Text Available In many polycrystalline ceramic materials, the main phase coexists with a secondary phase, generally glassy in nature. The existence of this phase is associated to the use of certain sintering additives. In a general sense, the secondary phase is located at “pockets” between various grains, or it is distributed as a thin film at the grain boundaries. From the viewpoint of the creep behaviour at high temperatures, the secondary glassy phase plays a triple role: firstly, the secondary phase may flow under the applied stress. Secondly, the grain boundaries occupied by the secondary phase constitute high-diffusivity trajectories, even at temperatures lower than those required for bulk diffusion. Finally, the regions with secondary phase are preferential locations for the nucleation of cavities. In this work, the deformation mechanisms characteristic of ceramic polycrystals with secondary glassy phases (viscous flow, solution-precipitation and cavitation creep, which are related to the triple role played by these phases. Particularly, the most significant models for each mechanism are presented, as well as a comparative with experimental results obtained in different materials.

    En un gran número de materiales cerámicos policristalinos, la fase mayoritaria coexiste con una fase secundaria, generalmente de naturaleza vítrea. La existencia de esta fase se debe al uso de determinados aditivos durante la sinterización. En general, la fase secundaria se acumula en “bolsas” entre varios granos, o bien se distribuye en forma de película delgada en las fronteras de grano. Desde el punto de vista de la fluencia a alta temperatura, la fase secundaria desempeña un triple papel: en primer lugar, esta fase puede fluir bajo la acción de la tensión aplicada. Por otra parte, las fronteras de grano ocupadas por la fase secundaria constituyen trayectorias de alta difusividad, incluso a temperaturas menores que las requeridas para la difusión por

  5. Procedimiento para la obtención de micro- o nanopartículas sólidas

    OpenAIRE

    Ventosa Rull, Nora; Veciana Miró, Jaume; Cano-Sarabia, Mary; Sala Vergés, Santiago

    2008-01-01

    Procedimiento para la obtencion de micro- o nanoparticulas solidas. La invencion proporciona un nuevo procedimiento para la obtencion de micro- o nanoparticulas solidas con estructura homogenea. Se proporciona un procedimiento que permite obtener micro- o nanoparticulas solidas de estructura homogenea, con un tamano de particula inferior a 10 ƒÊm donde el compuesto solido procesado revela la naturaleza, cristalina, amorfa, polimorfica, etc..., propia del compuesto d...

  6. Obtención de silicatos de calcio empleando como precursores residuos sólidos. Influencia del mezclado de reactivos en fase seca o fase húmeda

    Directory of Open Access Journals (Sweden)

    Corpas Iglesias, F. A.

    2011-02-01

    Full Text Available The suitability of re-using residues marble, remaining from cutting marble, as a source of calcium-oxide, as well as the resultant ashes from the combustion of the wastes generated in the process of manufacturing boards from derivates of wood, as a source of silica, as raw material for the production of calcium silicate products has been determined. First of all, the influence of water has been studied in the initial phase of mixing residues. Marble and ashes have been mixed in molar relation CaO:SiO2 of 1:1 using two different ways: using a planetary ball mill (while in solid state or agitating at 90 ºC (2 h using a 60 wt% of water (while in humid state. Later, both mixtures were sintered at 1100 ºC (24 h. In order to use the obtained calcium-silicates as ceramic insulating thermal materials, the samples were compressed at 15 Tm obtaining bricks from which the technological properties have been studied. The ceramic materials obtained from mixing the residues in dry phase, as well as those obtained in the wet phase, can be used as thermal insulators, showing values of conductivity of 0.18 and 0.12 w/m2K, with an elevated resistance to compressive strength.

    Se ha determinado la posibilidad de reutilizar los residuos procedentes del corte de mármol, como fuente de óxido de calcio, y las cenizas resultantes de la combustión de los residuos generados en el proceso de fabricación de tableros de derivados de madera, como fuente de sílice. A partir de ambas materias primas, se obtienen silicatos de calcio. Se ha estudiado la influencia de agua en la fase inicial de mezclado de los residuos. Para ello mármol y cenizas se han mezclado en relación molar CaO:SiO2 1:1, en una primera ruta, en fase seca, empleando un molino de bolas, o en una segunda ruta, en fase húmeda, mediante agitación a 90 ºC (2 h empleando un 60 % en peso de agua. Posteriormente, ambas mezclas se sinterizan a 1100 ºC (24 h. Con

  7. Multimodal evoked potentials and the ovarian cycle in young ovulating women Potenciais evocados nas diferentes fases do ciclo menstrual da mulher

    Directory of Open Access Journals (Sweden)

    LUIZ ANTONIO DE LIMA RESENDE

    2000-06-01

    Full Text Available There is controversy over how hormonal conditions influence cerebral physiology. We studied pattern-shift visual evoked potentials (PS-VEP, brain stem auditory evoked potentials (BAEP and short-latency somatosensory evoked potentials (SSEV in 20 female volunteers at different phases of the menstrual cycle (estrogen phase, ovulatory day and progesterone phase. Statistical analysis showed decreased latencies for P100 (PS-VEP, N19 and P22 (SSEV waves in the progesterone phase compared with the estrogen phase. There was no significant difference between the estrogen and the ovulation day values. Comparing the three above stages, there were no significant differences in the brainstem auditory evoked potentials. The reduction of the latencies of the potentials generated in multisynaptic circuits provides the first consistent neurophysiological basis for a tentative comprehension of human pre-menstrual syndrome.Há controvérsias sobre como variações hormonais do ciclo menstrual da mulher influenciam a neurofisiologia cerebral. Estudamos potenciais evocados de curta latência, visuais, auditivos e sômato-sensoriais, em 20 mulheres voluntárias normais, nas diferentes fases do ciclo menstrual (fase estrogênica, fase ovulatória, fase progestacional. Comparação entre fase estrogênica e ovulatória mostrou resultados similares. Ondas I, III, V dos potenciais evocados auditivos não apresentaram diferenças estatisticamente significativas entre as três fases do ciclo. Análise estatística dos resultados mostrou diminuição significativa das latências das ondas P100, N19 e P22 obtidas na fase progestacional, comparadas com aquelas obtidas na fase estrogênica. Como estas ondas são geradas em circuitos multissinápticos, tal redução de latências, na fase progestacional, fornece a primeira base neurofisiológica consistente para tentativa de compreensão da síndrome pré-menstrual da mulher.

  8. Evolution of Brasiliano-age granitoid types in a shear-zone environment, Umarizal-Caraubas region, Rio Grande do Norte, northeast Brazil

    Science.gov (United States)

    Galindo, A. C.; Dall'Agnol, R.; McReath, I.; Lafon, J. M.; Teixeira, N.

    1995-01-01

    A sequence of Brasiliano-age granitoid types is exposed in a small area near the cities of Umarizal and Caraúbas in Rio Grande do Norte State, Northeast Brazil. Porphyritic K-alkali-calcic monzogranite is an important facies of the oldest Caraúbas intrusion (RbSr whole rock isochron age of ca. 630 Ma), which suffered solid-state deformation due to movements on a major NE-trending shear zone. The intrusion of the Prado and part of the Quixaba bodies was probably controlled by the shear zone. These two bodies include mafic/intermediate rocks, some of which contain two pyroxenes, and have hybrid, partly alkaline and partly shoshonitic geochemical characteristics. Rock types and ages are similar to those of some Pan-African occurrences in southwestern Nigeria. The Tourão body, intruded at ca. 590 Ma, presents preferred mineral orientations which are probably largely magmatic, since little evidence is found for widespread solid-state deformation. On the other hand, its intrusion may have been facilitated by the presence of the shear-zone faults. The rocks form a monomodal felsic K-alkali-calcic suite. With the exception of the Quixaba body, all these earlier granitoids are magmatic epidote- and magnetite-bearing porphyritic monzogranites with trace element geochemical characteristics of modern syn-collisional granites. The latest intrusion at ca. 545 Ma is mainly represented by potassic quartz syenites and related rocks, some of which contain fayalite or ferrohypersthene. These rocks possess neither well developed mineral orientations of magmatic origin nor signs of solid-state deformation. They are mineralogically similar to, but younger than some of the "bauchites" of central Nigeria. Geochemical signatures are comparable with those of modern within-plate granites. All granitoids present high ( 87Sr/ 86Sr)i ratios which range from 0.708 to 0.712, and increase with decreasing age. Such ratios are compatible with important or dominant crustal contributions. On the

  9. The differentiation process of the I-type granitoids in southwest Japan and New South Wares in Australia

    Science.gov (United States)

    Kawakatsu, K.; Iwamoto, Y.; Ebisu, S.; Hasegawa, M.; Hiraiwa, N.; Kawakatsu, T.; Kitano, A.; Masuta, T.; Ootsubo, H.; Wakazono, R.

    2013-12-01

    Cretaceous-Paleogene Granitoids in the inner zone of southwest Japan have been divided into two series: the magnetite series that is distributed mainly in the San-in belt and the ilmenite series that is distributed mainly in San-yo belt. For 8 years, we have been investigating the two series to clear their processes of magmatic differentiation. Recently, we discovered oscillatory zoned structure, exsolution lamellae of amphibole, and relics of pyroxene left in the core of amphibole from Harima granodiorite, Nunobiki granodiorite (San-yo belt) and Daito-Yokota quartz diorite (San-in belt). The amphibole that has microstructure coexists with magnetite, ilmenite and pyrrhotite. We compared the two series for crystallization and re-equilibrium by ion substitution using the microstructure of the amphibole as 'time measure' during the differentitation process of acidic magma. While magnetites and ilmenites coexist with the core of the amphiboles, the oxygen fugacity of the San-yo belt magma was low until the later stage of magmatic differentiation where H2S from the Earth's crust mixed with it. In the subsolidus process, hydrothermal solutions circulated. On the other hand, the oxygen fugacity of the San-in belt magma began to rise in the early stage of magmatic differentiation. In the later stage, mafic magma was contaminated with SO2. The rims of amphiboles coexist with pyrrhotites in both of belts. Furthermore, the re-equilibrium of minerals underwent progressive oxidation and hydrothermal fluid circulated actively in the subsolidus process. Bingie Bingie Point at New South Wares (Eurobodalla National Park) is a peninsula about a meter around. The plutonic rocks were formed in the Devonian period and belong to the magnetite series. They are classified I-type granitoids such as those found in the inner zone of southwest Japan. They have only trace amounts of oxide minerals and pyrrhotite. The amphiboles of the granitoids have oscillatory zoned structures at pale green

  10. Measurement of CSF volume with 3D-FASE MRI

    International Nuclear Information System (INIS)

    Kanayama, Shoichi; Calderon, A.; Makita, Jun-ichi; Ohara, Yukou; Tsunoda, Akira; Sato, Kiyoshi.

    1997-01-01

    A noninvasive and fast cerebrospinal fluid (CSF) volume measurement method has been developed using 3D-FASE MRI and a semi-automatic segmentation process. Images with a high CSF/(gray and white matter) ratio (about 10-20) were obtained with a heavily T 2 weighted 3D-FASE sequence. The CSF region was segmented with a region growing method and the volume was calculated from the number of segmented voxels with a signal intensity weighted summation. Total measurement time was about 30 minutes for each study. The errors of the measured volumes were within 10% for the phantom experiments. Intracranial CSF volumes of normal volunteers ranged between about 100 and 200 cc and the ventricle/intracranial CSF ratio was about 10%. 3D display of the segmented intracranial and ventricle CSF regions was also carried out and proved to be useful to understand the anatomy. Increased intracranial and/or ventricle CSF volumes were obtained for a hydrocephalic patient and one patient with probable cerebral atrophy. The results suggest that the developed method could be used for the diagnosis of patients with neurological diseases. (author)

  11. Some Possibilities of Radiation Polymerization from the Gaseous Phase on Solid Bases; Possibilites de polymerisation radiochimique en phase gazeuse sur des lits de matiere solide; O nekotorykh vozmozhnostyakh radiatsionnoj polimerizatsii iz gazovoj fazy na tverdykh podlozhkakh; Perspectivas de la radiopolimerizacion en fase gaseosa sobre lechos de sustancias solidas

    Energy Technology Data Exchange (ETDEWEB)

    Tsetlin, B. L.

    1963-11-15

    composants; la fibre servant de lit et la fibre ''greffee'' peuvent, dans des conditions appropriees, presenter chacune son propre ensemble de proprietes mecaniques. (author) [Spanish] de vapores del monomero respectivo se caracteriza por los siguientes aspectos: los centros activos que inician la polimerizacion solo se forman en la superficie del lecho, obstaculizando el transporte de la cadena cinetica al monomero y las nuevas cadenas polimericas se desarrollan por influencia unilateral de las fuerzas moleculares en la superficie solida. Estas particularidades del proceso en fase gaseosa mejoran las perspectivas que ofrece el metodo de polimerizacion injertada. Asi, es factible extender la aplicacion del mismo a lechos inorganicos y emplearlo para la sintesis de compuestos organo-minerales. Por otra parte, si se emplean como lechos fibras sinteticas estiradas, las macromoleculas orientadas de estas fibras dirigen el desarrollo de las nuevas cadenas polimericas de modo que el polimero injertado se obtiene directamente en estado orientado. Como consecuencia, se forman fibras combinadas de dos componentes; las fibras del lecho y las fibras ''injertadas'' pueden, en condiciones apropiadas, ofrecer la suma de las propiedades mecanicas propias de cada tipo. (author) [Russian] Svoeobrazie sinteza privitykh polimerov putem oblucheniya tverdykh ''podlozhek'' v prisutstvii parov polimeriehuyushchikhsya monomerov sostoit v tom, chto aktivnye tsentry, initsiiruyushchie polimerizatsiyu, generiruyutsya prakticheski tol'ko na podlozhke, peredacha kineticheskoj tsepi monomeru zatrudnena, i novye polimernye tsepi rastut v usloviyakh odnostoronnego vliyaniya molekulyarnykh sil tverdoj poverkhnosti. Ehti osobennosti gazofaznogo protsessa rasshiryayut vozmozhnosti metoda privitoj polimerizatsii. Metod mozhet byt' rasprostranen v ehtom sluchae i na neorganicheskie podlozhki i ispol'zovan dlya sinteza mineral'no-organicheskikh produktov. S drugoj storony, pri ispol'zovanii v kachestve podlozhek

  12. Geocronología y geoquímica isotópica (Sr, Nd) de los granitoides de Pola de Allande (Asturias): ¿Relictos de un arco magmático cadomiense en la Zona Asturoccidental Leonesa?

    OpenAIRE

    Gutiérrez Alonso, Gabriel; Fernández Suárez, Javier

    1998-01-01

    [ES] Los granitoides pre-Variscos de Pola de Allande se sitúan en el Antiforme del Narcea, en el límite entre las zonas Cantábrica y Asturoccidental Leonesa de la cadena Varisca Ibérica. Estos granitoides, formados por tonalitas y granodioritas con afinidades geoquímicas de arco magmático, intruyeron en sedimentos siliciclásticos Neoproterozoicos y fueron posteriormente afectados por la deformación tangencial Varisca. La datación U-Pb de circones de dos intrusiones por el método de Ablación L...

  13. Geochemistry of the Serifos calc-alkaline granodiorite pluton, Greece: constraining the crust and mantle contributions to I-type granitoids

    Science.gov (United States)

    Stouraiti, C.; Baziotis, I.; Asimow, P. D.; Downes, H.

    2017-11-01

    The Late Miocene (11.6-9.5 Ma) granitoid intrusion on the island of Serifos (Western Cyclades, Aegean Sea) is composed of syn- to post-tectonic granodiorite with quartz monzodiorite enclaves, cut by dacitic and aplitic dikes. The granitoid, a typical I-type metaluminous calcic amphibole-bearing calc-alkaline pluton, intruded the Cycladic Blueschists during thinning of the Aegean plate. Combining field, textural, geochemical and new Sr-Nd-O isotope data presented in this paper, we postulate that the Serifos intrusion is a single-zoned pluton. The central facies has initial 87Sr/86Sr = 0.70906 to 0.7106, ɛNd(t) = - 5.9 to - 7.5 and δ18Οqtz = + 10 to + 10.6‰, whereas the marginal zone (or border facies) has higher initial 87Sr/86Sr = 0.711 to 0.7112, lower ɛ Nd(t) = - 7.3 to - 8.3, and higher δ18Οqtz = + 10.6 to + 11.9‰. The small range in initial Sr and Nd isotopic values throughout the pluton is paired with a remarkable uniformity in trace element patterns, despite a large range in silica contents (58.8 to 72 wt% SiO2). Assimilation of a crustally derived partial melt into the mafic parental magma would progressively add incompatible trace elements and SiO2 to the evolving mafic starting liquid, but the opposite trend, of trace element depletion during magma evolution, is observed in the Serifos granodiorites. Thermodynamic modeling of whole-rock compositions during simple fractional crystallization (FC) or assimilation-fractional crystallization (AFC) processes of major rock-forming minerals—at a variety of pressure, oxidation state, and water activity conditions—fails to reproduce simultaneously the major element and trace element variations among the Serifos granitoids, implying a critical role for minor phases in controlling trace element fractionation. Both saturation of accessory phases such as allanite and titanite (at SiO2 ≥ 71 wt%)(to satisfy trace element constraints) and assimilation of partial melts from a metasedimentary component (to

  14. Geochemical studies, magmatic evolution, microstructures and replacement mechanisms in Jebale-Barez granitoid Complex (East and Southeast Jiroft

    Directory of Open Access Journals (Sweden)

    Jamal Rasouli

    2017-08-01

    Full Text Available Introduction The Jebale-Barez Plutonic Complex (JBPC is composed of many intrusive bodies and is located in the southeastern province of Kerman on the longitude of the 57◦ 45 ' east to 58◦ 00' and Northern latitudes 28◦ 30' to 29◦ 00'. The petrologic composition is composed of granodiorite, quartzdiorite, granite, alkali-granite, and trace amounts of tonalite with dominant granodiorite composition. Previously, the JBPC was separated into three plutonic phases by Ghorbani (2014. The first plutonic phase is the main body of the complex with composition of quartz-diorite to granodiorite. After differentiation of magma in the magmatic chamber, the porphyritic and not fully consolidated magmas have intruded into the main body. Their compositions were dominantly granodiorite and granite that are defined as the second plutonic phase. Finally, the last phase was started by an intrusion of the holo- leucogranite into the previous bodies. This plutonic activity was pursued by the minor Quaternary basaltic volcanism that shows metamorphic haloes in the contacts. They are dominantly porphyric leucogranites. However, some bodies show dendritic texture that may imply the existence of silicic fluids in the latest crystallization stages. Materials and methods In this article different analysis methods were used. For example, we used a total of two hundred samples of the various granitoids that were selected for common thin section study. Forty four representative samples from the different granitic rocks were selected for whole rock chemical analyses. The analyses of both major and trace elements were performed at the Department of Earth Sciences, the University of Perugia, Italy. The analysis for all major elements was carried out by an X-ray fluorescence spectrometry (XRF using a tube completed with a Rn and W anode under conditions with acceleration voltage of 40-45 kV and electric current ranging from I=30-35 mA. After calcination of powdered

  15. Geological evolution of the center-southern portion of the Guyana shield based on the geochemical, geochronological and isotopic studies of paleoproterozoic granitoids from southeastern Roraima, Brazil; Evolucao geologica da porcao centro-sul do escudo das Guianas com base no estudo geoquimico, geocronologico e isotopico dos granitoides paleoproterozoicos do sudeste de Roraima, Brasil

    Energy Technology Data Exchange (ETDEWEB)

    Almeida, Marcelo Esteves

    2006-07-01

    This study focuses the granitoids of center-southern portion of Guyana Shield, southeastern Roraima, Brazil. The region is characterized by two tectonic-stratigraphic domains, named as Central Guyana (GCD) and Uatuma-Anaua (UAD) and located probably in the limits of geochronological provinces (e.g. Ventuari-Tapajos or Tapajos-Parima, Central Amazonian and Maroni-Itacaiunas or Transamazon). The aim this doctoral thesis is to provide new petrological and lithostratigraphic constraints on the granitoid rocks and contribute to a better understanding of the origin and geo dynamic evolution of Guyana Shield. The GCD is only locally studied near to the UAD boundary, and new geological data and two single zircon Pb-evaporation ages in mylonitic biotite granodiorite (1.89 Ga) and foliated hastingsite-biotite granite (1.72 Ga) are presented. These ages of the protholiths contrast with the lithostratigraphic picture in the other areas of Cd (1.96-1.93 Ga). Regional mapping, petrography, geochemistry and zircon geochronology carried out in the Urad have showed widespread Paleoproterozoic calc-alkaline granitic magmatism. These granitoid rocks are distributed into several magmatic associations with different Paleoproterozoic (1.97-1.89 Ga) ages, structural and geochemical affinities. Detailed mapping, petrographic and geochronological studies have distinguished two main sub domains in the UAD. In the northern UAD, the high-K calc-alkaline Martins Pereira (1.97 Ga) and Serra Dourada S-type granites (1.96 Ga) are affected by NE-SW and E-W ductile dextral shear-zones, showing coexistence of magmatic and deformational fabrics related to heterogeneous deformation. Inliers of basement (2.03 Ga) crop out northeast of this area, and are formed by meta volcano-sedimentary sequence (Cauarane Group) and TTG-like calc-alkaline association (Anaua Complex). Xenoliths of meta diorites (Anaua Complex) and para gneisses (Cauarane Group) reinforce the intrusive character of Martins Pereira

  16. Operação Liberdade Duradoura: A Segunda Fase?

    Directory of Open Access Journals (Sweden)

    Cristina Soreanu Pecequilo

    2011-09-01

    Full Text Available O presente artigo tem como tema as recentes afirmações por parte dos EUA e seus aliados com relação à instauração da segunda fase da Operação Liberdade Duradoura e dos impactos que essa terá para a atual política de combate ao terrorismo e de para a ocupação do Afeganistão.

  17. Geochemistry Petrography, thermobarometry and investigation of magmatic series in Mirabad- Chehel Khane granitoid body (east of Bouin– Miandasht, Isfahan province

    Directory of Open Access Journals (Sweden)

    Seyed Mohsen Tabatabaei Manesh

    2017-11-01

    Full Text Available On the base of petrology, the Mirabad- Chehel Khane granitoid, east of Bouin-Miandasht, dominantly consists of syenogranite, monzogranite, alkali granite and granodiorites. The main minerals of these rocks are quartz, alkali feldspar (Orthoclase, plagioclase (Albite - Oligoclase, biotite, ± amphibole with minor amount of allanite, zircon, titanite, apatite, ± tourmaline.  The biotite from the granites are Fe-rich type (annite and primary magmatic in origin. The composition of the biotites studied principally falls in the calc-alkaline subduction related I-type granite on the tectonomagmatic discrimination diagrams, which stand on their major element oxides. Which is consistent with the nature of their host rocks. The studied amphiboles are classified as calcic (ferro-hornblende which points to the I-type nature of the granitoid.  The tourmaline composition plots on the schorl - foitite field. The temperature for the alteration, on the base of chlorite composition from the syenogranite, is estimated around 350°C and from the monzogranite rocks about 341°C.  Based on the application of Al-in amphibole, a 3 Kbar pressure was determined for the syenogranite unit corresponding to the depth of 8-11 Km for the emplacement of the pluton. Hornblende- plagioclase thermometer shows 694 to 700°C for the equilibrium of these two minerals.

  18. Método para Medir Indirectamente la Velocidad de Fase en Sensores Surface Acoustic Wave

    Directory of Open Access Journals (Sweden)

    Leonardo Andrés Pérez

    2015-10-01

    Full Text Available El sensor de temperatura Surface Acoustic Wave (SAW ofrece amplias posibilidades para ser utilizado en ambientes hostiles. En teoría, las mediciones del SAW se pueden leer inalámbricamente sin integrar circuitos electrónicos en su estructura, permitiendo funcionalidades en mediciones a muy altas temperaturas. La literatura reporta que las variaciones de temperatura del SAW ocasionan corrimientos en su frecuencia de sincronismo, efecto que se atribuye a la sensibilidad térmica de la velocidad de fase del substrato piezoeléctrico. Caracterizar  apropiadamente el SAW requiere una buena medición de la velocidad de fase. No obstante, medir esta velocidad con respecto a la temperatura no es posible con la instrumentación actual. Este artículo reporta un método indirecto para medir estas variaciones de velocidad a través de  simulaciones basadas en el Modelo de Mason y mediciones de la respuesta en frecuencia de un prototipo SAW. Identificar la velocidad de fase del SAW conlleva a graficar, con aceptable precisión, la curva de funcionamiento del sensor, la cual puede utilizarse posteriormente como curva de calibración.

  19. Geotectonic evolution of granitoid-greenstone belts from Crixas, Guarinos, Pilar de Goias - Hidrolina (Goias), Brazil

    International Nuclear Information System (INIS)

    Montalvao, R.M.G. de.

    1985-01-01

    The area in discussion, in a geologic context, constitutes one of the most interesting and complex, within the South American Platform, in Brazilian territory, over which granitoid-greenstone belts are outstanding. The Goiano Complex is the oldest unit in the geologic column herein adopted and composed largely of granitoids, gneiss and migmatites, in the amphibolite facies. Dated samples of the complex have shown two isochrones of Rb/Sr reference, the oldest one is 2.926 +- 65 m.y. and the 87 Sr/ 86 Sr initial ratio of 0.7001 and the youngest on of 2.471 + 20 m.y. and 87 Sr/ 86 Sr initial ratio of 0.701. Although the initial ratios data of the Rb/Sr isochron, as well as the parameters in the Pb/Pb analyses may indicate material of mantle source, it may be interpreted, with the help of field data, that the youngest values may indicate the reworking of crustal sialic rocks formed 2.925 +- 65 m.y. ago (oldest isochron), with primitive material contribution. Before such reworking volcanic-sedimentary sequence was deposited over the already formed sialic crust, and it is denominated Pilar de Goias Supergroup which characterizes the Greenstone Belts in the region. The Archean age for the supergroup was evident through the age results of its ultramafic rocks, showing 2.600 m.y. isochron age, with Sm/Nd methods. Besides the geochronology and field studies, basic information for the construction of the geologic column herein presented, there has been done petrographic and litho geochemical studies, both in the Goiano Complex and Pilar de Goias Supergroup, as for the Pilar de Goias Supergroup, the studies were concentrated on its mafic-ultramafic rocks. (author)

  20. Radiation-Induced Polymerization of Aldehydes and Ketones; Polymerisation radiochimique des aldehydes et des cetones; Radiatsionnaya polimerizatsiya al'degidov i ketonov; Polimerizacion radioinducida de aldehidos y cetonas

    Energy Technology Data Exchange (ETDEWEB)

    Hayashi, K.; Yamaoka, H.; Fujiwara, K.; Sakamoto, M.; Mori, S.; Natori, T.; Yoshida, H.; Okamura, S. [Japanese Association for Radiation Research on Polymers, Neyagawa Osaka (Japan); Kyoto University, Kyoto (Japan)

    1963-11-15

    'aldehyde acetique et l'aldehyde propionique se polymerisent a peine en phase liquide pure, alors qu'ils se polymerisent facilement en presence de {gamma}-alumine. Dans le cas de polymerisation a l'etat solide, on obtient des polymeres cristallins et thermostables dans des- conditions appropriees. Le glyoxal peut se transformer en un polymere caracterise par un reseau a trois dimensions. Avec de l'aldehyde formique, il peut se copolymeriser en polyoxymethylene. Des cetones comme la chloracetone ou la bromacetone et la methylethylcetone ou le diacetyle peuvent se transformer a l'etat solide en polymeres qui sont instables. La cetene peut se transformer en polymere du type polyester dans le cas de polymerisation en phase liquide et en polymere du type polycetone dans le cas de polymerisation en phase solide. Le copolymere de l'aldehyde formique est legerement plus stable. La dimethylcetene se polymerise facilement en polyacetal a l'etat liquide comme a l'etat solide. Toutes ces polymerisations sont des exemples de reactions radiochimiques; les auteurs etudient certains details de la cinetique de ces reactions particulierement interessantes. (author) [Spanish] La irradiacion provoca la polimerizacion de varias clases de aldehidos y cetonas. El formaldehfdo puede transformarse en polioximetileno de elevado peso molecular por polimerizacion radioinducida en fase liquida a bajas temperaturas. Se considera que este proceso se verifica en virtud de una reaccion cationica en cadena, tanto cuando la sustancia se irradia en masa como cuando se irradia disuelta en cloruro de metileno o en tolueno, pero que dicha reaccion es de caracter anionico cuando la sustancia esta disuelta en eter dietilico. El acetaldehido y el propionaldehido son dificilmente polimerizables en fase liquida pura, en tanto que polimerizan con facilidad en presencia de {gamma} alumina. Por polimerizacion en fase solida, se obtienen productos cristalinos y termoestables en condiciones adecuadas. El glioxal polimeriza

  1. Contraste empírico del modelo de cinco fases de duelo de Kübler-Ross en mujeres con cáncer

    Directory of Open Access Journals (Sweden)

    José Moral de la Rubia

    2015-01-01

    Full Text Available Objetivos. (a Definir cinco escalas unidimensionales que permitan evaluar las cinco fases de duelo del modelo de Kübler-Ross y (b contrastar el modelo secuencial de cinco fases de duelo de Kübler-Ross. Método. Se aplicó la escala de las fases de duelo a una muestra no probabilística de 120 mujeres mexicanas con cáncer. Se usó análisis factorial y de senderos para analizar los datos. Resultados. Se definieron cinco modelos unidimensionales de medida para cada fase de duelo con consistencia interna alta, ajuste a los datos y validez de contenido. El modelo secuencial de cinco fases de duelo presentó un ajuste pobre a los datos. Las fases de duelo fueron independientes del tiempo transcurrido desde el diagnóstico de cáncer. Un modelo no secuencial tuvo buen ajuste a los datos. En este modelo, la negación predijo ira, negociación con un ser superior y depresión; por su parte, la ira predijo depresión; negociación con un ser superior predijo aceptación; y depresión predijo menor aceptación. Conclusión. En estas mujeres mexicanas con cáncer, más que una secuencia de fases en el proceso de duelo, se observaron seis respuestas psicológicas que se interrelacionan entre sí y con la pérdida de la salud. Los 39 ítems seleccionados pueden emplearse como una escala de seis factores y dos dimensiones correlacionadas, afecto positivo (promesas/pacto, fe/esperanza y aceptación y afecto negativo (negación, depresión e ira.

  2. Determinación de la composición de fases en circona mediante un procedimiento polimórfico simple

    Directory of Open Access Journals (Sweden)

    Hernández-Jiménez, A.

    2004-02-01

    Full Text Available In this work, we propose a polymorphic method for the quantitative analysis in zirconia. This procedure uses a square system of equations relating the intensities of a peaks groups set in the diffraction pattern with the weight fractions of the different phases present in the sample. In this system it is used as unknowns, besides the relative abundance of the phases, a group of parameters that incorporates the contribution from the tails of the groups adjacent to the intensity of a selected group. The described procedure has been applied to a simulated diffractogram corresponding to a composition of zirconia of 50% of cubic phase, 25% of tetragonal phase and 25% of monoclinic phase, and also to a sample of zirconia processed by the sol-gel method.

    En este trabajo se propone un método polimórfico para el análisis cuantitativo de fases en la circona. Este procedimiento emplea un sistema de ecuaciones compatible y determinado que relaciona las intensidades de un conjunto de grupos de picos del espectro de difracción con las fracciones en peso de las diferentes fases presentes en la muestra. En dicho sistema, además de las abundancias relativas de las fases, se utilizan como incógnitas un conjunto de parámetros que dan cuenta de la aportación de las colas de los grupos de picos adyacentes al grupo de picos considerado. Este procedimiento se ha aplicado a un difractograma simulado correspondiente a una circona con 50% de fase cúbica, 25% de fase tetragonal y 25% de fase monoclínica y también a una muestra en polvo de circona fabricada mediante técnicas sol-gel.

  3. Petrogenesis and geodynamic implications of Ediacaran highly fractionated A-type granitoids in the north Arabian-Nubian Shield (Egypt): Constraints from whole-rock geochemistry and Sr-Nd isotopes

    Science.gov (United States)

    Sami, Mabrouk; Ntaflos, Theodoros; Farahat, Esam S.; Mohamed, Haroun A.; Hauzenberger, Christoph; Ahmed, Awaad F.

    2018-04-01

    Mineral chemistry, whole-rock geochemical and Sr-Nd isotopic data are reported for the Abu-Diab granitoids in the northern Arabian-Nubian Shield (ANS) of Egypt, to investigate their petrogenesis and geodynamic significance. Gabal Abu-Diab constitute a multiphase pluton, consisting largely of two-mica granites (TMGs) enclosing microgranular enclaves and intruded by garnet bearing muscovite granites (GMGs) and muscovite granites (MGs). The granitoids are weakly peraluminous (A/CNK = 1.01-1.12) and show high SiO2 (>72.9 wt%) and alkali (K2O + Na2O = 8.60-9.13) contents. The geochemical features show that they are post-collisional and highly fractionated A-type granitoids. Compared to their host TMGs, the microgranular enclaves are strongly peraluminous (A/CNK = 1.18-1.24) with lower SiO2 and higher abundances of trace elements. The TMGs are depleted in Ba, Nb, P and Ti and are enriched in LREEs relative to HREEs with weakly negative Eu anomalies (Eu/Eu* = 0.45-0.64). In contrast, the GMGs and MGs are extremely depleted in Ba, Sr and Ti and have tetrad-type REE patterns (TE1-3 = 1.1-1.3) with strongly pronounced negative Eu anomalies (Eu/Eu* = 0.03-0.26), similar to rare metals bearing granites. The Ediacaran (585 ± 24 Ma) TMGs, are characterized by restricted and relatively low initial 87Sr/86Sr ratios (0.70337-0.70382) that suggests their derivation from a depleted mantle source, with little contamination from the older continental crust. In contrast, the GMGs and MGs have extremely high 87Rb/86Sr and 87Sr/86Sr ratios that reflect the disturbance of the Rb-Sr isotopic system and may give an indication for magmatic-fluid interaction. However, all the granitoids display positive εNd(t) (4.41-6.57) and depleted mantle model ages TDM2 between 777 and 956 Ma, which indicate their derivation from a Neoproterozoic juvenile magma sources and preclude the occurrence of pre-Neoproterozoic crustal rocks in the ANS. The microgranular enclaves represent globules of hot mafic

  4. Metallogenetic characterization of granitoid rocks through geochemical prospection: the Lagoa Real example related to uranium mineralization in Bahia state, Brazil; Caracterizacao metalogenetica de corpos gratinoides atraves de prospeccao geoquimica: o exemplo da suite intrusiva Lagoa Real relacionada a mineralizacoes de uranio no Estado da Bahia

    Energy Technology Data Exchange (ETDEWEB)

    Oliveira, J.E., E-mail: cprmsa@bahianet.com.br [Servico Geologico do Brasil (GEREMI/SUREG/SA/CPRM), Salvador, BA (Brazil)

    2011-07-01

    Within a broad metallogenetic evaluation program carried out by CPRM - Geological Survey of Brazil in covenant with the CBPM - Companhia Baiana de Pesquisa Mineral in the central part of the Sao Francisco Craton, the Lagoa Real granitoid rocks was one of the selected targets. The work included geochemical exploration supplemented by follow-in survey and integrated 1:200.000 scale geochemical cartography. The Lagoa Real granitoid was recognized with composition ranging from monzogranitic to alcaligranitic type. The geochemical surveying led to the definition of the metallogenetic specialization of the granitoid rock, with characteristic geochemical and mineralogic associations. These associations are related to uranium mineralization. The genetic model using stream sediment and pan concentrate data, show similarity with the metallogenetic model of zonal partitioning proposed by Routhier (1963), for plutonogenic lode deposits with potential for Sn, W, Nb, Be, REE, Au, and U. In this work emphasis is given to the importance of the integrated use of different prospective methods toward the evaluation of granitoid systems, particularly the combination of geochemical surveying methods with results for a better understanding of the geologic and metallogenetic settings. (author)

  5. [Analysis of X-Ray Fluorescence Spectroscopy and Plasma Mass Spectrometry of Pangxidong Composite Granitoid Pluton and Its Implications for Magmatic Differentiation].

    Science.gov (United States)

    Zeng, Chang-yu; Ding, Ru-xin; Li, Hong-zhong; Zhou, Yong-zhang; Niu, Jia; Zhang, Jie-tang

    2015-11-01

    Pangxidong composite granitoid pluton located in the southwestern margin of Yunkai massif. The metamorphic grade of this pluton increases from outside to inside, that is, banded-augen granitic gneisses, gneissoid granites and granites distribute in order from edge to core. X-Ray Fluorescence Spectroscopy and Plasma Mass Spectrometry are conducted to study the geochemical characteristics of the three types of rocks. The result shows that all the three types of rocks are peraluminous rocks and their contents of main elements and rare earth elements change gradually. From granitic gneisses to granites, the contents of Al₂O₃, CaO, MgO, TiO₂, total rare earth elements and light rare earth elements increase, but the contents of SiO₂ and heavy rare earth elements decrease. It is suggested that the phylogenetic relationship exists between granitic gneisses, gneissoid granites and granites during the multi-stage tectonic evolution process. Furthermore, the remelting of metamorphosed supracrustal rocks in Yunkai massif is probably an important cause of granitoid rocks forming. The evolutionary mechanism is probably that SiO₂ and heavy rare earth elements were melt out from the protolith and gradually enriched upward, but Al₂O₃, CaO, MgO, TiO₂ and light rare earth elements enriched downward.

  6. Rb-Sr isochronous dating of granitoids of Dumbier zone of Low Tatras (Western Carpathians)

    International Nuclear Information System (INIS)

    Bagdasaryan, G.P.; Gukasyan, R.Kh.; Cambel, B.; Vesel'skij, J.

    1985-01-01

    The results are discussed of isotopic-geochronological research and age determination of characteristic samples of granitoid rocks, obtained by the Rb/Sr isochronous method. The samples were biotite granodiorites and granites taken from various parts of the Dumbier massif and small granite bodies of the Kralicka type. Rb/Sr isochrones of the rock samples show identical age values: 362+-21 m.y. for the Dumbier massif and 365+-17 m.y. correspnding to the Middle - Upper Devonian. Initial 87 Sr/ 86 Sr ratios equal to 0.7079 and 0.7157, respectively, allow to make a presumption that the rocks of the Dumbier massif may have been derived both from crustal and from mantle sources while granites of the Kralicka type are close to the rocks of the crustal origin

  7. Crustal melting and recycling: geochronology and sources of Variscan syn-kinematic anatectic granitoids of the Tormes Dome (Central Iberian Zone). A U-Pb LA-ICP-MS study

    Science.gov (United States)

    López-Moro, F. J.; López-Plaza, M.; Gutiérrez-Alonso, G.; Fernández-Suárez, J.; López-Carmona, A.; Hofmann, M.; Romer, R. L.

    2018-04-01

    In this study, we report U-Pb Laser Ablation ICP-MS zircon and ID-TIMS monazite ages for peraluminous granitoid plutons (biotite ± muscovite ± cordierite ± sillimanite) in the Tormes Dome, one of the gneiss-cored domes located in the Central Iberian Zone of the Variscan belt of northern Spain. Textural domains in zircon, interpreted to represent the magmatic crystallization of the granitoids (and one monazite fraction in the Ledesma pluton) yielded ages around 320 Ma, in agreement with other geochronological studies in the region. This age is interpreted to date the timing of decompression crustal melting driven by the extensional collapse of the orogenic belt in this domain of the Variscan chain of western Europe. In addition, there are several populations of inherited (xenocrystic) zircon: (1) Carboniferous zircon crystals (ca. 345 Ma) as well as one of the monazite fractions in the coarse-grained facies of the Ledesma pluton that also yielded an age of ca. 343 Ma. (2) Devonian-Silurian zircon xenocrysts with scattered ages between ca. 390 and 432 Ma. (3) Middle Cambrian-Ordovician (ca. 450-511 Ma). (4) Ediacaran-Cryogenian zircon ages (ca. 540-840 Ma). (5) Mesoproterozoic to Archaean zircon (900-2700 Ma). The abundance of Carboniferous-inherited zircon shows that crustal recycling/cannibalization may often happen at a fast pace in orogenic scenarios with only short lapses of quiescence. In our case study, it seems plausible that a "crustal layer" of ca. 340 Ma granitoids/migmatites was recycled, partially or totally, only 15-20 My after its emplacement.

  8. Analysis and control of erosion by solid particles in the elements of the flow system of steam turbines; Analisis y control de erosion por particulas solidas en los elementos del sistema de flujo de turbinas de vapor

    Energy Technology Data Exchange (ETDEWEB)

    Mazur Czerwiec, Zdzislaw; Campos Amezcua, Alfonso; Campos Amezcua, Rafael [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)

    2010-07-01

    The analysis of erosion by solid particles is presented of different elements of the flow channel of the steam turbines that operate in Mexico: nozzles, stop valves, blade bosses, labyrinth seals and rotor disc; using tools of of Computational Fluid Dynamics (CFD). In these main elements of turbines a strong problem of erosion was registered that threatens the reliable operation of the turbines, its availability and its optimal yield. With base on the results of the numerical analyses, the design modifications of the different elements were developed from the flow channel of the steam turbines, in order to reduce the erosion and thus diminishing the energy losses and increasing the steam turbine efficiency. This work presents the main benefits that the Thermoelectric Power Plants obtain with the reduction of the erosion by solid particles that affect the critical components of steam turbines: extension of the period between maintenance, replacement of components, reduction of operation and maintenance costs of the turbines, and extension of the useful life of the main components. [Spanish] Se presenta el analisis de erosion por particulas solidas de diferentes elementos del canal de flujo de las turbinas de vapor que operan en Mexico: toberas, valvula de paro, tetones de los alabes, sellos de laberinto y disco del rotor; utilizando herramientas de Dinamica de Fluidos Computacional (DFC). En estos elementos principales de turbinas se registro un fuerte problema de erosion que amenaza la operacion confiable de las turbinas, su disponibilidad y su rendimiento optimo. Con base en los resultados de los analisis numericos, se desarrollaron las modificaciones de diseno de los diferentes elementos del canal de flujo de las turbinas de vapor, con el proposito de reducir la erosion y asi, disminuir las perdidas de energia e incrementar el rendimiento de las turbinas de vapor. Este trabajo presenta los principales beneficios que obtienen las Centrales Termoelectricas con la

  9. A influência das fases oral e faríngea na dinâmica da deglutição

    OpenAIRE

    Yamada,Elaine Keiko; Siqueira,Karina Oliveira de; Xerez,Denise; Koch,Hilton Augusto; Costa,Milton Melciades B.

    2004-01-01

    RACIONAL: Embora a dinâmica da deglutição ocorra de forma integrada, a fase oral não tem sido tão valorizada quanto a fase faríngea. OBJETIVOS: Avaliar, através do método videofluoroscópico, a fase oral da deglutição, para observar as características da organização do bolo líquido em voluntários sadios e as variações desta organização em exames de pacientes disfágicos. Estabelecer a inter-relação funcional dos estágios de organização e ejeção oral do bolo. Verificar a presença (ou ausência) d...

  10. The Sr:Ba:Rb ratio and zircon typology in granitoid complexes of Sao Paulo, Parana and Minas Gerais states (Brazil)

    International Nuclear Information System (INIS)

    Wernick, E.; Galembeck, T.M.B.; Artur, A.C.; Rigo Junior, L.; Weber-Diefenbach, K.

    1990-01-01

    Chemical (Sr: Ba: Rb) and zircon typology data from the Nazare Paulista, Mairipora/Cantareira, Cunhaporanga, Tres Corregos, Morungaba, Socorro, Itu, Graciosa and Serra Carambei granitoid complexes from the states of Minas Gerais, Sao Paulo and Parana (SE/S Brazil) are presented and discussed. By the zircon typology method these complexes are reffered, respectively, to the 2nd crustal, 3rd crustal/low temperature C-A, low temperature C-A, medium temperature C-A, medium/high temperature C-A, K-SA/Alkaline and alkaline serie which are considered as generated under increasing temperature associated with a progressive major participation of mantellic material. All these series, with the exception of the medium to high temperature calc-alkaline complexes Socorro and Morungaba whose chemical data come from several laboratories, display different positions and behaviour in the Sr: Ba: Rb diagram which reinforce the use of the zircon typology method in the study of granitoids. From the 2nd crustal serie up to the medium temperature C-A serie the complexes show a regular shift in their chemical composition which became progressively richer in Sr and depleted in Rb. The highly differentiades hypersolvus Serra do Carambei granite is strongly enriched in Rb and impoverish in Ba with respect to the Itu and the Graciosa complex which itself is slighly more depleted in Sr than the Itu granite. (author)

  11. Fase de convalecencia en la rehabilitación cardíaca. Protocolo de actuación

    Directory of Open Access Journals (Sweden)

    Susana Hernández García

    2015-03-01

    Full Text Available La fase de convalecencia de la rehabilitación cardíaca tiene como propósito fundamental mejorar la capacidad funcional y fomentar un cambio del estilo de vida a través de todos los aspectos que integra la prevención secundaria fundamentalmente, en la incorporación a un programa de entrenamiento físico y en el control de los factores de riesgo cardiovascular, lo que favorece la reincorporación social y laboral de los enfermos. Con el objetivo de actualizar el protocolo de actuación de esta fase en nuestra institución se establecieron diferentes ejercicios con sus dosificaciones y recomendaciones para la rehabilitación de diferentes poblaciones, así como controles de la sesión de entrenamiento físico a tener en cuenta. Este protocolo permitirá aunar estrategias para mejorar la intervención fisioterapéutica en la fase de convalecencia del Programa Nacional de Rehabilitación Cardíaca en Cuba.

  12. Petrochemical and Mineralogical Constraints on the Source and Processes of Uranium Mineralisation in the Granitoids of Zing-Monkin Area, Adamawa Massif, NE Nigeria

    International Nuclear Information System (INIS)

    Haruna, I. V.; Orazulike, D. M.; Ofulume, A. B.; Mamman, Y. D.

    2011-01-01

    Zing-Monkin area, located in the northern part of Adamawa Massif, is underlain by extensive exposures of moderately radioactive granodiorites, anatectic migmatites, equigranular granites, porphyritic granites and highly radioactive fine-grained granites with minor pegmatites. Selected major and trace element petrochemical investigations of the rocks show that a progression from granodiorite through migmatite to granites is characterised by depletion of MgO, CaO, Fe 2 O 3, Sr, Ba, and Zr, and enrichment of SiO 2 and Rb. This trend is associated with uranium enrichment and shows a chemical gradation from the more primitive granodiorite to the more evolved granites. Electron microprobe analysis shows that the uranium is content in uranothorite and in accessories, such as monazite, titanite, apatite, epidote and zircon. Based on petrochemical and mineralogical data, the more differentiated granitoids (e.g., fine-grained granite) bordering the Benue Trough are the immediate source of the uranium prospect in Bima Sandstone within the Trough. Uranium was derived from the granitoids by weathering and erosion. Transportation and subsequent interaction with organic matter within the Bima Sandstone led to precipitation of insoluble secondary uranium minerals in the Benue Trough.

  13. ECO-driving met behulp van serious gaming en social media (fase 1)

    NARCIS (Netherlands)

    Kuiper, H.; Boonekamp, R.C.; Bijlsma, T.; Jansen, S.T.H.; Obdeijn, C.; Stuiver, A.; Spronkmans, S.; Bijnen, D.; Versteegh, T.

    2013-01-01

    Dit rapport beschrijft fase 1 van een EL&I cofinancieringstraject waarin onderzoek wordt gedaan naar gedragsbeïnvloeding bij automobilisten om CO2-reductie te bereiken met behulp van Serious gaming en Social Media. Het onderzoek sluit goed aan bij het overheidswerkprogramma “Schoon en Zuinig”

  14. A prolonged granitoid formation in Saglek Block, Labrador: Zonal growth and crustal reworking of continental crust in the Eoarchean

    Directory of Open Access Journals (Sweden)

    Tsuyoshi Komiya

    2017-03-01

    We made a detailed sketch of a small outcrop in St. John's Harbour South (SJHS area, and classified the orthogneisses and mafic enclaves into seven generations based on the geologic occurrence. The first and second generations comprise mafic rocks and lack magmatic zircons. We conducted CL imaging and U-Pb dating of zircons from the third, sixth and seventh generation of the orthogneisses to estimate the protolith ages at 3902 ± 25, 3892 ± 33 and 3897 ± 33 Ma for each, supporting the presence of the over 3.9 Ga Iqaluk Gneiss. The geological occurrence that the mafic rocks occur as enclaves within the 3.9 Ga Iqaluk Gneiss indicates that they are the oldest supracrustal rocks in the world. Our geochronological and geological studies show the Uivak Gneiss is quite varied in lithology and age from 3.6 to >3.9 Ga, and tentatively classified into six groups based on their ages. The oldest Uivak Gneiss components including the Iqaluk Gneiss are present around the SJHS area, and the orthogneisses become young as it is away. The lines of evidence of overprinting of younger granitoid on older granitoid in small outcrops and geological-map scale as well as presence of inherited zircons even in the oldest suite suggests that crustal reworking played an important role on erasing the ancient crusts.

  15. Equilibrio entre fases para la aplicación de solventes verdes en tecnología de alimentos

    OpenAIRE

    Hernández, Elvis J.

    2010-01-01

    [ES]: En este trabajo se presentan los resultados obtenidos del estudio (experimental y teórico) del equilibrio entre fases de compuestos alimentarios y solventes verdes, aportando nuevos resultados a los fundamentos de los procesos de separación por contacto en equilibrio de la tecnología de alimentos. Se obtuvieron nuevos datos de equilibrio entre fases, aplicando métodos experimentales a altas presiones (equilibrio líquido – fluido supercrítico, para el disolvente dióxido de carbono) y ...

  16. Permo-Triassic arc-like granitoids along the northern Lancangjiang zone, eastern Tibet: Age, geochemistry, Sr-Nd-Hf isotopes, and tectonic implications

    Science.gov (United States)

    Wang, Xinyu; Wang, Shifeng; Wang, Chao; Tang, Wenkun

    2018-05-01

    Large volumes of Permo-Triassic granitoids are exposed along the Northern Lancangjiang zone, eastern Tibet, and these rocks provide insights into the tectonic evolution of the Paleo-Tethys Ocean. We conducted detailed geological fieldwork and geochemical analysis of the Xiaochangdu and Kagong plutons that crop out along the Northern Lancangjiang magmatic belt. Zircon U-Pb data constrain the emplacement of the Xiaochangdu quartz diotites to between 263 and 257 Ma, and the Kagong granites and diorites to between 234 and 232 Ma. The Xiaochangdu quartz diorites are enriched in light rare earth (LREE) and large ion lithophile elements (LILE), depleted in high field strength elements (HFSE), have low (87Sr/86Sr)i ratios, and near-positive εNd(t) (-0.26 to 1.58) and εHf(t) (0.68-8.83) values, similar to typical subduction- related mantle-derived arc magmas. They are also characterized by high Al2O3 concentrations and low Nb/U (3.48-7.59) and Ce/Pb (3.22-4.86) ratios, indicating that their mantle source was modified by subducted pelagic sediments; Coeval granites and diorites from the Kagong pluton exhibit low A/CNK values, high LREE/HREE (heavy rare earth element) ratios, enrichment in LILE, and depletion in HFSE, also characteristic of typical arc magmas. Their variable SiO2 contents (57%- 75%), (87Sr/86Sr)i ratios, and εNd(t) (1.02-4.49) and εHf(t) (2.52-6.93) values, and relatively high zircon saturation temperatures (721-827 °C), suggest underplating of mantle-derived mafic melts beneath the lower crust. Their magmatic evolution can be explained using a MASH model. In combination with regional geological studies, our geochemical and geochronological results suggest that the late Permian Xiaochangdu and Late Triassic Kagong arc-like granitoids represent a section of a Permo-Triassic magmatic arc that was associated with the eastward subduction of the Paleo-Tethys oceanic slab beneath the Northern Qiangtang-Changdu terrane. Combined with other geological evidence

  17. Geological evolution of the center-southern portion of the Guyana shield based on the geochemical, geochronological and isotopic studies of paleoproterozoic granitoids from southeastern Roraima, Brazil

    International Nuclear Information System (INIS)

    Almeida, Marcelo Esteves

    2006-01-01

    This study focuses the granitoids of center-southern portion of Guyana Shield, southeastern Roraima, Brazil. The region is characterized by two tectonic-stratigraphic domains, named as Central Guyana (GCD) and Uatuma-Anaua (UAD) and located probably in the limits of geochronological provinces (e.g. Ventuari-Tapajos or Tapajos-Parima, Central Amazonian and Maroni-Itacaiunas or Transamazon). The aim this doctoral thesis is to provide new petrological and lithostratigraphic constraints on the granitoid rocks and contribute to a better understanding of the origin and geo dynamic evolution of Guyana Shield. The GCD is only locally studied near to the UAD boundary, and new geological data and two single zircon Pb-evaporation ages in mylonitic biotite granodiorite (1.89 Ga) and foliated hastingsite-biotite granite (1.72 Ga) are presented. These ages of the protholiths contrast with the lithostratigraphic picture in the other areas of Cd (1.96-1.93 Ga). Regional mapping, petrography, geochemistry and zircon geochronology carried out in the Urad have showed widespread Paleoproterozoic calc-alkaline granitic magmatism. These granitoid rocks are distributed into several magmatic associations with different Paleoproterozoic (1.97-1.89 Ga) ages, structural and geochemical affinities. Detailed mapping, petrographic and geochronological studies have distinguished two main sub domains in the UAD. In the northern UAD, the high-K calc-alkaline Martins Pereira (1.97 Ga) and Serra Dourada S-type granites (1.96 Ga) are affected by NE-SW and E-W ductile dextral shear-zones, showing coexistence of magmatic and deformational fabrics related to heterogeneous deformation. Inliers of basement (2.03 Ga) crop out northeast of this area, and are formed by meta volcano-sedimentary sequence (Cauarane Group) and TTG-like calc-alkaline association (Anaua Complex). Xenoliths of meta diorites (Anaua Complex) and para gneisses (Cauarane Group) reinforce the intrusive character of Martins Pereira

  18. Sensibilidade as catecolaminas dos atrios direitos das ratas : influencia das fases do ciclo estral e do "stress"

    OpenAIRE

    Monica Luiza Viegas Rodrigues

    1993-01-01

    Resumo: Os objetivos deste trabalho foram: analisar a sensibilidade ao efeito cronotrópico da isoprenalina, noradrenalina e adrenalina de átrios direitos isolados de ratas normais, em cada uma das fases do ciclo estral, ou após 50 minutos de natação, durante o estro ou o diestro; correlacionar as alterações de sensibilidade com as fases do ciclo estral e/ou com os níveis plasmáticos de corticosterona. Utilizamos ratas adultas, Wistar, normais, sedentárias, ou imediatamente após 50 min de nata...

  19. Cálculo termodinámico de los diagramas de fases

    OpenAIRE

    Pena, Pilar; Aza Pendas, Salvador de

    1980-01-01

    Partiendo del concepto de energía libre de Gibbs como criterio de equilibrio^e hace una breve introducción sobre las posibilidades de los métodos termodinámicos para el calculo de los diagramas de equilibrio de fases. A continuación se presentan varias aplicaciones concretas para la constmcción de diagramas binarios del tipo de solubilidad sólida completa y del tipo eutéctico.

  20. Zircon U-Pb ages and Hf isotopic compositions of neoarchaean granitoids from Karimnagar, Eastern Dharwar craton, Southern India: LA-ICPMS results

    International Nuclear Information System (INIS)

    Babu, E.V.S.S.K.; Vijaya Kumar, T.; Sreenivas, B.; Khadke, Namrata; Vijaya Gopal, B.; Bhaskar Rao, Y.J.

    2015-01-01

    The Archaean Dharwar and Bastar cratons of Peninsular India are separated by the NE-SW trending Godavari Graben. This zone is involved in recurrent rifting. It is generally believed that earlier phase of rifting dates back to Mesoproterozoic and the younger phase is related to the deposition of Permo-carboniferous coal-bearing sediments. A belt of high-grade rocks (∼ 150 x 45 km) - the Karimnagar granulite terrane (KGT) along the southern flank of the graben. The KGT comprises high-grade lithologies such as orthopyroxene-bearing quarto-feldspathic gneiss, amphibolite-granulite facies supracrustal belts that include metamorphosed quartz-arenites, pelites, carbonates, iron formation and mafic rocks as well as several zones of migmatite and younger granitoid intrusives. The study presented new LA-ICPMS zircon U-Pb age data for five granitoid (charnockite and granite) samples (KRN-90-24, KRN-90-30, KRN-13-02, KRN-13-03 and KRN-13-05; a closer constraint of the age crystallization of protoliths and high-grade metamorphism of felsic granulites and orthogneisses from the KGT. Hf isotopic compositions were also obtained for selected zircons from two samples (KRN-90-24 and KRN-90-30) using New Wave UP-213 Laser Ablation system coupled to Nu Plasma HR MC-ICPMS to constraint the nature of the felsic protoliths of the charnockite and granite gneisses in the KGT

  1. Virtual endoscopic images by 3D FASE cisternography for neurovascular compression

    International Nuclear Information System (INIS)

    Ishimori, Takashi; Nakano, Satoru; Kagawa, Masahiro

    2003-01-01

    Three-dimensional fast asymmetric spin echo (3D FASE) cisternography provides high spatial resolution and excellent contrast as a water image acquisition technique. It is also useful for the evaluation of various anatomical regions. This study investigated the usefulness and limitations of virtual endoscopic images obtained by 3D FASE MR cisternography in the preoperative evaluation of patients with neurovascular compression. The study included 12 patients with neurovascular compression: 10 with hemifacial spasm and two with trigeminal neuralgia. The diagnosis was surgically confirmed in all patients. The virtual endoscopic images obtained were judged to be of acceptable quality for interpretation in all cases. The areas of compression identified in preoperative diagnosis with virtual endoscopic images showed good agreement with those observed from surgery, except in one case in which the common trunk of the anterior inferior cerebellar artery and posterior inferior cerebellar artery (AICA-PICA) bifurcated near the root exit zone of the facial nerve. The veins are displayed in some cases but not in others. The main advantage of generating virtual endoscopic images is that such images can be used for surgical simulation, allowing the neurosurgeon to perform surgical procedures with greater confidence. (author)

  2. Les granitoïdes néoprotérozoïques de Khzama, Anti-Atlas central, Maroc: marqueurs de l'évolution d'un magmatisme d'arc à un magmatisme alcalineNeoproterozoic granitoids from Khzama, central Anti-Atlas, Morocco: evolution markers from arc magmatism to alkaline magmatism

    Science.gov (United States)

    El-Khanchaoui, T.; Lahmam, M.; El-Boukhari, A.; El-Beraaouz, H.

    2001-05-01

    Petrological study and zircon typology provide important information that is related to the classification and genesis of Neoproterozoic granitoids in the Khzama area (northeast Siroua). The Pan-African granitoids show a transition from island-arc magmatism to alkaline magmatism. A space and time zonation of magmatism from the north to the south is evident. Early Pan-African granitoids were generated from various magma sources through different petrogenetic mechanisms. The first association corresponds to the low-K calc-alkaline plutons of Ait Nebdas, the second one correponds to high-K calc-alkaline post-collisional granites (Tamassirte-Tiferatine and Ifouachguel). Finally, shoshonitic magmatism (Irhiri) ends the magmatic evolution of the region. Thus, the late Pan-African granitic plutonism began with calc-alkaline associations and ended with K-alkaline magmatism in a transtensional setting, heralding the onset of the Moroccan Palæozoic cycle.

  3. Inactivation of Vibrio cholerae O1 El Tor inoculated into Peruvian ''choro'' mussels (Aulacomya ater) and two species of clams (Argopecten purpuratus and Gari solida) using medium-dose irradiation

    International Nuclear Information System (INIS)

    Torres, Z.; Bernuy, B.; Kahn, G.; Zapata, G.; Vivanco, M.; Guzman, E.; Leon, R.

    2001-01-01

    The radiation decimal reduction dose (D 10 ) for Vibrio cholerae O1 biotype El Tor inoculated through the natural feeding system into three species of bivalve mollusks from the Peruvian Pacific coast: ''choro'' mussels (Aulacome ater), ''abanico'' clams (Argopecten purpuratus), and common clams (Gari solida), was determined in vivo. The D 10 value obtained in vivo was 0.14 kGy in all mollusks tested. Concurrent studies conducted to determine the potential use of irradiation to extend the microbiological shelf-life of the mollusks during post-irradiation storage at 0-1 deg. C indicated that a dose of 1.0 kGy was optimal for choro mussels and abanico clams, whereas 2.0 kGy produced the best results when treating common clams. Shelf-life extension thus achieved was 31 days for choro mussels, 16 days for abanico clams, and 21 days for common clams. Non-irradiated control samples of all mollusks spoiled after 17 days of refrigerated storage. There were no significant (p<.05) adverse effects from the application of the optimal radiation treatments on the sensory characteristics (i.e. appearance, odor, flavor, and texture) of the mollusks. Total volatile basic nitrogen (VBN) and pH values were examined for use as indexes of seafood freshness. (author)

  4. Geochronology Intermediary Laboratory implantation at the Rio Grande do Norte Federal University: the dating of the Serrinha Granitoid (RN) and the correlate Brasiliana extensional deformation; Implantacao do Laboratorio Intermediario de Geocronologia na UFRN: a datacao do granitoide de Serrinha (RN) e da deformacao extensional brasiliana correlata

    Energy Technology Data Exchange (ETDEWEB)

    Macedo, Maria Helena F.; Sa, Emanuel F. Jardim de; Souza, Zorano S. [Pernambuco Univ., Recife, PE (Brazil). Nucleo de Pesquisa em Geodinamica e Geofisica; Mendes, Franklin S. [Pernambuco Univ., Recife, PE (Brazil). Curso de Quimica; Ramalho, Karlos A.C. [Pernambuco Univ., Recife, PE (Brazil). Curso de Geologia

    1997-12-31

    The article describes the activities developed by the Geochronology Intermediary Laboratory at the Federal University of the Rio Grande do Norte, a Brazilian university, where there were the preoccupation of establishing strategies for a geochronological development. It relates the Rubidium-Strontium (Rb/Sr) and Samarium-Neodymium (Sm/Nd) methods, describing the analysis realized in these methodologies. Afterward, it presents the geological and petrographic situation of the Granitoide de Serrinha, located at Rio Grande do Norte State, Brazil and its geochronological data 8 refs., 2 figs.

  5. Exigência de metionina + cistina para frangas de reposição na fase cria de sete a 12 semanas de idade

    Directory of Open Access Journals (Sweden)

    P. D'Agostini

    2012-12-01

    Full Text Available Determinou-se a exigência de metionina + cistina para frangas de sete a 12 semanas de idade e verificou-se seu efeito sobre a fase de postura. O experimento foi dividido em duas fases, de cria e de produção, esta de 22 a 33 semanas de idade. Na primeira fase, utilizaram-se 640 aves - 50% Lohmann LSL e 50% Lohmann Brown - com sete a 12 semanas de idade, distribuídas em delineamento inteiramente ao acaso, em esquema fatorial 5x2 (porcentagem de met+cis e linhagem, com quatro repetições e 16 aves por repetição. As porcentagens de met+cis total estudadas foram 0,471; 0,541; 0,611; 0,681 e 0,751%. Ao atingirem 22 semanas de idade, 240 aves foram utilizadas para verificar o efeito residual das dietas fornecidas na fase de cria. A dieta fornecida nesta fase foi igual para todas as aves. As exigências de metionina + cistina para aves de reposição, leves e semipesadas, no período de sete a 12 semanas de idade, foram de 0,710 % de met+cis total (0,639% de met+cis digestível e 0,706% de met+cis total (0,635% de met+cis digestível, respectivamente.

  6. Molybdenite Re/Os dating, zircon U-Pb age and geochemistry of granitoids in the Yangchuling porphyry W-Mo deposit (Jiangnan tungsten ore belt), China: Implications for petrogenesis, mineralization and geodynamic setting

    Science.gov (United States)

    Mao, Jingwen; Xiong, Bikang; Liu, Jun; Pirajno, Franco; Cheng, Yanbo; Ye, Huishou; Song, Shiwei; Dai, Pan

    2017-08-01

    The Yangchuling W-Mo deposit, located in the Jiangnan porphyry-skarn (JNB) tungsten ore belt, is the first recognized typical porphyry W-Mo deposit in China in the 1980's. Stockworks and disseminated W-Mo mineralization occur in the roof pendant of a 0.3 km2 monzogranitic porphyry stock that intruded into a granodiorite stock, hosted by Neoproterozoic phyllite and slate. LA-ICPMS zircon U-Pb analyses suggest that of the monzogranitic porphyry and granodiorite were formed at 143.8 ± 0.5 Ma and 149.8 ± 0.6 Ma, respectively. Six molybdenite samples yielded a Re-Os weighted mean age of 146.4 ± 1.0 Ma. Geochemical data show that both granodiorite and monzogranitic porphyry are characterized by enrichment of large ion lithophile elements (LILE) relative to high field strength elements (HFSE), indicating a peraluminous nature (A/CNK = 1.01-1.08). Two granitoids are characterized by a negative slope with significant light REE/heavy REE fractionation [(La/Yb)N = 8.38-23.20] and negative Eu anomalies (Eu/Eu* = 0.69-0.76). The P2O5 contents of the Yangchuling granitoids range from 0.12% to 0.17% and exhibit a negative correlation with SiO2, reflecting that they are highly fractionated I-type. They have high initial 87Sr/86Sr ratios (0.7104-0.7116), low negative εNd(t) (- 5.05 to - 5.67), and homogeneous εHf(t) between - 1.39 and - 2.17, indicating similar sources. Additionally, two-stage Nd model ages (TDM2) of 1.3-1.4 Ga and two-stage Hf model ages (TDM2) of 1.2-1.3 Ga are consistent, indicating that Neoproterozoic crustal rocks of the Shuangqiaoshan Group could have contributed to form the Yangchuling magmas. Considering the two groups of parallel Late Mesozoic ore belts, namely the Jiangnan porphyry-skarn tungsten belt (JNB) in the south and the Middle-Lower Yangtze River porphyry-skarn Cu-Au-Mo-Fe ore belt (YRB) in the north, the Nanling granite-related W-Sn ore belt (NLB) in the south, the neighboring Qin-Hang porphyry-skarn Cu-Mo-hydrothermal Pb-Zn-Ag ore belt (QHB

  7. A cryptic Early Palaeozoic event in the Narcea Antiform? 40Ar/39Ar amphibole data in the Puente de Selce granitoid

    OpenAIRE

    Gutiérrez Alonso, Gabriel; Fernández Suárez, J.; Keppie, J. D.; Ortega Rivera, M. A.; Lee, J. K. W.; Murphy, J. B.

    2005-01-01

    Las edades 40Ar/39Ar obtenidas a partir de anfíboles del granitoide Neoproterozoico de Puente de Selce, localizado en el Antiforme del Narcea junto con la existencia de fábricas de deformación relictas generadas en condiciones de media-alta temperatura en las mismas rocas puede ser interpretada como debida a un evento críptico de edad Paleozoico Inferior fuertemente retrabajado durante la deformación varisca. La naturaleza y la cinemática de este posible evento no pueden precisars...

  8. Oxidation state inherited from the magma source and implications for mineralization: Late Jurassic to Early Cretaceous granitoids, Central Lhasa subterrane, Tibet

    Science.gov (United States)

    Cao, MingJian; Qin, KeZhang; Li, GuangMing; Evans, Noreen J.; McInnes, Brent I. A.; Li, JinXiang; Zhao, JunXing

    2018-03-01

    Arc magmas are more oxidized than mid-ocean ridge basalts; however, there is continuing debate as to whether this higher oxidation state is inherited from the source magma or developed during late-stage magmatic differentiation processes. Well-constrained Late Jurassic to Early Cretaceous arc-related intermediate to felsic rocks derived from distinct magma sources provide us with a good opportunity to resolve this enigma. A series of granitoids from the western Central Lhasa subterrane were analyzed for whole-rock magnetic susceptibility, Fe2O3/FeO ratios, and trace elements in zircon. Compared to Late Jurassic samples (1.8 ± 2.0 × 10-4 emu g-1 oe-1, Fe3+/Fetotal = 0.32 ± 0.07, zircon Ce4+/Ce3+* = 15.0 ± 13.4), Early Cretaceous rocks show higher whole-rock magnetic susceptibility (5.8 ± 2.5 × 10-4 emu g-1 oe-1), Fe3+/Fetotal ratios (0.43 ± 0.04), and zircon Ce4+/Ce3+* values (23.9 ± 22.3). In addition, positive correlations among whole-rock magnetic susceptibility, Fe3+/Fetotal ratios, and zircon Ce4+/Ce3+* reveal a slight increase in oxidation state from fO2 = QFM to NNO in the Late Jurassic to fO2 = ˜NNO in the Early Cretaceous. Obvious linear correlation between oxidation indices (whole-rock magnetic susceptibility, zircon Ce4+/Ce3+*) and source signatures (zircon ɛHf(t), TDM C ages) indicates that the oxidation state was predominantly inherited from the source with only a minor contribution from magmatic differentiation. Thus, the sources for both the Late Jurassic and Early Cretaceous rocks were probably influenced by mantle wedge-derived magma, contributing to the increased fO2. Compared to ore-forming rocks at giant porphyry Cu deposits, the relatively low oxidation state (QFM to NNO) and negative ɛHf(t) (-16 to 0) of the studied granitoids implies relative infertility. However, this study demonstrates two potential fast and effective indices ( fO2 and ɛHf(t)) to evaluate the fertility of granitoids for porphyry-style mineralization. In an

  9. Analysis of xanthines in beverages using a fully automated SPE-SPC-DAD hyphenated system

    Energy Technology Data Exchange (ETDEWEB)

    Medvedovici, A. [Bucarest Univ., Bucarest (Romania). Faculty of Chemistry, Dept. of Analytical Chemistry; David, F.; David, V.; Sandra, P. [Research Institute of Chromatography, Kortrijk (Belgium)

    2000-08-01

    Analysis of some xanthines (caffeine, theophylline and theobromine) in beverages has been achieved by a fully automated on-line Solid Phase Extraction - Supercritical Fluid Chromatography - Diode Array Detection (Spe - Sofc - Dad). Three adsorbents have been tested for the Spe procedure: octadecyl modified silicagel (ODS) and two types of styrene-divinylbenzen copolymer based materials, from which Porapack proved to be the most suitable adsorbent. Optimisation and correlation of both Spe and Sofc operational parameters are also discussed. By this technique, caffeine was determined in ice tea and Coca-Cola in a concentration of 0.15 ppm, theobromine - 1.5 ppb, and theophylline - 0.15 ppb. [Italian] Si e' realizzata l'analis di alcune xantine (caffeina, teofillina e teobromina) mediante un sistema, in linea, completamente automatizzato basato su Estrazione in Fase Solida - Cromatografia in Fase Supercritica - Rivelazione con Diode Array (Spe - Sfc - Dad). Per la procedura Spe sono stati valutati tre substrati: silice ottadecilica (ODS) e due tipi di materiali polimerici a base stirene-divinilbenzene, di cui, quello denominato PRP-1, e' risultato essere il piu' efficiente. Sono discusse sia l'ottimizzazione che la correlazione dei parametri operazionali per la Spe e la Sfc. Con questa tecnica sono state determinate, in te' ghiacciato e Coca-Cola, la caffeina, la teobromina e la teofillina alle concentrazini di 0.15, 1.5 e 0.15 ppm.

  10. Backarc extension, detachments and granitoids in the Aegean, their relations to slab tear and asthenospheric flow

    Science.gov (United States)

    Jolivet, Laurent; Menant, Armel; Rabillard, Aurélien; Arbaret, Laurent; Augier, Romain; Gumiaux, Charles

    2013-04-01

    The Cycladic granitoids (Ikaria, Mykonos, Naxos, Kos, Lavrion, Serifos, Tinos) intruded the Aegean crust during a rather short period (17-10 Ma) compared to the much longer Oligo-Miocene crustal thinning phase (35 Ma to the Present). Their geochemical characteristics show that their sources have changed through time and space, with a progressive decreasing component of continental crust contamination with time and from east to west. They all interacted with large-scale detachments, namely the North Cycladic Detachment System (NCDS) in the north and the West Cycladic Detachment System (WCDS) in the south. In Mykonos, Naxos, Serifos and Ikaria the plutons are also associated with a high-temperature metamorphic dome of Miocene age. Their intrusion period roughly covers the same time window as the fast clockwise rotation of the western Aegean evidenced by paleomagnetic measurements and they are contemporaneous with a surge of alkaline volcanism in the eastern Aegean that can be related to a slab tear imaged below western Anatolia. The continental crust component in the Middle Miocene Cycladic plutons is not found in the early Miocene plutons of the northern Aegean, like in Kavala and Vrondou. They thus probably record a quite sudden thermal event in the Cyclades that led to the partial melting of the extending deep crust. We propose a model involving slab tear starting at ~17 Ma, fast retreat of the slab west of the tear and southwestward influx of hot asthenospheric material below the Aegean crust, leading to melting of the lower crust. Partial melting of the whole lower crust above the hot asthenospheric flow could explain the flat Moho observed below the Cyclades. The close proximity of plutons with the detachments suggests that their ascent toward the upper crust is favoured by the extreme extension at work there. The first granitoids in the region of the tear (Ikaria) are the richest in crustal component and this component decreases while the crust thins more and

  11. Primeiro consenso brasileiro do tratamento da fase aguda do acidente vascular cerebral

    Directory of Open Access Journals (Sweden)

    2001-01-01

    Full Text Available Este texto apresenta a síntese das conclusões do Iº Consenso Brasileiro do Tratamento da Fase Aguda do Acidente Vascular Cerebral (AVC. Tratou-se de reunião patrocinada e coordenada pela Sociedade Brasileira de Doenças Cerebrovasculares, com neurologistas especializados nas doenças cerebrovasculares, que analisaram os principais itens da conduta dos AVC.

  12. A cryptic Early Palaeozoic event in the Nacea Antiform? 40Ar/39Ar amphibole data in the Puente de Selce granitoid

    OpenAIRE

    Gutiérrez Alonso, Gabriel; Fernández Suárez, Javier; Ortega Rivera, M. A.; Lee, J. k. W.; Murphy, J. B.

    2005-01-01

    Las edades 40Ar/39Ar obtenidas a partir de anfíboles del granitoide Neoproterozoico de Puente de Selce, localizado en el Antiforme del Narcea junto con la existencia de fábricas de deformación relictas generadas en condiciones de media-alta temperatura en las mismas rocas puede ser interpretada como debida a un evento críptico de edad Paleozoico Inferior fuertemente retrabajado durante la deformación varisca. La naturaleza y la cinemática de este posible evento no pueden precisarse pero si se...

  13. Automatización de procesos de generación y medición de fases geométricas

    OpenAIRE

    Verástegui Salvador, Francis Luis

    2016-01-01

    Dentro de los diversos temas que investiga el grupo de óptica cuántica de la PUCP, se encuentra el estudio teórico y experimental de fases geométricas. La fase geométrica es estudiada a través de los métodos interferométrico y polarimétrico que dependen de la disposición de los componentes ópticos (placas retardadoras, polarizadores, etc.) según el arreglo experimental. Con estos componentes ópticos se logran manipular los estados de polarización de la luz. Para ello es de suma...

  14. Automatización de Proceso de Generación y Medición de Fases Geométricas.

    OpenAIRE

    Verástegui Salvador, Francis Luis

    2016-01-01

    RESUMEN Dentro de los diversos temas que investiga el grupo de óptica cuántica de la PUCP, se encuentra el estudio teórico y experimental de fases geométricas. La fase geométrica es estudiada a través de los métodos interferométrico y polarimétrico que dependen de la disposición de los componentes ópticos (placas retardadoras, polarizadores, etc.) según el arreglo experimental. Con estos componentes ópticos se logran manipular los estados de polarización de la luz. Para ello es de suma im...

  15. Uranium in accessory sphene from granitoids and its behaviour during mineral's alteration (Muzbekskij pluton at Mogol-Tau, Central Asia)

    International Nuclear Information System (INIS)

    Simonova, L.I.; Maksimova, I.G.; Nad'yarnykh, V.G.; Voronikhin, V.A.

    1982-01-01

    Uranium behaviour in accessory spbene and products of its alteration at different stages of granitoid transformation with characteristic association of zirconium-apatite-sphene and magnetite of accessory minerals, is shown. The products of sphene alteration (due to propylitization of granatoids the sphene is replaced by leucoxene) are determined by MS-46 electron probe microanalyzer and MA-1 lazer microanalyzer. Uranium distribution in leucoxene is studied by the method of fragmentary radiography. Leucoxene pseudomorphoses at a high oxygen potential are capable of giving into solution Uranium previously sorbed by leucoxene. This fact should be taken into account when determining source of metal of hydrogenous deposits

  16. FASES DE RESOLUCIÓN DE UNA SITUACIÓN-PROBLEMA UTILIZANDO ELEMENTOS DE COMPETENCIAS

    Directory of Open Access Journals (Sweden)

    Ester Ruda

    2012-01-01

    Full Text Available El objetivo de este trabajo fue analizar las fases utilizadas para resolver una situación-problema a través de elementos de competencias en el proceso de enseñanza y aprendizaje de una asignatura universitaria. Se analizan las fases a desarrollar (análisis de la situación-problema, identificación de los esquemas de actuación, selección, disposición y aplicación estratégica de los esquemas de actuación; conocimiento, dominio y transferencia de los componentes de la competencia y las evidencias de logro del dominio de los componentes de la competencia. Se aplican los conceptos a un ejemplo para una asignatura del ciclo superior de una carrera relacionada con la química y se discuten los resultados obtenidos. La resolución de una situación-problema implica que los alumnos han adquirido elementos de competencias, han sorteado distintos pasos que implican el dominio de procedimientos que aparecen en toda acción competente y han aplicado interrelacionadamente contenidos conceptuales, actitudinales y procedimentales.

  17. Barrido de frecuencia en coordenadas de fase Frequency scan on phase-coordinates

    Directory of Open Access Journals (Sweden)

    Ignacio Pérez Abril

    2012-02-01

    Full Text Available El análisis de redes eléctricas ha transitado de modelos en componentes de secuencia a modelos en coordenadas de fase. La formulación del barrido de frecuencia en coordenadas de fase, además de facilitar la modelación más precisa de las redes desequilibradas, permite especificar inyecciones armónicas de cualquier tipo: monofásicas o trifásicas de la secuencia deseada. Por lo que puede estudiarse el efecto de las cargas no lineales de acuerdo a sus características y conexión al circuito. El presente trabajo desarrolla el modelo en coordenadas de fase de una red eléctrica, considerando la representación de bancos de transformadores monofásicos de tres o dos transformadores, así como otros tipos de asimetrías que pueden encontrarse en los sistemas eléctricos de instalaciones industriales, de edificios comerciales o de servicio. El modelo desarrollado se prueba con un ejemplo sencillo de un sistema delta a cuatro hilos que permite destacar las posibilidades del modelo.The electric networks analysis has upgraded from the sequence components frame models to the phase- coordinates frame models. The formulation of the frequency scan method in a phase- coordinates frame, besides allowing for a more accurate modeling of unbalanced networks, allows the specification of harmonic injections of any type: single-phase or three-phase of the desired sequence. Therefore, it is possible to study the effect of the non-linear loads according to its features and connection to the circuit. This paper develops the phase-coordinates model of a distribution power system, considering the representation of three-phase transformer banks of three or two single-phase transformers, as well as other asymmetries that can be found in the electrical systems of industrial plants, commercial or service facilities. The frequency scan based on the presented model is tested with a simple example of a four-wire delta system that highlights the possibilities of the model

  18. Barrido de frecuencia en coordenadas de fase; Frequency scan on phase-coordinates

    Directory of Open Access Journals (Sweden)

    Ignacio Pérez Abril

    2014-04-01

    Full Text Available El análisis de redes eléctricas ha transitado de modelos en componentes de secuencia a modelos en coordenadas de fase. La formulación del barrido de frecuencia en coordenadas de fase, además de facilitar la modelación más precisa de las redes desequilibradas, permite especificar inyecciones armónicas de cualquier tipo: monofásicas o trifásicas de la secuencia deseada. Por lo que puede estudiarse el efecto de las cargas no lineales de acuerdo a sus características y conexión al circuito. El presente trabajo desarrolla el modelo en coordenadas de fase de una red eléctrica, considerando la representación de bancos de transformadores monofásicos de tres o dos transformadores, así como otros tipos de asimetrías que pueden encontrarse en los sistemas eléctricos de instalaciones industriales, de edificios comerciales o de servicio. El modelo desarrollado se prueba con un ejemplo sencillo de un sistema delta a cuatro hilos que permite destacar las posibilidades del modelo.  The electric networks analysis has upgraded from the sequence components frame models to the phase- coordinates frame models. The formulation of the frequency scan method in a phase- coordinates frame, besides allowing for a more accurate modeling of unbalanced networks, allows the specification of harmonic injections of any type: single-phase or three-phase of the desired sequence. Therefore, it is possible to study the effect of the non-linear loads according to its features and connection to the circuit. This paper develops the phase-coordinates model of a distribution power system, considering the representation of three-phase transformer banks of three or two single-phase transformers, as well as other asymmetries that can be found in the electrical systems of industrial plants, commercial or service facilities. The frequency scan based on the presented model is tested with a simple example of a four-wire delta system that highlights the possibilities of the

  19. SINTESE DA FASE SODALITA COM O USO DO CAULIM DA REGIÃO BORBOREMA-SERIDÓ (RN/PB ATIVADO TERMICAMENTE

    Directory of Open Access Journals (Sweden)

    Cássia Guerra Marques Santos

    2012-10-01

    Full Text Available A fase mineral sodalita foi obtida com sucesso a partir de reações hidrotérmicas com o uso de caulim proveniente da região Borborema-Seridó (RN/PB, hidróxido e carbonato de sódio. Desse modo, o caulim, com granulometria menor que 37 μm, foi tratado inicialmente em diferentes temperaturas. A calcinação foi realizada nas temperaturas de 500, 700 e 900°C com o objetivo de formar a metacaulinita. Os produtos calcinados foram submetidos à síntese hidrotermal por 1 e 4h, no qual foram utilizados Na2CO3 e NaOH. De acordo com os resultados, nos caulins calcinados a 700 e 900°C ocorreu a completa transição de fase da caulinita para a metacaulinita e, para a síntese no qual utilizou o caulim calcinado a 700°C ocorreu a formação da fase zeolítica sodalita básica caracterizada por difração de raios X e espectroscopia vibracional no infravermelho que mostrara picos e bandas intensas e definidas indicando maior cristalinidade do material.

  20. Fixing arsenic contained in a gas phase using solid hematite; Fijacion de arsenico en fase gas con hematita solida

    Energy Technology Data Exchange (ETDEWEB)

    Balladares, E.; Gonzalez, A.; Rarra, R.; Sanchez, M.

    2004-07-01

    Feasibility to obtain ferric arsenate starting from arsenic containing gas in contact with Fe{sub 3}O{sub 3} has been studied. Thermodynamic stability of the system Fe-As-O was analysed in order to verify conditions to form Fe{sub x}As{sub y}O{sub z} type compounds. Experiments were made using a hematite sample suspended in a thermogravimetric device. As{sub 4}O{sub 6} was generated starting from solid As{sub 2}O{sub 3} which was circulating through the iron oxide. Final samples were analysed chemically and by means of DRX, verifying the formation of FeAsO{sub 4}, FeAsO{sub 4}.2h{sub 2}O and FeAsO{sub 4}.(H{sub 2}O){sub 2} in small quantities. Tests in porous bed and pellets were carried out, studying the effect of: porosity, temperature and oxygen potential. The largest conversion obtained was 10% at 800 degree centigree, pO{sub 2}=50% and porosity=0.883. (Author) 9 refs.

  1. Obtención del punto de equilibrio de reacciones en fase gaseosa

    OpenAIRE

    Ewerts S., M.

    2009-01-01

    Castellan (Physical Chenaistry, la ed, . p 214) indica un método gráfico para hallar la coordenada de reacción a partir de los potenciales químicos Lt(T,P) para una reacción en fase gaseosa. El método, que posiblemente se presta bien al estudio de equilibrios simples, esincómodo cuando se quiere aplicar por ejemplo a la reacción.

  2. Studi Perbandingan Komposisi Asam Lemak Daging Ikan Sidat (Anguilla marmorata (Q. Gaimard Fase Yellow Eel Dari Sungai Palu Dan Danau Poso

    Directory of Open Access Journals (Sweden)

    Jamaluddin Jamaluddin

    2018-04-01

    Full Text Available Ikan sidat (Anguilla marmorata (Q. Gaimard memiliki keunggulan gizi atau nutrisi yang tinggi seperti vitamin A, vitamin B, vitamin C, vitamin D, vitamin E, protein, mineral, dan asam lemak yang baik bagi kesehatan. Penelitian ini bertujuan untuk menentukan kadar asam lemak, dan membandingkan komposisi asam lemak dari ikan sidat fase yellow eel asal sungai Palu dan danau Poso. Penelitian ini menggunakan metode kromatografi gas dengan mengubah ekstrak lemak menjadi metil ester asam lemak. Hasil analisis komposisi asam lemak daging ikan sidat (Anguilla marmorata (Q. Gaimard fase yellow eel asal sungai Palu dan Danau Poso menunjukan kadar asam lemak jenuh masing-masing 2,766g/100g dan 0,275g/100g; asam lemak tak jenuh tunggal 4,029g/100g dan 0,276g/100g; dan asam lemak tak jenuh ganda 0,541g/100g dan 0,102g/100g. Terdapat perbedaan secara statistik (p<0.05 komposisi dan kadar asam lemak antara daging ikan sidat fase yellow eel asal sungai Palu dan danau Poso. Komposisi asam lemak ikan sidat fase yellow eel asal sungai Palu dan danau Poso masing-masing adalah 23 dan 18 jenis. Asam lemak yang ditemukan pada daging ikan sidat sungai Palu dan tidak ditemukan pada ikan sidat danau Poso adalah asam heneikosenoat, asam miristoleat, Cis-10-pentadekanoat, asam gamma linoleat, dan Cis-11,14,17-eikosatrinoat.

  3. Microestrutura, fases cristalinas e propriedades elétricas de porcelanas aluminosas contendo diferentes concentrações de Fe2O3sinterizadas em atmosfera redutora e oxidante

    Directory of Open Access Journals (Sweden)

    D. H. Piva

    2015-09-01

    Full Text Available ResumoPorcelanas aluminosas contendo diferentes concentrações de Fe2O3 foram sinterizadas em atmosfera oxidante e redutora. A microestrutura e fases formadas foram investigadas com o auxílio de difração de raios X e microscopia eletrônica de varredura. Espectroscopia de impedância foi utilizada para estudar as propriedades elétricas. Os resultados indicaram que todas as amostras apresentaram mulita e coríndon como fases majoritárias e pequenas frações de quartzo. A adição de Fe2O3 provocou o surgimento de hematita nas amostras sinterizadas em atmosfera oxidante e, ferro metálico nas amostras contendo > 3%p sinterizadas em atmosfera redutora. Os espectros de impedância indicam que as características da fase vítrea e interface entre fase vítrea /fases cristalinas regem o comportamento elétrico global das amostras. Não obstante, diferentes atmosferas de queima provocam efeitos opostos na resistividade elétrica das porcelanas contendo Fe2O3. A presença de hematita foi considerada a responsável pela diminuição da resistividade elétrica nas amostras sinterizadas em atmosfera oxidante, enquanto que o aumento na resistividade elétrica das amostras sinterizadas em atmosfera redutora foi atribuído à elevada quantidade de fase vítrea e porosidade. Estes resultados indicam que atmosfera redutora durante a queima pode favorecer o uso de matérias-primas com maiores concentrações de Fe2O3, desde que todo óxido de ferro tenha se dissolvido na fase liquida durante a queima.

  4. ESTIMATIVA DA FASE DO CICLO ESTRAL POR CITOLOGIA VAGINAL EM CADELAS (Canis familiaris, LINNAEUS, 1758) DA REGIÃO DE ITUVERAVA-SP

    OpenAIRE

    Ferreira da Costa, Elaine Cristina; Fafram; Léga, Elzylene; Fafram; Neves, Letícia; Fafram

    2009-01-01

    O ciclo estral da cadela se divide em fases sucessivas e individualizadas, sendo elas: proestro, estro, metaestro e diestro, seguido de anestro. Estas fases podem ser diferenciadas por exames hormonais ou citológicos, o que permite estimar o período de fertilidade, distúrbios do ciclo estral e inatividade sexual. Desta forma, o presente trabalho teve o intuito de realizar exames citológicos vaginais em cadelas e identificar seus escores reprodutivos. Para tanto, foram realizados exames em 91 ...

  5. La deglaciación de la alta montaña. Morfología, evolución y fases morfogenéticas glaciares en el macizo del Posets (Pirineo Aragonés)

    OpenAIRE

    Serrano Cañadas, Enrique; Agudo Garrido, Carlos; González Trueba, Juan José

    2002-01-01

    RESUMEN.El Posets es un macizo de alta montaña prácticamente deglaciado, donde las formas glaciares dominan en un medio crionival actual. Mediante la elaboración de la cartografía geomorfológica, la reconstrucción de las distintas fases glaciares y la estimación de los límites de equilibrio glaciar de cada fase, se establece la evolución de la deglaciación y la transición de un medio glaciar a periglaciar. Se han detectado cinco fases morfogenéticas principales en la alta montaña, Fase I, Ple...

  6. Obtención del punto de equilibrio de reacciones en fase gaseosa

    Directory of Open Access Journals (Sweden)

    M. Ewerts S.

    2009-05-01

    Full Text Available Castellan (Physical Chenaistry, la ed, . p 214 indica un método gráfico para hallar la coordenada de reacción a partir de los potenciales químicos Lt(T,P para una reacción en fase gaseosa. El método, que posiblemente se presta bien al estudio de equilibrios simples, esincómodo cuando se quiere aplicar por ejemplo a la reacción.

  7. El retrato de fase como una herramienta de análisis del comportamiento motor

    Directory of Open Access Journals (Sweden)

    Rosa Angulo-Barroso

    2016-04-01

    Full Text Available Existe un gran número de investigaciones centradas en la adquisición y perfeccionamiento de habilidades motrices. Estas investigaciones intentan explicar cuál es la fuente y los procesos de cambio de los comportamientos motores que permiten al individuo adquirir o perfeccionar una habilidad. La ventaja de la Teoría de los Sistemas Dinámicos (TSD como marco de referencia es la inclusión de un análisis contextual en el proceso de aprendizaje. El objetivo de este artículo es dar a conocer una metodología llamada retrato de fase, la cual facilita el estudio del comportamiento motor basándose en los principios de la TSD. Datos biomecánicos tratados con una técnica de reducción adecuada constituyen una buena herramienta para describir y entender los cambios que suceden en el comportamiento motor. Los retratos de fase, mediante un gráfico (posición angular, velocidad angular, son capaces de capturar el complejo juego de fuerzas que influyen en el comportamiento motor. En este artículo, las formas de las trayectorias de los gráficos nos indicaron: (1 cómo el organismo se comporta durante la realización de las habilidades motoras analizadas mostrando sus patrones generales; (2 las singularidades poblacionales (con deficiencias y sin deficiencias o individuales; (3 los comportamientos adquiridos en el proceso de aprendizaje (novato y experto; y (4 los cambios producidos por manipulación del entorno. No obstante, los retratos de fase aunque muy útiles para resumir el comportamiento motor, no son representaciones completas del mismo y deberíamos completarlos con otras técnicas de análisis.

  8. L’anàlisi de conglomerats bietàpic o en dues fases amb SPSS

    Directory of Open Access Journals (Sweden)

    Maria-José Rubio-Hurtado

    2017-01-01

    Full Text Available El procediment d'anàlisi de conglomerats en dues fases, també anomenat bietàpic, és una eina d'exploració dissenyada per descobrir les agrupacions naturals d'un conjunt de dades. Permet la generació de criteris d'informació, freqüències dels conglomerats i estadístics descriptius per conglomerat, així com gràfics de barres, sectors i gràfics d'importància de les variables. El mètode d'anàlisi de conglomerats en dues fases té unes funcions úniques respecte a altres mètodes de conglomeració tradicionals, com són: un procediment automàtic del nombre òptim de conglomerats, la possibilitat de crear models de conglomerats amb variables tant categòriques com contínues, o la possibilitat de treballar amb arxius de dades de grans dimensions.

  9. NECESSIDADES BÁSICAS DAS ESPOSAS DE PACIENTES INFARTADOS, NA FASE AGUDA DO TRATAMENTO

    Directory of Open Access Journals (Sweden)

    Edna Ikumi Umebayashi Takahashi

    Full Text Available Trata-se de um estudo exploratório que teve por finalidade identificar as necessidades básicas das esposas de pacientes infartados, na fase aguda do tratamento. Foi utilizado como referencial para análise os conceitos de Necessidades Básicas de Maslow. Os resultados permitiram identificar como principais necessidades afetadas das esposas: segurança, amor e gregária, estima.

  10. Formación de fase sigma en uniones soldadas de acero inoxidable súper dúplex fundido

    Directory of Open Access Journals (Sweden)

    Garin, J. L.

    2011-08-01

    Full Text Available This paper decribes the microstructural characteristics of weldments of cast super duplex stainless steel (J93404, being subjected to annealing processes to induce formation of sigma-phase at high temperatures. The influence of heating time at 1073 K, 1123 K and 1173 K upon precipitation of sigma in the heat affected zone, base metal and fusion zone of the weldments was analyzed. The experimental results revealed the formation of this intermetallic compound throughout decomposition of the ferritic phase into austenite and sigma. At earlier stages of the transformation the phase rapidly nucleates and growth along the ferrite-austenite grain boundaries, and then massively advances towards the bulk of the ferritic zone with greater effectiveness as temperature increases. The formation of sigma-phase in all weldments resembles the Johnson-Mehl-Avrami’s mechanism stated for nucleation and growth.

    El presente trabajo describe las características microestructurales de uniones soldadas de acero súper dúplex fundido (J93404, al ser sometidas a procesos de recocido para inducir la formación de fase sigma a altas temperaturas. Se analizó la influencia del tiempo de calentamiento a 1.073 K, 1.123 K y 1.173 K sobre la precipitación de fase sigma en la zona afectada térmicamente, metal base y zona de fusión de los conjuntos soldados. Los resultados experimentales evidenciaron la formación de este compuesto intermetálico por descomposición de la fase ferrítica en austenita y sigma. Al comienzo de la transformación la fase nuclea y crece rápidamente en los bordes de grano austenita-ferrita, extendiéndose luego masivamente hacia el seno de la zona ferrítica, con mayor efectividad en términos del aumento de la temperatura de proceso. La formación de sigma en todas las uniones soldadas obedece a un mecanismo de nucleación y crecimiento del tipo Jonson-Mehl-Avrami.

  11. Morfogénesis de la fase sexual del helecho Arachniodes denticulata (Dryopteridaceae

    Directory of Open Access Journals (Sweden)

    Aniceto Mendoza

    1999-12-01

    Full Text Available Se describe la morfología de la espora y desarrollo de la fase sexual de Arachniodes denticulata (Sw. Ching. El material fue recolectado en los estados de Hidalgo, Oaxaca y Veracruz, México (una muestra por cada localidad. Las esporas fueron sembradas en medio de Thompson con agar (30 cajas. Sus esporas son monoletes con perina, elipsoidales, no clorofílicas. Su germinación es tipo Vittaria y su desarrollo protálico tipo Aspidium, el gametofito adulto es cordiforme-espatulado a cordiforme-reniforme; presentan tricomas marginales y superficiales, unicelulares, capitados; los rizoides no tienen cloroplastos; sus gametangios son del tipo común de los helechos leptosporangiados. Después de 200 días de haber sido sembradas las esporas, no se formaron esporofitos. Se concluye que A. denticulata comparte características comunes con A. aristata, A. assamica y con especies de los géneros Cyrtomium, Dryopteris, Polystichum, como son el tipo de germinación y desarrollo protálico, así como la presencia de tricomas unicelulares desde jóvenes protalos. Mientras que Didymochlaena truncatula difiere de las anteriores por presentar un patrón de desarrollo protálico tipo Adiantum y por la ausencia de tricomas en toda su fase sexual.Spore morphology and sexual fase development of Arachniodes denticulata (Sw. Ching are described from material collected in states of Hidalgo, Oaxaca and Veracruz, Mexico (one sample from each locality. The spores were sown in Thompson medium with agar (30 Petri dishes. The spores are monolete, with perine, ellipsoid in shape and non chlorophyllic. The germination is Vittaria-type and the prothallial development Aspidium-type; the gametophytes are cordiform-spatulate to cordiform-reniform in shape, with unicellular capitate trichome in margin and surface; rhizoids without chloroplasts; gametangia are the common type in leptosporangiate homosporous ferns. No sporophytes were observed after 200 days of culture. It is

  12. Using apatite to discriminate synchronous ore-associated and barren granitoid rocks: A case study from the Edong metallogenic district, South China

    Science.gov (United States)

    Duan, Deng-Fei; Jiang, Shao-Yong

    2018-06-01

    In order to find criteria to discriminate the synchronous ore-associated and barren granitoid rocks, we have determined apatite chemistry associated with ore-associated (Cu-Au) and barren granitoid rocks in the Edong district of the Middle and Lower Yangtze River metallogenic belt, South China. Both rock types give zircon U-Pb ages between 135.0 and 138.7 Ma. Apatite has a higher volatile and Li content (Cl: 0.19-0.57 wt%, average 0.35 wt%, SO3: 0.08-0.71 wt%, average 0.32 wt%, Li: 0.49-7.99 ppm, average 3.23 ppm) in ore-associated rocks than those in barren rocks (Cl: 0.09-0.31 wt%, average 0.16 wt%, SO3: 0.06-0.28 wt%, average 0.16 wt%, Li: 0.15-0.89 ppm, average 0.36 ppm). Apatite (La/Yb)N ratios and Eu/Eu* values are relatively high and show wider variation in ore-associated rocks than those in barren rocks. Apatite (La/Sm)N and (Yb/Sm)N show positive correlation in ore-associated rocks but negative in barren rocks. The higher volatile content occurs in ore-associated magma, favoring Cu-Au transportation and deposition. Furthermore, amphibole fractional crystallization in ore-associated magma further enriched the ore elements in the residual melt. Barren rocks may have undergone fluid exsolution before emplacement, which makes it barren in Cl, S and ore elements (Cu, S). These signatures emphases the significance of volatile and magma evolution in mineralization and indicate that analyses of magmatic apatite can serve to distinguish ore-associated from barren intrusions.

  13. Origin of the mafic microgranular enclaves (MMEs) and their host granitoids from the Tagong pluton in Songpan-Ganze terrane: An igneous response to the closure of the Paleo-Tethys ocean

    Science.gov (United States)

    Chen, Qiong; Sun, Min; Zhao, Guochun; Yang, Fengli; Long, Xiaoping; Li, Jianhua; Wang, Jun; Yu, Yang

    2017-10-01

    The Songpan-Ganze terrane is mainly composed of a Triassic sedimentary sequence and late Triassic-Jurassic igneous rocks. A large number of plutons were emplaced as a result of tectono-magmatic activity related to the late stages of Paleo-Tethys ocean closure and ensuing collision. Granitoids and their hosted mafic enclaves can provide important constraints on the crust-mantle interaction and continental crustal growth. Mesozoic magmatism of Songpan-Ganze remains enigmatic with regard to their magma generation and geodynamic evolution. The Tagong pluton (209 Ma), in the eastern part of the Songpan-Ganze terrane, consists mainly of monzogranite and granodiorite with abundant coeval mafic microgranular enclaves (MMEs) (ca. 208-209 Ma). The pluton comprises I-type granitoid that possesses intermediate to acidic compositions (SiO2 = 61.6-65.8 wt.%), high potassium (K2O = 3.2-4.1 wt.%), and high Mg# (51-54). They are also characterized by arc-type enrichment of LREEs and LILEs, depletion of HFSEs (e.g. Nb, Ta, Ti) and moderate Eu depletions (Eu/Eu* = 0.46-0.63). Their evolved zircon Hf and whole-rock Nd isotopic compositions indicate that their precursor magmas were likely generated by melting of old lower continental crust. Comparatively, the MMEs have lower SiO2 (53.4-58.2 wt.%), higher Mg# (54-67) and show covariation of major and trace elements, coupled with field and petrographic observations, such as the disequilibrium textures of plagioclase and amphibole, indicating that the MMEs and host granitoids were originated from different magma sources but underwent mafic-felsic magma mixing process. Geochemical and isotopic data further suggest that the precursor magma of the MMEs was formed in the continental arc setting, mainly derived from an ancient metasomatized lithospheric mantle wedge. The Triassic granitoids from the Songpan-Ganze terrane show remarkable temporal-spatial-petrogenetic affinities to the counterparts of subduction zones in the Yidun and Kunlun arc

  14. Geochronology Intermediary Laboratory implantation at the Rio Grande do Norte Federal University: the dating of the Serrinha Granitoid (RN) and the correlate Brasiliana extensional deformation

    International Nuclear Information System (INIS)

    Macedo, Maria Helena F.; Sa, Emanuel F. Jardim de; Souza, Zorano S.; Mendes, Franklin S.; Ramalho, Karlos A.C.

    1997-01-01

    The article describes the activities developed by the Geochronology Intermediary Laboratory at the Federal University of the Rio Grande do Norte, a Brazilian university, where there were the preoccupation of establishing strategies for a geochronological development. It relates the Rubidium-Strontium (Rb/Sr) and Samarium-Neodymium (Sm/Nd) methods, describing the analysis realized in these methodologies. Afterward, it presents the geological and petrographic situation of the Granitoide de Serrinha, located at Rio Grande do Norte State, Brazil and its geochronological data

  15. Uso da Valeriana officinalis em dietas de codornas japonesas na fase de postura

    Directory of Open Access Journals (Sweden)

    Rodrigo Antonio Gravena

    2009-06-01

    Full Text Available http://dx.doi.org/10.5007/2175-7925.2009v22n4p185 Este estudo teve como objetivo avaliar o efeito da Valeriana officinalis sobre o estresse de codornas japonesas na fase postura, analisando-se parâmetros de desempenho, comportamental e fisiolόgico. Foram utilizadas 192 aves dos 43 aos 140 dias de idade, distribuídas em blocos casualizados e submetidas a quatro níveis de valeriana (controle, 250, 500 e 750mg/Ng de ração com oito repetições e seis aves por parcela. Foram avaliados parâmetros de desempenho (conversão alimentar por dúzia de ovos, conversão alimentar por massa de ovos, consumo de ração, peso dos ovos, porcentagem de postura e viabilidade, comportamentais (tempo em imobilidade tônica, observação focal e ferimentos corporais e fisiolόgicos (níveis plasmáticos de corticosterona e relação heterόfilo:linfόcito. Os resultados obtidos na fase de postura demonstraram que a valeriana adicionada na dieta não foi capaz de reduzir o estresse das aves e não afetou o desempenho produtivo.

  16. Transformaciones de fase en aleaciones Zn-22%Al-2%Cu y Zn-22%Al-2%Cu-X (X = 1, 2 y 3%Ag envejecidas isotérmicamente

    Directory of Open Access Journals (Sweden)

    Flores-Ramos, Alfredo

    2014-12-01

    Full Text Available The study of phase transformations that take place in Zn-22%Al-2%Cu and Zn-22%Al-2%Cu-X (X = 1, 2 and 3%Ag alloys was carried out using X-Ray Diffraction (XRD and Scanning Electron Microscopy (SEM. Alloys were homogenized at 350 °C during 10 days and quenched at ~2 °C. Subsequently, samples were aged at 200 °C for different times. The initial microstructure consists in a matrix of fine equiaxial grains of α and η phases for all the alloys. Besides isolated particles of ε and Φ were observed without and with Ag addition, respectively. During the aging, the four phase reaction, α + ε→η + τ’, takes place to obtain the equilibrium η, α and τ’ phases. However, the Ag addition promotes the formation of the Φ phase, which retards or inhibits the four phase reaction. The stability of the Φ phase is obtained with 3%Ag, which could improve the dimensional stability of the alloy for future industrial applications.En el presente estudio sobre las transformaciones de fase en las aleaciones Zn-22%Al-2%Cu y Zn-22%Al-2%Cu-X (X = 1, 2 y 3%Ag se utilizó Difracción de Rayos X (DRX y Microscopía Electrónica de Barrido (MEB. Las aleaciones fueron homogeneizadas a 350 °C durante 10 días, templadas a ~2 °C y posteriormente envejecidas a 200 °C durante diferentes tiempos. Todas las aleaciones ensayadas presentaron una microestructura inicial formada por una matriz de granos finos y equiaxiales de las fases α y η. Además, para las aleaciones sin Ag se observa la presencia de partículas de la fase ε (CuZn4 y de Φ ((Ag, Cu Zn4 en las que se adicionó Ag. Durante el envejecido, ocurre la reacción de cuatro fases, α + ε→η + τ’, para obtener las fases de equilibrio η, α y τ’. Sin embargo, la adición de Ag promueve la formación de la fase Φ, la cual retarda e incluso inhibe la reacción de cuatro fases. La estabilidad de la fase Φ se obtiene con 3%Ag, lo que podría mejorar la estabilidad dimensional de la aleación para

  17. Evaluation of digesters in the Netherlands. Phase 2; Evaluatie van de vergisters in Nederland. Fase 2

    Energy Technology Data Exchange (ETDEWEB)

    Velghe, F.; Wierinck, I. [Organic Waste Systems, Gent (Belgium)

    2013-10-15

    The goal of phase 1 was mapping the digestion sector, including the current bottlenecks. All digestion plants with a grant decision by NL Agency were contacted to support this study. 79 plant operators participated to the comprehensive questionnaire. The phase 1 study relates to the year 2010 and consequently does not include new developments such as green gas. In this report (phase 2) the results of monitoring of 20 digesters for a year are presented. The focus was on cost effectiveness and optimization of the digestion process [Dutch] Een gezonde en kosteneffectieve vergistingssector is van belang voor verdere ontwikkeling van de vergistingsketen. De basis voor deze inventarisatie was een enquete (fase 1). Dat rapport baseerde zich op gegevens van installaties die in 2010 volledig in bedrijf waren. In fase 2 is een twintigtal vergisters een jaar lang gemonitord. De nadruk ligt hier op het verbeteren van de kosteneffectiviteit van het vergistingproces door procesoptimalisatie.

  18. The 226Ra isotope activities in ground water samples drawn of two wells from the Meridional Pluton, Morungaba Granitoids, eastern Sao Paulo State; Atividades do 226Ra em aguas subterraneas extraidas de dois pocos localizados no pluton meridional, granitoides de Morungaba, SP

    Energy Technology Data Exchange (ETDEWEB)

    Lucas, Fabio de Oliveira; Silva Junior, Mario Goncalves da; Bertolla, Luciana; Ribeiro, Fernando Brenha [Sao Paulo Univ., SP (Brazil). Inst. de Astronomia, Geofisica e Ciencias Atmosfericas. Dept. de Geofisica]. E-mail: brenha@iag.usp.br

    2005-07-01

    The 226Ra activities, both in solution and associated with suspended solids, were measured in ground water samples drawn from two wells drilled in a fractured granitic aquifer from the Meridional Pluton, Morungaba Granitoids, eastern Sao Paulo State. The 226Ra isotope activities were measured in a sequence of samples collected about one month apart between March, 2003 and April 2004. The 226Ra activities were measured by radon gas emanometry. The mean dissolved 226Ra activity concentration activities observed in the two wells were (44.9 {+-} 7.1) mBq/L and (51.6 {+-} 8.8) mBq/L. The 226Ra activity of the suspend solids in a liter of these waters varied between (0,6 {+-} 0,1) mBq and (13 {+-} 1) mBq, respectively. (author)

  19. TransiÃÃes de fase em monocristais de D-Metionina

    OpenAIRE

    Wanessa David Canedo Melo

    2012-01-01

    Nesse trabalho investigamos as propriedades vibracionais em monocristais D-Metionina, utilizando as espectroscopias Raman e Infravermelho. As medidas de espectroscopia Raman foram realizadas sob a variaÃÃo de pressÃo hidrostÃtica no intervalo de 0GPA atà 7GPa, mostraram duas transiÃÃes de fase, uma por volta 2.0GPa e outra em 2.5GPa, as quais foram detectadas no espectro Raman atravÃs das mudanÃas exibidas pelos picos associados principalmente Ãs vibraÃÃes atribuÃdas à carboxila (CO2-), amina...

  20. Necessidades básicas das esposas de pacientes infartados na fase aguda do tratamento

    Directory of Open Access Journals (Sweden)

    Edna Ikumi Umebayashi Takahashi

    1990-12-01

    Full Text Available Trata-se de um estudo exploratório que teve por finalidade as necessidades básicas das esposas de pacientes infartados, na fase aguda do tratamento. Foi utlizado como referencial para análise os conceitos de Nacessidades Básicas de MASLOW. Os resultados permitiram identificar como principais necessidades afetadas das esposas: segurança, amor e gregária, estima.

  1. Necessidades básicas das esposas de pacientes infartados na fase aguda do tratamento

    Directory of Open Access Journals (Sweden)

    Edna Ikumi Umebayashi Takahashi

    Full Text Available Trata-se de um estudo exploratório que teve por finalidade as necessidades básicas das esposas de pacientes infartados, na fase aguda do tratamento. Foi utlizado como referencial para análise os conceitos de Nacessidades Básicas de MASLOW. Os resultados permitiram identificar como principais necessidades afetadas das esposas: segurança, amor e gregária, estima.

  2. LA ULTIMA FASE. LA ELIMINACIÓN

    Directory of Open Access Journals (Sweden)

    Rafael Nájera Morrondo

    2013-01-01

    Full Text Available En este artículo se presentan lo que se considera la última fase de la erradicación de la poliomielitis en España, la cual llevó 25 años, duran- te el período 1963-88, a raiz del brusco descenso que produjo en la incidencia de la enfermedad la introducción de la vacuna Sabin con cepas atenuadas en el año 1963. Ello debería haber conducido a la desaparición de la enfermedad en un corto período de tiempo, aunque no fue así a causa de la disminución de la vacunación y la vigilancia epidemiológica, que no se retomaron con seriedad hasta 1976. El último caso autóctono se produjo en 1988. Tras asumir Rafael Nájera la dirección del centro Nacional de Microbiología, Virología e Inmunología Sanitarias, el primer objetivo de su equipo fue la erradicación de la poliomielitis de nuestro país, introduciendo los criterios de clasificación de la OMS y los estudios de caracterización intertípica de las cepas aisladas de virus.

  3. Conservadorismo Contábil no Reconhecimento de Ativos Intangíveis em Fase de Pesquisa e Desenvolvimento: Um Estudo em Empresas da BM&FBovespa

    Directory of Open Access Journals (Sweden)

    Ilse Maria Beuren

    2013-04-01

    Full Text Available Conservadorismo contábil pode implicar assimetrias no reconhecimento de ativos intangíveis em fase de pesquisa e desenvolvimento, desde o registro indevido até a sua não contabilização. Este estudo objetiva examinar o conservadorismo contábil no reconhecimento de ativos intangíveis em fase de pesquisa e desenvolvimento de empresas da BM&FBovespa. A pesquisa descritiva foi realizada por meio de análise documental, com abordagem quantitativa, utilizando, no cálculo do conservadorismo contábil o modelo de Ball e Shivakumar (2005 e a aplicação de regressão linear e correlação de Pearson para relações entre variáveis. A população da pesquisa compreendeu as 236 empresas listadas na BM&FBovespa, com saldo em ativos intangíveis nos anos de 2009 e 2010, e a amostra as 34 com ativos intangíveis em fase de pesquisa e desenvolvimento. Os resultados mostram que no período analisado ocorreu conservadorismo contábil nas empresas pesquisadas. Todavia, não se constatou relação positiva do conservadorismo contábil e dos ativos intangíveis em fase de pesquisa e desenvolvimento com tamanho, alavancagem, setor e nível de governança corporativa das empresas. Com a aplicação da correlação de Pearson, tal resultado foi confirmado, com exceção de 2009 nas empresas pertencentes ao setor de Construção e Transporte. Assim, conclui-se que houve conservadorismo contábil no reconhecimento de ativos intangíveis em fase de pesquisa e desenvolvimento nas empresas pesquisadas, mas não se constatou associação com as variáveis de controle.

  4. A salinomicina para o controle da eimeriose de caprinos leiteiros nas fases de cria e recria

    Directory of Open Access Journals (Sweden)

    Vieira Luiz da Silva

    2004-01-01

    Full Text Available A salinomicina foi avaliada no controle da eimeriose caprina em 27 cabritos mestiços distribuídos aleatoriamente em três tratamentos num delineamento inteiramente casualizado: T0, não medicados (grupo controle; T1 e T2, medicados com doses de 1 e 2mg de salinomicina/kg de peso vivo/dia, respectivamente. Na fase de cria, não houve diferença estatística (P>0,005 no ganho médio de peso (GP entre os três tratamentos. Na fase de recria, o grupo T0 apresentou GP significativamente inferior (P0,005. O número médio de oocistos por grama de fezes (OOPG do grupo T0, nas duas fases estudadas, foi significativamente maior (P0,005 entre si. O grupo T0 apresentou rendimento médio de carcaça (RC significativamente inferior (P0,005. O peso médio da massa corporal (MC do grupo T0 foi inferior (P0,005 do grupo T1; entre os grupos T1 e T2, não houve diferença significativa (P>0,005 no peso médio da massa corporal (MC. O uso da salinomicina nas doses de 1 e 2mg/kg, resultou em maior ganho de peso dos animais dos grupos T1 e T2 e, consequentemente, maior valor da margem bruta destes tratamentos. Os resultados obtidos mostraram que os T1 e T2 foram equivalentes para o controle da eimeriose caprina, uma vez que ambos os tratamentos apresentaram maior ganho de peso e oocistograma inferior ao grupo T0. Conclui-se que o tratamento com a salinomicina na dose de 1,0mg/kg é eficaz, desde que seja administrada a partir da segunda semana de vida.

  5. Sr and Nd isotopic compositions, age and petrogenesis of A-type granitoids of the Vernon Supersuite, New Jersey Highlands, USA

    Science.gov (United States)

    Volkert, R.A.; Feigenson, M.D.; Patino, L.C.; Delaney, J.S.; Drake, Avery A.

    2000-01-01

    Voluminous late Mesoproterozoic monzonite through granite of the Vernon Supersuite underlies an area of approximately 1300 km2 in the Highlands of northern New Jersey. The Vernon Supersuite consists of hastingsite ?? biotite-bearing granitoids of the Byram Intrusive Suite (BIS) and hedenbergite-bearing granitoids of the Lake Hopatcong Intrusive Suite (LHIS). These rocks have similar major and trace element abundances over a range of SiO2 from 58 to 75 wt.%, are metaluminous to weakly peraluminous, and have a distinctive A-type chemistry characterized by high contents of Y, Nb, Zr, LREE, and Ga/Al ratios, and low MgO, CaO, Sr and HREE. Whole-rock Rb-Sr isochrons of BIS granite yield an age of 1116 ?? 41 Ma and initial 87Sr/86Sr ratio of 0.70389, and of LHIS granite an age of 1095 ?? 9 Ma and initial 87Sr/86Sr ratio of 0.70520. Both suites have similar initial 143Nd/144Nd ratios of 0.511267 to 0.511345 (BIS) and 0.511359 to 0.511395 (LHIS). Values of ??(Nd) are moderately high and range from +1.21 to +2.74 in the BIS and +2.24 +2.95 in the LHIS. Petrographic evidence, field relationships, geochemistry, and isotopic data support an interpretation of comagmatism and the derivation of both suites from a mantle-derived or a juvenile lower crustal parent with little crustal assimilation. Both suites crystallized under overlapping conditions controlled by P-T-f(H(2)O). Lake Hopatcong magma crystallized at a liquidus temperature that approached 900??C and a pressure of about 6 kbar, and remained relatively anhydrous throughout its evolution. Initial P-T conditions of the Byram magma were ??? 850??C and about 5.5 kbar. BIS magma was emplaced contemporaneous with, or slightly preceding LHIS magma, and both magmas were emplaced during a compressional tectonic event prior to granulite facies metamorphism that occurred in the Highlands between 1080 and 1030 Ma. (C) 2000 Elsevier Science B.V. All rights reserved.

  6. PRENDIMIENTO DE DOS TIPOS DE INJERTOS EN CACAO EN DISTINTAS FASES LUNARES, SIUNA 2014

    Directory of Open Access Journals (Sweden)

    Mario Reyes Martínez

    2016-05-01

    Full Text Available Sin duda, los productores saben de la influencia lunar y sobre el movimiento de la savia en las plantas en determinados momentos, debido a los conocimientos ancestrales y experiencias adquiridas. Sin embargo, en relación al prendimiento de injertos en cacao (Theobroma cacao, existen pocos estudios científicos que demuestren tales efectos. El objetivo principal del estudio fue comparar los efectos de las fases lunares en el prendimiento de dos tipos de injertos en cacao. Para ello se utilizó un diseño completamente al azar con arreglo bifactorial, con tres repeticiones por cada una de las fases y un universo de 576 plantas. La variable de medición únicamente fue el prendimiento de las plantas que se injertaron. Los datos fueron procesados en el programa Statistical Product and Service Solutions (SPSS versión 21 y se sometieron al análisis de varianza ANDEVA con un nivel de confianza del 95%. Los análisis revelan que existen diferencias significativas para las técnicas de injertación (p=0.011<0.05 y se obtuvo mayores prendimientos en los injertos de yema sobre los de bisel. Con respecto al efecto de las fases lunares sobre los dos tipos de injertos no se encontró evidencia estadística (p=0.950>0.05. En base al análisis combinado de varianza no existen diferencias significativas para la interacción fases lunares y técnicas de injertación puesto que (p=0.761>0.05. Summary There is no doubt the producers know of the moon influence and the sap movement in plants at certain moments, due to the ancestral knowledge and experiences gained. However, in relation to the root taking of grafts in cocoa (Theobroma cacao, there are few scientific studies that demonstrate such effects. The main objective of this study was to compare the effects of moon phases in the root taking of two types of grafts in cocoa. To do this we used a complete randomized design with bifactorial order, with three replays for each of the phases and a universe of 576

  7. Mapas conceptuales como primera fase del diseño de bases de datos

    OpenAIRE

    Gómez Gauchía, Héctor

    2005-01-01

    En nuestra asignatura de Bases de Datos los alumnos no entienden el proceso de diseño de bases de datos fácilmente. Hemos descubierto que es un problema previo a donde empieza el diseño de base de datos habitual, el problema está en la fase de formación de conceptos. Nuestra propuesta consiste en incluir, en el proceso, el uso de mapas conceptuales. Y, así, representar conocimiento declarativo a un nivel muy bajo, usando conceptos relacionados con frases de enlac...

  8. Determinação direta das fases na difração de raios-X em cristais sem centro de simetria

    OpenAIRE

    Jose Antonio Prado Valladares

    1984-01-01

    Resumo: Um método experimental é proposto para solucionar o problema da fase na difração de raios-X em cristais sem centro de simetria, usando difração múltipla caso três-feixes tipo-Bragg. Este método resulta da consideração da dependência da fase com a assimetria dos perfis de linha, com o sentido da rotação da rede cristalina e com o comprimento de onda da radiação incidente. Casos em que o comprimento de onda da radiação incidente está acima e abaixo da borda de absorção, lE, do átomo mai...

  9. The study of the mineralogy and rare earth elements behavior in the hydrothermal alteration zones of the Astaneh granitoid massif (SW Arak, Markazi province, Iran)

    International Nuclear Information System (INIS)

    Esmaeily, D.; Afshooni, S. Z.; Valizadeh, M. V.

    2009-01-01

    The Astaneh granitoid massif is located about 40 km to Arak city, central Iran, is a part of Sanandaj-Sirjan structural zone. These intrusive rocks which are mainly composed of gronodioritic rocks, widely affected under hydrothermal alteration. The alteration zones, on the basis of field studies and mineralogy as well as the study of the REE behavior, are investigated in this paper. Eight alteration zones including phyllic (sericitic) with quartz, sericite and pyrite; chloritic with quartz, sericite and chlorite; propylitic with chlorite, epidot, calcite and albite; argillic with clay minerals (chlorite and illite); silicic with abundant quartz; albitic with albite, chlorite and quartz; hematitisation with hematite, Fe-carbonates (ankerite and siderite) and tourmalinisation with tourmaline (dravite) are identified. The results demonstrate notable differences in the REE behavior in the different alteration zones. Accordingly, comparison with the fresh rocks, in the phyllic (sericitic) alteration, LREE are enriched, but HREE, except Yb which enriched, unchanged. Also in chloritic alteration zone, LREEs are depleted, but HREEs represent different behaviors. In the argillic and propylitic alteration zones, all REE are depleted, but compared with HREE, the LREE represent more depletion. In the silicic and hematitisation alteration zones, compared with HREE, the LREE are enriched. Finally, in the albitic and tourmalinisation alteration zones all REE are depleted. These features indicate that the behavior of REE in the hydrothermal alteration zones of the Astaneh granitoid rocks is mainly controlled by p H, availability of complexing ions in the fluid as well as the presence of secondary phases as host REE minerals

  10. Petrology and isotope systematics of magma mushes: some porphyritic granitoids of northeastern Brazil

    International Nuclear Information System (INIS)

    McMurry, J.; Long, L.E.; Sial, A.N.

    1987-01-01

    More than 80 coarsely porphyritic granitoid plutons with K-feldspar megacrysts (Itaporanga-type granites) intrude metamorphic rocks of Northeastern Brazil. Textural evidence for filter pressing and flow foliation indicates that these bodies were emplaced as viscous, crystal-laden mushes. A representative Itaporanga-type pluton, the Monte das Gameleiras intrusion, consists of a variety of rock types with SiO 2 ranging from 49.5 to 71.6 weight percent. Chemically and petrographically, this hornblende-bearing pluton has I-type characteristics with some S-type affinities. Whole-rock oxygen isotope data are in keeping with the distribution of δO 18 , for unaltered granitic rocks. Similarly, REE data suggest a single magmatic process, at least for the more felsic rock types, without post-intrusive effects. A 5-point, whole-rock Rb-Sr isochron for the Monte das Gameleiras pluton gives t = 511 ± 26 Ma andan initial, 87 Sr/ 86 Sr = 0.7099 ± 0.0004. This is contrasted with disparate ages calculated from texturally similar bodies such as the Fazenda Nova pluton, for which a 5-point whole-rock isochron gives t = 630 ± 24 Ma with initial 87 Sr/ 86 Sr = 0.7065 ± 0.0005, and the type locality Itaporanga pluton, for which a 6-point isochron gives t= 625 ± 22 Ma. (author) [pt

  11. Mineral chemistry and geochemistry of the Late Neoproterozoic Gabal Abu Diab granitoids, Central Eastern Dessert, Egypt: Implications for the origin of rare metal post-orogenic A-type granites

    Science.gov (United States)

    Sami, Mabrouk; Ntaflos, Theodoros; Farahat, Esam S.; Ahmed, Awaad F.; Mohamed, Haroun A.

    2015-04-01

    The Neoproterozoic Gabal Abu Diab pluton is a part of the Arabian Nubian shield (ANS) continental crust and located in the Central Eastern Desert (CED) of Egypt. It constitutes multiphase granitic pluton intruded into granodiorite and metagabbro-diorite rocks with sharp and nonreactive contacts. Based on field observations, colors, structural variations and petrographic investigations, this granitic outcrop consists of an inner core of two-mica granite (TMG) followed outward by garnet bearing muscovite granite (GBMG) and albite granite (AG). Petrographical study indicated that medium to coarse-grained TMG is dominated by K-feldspar (Or88-98), quartz, plagioclase (albite, An0-7), muscovite and biotite with hypidiomorphic texture. With exception the appearance of garnet and the disappearance of biotite the GBMG resembles the TGM, while AG is leucocratic without any mafic mineral. The main accessories are zircon, Nb and Ta-bearing rutile, columbite, ilmenorutile, ilmenite, magnetite and apatite. This mineralogical similarity and the existence of columbite group minerals (CGM) in all granitoids, indicates a cogenetic relationship. Microprobe analyses reveal that, besides the CGM, rutile and ilmenite are the main repository phases for Nb-Ta-Ti. Columbite-(Mn) exists as individual subhedral crystals (up to 100μm in size) or intimate intergrowth with Nb-bearing rutile and/or ilmenite. The CGM are represented mostly by columbite-(Mn) with Ta/(Ta+Nb) and Mn/(Mn+Fe) ratio ranging from 0.02-0.08 and 0.4-0.9, respectively suggesting extreme degree of magmatic fractionation. Rutile contains significant amounts of Ta (up to 4 wt.% Ta2O5) and Nb (up to 22 wt.% Nb2O5). Biotites are phlogopite-annite in composition (Ann47-60Phlog40-53,on average) and are enriched with AlIV that characterize peraluminous granites. Garnets contain 60-69 mol.% spessartine and 28-36 mol.% almandine where, the ratio of spessartine and almandine together exceeds 95 mole percent, similar to garnet occur

  12. Addition of amines to naphthoquinone in water and solid phase; Adicao de anilinas a naftoquinona em agua e em fase solida

    Energy Technology Data Exchange (ETDEWEB)

    Martinez, Sabrina T.; Silva, Barbara V.; Pinto, Angelo C., E-mail: sabrinatmartinez@yahoo.com.br [Instituto de Quimica, Universidade Federal do Rio de Janeiro, RJ (Brazil); Ferreira, Vitor F.; Silva, Fernando de Carvalho da [Instituto de Quimica, Universidade Federal Fluminense, Niteroi - RJ (Brazil)

    2012-07-01

    Considering all the aspects of the principles of green chemistry, we present herein the addition reactions of amines to 1,4-naphthoquinone in water as solvent and also in solid phase. These reactions resulted in very colorful products that were easily monitored by thin layer chromatography and consequently easy to separate. Therefore, they are interesting experiments for experimental organic chemistry in the classrooms or in the laboratories. (author)

  13. Identificação das fases do processo de morrer pelos profissionais de Enfermagem La identificación de las fases del proceso de muerte para los profesionales de Enfermería Identification of the dying process phases by Nursing professionals

    Directory of Open Access Journals (Sweden)

    Tatiana Thaller Susaki

    2006-06-01

    Full Text Available OBJETIVO: verificar se o enfermeiro consegue identificar as cinco fases do processo de morrer, descritas por Elizabeth Kübler-Ross, nos pacientes sob seus cuidados e que se encontram fora de possibilidades terapêuticas. MÉTODOS: foi questionado se percebem os sinais da comunicação não-verbal para prestar esse atendimento e fazer essa identificação. Os dados foram coletados em janeiro de 2004 por meio de entrevista individual, pré-agendada, com enfermeiros, em hospital público vinculado ao ensino na cidade de São Paulo. RESULTADOS: constatamos que 92% dos enfermeiros conseguiram identificar pelo menos uma das fases do processo de morrer na vivência com pacientes terminais, sendo citadas, em média, três. A aceitação (85%, a negação (69% e a depressão (61% são as mais freqüentemente percebidas. Verificamos o uso e entendimento da comunicação não-verbal na identificação das fases nas falas de 54% dos enfermeiros. CONCLUSÃO: os resultados também evidenciaram as dificuldades enfrentadas pelo enfermeiro quanto essa temática e, percebe-se que existe uma lacuna evidente entre a formação do profissional e a manutenção do seu treinamento e suporte na instituição de saúde.OBJETIVO: verificar a la enfermera consigue identificar las cinco fases del proceso de muerte, descrito por Elizabeth Kübler-Ross, en los pacientes bajo sus cuidados y esa reunión fuera de posibilidades terapéuticas. METODOS: fue cuestionado si nota las señales de la comunicación no-verbal para dar esa asistencia y hacer esa identificación. Los datos eran reunido en enero de 2004 por medio de la entrevista individual, pré-agendada, con enfermeras, en hospital público se unido a la enseñanza en la ciudad de São Paulo. RESULTADOS: verificamos que 92% de las enfermeras consiguieron identificar uno de las fases del proceso de muerte en la existencia con términos de los pacientes por lo menos, mencionándose, en promedio, tres. La aceptación (85

  14. A Proposed Activity for a Meaningful Learning about the Moon Phases. (Breton Title: Uma Proposta de Atividade Para a Aprendizagem Significativa sobre as Fases da Lua.) Una Actividad Propuesta Para EL Aprendizaje Significativo Acerca de Las Fases de la Luna

    Science.gov (United States)

    Martins, Bruno Andrade; Langhi, Rodolfo

    2012-12-01

    This paper presents one of the concepts of Astronomy and its consequent failure in teaching this topic in high school, even when the official documents point out the necessity of Astronomy teaching at this school level. Among the spontaneous conceptions in Astronomy that high school students carry with them, even after the end of the school, we emphasized in this research the Moon phases. The development of different strategies in relation to traditional methods, aimed to teaching-learning process on this topic was considered in this study. These strategies were devised based on the reference frame of the Meaningful Learning, as elaborated by Ausubel. The proposals presented here include the active participation of students in experimental activities and other didactic activities, for their continuous evaluation during the process. These activities finished with a Comics elaboration about the Moon phases. Therefore, the objective of this paper is to present a proposal for differentiated teaching activity about Moon phases supported by the theoretical principles of Meaningful Learning at Physics classes. Este texto foca um dos conteúdos de Astronomia e a consequente falha no ensino deste tema no ensino médio, apesar de os documentos oficiais apresentarem a necessidade de se trabalhar a Astronomia neste nível de ensino. Dentre as concepções alternativas em Astronomia que os alunos do ensino médio carregam consigo, mesmo após o término dos estudos, destacamos, nesta pesquisa, o fenômeno das fases da Lua. O desenvolvimento de estratégias diferenciadas em relação ao ensino tradicional, visando o processo de ensino-aprendizagem sobre este tema, foi contemplado neste trabalho como um dos resultados obtidos sob a luz dos referenciais da aprendizagem significativa, fundamentados em Ausubel. Segundo a proposta aqui apresentada, a participação ativa dos alunos na execução de uma atividade experimental e outras atividades didáticas, que visam sua cont

  15. Comparative study of 3D TOF-SPGR and 3D FASE on the display of the relationship between cranial nerves and peripheral vessels

    International Nuclear Information System (INIS)

    Sun Wenge; Li Yanliang; Zhang Lina; Qi Xixun; Jin Anyu; Xu Ke; Tong Zhiyong; Liu Jing

    2004-01-01

    Objective: To select a better sequence which can supply reliable radiological information for vessel compression on cranial nerves in patients with facial spasm or trigeminal neuralgia. Methods: 3D TOF-SPGR and 3D FASE were used in 40 patients with facial spasm or trigeminal neuralgia to display the relationship between cranial nerves (facial nerve and trigeminal nerve) and peripheral vessels. Results: 38 patients got surgical results. 33 unilateral vessel compression or contact on facial nerves or trigeminal nerves was found on 3D TOF-SPGR, while no contact was found in 5. 26 unilateral vessel compression or contact on facial nerves or trigeminal nerves was found on 3D FASE, while no contact was found in 12. Significant difference between the two sequences on the display of vessel compression on facial nerves or trigeminal nerves was found by statistical analysis (χ 2 =5.14, P=0.016). Conclusion: 3D TOF-SPGR is better than 3D FASE on display of the relationship between nerves and peripheral vessels, and it should be the primary MRI sequence for patients with facial spasm or trigeminal neuralgia clinically. (author)

  16. Manejo de desechos peligrosos (II fase

    Directory of Open Access Journals (Sweden)

    Juan Carlos Salas Jiménez

    2006-05-01

    Full Text Available Este trabajo corresponde a la segunda fase del proyecto de Manejo de Desechos Peligrosos que se generan en los laboratorios del Instituto Tecnológico de Costa Rica (ITCR, el cual continuó con las etapas de implementación de un sistema de gestión de manejo de desechos en los laboratorios de docencia e investigación del ITCR. Las actividades que se desarrollaron fueron: capacitación e implementación de algunas etapas del sistema de gestión, cuantificación y caracterización de los desechos, desarrollo de un programa para el control de inventarios y pruebas de laboratorio para el tratamiento de los desechos peligrosos de mayor volumen. De esta investigación, se obtuvieron los siguientes resultados: 1.Se cuenta con un grupo de funcionarios comprometidos y capacitados para implementar el sistema de gestión. 2. Tres métodos efectivos para los tres desechos que se generan en gran cantidad de masa o volumen. 3. Un sistema de inventarios estandarizados que ha sido instalado en nueve laboratorios de la Sede de Cartago. 4.Una “Guía de manejo de los desechos peligrosos de los laboratorios del ITCR”, que sirva de documento base para los funcionarios de los laboratorios. 5. Una normativa en trámite de aprobación para institucionalizar el Programa de Manejo de desechos peligrosos.

  17. Pengoperasian Beban Listrik Fase Tunggal Terkendali Melalui Minimum System Berbasis Mikrokontroler Dan Sensor Voice Recognition (Vr)

    OpenAIRE

    Goeritno, Arief; Ginting, Sandy Ferdiansyah; Yatim, Rakhmad

    2017-01-01

    Minimum system berbasis mikrokontroler dan sensor voice recognition (VR) sebagai pengendali aktuator telah digunakan untuk pengoperasian beban listrik fase tunggal. Minimum system adalah suatu sistem yang tersusun melalui 2 (dua) tahapan, yaitu (a) diagram rangkaian dan bentuk fisis board dan (b) pengawatan terintegrasi terhadap minimum system pada sistem mikrokontroler ATmega16. Keberadaan sistem mikrokontroler pada minimum system perlu program tertanam melalui pemrograman berbasis bahasa ...

  18. Viscoelasticidad lineal de la fase líquido-cristalina laminar de un sistema tensioactivo no iónico/hidrocarburo/agua

    Directory of Open Access Journals (Sweden)

    Gallegos, C.

    2000-08-01

    Full Text Available A linear viscoelastic characterization by small amplitude oscillatory shear tests was carried out for heptane/polyoxyethylene glycol nonylphenyl ether (EOa=10/water system exhibiting a lamellar liquid crystalline structure. The influence of composition on the dynamic functions was considered. The lamellar liquid crystalline phase shows a small linear viscoelastic range. The relaxation spectrum of the lamellar liquid crystalline phase presents two regions: the transition region and the plateau region, characteristic of highly structured systems. The maximum values of the plateau modulus correspond to the systems of intermediate compositions within the realm of existence of the lamellar mesophase.En este estudio se ha caracterizado la respuesta viscoelástica lineal, en cizalla oscilatoria, de la fase líquido-cristalina laminar de sistemas alcohol polietoxilado/heptano/agua, estableciendo las influencias de los distintos componentes en la evolución de las funciones viscoelásticas dinámicas. De los resultados obtenidos puede concluirse que la fase líquido-cristalina laminar se caracteriza por presentar un pequeño intervalo viscoelástico lineal; su espectro de relajación muestra, fundamentalmente, dos regiones, la región de transición y la región plateau, siendo esta última característica de sistemas altamente estructurados; el módulo plateau presenta valores máximos para sistemas con concentraciones intermedias de tensioactivo y heptano dentro del intervalo de existencia de la fase laminar.

  19. Programa de mentoria online para professores iniciantes: fases de um processo On-line mentoring program for novice teachers: phases of a process

    Directory of Open Access Journals (Sweden)

    Aline M. de M. R. Reali

    2010-08-01

    Full Text Available Neste artigo analisamos as fases evidenciadas no desenvolvimento do Programa de Mentoria do Portal dos Professores da Universidade Federal de São Carlos (SP. O programa se caracteriza por ser online e é dirigido para professores dos anos iniciais do ensino fundamental com até cinco anos de experiência. Foi conduzido por três pesquisadoras e onze mentoras (professoras experientes que acompanharam individualmente, a distância e por meio de correspondências eletrônicas, 56 professoras iniciantes durante períodos entre seis meses a dois anos e meio. Do ponto de vista teórico consideramos a literatura relativa à aprendizagem e desenvolvimento profissional da docência; início da carreira docente; processos de mentoria e educação a distância. Metodologicamente desenvolvemos uma pesquisa-ação a partir de estratégias construtivo-colaborativas. As principais fontes de dados foram as correspondências trocadas entre mentoras e professoras iniciantes; diários reflexivos de mentoras e professoras iniciantes; redação de casos de ensino pelas professoras iniciantes; registros de observação das reuniões semanais ocorridos entre pesquisadoras e mentoras. Os resultados apontam que os processos de mentoria investigados ocorrem segundo fases distintas (fase inicial ou de aproximação; fase de desenvolvimento ou aprofundamento; fase de desligamento com características, objetivos e procedimentos próprios.This article analyzes the development phases of the On-line Mentoring Program at the Teachers Portal of Universidade Federal de São Carlos. The mentoring program is an on-line program aimed at elementary school teachers at the first grades with up to five years of experience. It is carried out by ten mentors coaching by electronic 56 novice teachers during six to 28 months. Its theoretical framework includes literature on teacher learning and professional development, the first years of teaching, mentoring processes and distance education

  20. Late Paleozoic-Early Mesozoic tectonic evolution of the Paleo-Asian Ocean: geochronological and geochemical evidence from granitoids in the northern margin of Alxa, Western China

    Science.gov (United States)

    Sha, Xin; Wang, Jinrong; Chen, Wanfeng; Liu, Zheng; Zhai, Xinwei; Ma, Jinlong; Wang, Shuhua

    2018-03-01

    The Paleo-Asian Ocean (Southern Mongolian Ocean) ophiolitic belts and massive granitoids are exposed in the Alxa block, in response to oceanic subduction processes. In this work, we report petrographic, geochemical, and zircon U-Pb age data of some granitoid intrusions from the northern Alxa. Zircon U-Pb dating for the quartz diorite, tonalite, monzogranite, and biotite granite yielded weighted mean 206Pb/238U ages of 302±9.2 Ma, 246.5±4.6 Ma, 235±4.4 Ma, and 229.5±5.6 Ma, respectively. The quartz diorites ( 302 Ma) exhibit geochemical similarities to adakites, likely derived from partial melting of the initially subducted Chaganchulu back-arc oceanic slab. The tonalites ( 246.5 Ma) display geochemical affinities of I-type granites. They were probably derived by fractional crystallization of the modified lithospheric mantle-derived basaltic magmas in a volcanic arc setting. The monzogranites ( 235 Ma) are characterized by low Al2O3, but high Y and Yb with notably negative Eu anomalies. In contrast, the biotite granites ( 229.5 Ma) show high Al2O3 but low Y and Yb with steep HREE patterns and the absence of negative Eu anomalies. Elemental data suggested that the biotite granites were likely derived from a thickened lower crust, but the monzogranites originated from a thin crust. Our data suggested that the initial subduction of the Chaganchulu oceanic slab towards the Alxa block occurred at 302 Ma. This subduction process continued to the Early Triassic ( 246 Ma) and the basin was finally closed before the Middle Triassic ( 235 Ma). Subsequently, the break-off of the subducted slab triggered asthenosphere upwelling (240-230 Ma).

  1. Een analyse van de mogelijke gevolgen van de aanleg van IJburg tweede fase voor watervogels in de SBZ IJmeer

    NARCIS (Netherlands)

    Schekkerman, H.; Eerden, van M.E.; Rijn, van S.; Roos, M.

    2006-01-01

    De gemeente Amsterdam heeft vergevorderde plannen om in het IJmeer, grenzend aan het Vogelrichtlijngebied (SBZ, Natura 2000 gebied) IJmeer, de tweede fase van de wijk IJburg te realiseren. In dit rapport wordt (1) beschreven welke specifieke waarden van het IJmeer volgens de Vogelrichtlijn dienen te

  2. Petrography and geochronology (U/Pb-Sm/Nd) the Passagem Granite, Pensamiento Granitoid Complex, Paragua Terrane, SW Amazon Craton, Mato Grosso, Brazil; Petrologia e geocronologia (U/Pb-Sm/Nd) do Granito Passagem, Complexo Granitoide Pensamiento, SW do Craton Amazonico (MT)

    Energy Technology Data Exchange (ETDEWEB)

    Jesus, Gisely Carmo de, E-mail: giselycarmo@hotmail.co [Universidade Federal de Mato Grosso (ICET/UFMT), Cuiaba, MT (Brazil). Inst. de Ciencias Exatas e da Terra. Programa de Pos-Graduacao em Geociencias; Sousa, Maria Zelia Aguiar de, E-mail: mzaguiar@terra.com.b [Universidade Federal de Mato Grosso(ICET/UFMT), Cuiaba, MT (Brazil). Inst. de Ciencias Exatas e da Terra. Dept. de Recursos Minerais; Ruiz, Amarildo Salina; Matos, Joao Batista de, E-mail: asruiz@gmail.co, E-mail: jmatos@cpd.ufmt.b [Universidade Federal de Mato Grosso (ICET/UFMT), Cuiaba, MT (Brazil). Inst. de Ciencias Exatas e da Terra. Dept. de Geologia Geral

    2010-09-15

    The Passagem granite includes stocks, plugs and dikes located in the Ricardo Franco hill - Vila Bela da Santissima Trindade region - state of Mato Grosso, central Brazil. The Passagem Granite is included in the Paragua terrane - SW Amazonian Craton. It consists of isotropic monzogranite, sienogranite and more rarely granodiorites with leucocratic dark gray to white color. These rocks range from hypidomorphic inequigranular to xenomorphic texture, fine to medium grained. Biotite is the only primary mafic present as essential phase and characterize an expanded slightly acid sequence formed by a sub-alkaline magmatism of high-potassium calc-alkaline, slightly peraluminous composition from arc magmatic tectonic environment during a post-collisional period. Mechanism of fractional crystallization of plagioclase, biotite, titanite, apatite and zircon associated with simultaneous crustal assimilation are suggested for the evolution of these rocks. The results support the hypothesis of a post-collisional magmatism in the Paragua terrane at 1284 +- 20 Ma corresponding to the crystallization age of the Passagem granite. This paper propose that Passagem Granite represents as an extension in Brazilian terrane of the Pensamiento Granitoid Complex. (author)

  3. Distribución de potencia en los alimentadores de baja tensión con varios conductores por fase; Power Distribution in Low Tension Feeders with Several Phase Conductors

    Directory of Open Access Journals (Sweden)

    Héctor S Llamo Laborí

    2011-02-01

    Full Text Available En las redes de distribución a 120/208 V, las corrientes debidas a las cargas son muy altas y ello obliga ainstalar varios conductores en paralelo por fase. La mayor o menor asimetría de las corrientes que circulan porcada uno de los conductores que forman cada fase no son función del balanceo que se haga de la carga ni delmayor o menor desbalance de las tensiones sino de la disposición de las fases. En este trabajo se presentanlas características y los resultados de un algoritmo para determinar cuál es la disposición de las fases quepermiten obtener el mejor aprovechamiento de la capacidad instalada en los conductores del alimentador. In the 120/208 distribution grids, the loads currents are very high. In this case it is necessary to install severalconductors in parallel. The more o less asymmetry of currents in the different conductors that form everyphase is function of the phase disposition and not of the more or less unbalance of the tension or the loadscurrents. In this work are presented the characteristics and the results of algorithms that permit to determinewhich the phase disposition is that bring the better use of the installed capacity of the feeder.

  4. Semi-brittle flow of granitoid fault rocks in experiments

    Science.gov (United States)

    Pec, Matej; Stünitz, Holger; Heilbronner, Renée.; Drury, Martyn

    2016-03-01

    Field studies and seismic data show that semi-brittle flow of fault rocks probably is the dominant deformation mechanism at the base of the seismogenic zone at the so-called frictional-viscous transition. To understand the physical and chemical processes accommodating semi-brittle flow, we have performed an experimental study on synthetic granitoid fault rocks exploring a broad parameter space (temperature, T = 300, 400, 500, and 600°C, confining pressure, Pc ≈ 300, 500, 1000, and 1500 MPa, shear strain rate, γṡ ≈ 10-3, 10-4, 10-5, and 10-6 s-1, to finite shear strains, γ = 0-5). The experiments have been carried out using a granular material with grain size smaller than 200 µm with a little H2O added (0.2 wt %). Only two experiments (performed at the fastest strain rates and lowest temperatures) have failed abruptly right after reaching peak strength (τ ~ 1400 MPa). All other samples reach high shear stresses (τ ~ 570-1600 MPa) then weaken slightly (by Δτ ~ 10-190 MPa) and continue to deform at a more or less steady state stress level. Clear temperature dependence and a weak strain rate dependence of the peak as well as steady state stress levels are observed. In order to express this relationship, the strain rate-stress sensitivity has been fit with a stress exponent, assuming γ˙ ∝ τn and yields high stress exponents (n ≈ 10-140), which decrease with increasing temperature. The microstructures show widespread comminution, strain partitioning, and localization into slip zones. The slip zones contain at first nanocrystalline and partly amorphous material. Later, during continued deformation, fully amorphous material develops in some of the slip zones. Despite the mechanical steady state conditions, the fabrics in the slip zones and outside continue to evolve and do not reach a steady state microstructure below γ = 5. Within the slip zones, the fault rock material progressively transforms from a crystalline solid to an amorphous material. We

  5. Estudo longitudinal do eletrocardiograma na doença de Chagas desde a fase aguda

    Directory of Open Access Journals (Sweden)

    Roberto C. Pedrosa

    1993-09-01

    Full Text Available Vários trabalhos com eletrocardiograma na doença de Chagas têm sido feitos. Alguns referindo-se a grupos selecionados de casos, outros a estudos longitudinais, relatam as características da mortalidade nas diversas fases da doença. Com o objetivo de avaliar o valor do eletrocardiograma como índice de avaliação terapêutica e de seu comportamento na doença de Chagas desde a fase aguda, no presente trabalho, analisou-se evolutivamente o eletrocardiograma de 42 pacientes (18 mulheres e 24 homens procedentes da zona rural do Norte de Minas Gerais; predomínio etário foi nas duas primeiras décadas; todos com comprometimento cardíaco; todos receberam tratamento específico. O acompanhamento dos 42 pacientes foi de 9 anos dos quais 3 pacientes tiveram seguimento de 20 anos. Foram analisados 270 eletrocardiogramas. Nós utilizamos os seguintes critérios para a análise do ECG: código de Minnesota modificado para doença de Chagas; WHO/I. S. F. C. TASK FORCE para condução intraventricular e critérios de Pieretti para área eletricamente inativa. Concluímos que as alterações eletrocardiográficas agravam com a evolução da doença e que o eletrocardiograma não serve de índice de avaliação terapêutica.

  6. Efectos diferenciales del bienestar subjetivo, autorrealización y celos en las fases del amor pasional

    OpenAIRE

    Rozzana Sánchez Aragón

    2009-01-01

    El presente estudio exploró en 348 hombres y mujeres de dos ciudades de la República Mexicana las diferencias en la autorrealización, el bienestar subjetivo y los celos en las cuatro fases del amor pasional: atracción, enamoramiento, amor obsesivo y amor desesperado. Los resultados indican los efectos diferenciales por sexo, ciudad de procedencia y etapas de la pasión en dichas áreas.

  7. [La combinazione di gemcitabina e oxaliplatino (GEMOX) nel trattamento del carcinoma pancreatico in fase avanzata di malattia: le notizie sulla mia morte sono state esagerate?

    Science.gov (United States)

    Giuliani, Jacopo; Bonetti, Andrea

    2017-12-01

    Riassunto. L'analisi è stata condotta al fine di valutare l'effetto sia sulla sopravvivenza globale (OS) sia sulla sopravvivenza libera da progressione di malattia (PFS) della chemioterapia di combinazione in prima linea per il carcinoma pancreatico in fase avanzata di malattia. La presente analisi è limitata agli studi randomizzati controllati (RCT) di fase III. Successivamente è stata applicata la European Society for Medical Oncology Magnitude of Clinical Benefit Scale (ESMO-MCBS) agli RCT di fase III analizzati per ricavare uno score relativo all'entità del beneficio clinico ottenuto per ciascun RCT. Sono state calcolate inoltre le differenze in termini di PFS tra i diversi bracci di trattamento rapportandole con i costi dei farmaci necessari per ottenere il beneficio di PFS. La nostra analisi ha valutato 11 RCT di fase III, per un totale di 4572 pazienti. Combinando i costi della terapia con la misura dell'efficacia espressa dalla PFS, è stato ottenuto un costo di 74,12 euro (€) per mese di vita guadagnato in termini di PFS con la combinazione di 5-fluorouracil, leucovorin, irinotecan e oxaliplatino (FOLFIRINOX), 90,14 € per la combinazione di gemcitabina e oxaliplatino (GEMOX) e 4708,7 € per la combinazione di nab-paclitaxel e gemcitabina. Da questo punto di vista riteniamo che l'utilizzo delle "vecche chemioterapie di combinazione" (per es., GEMOX) non dovrebbe essere completamente abbandonato, ma valutato sul singolo paziente, sulla base di diversi fattori (età, ECOG PS, comorbilità, carico di malattia), al fine di ottenere una reale "tailored therapy".

  8. Efeito da relação das fases líquida e sólida da uva na composição química e na característica sensorial do vinho Cabernet

    Directory of Open Access Journals (Sweden)

    RIZZON Luiz Antenor

    1999-01-01

    Full Text Available A intensidade de cor, os polifenóis totais, o extrato seco e os minerais do vinho variam em função da proporção entre as fases líquida e sólida da uva. O rendimento em mosto é variável de uma cultivar a outra e, para a mesma cultivar, sendo que aumentos importantes podem ocorrer em conseqüência de precipitações pluviométricas durante a maturação da uva. Com o objetivo de estudar o efeito da relação das fases líquida e sólida da uva na composição química e na qualidade do vinho, foram realizados estudos através de microvinificação com uvas Cabernet Franc nas safras de 1987 a 1990. Os tratamentos consistiram em variar a fase líquida em relação à fase sólida da uva, nas proporções (% de 78/22, 74/26, 72/28, 70/30, 68/32, 66/34 e 62/38. O aumento da proporção da fase sólida em relação à líquida foi responsável principalmente por um acréscimo dos componentes que constituem o corpo do vinho (extrato seco, cinzas e compostos fenólicos enquanto que o aumento da fase líquida contribuiu para a obtenção de vinhos mais leves.

  9. Natural radioactivity (226Ra, 232Th and 40K) and assessment of radiological hazards in the Kestanbol granitoid, Turkey.

    Science.gov (United States)

    Canbaz, Buket; Cam, N Füsun; Yaprak, Günseli; Candan, Osman

    2010-09-01

    The surveys of natural gamma-emitting radionuclides in rocks and soils from the Ezine plutonic area were conducted during 2007. Direct dose measurement using a survey meter was carried out simultaneously. The present study, which is part of the survey, analysed the activity concentrations of (238)U, (232)Th and (40)K in granitoid samples from all over the region by HPGe gamma spectrometry. The activity concentrations of (226)Ra ranged from 94 to 637 Bq kg(-1), those of (232)Th ranged from 120 to 601 Bq kg(-1)and those of (40)K ranged from 1074 to 1527 Bq kg(-1) in the analysed rock samples from different parts of the pluton. To evaluate the radiological hazard of the natural radioactivity in the samples, the absorbed dose rate (D), the annual effective dose rate, the radium equivalent activity (Ra(eq)) and the external (H(ex)) hazard index were calculated according to the UNSCEAR 2000 report. The thorium-to-uranium concentration ratios were also estimated.

  10. Alterações de estados de ânimo presentes em atletas de voleibol, avaliados em fases do campeonato Alteraciones de estados de ánimo presentes en atletas de voleibol, evaluados en fases de campeonato Volleyball athletes’ mood changes in different competition phases

    Directory of Open Access Journals (Sweden)

    José Lino Oliveira Bueno

    2007-04-01

    Full Text Available O objetivo desta pesquisa foi avaliar as alterações de estados de ânimo em atletas de voleibol em função do sexo dos participantes e das fases da competição. Treze atletas do grupo feminino e 11 do grupo masculino preencheram a Lista de Estados de Ânimo Presentes, nos jogos da semifinal e final do campeonato. Os resultados descrevem um perfil comum para os dois grupos, independentemente da fase do campeonato, entretanto, o gênero feminino mostrou uma maior percepção em avaliar os estados de ânimo e um maior número de locuções. As locuções que apresentaram diferenças significativas no fator jogo mostram que a importância do jogo e a incerteza do resultado podem alterar estados de ânimo do atleta.El objetivo de esta investigación fue el de evaluar las alteraciones de estados de ánimo en atletas de voleibol, en función del género de los participantes y de las fases de la competición. Trece atletas del grupo femenino y once del grupo masculino rellenaron la Lista de Estados de Ánimo Presentes, en los juegos de la semifinal y final del campeonato. Los resultados describen un perfil común para los dos grupos, independientemente de la fase del campeonato; sin embargo, el género femenino mostró una mayor percepción al evaluar los estados de ánimo y un mayor número de locuciones. Las locuciones que presentaron diferencias significativas, en lo que respecta al factor juego, muestran que la importancia del juego y la incertidumbre del resultado pueden alterar estados de ánimo del atleta.Mood alterations in volleyball athletes with regard to the gender of participants and to different competition phases are provided. Thirteen female and eleven male athletes at a competition semifinals and finals accepted to fill the Present Mood States list. Results show that, regardless of the competition phase, a common outline for both groups is extant. Female athletes demonstrated a greater perception in evaluating mood states and used a

  11. Comparación de dos metodologías para la determinación de residuos de plaguicidas en agua potable

    Directory of Open Access Journals (Sweden)

    Jairo Arturo Guerrero Dallos

    2014-01-01

    Full Text Available Se realizó un estudio comparativo de dos metodologías para la determinación de residuos de plaguicidas en agua potable con el fin de establecer cuál de ellas es más adecuada como metodología de análisis. Las metodologías evaluadas involucraron extracción en fase sólida empleando el adsorbente polimérico LiChrolut®EN y extracción líquido-líquido utilizando n-hexano como solvente de extracción. La determinación se realizó por cromatografía de gases con detectores μ-ECD y NPD. El estudio involucró 50 plaguicidas, entre los que se encuentran diferentes familias químicas, tales como organofosforados, organoclorados y piretroides entre otros. Para comparar las metodologías, se evaluó la capacidad de detección y cuantificación estableciendo los límites de detección y cuantificación; la exactitud con experimentos de recuperación y la dispersión por medio de la precisión. Se estableció que estas presentan detección adecuada frente a las concentraciones máximas permitidas por la normativa colombiana, excepto para el insecticida monocrotofos, para el cual se obtuvo un límite de detección superior al exigido. Los experimentos de recuperación mostraron que la totalidad de plaguicidas organoclorados y piretroides pueden ser analizados empleando extracción líquido-líquido, mientras que la extracción en fase sólida es más adecuada para los plaguicidas más polares, tales como los organofosforados y azoles. Se determinó que 22 compuestos se pueden analizar por cualquiera de las dos metodologías, que por extracción en fase solida es posible analizar 36 de los 50 compuestos evaluados mientras que empleando extracción líquido-líquido se pueden analizar 28 de ellos.

  12. Crustal basement controls granitoid magmatism, and implications for generation of continental crust in subduction zones: A Sr-Nd-Hf-O isotopic study from the Paleozoic Tongbai orogen, central China

    Science.gov (United States)

    Wang, Hao; Wu, Yuan-Bao; Yang, Jin-Hui; Qin, Zheng-Wei; Duan, Rui-Chun; Zhou, Lian; Yang, Sai-Hong

    2017-06-01

    Ascertaining the petrogenesis of granitoid rocks in subduction zones holds the key for understanding the processes of how continental crust is produced. The synchronous Taoyuan and Huanggang plutons occur in two different geological units of the Paleozoic Tongbai orogen of central China. They provide an optimal opportunity for a study to address the role of the crustal basement in generating voluminous granitoid magmatism in subduction zones. The Taoyuan and Huanggang plutons have identical U-Pb zircon crystallization ages of 440-444 Ma, which are temporally related to northward subduction of the Paleotethyan Ocean. The Taoyuan samples show high SiO2 (73.36-79.16%) and low Al2O3 (12.00-13.45%) contents, Mg numbers (20.6-38.2), and Sr/Y (2.04-10.1) and (La/Yb)N (2.34-7.32) ratios with negative Eu anomalies (Eu/Eu* = 0.33-0.93). They yielded positive εNd(t) (+ 3.0 to + 6.7) and εHf(t) (+ 11.8 to + 13.2) values, elevated initial Sr isotopic ratios (0.7040-0.7057) and relatively low zircon δ18O values of 4.62-5.39‰. These suggest that they were produced through partial melting of hydrothermally altered lower crust of the accreted Erlangping oceanic arc. In contrast, the Huanggang samples exhibit variable whole-rock geochemical and isotopic compositions with SiO2 contents of 57.01-64.42 wt.%, initial Sr isotopic ratios of 0.7065-0.7078, and εNd(t) values of - 5.7 to - 9.4. Additionally, they have high zircon δ18O values of 7.57-8.45‰ and strongly negative zircon εHf(t) values of - 14.4 to - 10.5. They were suggested to have been mainly derived from ancient continental crust of the Kuanping crustal unit with the addition of 20-40% juvenile, mantle-derived material. Accordingly, the granitoids in both oceanic and continental arcs are likely to be mainly derived from intracrustal melting of their crustal basement. It is revealed by the Huanggang pluton that little net continental crust growth occurs in continental arcs, and addition of new volume of continental

  13. Ritmo circadiano de atividade motora e distribuição diária dos comportamentos afiliativos ao longo da fase juvenil em saguis (callithrix jacchus)

    OpenAIRE

    Melo, Paula Rocha de

    2012-01-01

    A alocação temporal da fase ativa em relação ao ciclo claro e escuro (CE) modifica-se durante a puberdade em humanos, degus, ratos e rhesus. Em sagui, modelo animal utilizado em diversas pesquisas biomédicas, há evidências de um avanço no início da fase ativa e um aumento no total diário da atividade após a entrada na puberdade. Entretanto, como este aspecto foi avaliado em animais mantidos em condições ambientais naturais, não foi possível distinguir entre os efeitos da puberd...

  14. Planeamiento del proceso constructivo del PAD I fase III en la mina Cerro Verde

    OpenAIRE

    Tomas Loayza, Mariela Irma; Tomas Loayza, Mariela Irma; Tomas Loayza, Mariela Irma

    2015-01-01

    El planeamiento constructivo del PAD 1 Fase III ha sido elaborado detalladamente teniendo en cuenta un trabajo calificado de investigación, plasmando los resultados en el cronograma de ejecución y corroborando la ejecución de la obra mediante el ciclograma. Los alcances del proyecto son los estudios de topografía, estudios geotécnicos, geológicos y diseño civil, que son dados en el capítulo 11. La topografía es el relieve que representa la zona caracterizándose por taludes con elevada p...

  15. Histopatologia da esquistossomose mansoni em fígado de Mus musculus infectado por amostras humanas de fase aguda e crônica da periferia de Belo Horizonte, Minas Gerais

    Directory of Open Access Journals (Sweden)

    Amélia Dulce Vilela de Carvalho

    1986-06-01

    Full Text Available Exemplares de Biomphalaria glabrataforam infectados com miracídios obtidos de ovos de Schistosoma mansoni, encontrados em fezes de indivíduos de 7 a 18 anos, da região de Lagoa da Pampulha, Belo Horizonte, MG. Os pacientes de fase aguda se infectaram em uma primeira visita ao foco. Os da fase crônica eram moradores próximos aos focos. Para cada caso clínico, isolou-se a respectiva amostra do parasita. Foram infectados pela cauda 55 camundongos fêmeas com 70 ± 10 cercárias. Cortes histológicos de fígados, corados por HE, tricrômico de Gomori, impregnação metálica pela prata, e PAS foram observados à microscopia óptica. Não houve diferenças estatísticas em relação às médias das mensurações dos diâmetros dos granulomas referentes às amostras e datas de sacrifícios. Os granulomas apresentaram fase exsudativa do tipo Ha (reação de inflamação mista e IIIa (granuloma com células epitelióides. Com amostras de pacientes em fase aguda o padrão predominante foi a Ha na 7ª semana. Na 10.ª semana predominaram granulomas do tipo IIIa. Nas amostras de pacientes em fase crônica, verificou-se uma mescla de granulomas do tipo Ha e IIIa na 7ª semana. Na 10ª semana predominou o tipo IIIa. Alguns aspectos histopatológicos de fígados foram descritos e comparados com aqueles existentes na literatura.

  16. Postmodern Movement and Culture: dividing in into periods and discussing its phases Movimento Pós-Moderno e Cultura: periodizando e discutindo suas fases

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    Rosana Figueiredo Salvi

    2002-11-01

    Full Text Available This research tried to divide into periods the postmodern thought starting from the analysis of transformations, which happened inside the movement itself. So, three fundamental phases were emphasized. The first one is responsible for to formation of the postmodern thought in the area of Languages, Arts and Architecture, specifically. The second one is the phase that involves wide dissemination, migration and great controversies about this movement. Finally, the third phase demonstrates relative maturation of the postmodern movement, whose production of theories take place in several fields of knowledge.Esta pesquisa procurou estabelecer uma periodização do pensamento pós-moderno a partir da análise das transformações ocorridas dentro do próprio movimento. Assim, três fases fundamentais foram destacadas. A primeira é entendida como aquela responsável pela formação do pensamento pós-moderno especificamente nas áreas de letras, artes e arquitetura. A segunda é aquela fase que envolve ampla difusão, migração e grandes polêmicas sobre este movimento. Por fim, a terceira fase demonstra relativo amadurecimento do movimento pós-moderno, cuja produção cada vez mais acentuada de teorias ocorre em variadas áreas do conhecimento.

  17. Difficult aspects in the e-social pre implementation fase in higher education community institutions in Santa Catarina

    Directory of Open Access Journals (Sweden)

    Antonio Zanin

    2017-06-01

    Full Text Available Brazilian financial control is changing, mainly because of the implementation of new control tools which try to regulate the relation between the revenue and contributors. One of these changes is the EFD- Social implementation, which the organizations are putting a huge effort, because it is something new, where its demands is not only of processes but also of the management culture. Under this context, this study had as objective analyse the difficulties of the Higher Education Community Institutions  - ICES – in Santa Catarina, associated to ACAFE, in the accession adaptation of E-social in the pre implementation fase. The research is exploratory, descritive and quantitative. The sample is composed with about 60% of the researched population and the data collect was made through questionaries collected from february to may of 2015. The data analysis revealed that ICES are in distintives fases of EFD-Social implementation. It is also possible to verify, in the perspective of the researched  ICES, that the EFD-Social implementation will bring more advantages than disadvantages, suggesting the beginning of a cultural change in the organizations, which realize this instrument as a management tool not only financial control.

  18. Cuidando de pacientes em fase terminal: a perspectiva de alunos de enfermagem El cuidando de pacientes en fase terminal: la perspectiva de los alumnos de enfermería Taking care of terminal patients: nursing student's perspective

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    Maria Lúcia Araújo Sadala

    2009-06-01

    Full Text Available Este estudo busca compreender como alunos de graduação em Enfermagem percebem a si mesmos ao cuidar de pacientes em fase terminal e expor os significados da experiência vivida. Foram entrevistados 14 alunos, respondendo à questão: Como se mostra a você o cuidar do paciente na fase terminal? Para os alunos, é sempre uma experiência dolorosa, que os coloca face a face com suas fragilidades e inseguranças. Eles atribuem suas dificuldades à própria incapacidade de aceitar a morte e ao despreparo e inexperiência. Relatam que falta apoio dos profissionais com quem compartilham esse cuidado. No que se refere à formação profissional, para alguns a experiência foi positiva, apesar das dificuldades; outros a avaliam negativamente, resultando em rejeição a situações semelhantes. Novas investigações sobre o tema são necessárias para aprofundar e ampliar a reflexão para o âmbito da formação dos enfermeiros em nível nacional.Este estudio busca comprender como los alumnos del curso de Enfermería perciben el cuidar de pacientes en fase terminal y exponer los significados de la experiencia vivida. Fueron entrevistados 14 alumnos, respondiendo a la pregunta: ¿Qué le parece a usted cuidar de un paciente en fase terminal? Para los alumnos, siempre es una experiencia dolorosa, que los coloca frente a frente con sus fragilidades e inseguridades. Atribuyen sus dificultades a la propia incapacidad de aceptar la muerte y a la falta de preparación e inexperiencia. Relatan que les falta apoyo de los profesionales con quien comparten ese cuidado. En lo que se refiere a la formación profesional, para algunos la experiencia fue positiva, a pesar de las dificultades; otros la evalúan negativamente, resultando en rechazo a situaciones semejantes. Nuevas investigaciones sobre el tema son necesarias, en el sentido de profundizar y ampliar la reflexión dentro del ámbito de formación de los enfermeros a nivel nacional.The aim of this study is

  19. Validasi Sistem Skoring Rondinelli untuk Mendeteksi Komplikasi Infeksi Berat pada Pasien Leukemia Limfoblastik Akut L1 dengan Demam Neutropenia Selama Kemoterapi Fase Induksi

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    Renno Hidayat

    2016-11-01

    Kesimpulan. Sistem skoring Rondinelli merupakan instrumen yang cukup baik untuk mendeteksi komplikasi infeksi berat pada anak dengan LLA-L1 yang mengalami demam neutropenia selama pemberian kemoterapi fase induksi.

  20. Diagnóstico angiográfico dos hematomas subdurais: valor da fase venosa em incidência sagital

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    José Zaclis

    1955-12-01

    Full Text Available Êste trabalho tem por fim demonstrar o valor da fase venosa em incidência sagital no diagnóstico angiográfico dos hematomas subdurais. Êle é baseado em 8 casos verificados cirürgicamente, dois dos quais com hematoma bilateral, compreendendo um total de 10 hematomas subdurals demonstrados pela angiografia cerebral. Em 9 exemplares a elipse avascular que caracteriza essa entidade nosológica só apareceu na fase venosa; sòmente em um caso êsse sinal patognomônico foi claramente revelado na fase arterial em incidência ântero-posterior. O arteriograma mostra, apenas, às mais das vêzes, deslocamento da artéria cerebral anterior e seus ramos para o lado oposto àquele em que se encontra o hematoma, como acontece nos casos de lesões expansivas em geral. Menos freqüentemente os principais troncos arteriais do encéfalo não sofrem modificações no seu trajeto, apesar do espaço intracraniano ocupado pelos hematomas. A existência de hematoma subdural no interior de um hemicrânio sem desvio da artéria cerebral anterior, embora não implique necessàriamente na existência de outra coleção sangüínea do lado oposto, é altamente sugestiva dessa dupla lesão. A exploração bilateral nesses casos é, portanto, obrigatória. Dos três casos desta série em que a angiografia em um dos lados revelou a elipse avascular característica e artéria cerebral anterior com trajeto normal, a angiografia do lado oposto resultou positiva em dois dêles e negativa em um. Pôsto que alguns Serviços especializados não sejam dotados de equipamento para angiografia em séries, o autor recomenda o flebograma em incidência sagital como tempo obrigatório, mesmo que para tanto seja necessária nova injeção de contraste.

  1. Petrology and geochemistry of the orbicular granitoid of Caldera, northern Chile. Models and hypotheses on the formation of radial orbicular textures

    Science.gov (United States)

    Díaz-Alvarado, Juan; Rodríguez, Natalia; Rodríguez, Carmen; Fernández, Carlos; Constanzo, Ítalo

    2017-07-01

    The orbicular granitoid of Caldera, located at the northern part of the Chilean Coastal Range, is a spectacular example of radial textures in orbicular structures. The orbicular body crops out as a 375 m2 tabular to lensoidal intrusive sheet emplaced in the Lower Jurassic Relincho pluton. The orbicular structures are 3-7 cm in diameter ellipsoids hosted in a porphyritic matrix. The orbicules are comprised by a Qtz-dioritic core (3-5 cm in diameter) composed by Pl + Hbl + Qtz + Bt ± Kfs with equiaxial textures and a gabbroic shell (2-3 cm in diameter) characterized by feathery and radiate textures with a plagioclase + hornblende paragenesis. The radial shell crystals are rooted and orthogonally disposed in the irregular contact with the core. The radial shell, called here inner shell, is in contact with the granodioritic equiaxial interorbicular matrix through a 2-3 mm wide poikilitic band around the orbicule (outer shell). The outer shell and the matrix surrounding the orbicules are characterized by the presence of large hornblende and biotite oikocrystals that include fine-grained rounded plagioclase and magnetite. The oikocrystals of both the outer shell and the matrix have a circumferential arrangement around the orbicule, i.e. orthogonal to the radial inner shell. The coarse-grained granodioritic interorbicular matrix present pegmatitic domains with large acicular hornblende and K-feldspar megacrysts. This work presents a review of the textural characteristics of the orbicules and a complete new mineral and whole-rock geochemical study of the different parts of the orbicular granitoid, together with thermobarometric and crystallographic data, and theoretical modeling of the crystallization and element partitioning processes. We propose a model for the formation of the orbicular radial textures consisting of several processes that are suggested to occur fast and consecutively: superheating, volatile exsolution, undercooling, geochemical fractionation and

  2. A radiological survey of the Eğrigöz granitoid, Western Anatolia/Turkey.

    Science.gov (United States)

    Canbaz Öztürk, B; Yaprak, G; Çam, N F; Candan, O

    2015-06-01

    A radiological survey of the granitoid areas throughout Western Anatolia was conducted during 2007-14. As a part of this radiological survey, this article presents results obtained from Eğrigöz pluton, which lies in the northeastern region of Western Anatolia. In the investigated area, the activity measurements of the natural gamma-emitting radionuclides ((226)Ra, (232)Th and (40)K) in the granitic rock samples and soils have been carried out by means of the NaI(Tl) gamma-ray spectrometry system. The activity concentrations of the relevant natural radionuclides in the granite samples appeared in the ranges as follows: (226)Ra, 28-95 Bq kg(-1); (232)Th, 50-122 Bq kg(-1) and (40)K, 782-1365 Bq kg(-1), while the typical ranges of the (226)Ra, (232)Th and (40)K activities in the soil samples were found to be 7-184, 11-174 and 149-1622 Bq kg(-1), respectively. Based on the available data, the radiation hazard parameters associated with the surveyed rocks/soils are calculated. The corresponding absorbed dose rates in air from all those radionuclides were always much lower than 200 nGy h(-1) and did not exceed the typical range of worldwide average values noted in the UNSCEAR (2000) report. Furthermore, the data are also used for the mapping of the surface soil activity of natural radionuclides and the corresponding gamma dose rates of the surveyed area. © The Author 2015. Published by Oxford University Press. All rights reserved. For Permissions, please email: journals.permissions@oup.com.

  3. Avaliação morfológica do oviduto e qualidade de ovos de poedeiras comerciais (Gallus gallus) em diferentes fases de produção.

    OpenAIRE

    Fátima Naomi Takata

    2006-01-01

    As linhagens de poedeiras comerciais existentes atualmente no mercado foram melhoradas geneticamente para produzir o máximo de ovos a um custo mínimo. Um fato importante para a continuidade desta evolução, é o conhecimento celular do oviduto ("fabrica do ovo"). Na galinha (Gallus gallus) o oviduto é descrito como sendo um tubo muscular tortuoso, cujo comprimento é estimado entre 14 e 19 cm na fase de não postura e de 42 a 86 cm durante a fase de postura. Abre-se próximo ao ovário e termina na...

  4. UM MODELO MARKOVIANO DE DECISÃO PARA A OTIMIZAÇÃO DE UM SISTEMA DE MANUTENÇÃO COM TEMPOS DE REPARO COXIANOS E FASES NÃO OBSERVÁVEIS

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    Rodrigues Rita de Cássia Meneses

    2001-01-01

    Full Text Available Neste artigo analisa-se um sistema de manutenção de máquinas com dois servidores diferentes, tempos até a quebra das máquinas exponencialmente distribuídos e tempos de reparo seguindo uma distribuição do tipo fase com configuração de Cox. Consideram-se dois modelos que se diferenciam pela possibilidade ou não de se observar as fases das distribuições do tipo fase: um modelo com informação completa e um modelo com informação parcial. No primeiro caso, modela-se o sistema por um processo markoviano de decisão a tempo contínuo e no segundo por um processo markoviano de decisão com informação parcial, conforme este é definido em Hordijk & Loeve (1994. Resultados numéricos são apresentados

  5. ESTUDIO DE LAS FASES MINERALÓGICAS DEL CLÍNKER EN UNA CEMENTERA ESPAÑOLA, UTILIZANDO EL MÉTODO DE RIETVELD

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    ANA M. CASTAÑÓN

    2012-01-01

    Full Text Available Con el objetivo de implantar un método de control de calidad de forma continua en una fábrica de cementos española, para mejorar las características del producto final, se están desarrollando nuevas metodologías de caracterización. El método de Rietveld [1] se ha utilizado con éxito para analizar la composición de las fases principales del clínker. Utilizando esta metodología, se ha llevado a cabo un estudio para cuantificar adecuadamente la fase minoritaria de Cal Libre, de gran importancia en la calidad del clínker. El método ha permitido obtener unos resultados satisfactorios en muestras cuyos contenidos superan el 3% de CaO. Estos resultados son posibles combinando adecuadamente las técnicas de difracción y fluorescencia de rayos-X, así como los resultados del análisis por vía química.

  6. Equilibrio de fases de sistemas compostos por oleos vegetais, acidos graxos e etanol hidratado.

    OpenAIRE

    Cintia Bernardo Gonçalves

    2004-01-01

    Resumo: Este trabalho de tese de doutoramento teve como objetivo avaliar vários aspectos do processo de extração líquido-líquido (ELL) como uma rota alternativa para a desacidificação de óleos vegetais. O conhecimento do equilíbrio de fases do sistema de interesse é essencial para o bom planejamento e desenvolvimento do processo de ELL. O presente trabalho apresenta dados de equilíbrio para sistemas compostos por óleos vegetais (milho/palma), ácidos graxos (oléico/ palmítico) e solvente (etan...

  7. Uranium distributions in the mineral constituents of granitoid rocks and the associated pegmatites at Wadi Abu Had, north eastern desert, Egypt

    International Nuclear Information System (INIS)

    Nossair, L.M.; Moharem, A.F.; Abdel Warith, A.

    2007-01-01

    Wadi Abu Had area is located at the northern part of the Eastern Desert of Egypt. It covers about 55 km2 of the crystalline basement rocks stretching between latitudes 28o 15'- 28o 25' N and longitudes 32o 25' - 32o 35' E. Abu Had younger granites are fertile (uraniferous) granites as they possess U-contents greater than 11 ppm. Their associated pegmatites show higher U-contents than those of granitoid rocks and hosting secondary uranium minerals. Numerous unzoned and zoned pegmatite pockets are associated with the marginal parts of granodiorite and within younger granites. Zoned pegmatites are the most radioactive ones. They are composed of extremely coarse-grained milky quartz core, intermediate zone of mica and wall zone of feldspars. An alteration zone with secondary uranium minerals (uranophane and beta-uranophane) is found at the contact between quartz core and the intermediate zone.

  8. en fase líquida

    Directory of Open Access Journals (Sweden)

    Alba Nelly Ardila Arias

    2007-01-01

    Full Text Available Se comparó la reactividad del hidrógeno puro, el isopropanol y el ácido fórmico como agentes reductores en la hidrodecloración catalítica de percloroetileno en fase líquida con 0,8% Pd/TiO2 sol-gel bajo condiciones de reacción moderadas. Además, se estudió el efecto de la cantidad de agua y de hidróxido de sodio adicionados a la mezcla de reacción. Los catalizadores frescos y usados se caracterizaron por espectroscopia de absorción atómica (AAS, quimisorción de H2,adsorción-desorción de N2, difracción de rayos X (DRX, reducción con hidrógeno a temperatura programada (TPR-H2, análisis termogravimétrico (TGA-DTG, espectroscopia de reflectancia difusa UV-Vis (UV-Vis DRS, desorción de NH3 a temperatura programada (TPD-NH3 y microscopía de transmisión electrónica (TEM. Los mejores resultados de HDC se obtuvieron con hidrógeno e isopropanol como agentes reductores. La adición de NaOH aumenta significativamente la conversión del PCE con los tres agentes reductores; no obstante, es importante optimizar la cantidad que se debe adicionar, ya que un exceso afecta negativamente la reacción de HDC. Los resultados de la caracterización realizada a los catalizadores frescos y usados revela ciertos cambios como: disminución del área superficial, incremento de la acidez superficial, disminución de la dispersión y aumento en el tamaño de las partículas de paladio. Sin embargo, algunas características como la carga de paladio, la estructura cristalina del soporte y los estados de oxidación del paladio no se modificaron.

  9. Age and geochemistry of Neoproterozoic granitoids in the Songnen-Zhangguangcai Range Massif, NE China: Petrogenesis and tectonic implications

    Science.gov (United States)

    Luan, Jin-Peng; Xu, Wen-Liang; Wang, Feng; Wang, Zhi-Wei; Guo, Peng

    2017-10-01

    This study presents new zircon U-Pb ages and geochemical data for Neoproterozoic granitoids in the Songnen-Zhangguangcai Range Massif (SZRM) of NE China. This dataset provides insights into the Neoproterozoic tectonic setting of the SZRM and the links between this magmatism and the evolution of the Rodinia supercontinent. The zircon U-Pb dating indicates that the Neoproterozoic magmatism within the SZRM can be subdivided into two stages: (1) a ∼917-911 Ma suite of syenogranites and monzogranites, and (2) an ∼841 Ma suite of granodiorites. The 917-911 Ma granitoids contain high concentrations of SiO2 (67.89-71.18 wt.%), K2O (4.24-6.91 wt.%), and Al2O3 (14.89-16.14 wt.%), and low concentrations of TFe2O3 (1.63-3.70 wt.%) and MgO (0.53-0.88 wt.%). They are enriched in the light rare earth elements (LREE) and the large ion lithophile elements (LILE), are depleted in the heavy REE (HREE) and the high field strength elements (HFSE; e.g., Nb, Ta, and Ti), and have slightly positive Eu anomalies, indicating that they are geochemically similar to high-K adakitic rocks. They have zircon εHf (t) values and TDM2 ages from -4.4 to +1.5 and 1915 Ma to 1592 Ma, respectively, suggesting that they were derived from a primary magma generated by the partial melting of ancient thickened lower crustal material. In comparison, the 841 Ma granodiorites contain relatively low concentrations of Al2O3 (14.50-14.58 wt.%) and K2O (3.27-3.29 wt.%), relatively high concentrations of TFe2O3 (3.78-3.81 wt.%) and the HREE, have negative Eu anomalies, and have zircon εHf (t) values and TDM2 ages from -4.7 to +1.0 and 1875 to 1559 Ma, respectively. These granodiorites formed from a primary magma generated by the partial melting of ancient crustal material. The ∼917-911 Ma magmatism within the SZRM is inferred to have formed in an orogenic setting, whereas the ∼841 Ma magmatism formed in an anorogenic setting related to either a post-orogenic tectonic event or the onset of Neoproterozoic

  10. Relação Hipsométrica para Pinus taeda L. em Diferentes Fases do Ciclo de Corte

    Directory of Open Access Journals (Sweden)

    Marcos Felipe Nicoletti

    Full Text Available RESUMO O objetivo deste estudo foi avaliar as diferentes etapas do ciclo de corte, buscando uma relação hipsométrica adequada para estimar alturas dessas diferentes fases em um reflorestamento de Pinus taeda. Foram realizados cinco tratamentos, sendo o quinto a junção dos dados pertencentes aos demais tratamentos (modelo reduzido. A amostragem seguiu o método de área fixa, no qual o tamanho das parcelas e o número de árvores dominantes diferenciaram-se nos ciclos de corte. Definiu-se a localização das parcelas através de amostragem aleatória simples (oito parcelas por ciclo de corte. Foram determinadas as estatísticas de ajustes, coeficiente de determinação ajustado, erro-padrão e análise de resíduos. Efetuou-se o teste de identidade de Graybill para verificação da necessidade da utilização de diferentes modelos para distintas classes de idade. Os resultados comprovaram que existem diferenças significativas entre adotar-se um modelo específico para cada fase e utilizar um único melhor modelo para o povoamento total.

  11. Incorporación de la fase Zn7Sb2O12 previamente sintetizada en varistores cerámicos basados en ZnO

    Directory of Open Access Journals (Sweden)

    Caballero, A. C.

    2002-02-01

    Full Text Available During the sintering process of ZnO-Bi2O3-Sb2O3 based varistors, different reactions take place. The formation of the Zn7Sb2O12 spinel phase occurs between 900 and 1100ºC depending on the composition of the material. The spinel phase acts as ZnO grain growth inhibitor and its distribution on the whole material as a secondary phase in the matrix of ZnO grains determines the kinetics of grain growth. However, it is difficult to control the nucleation and growth of this phase, and this concerns on the final grain size and consequently on the characteristics of the varistor device. The present study has focused on the incorporation of the previously synthesized spinel phase. Scanning Electronic Microscopy analysis of sintered samples reveals a better control of microstructure in those materials with the synthesized spinel phase. The electrical behaviour of these materials agrees with the microstructural features and a greater reproducibility is observed.Una de las reacciones que tiene lugar durante la sinterización de varistores cerámicos basados en el sistema ZnO-Bi2O3-Sb2O3 es la formación de la fase Zn7Sb2O12, de estructura tipo espinela, que ocurre en el intervalo de temperaturas comprendido entre 900 y 1100ºC, dependiendo de la composición específica del material. Esta fase es la responsable del control del crecimiento de grano y su distribución en el seno del material como una segunda fase dispersa en la matriz mayoritaria de granos de ZnO determinará la cinética del crecimiento de los granos. Sin embargo, el proceso de nucleación y crecimiento de esta fase resulta difícil de controlar cuantitativamente, aspecto que se refleja en las características finales del dispositivo varistor obtenido. En el presente trabajo se analiza el efecto de la incorporación de la fase espinela previamente sintetizada a partir de los óxidos de zinc y antimonio. El análisis mediante Microscopía Electrónica de Barrido (MEB de la microestructura de

  12. O valor da fase sem contraste na tomografia computadorizada do abdome The role of the unenhanced phase in the routine abdominal computed tomography

    Directory of Open Access Journals (Sweden)

    Ana Paula Klautau Leite

    2008-10-01

    Full Text Available OBJETIVO: Determinar o valor agregado da fase sem meio de contraste da tomografia computadorizada do abdome em pacientes sem diagnóstico determinado ou em estadiamento tumoral. MATERIAIS E MÉTODOS: Estudo prospectivo e transversal em 100 pacientes consecutivos submetidos a tomografia computadorizada abdominal sem e com meio de contraste intravenoso. Dois examinadores avaliaram todos os exames, procurando estabelecer, através da fase com meio de contraste intravenoso (primeira análise e posteriormente através da fase sem contraste (segunda análise, o diagnóstico principal e os secundários em função da indicação clínica do exame. Mediu-se a freqüência de mudança diagnóstica decorrente da análise combinada das fases pré- e pós-contraste intravenoso. Casos que tiveram mudança diagnóstica foram avaliados por especialistas clínicos para determinar se implicaria mudanças de conduta. RESULTADOS: Diagnósticos principal e secundário foram modificados em 1 e 18 casos, respectivamente (p = 1,000; p = 0,143. Os diagnósticos modificados foram: esteatose, definição de nódulo em adrenal, nefrolitíase, classificação de cistos renais e calcificação hepática. Nos casos em que a fase sem contraste modificou o diagnóstico, os especialistas mudaram sua conduta em 14/19 (73% dos pacientes (p = 0,038. CONCLUSÃO: A fase sem contraste não modificou significativamente o diagnóstico principal ou secundário. Porém, as mudanças nos diagnósticos secundários influenciaram na conduta adotada pelos especialistas.OBJECTIVE: To determine the role of the unenhanced phase of abdominal computed tomography in patients without a definite diagnosis or undergoing tumor staging. MATERIALS AND METHODS: A prospective and transversal study was developed with 100 consecutive patients submitted to unenhanced and contrast-enhanced abdominal computed tomography. Two observers evaluated all the computed tomography images in the contrast-enhanced phase

  13. La transición de fase I4/mcm→Pm3m en Sr0.5Ba0.5HfO3-δ

    Directory of Open Access Journals (Sweden)

    Lamas, D.

    2001-08-01

    Full Text Available The effect of partial substitution of cations in AMO3 compounds have been studied because the physical properties and applications of these materials can be improved. In particular we are interested in the Sr1-xBaxHfO3 family. In SrHfO3 the phase transition to cubic structure has been observed to occur when the angle between two consecutive oxygen octahedra tends to zero. Instead in BaHfO3 no phase transition was observed. These facts were attributed to depend on the atomic radius of A cation. In this contribution the study of Sr0.5Ba0.5HfO3 oxide is shown. The compound was prepared by the high temperature solid state reaction method and analyzed by X-ray diffraction and Perturbed Angular Correlation (PAC Spectroscopy at different temperatures. Diffraction studies revealed that about 400-420º C a structural phase transition from I4/mcm to Pm3m occurred by tending to zero the rotation angle. By PAC this transition was also observed. In the cubic phase the electric field gradient EFG measured were produced by defects. The same model applied to interpreted the results of BaTi1-xHfxO3 and the atomic positions determined by X-ray diffraction were used. This calculation reproduces reasonably the temperature dependence of the EFG measured by PAC.Los AMO3, llamados perovskitas, forman una gran familia de compuestos que presentan a su vez diversas propiedades físicas así como enormes aplicaciones tecnológicas. Es posible expandir esta familia y sus propiedades y aplicaciones, sustituyendo los cationes Ay M originales por diferentes A’ y M’. En este trabajo presentamos el estudio del compuesto Sr1-xBaxHfO3 con x=0.5. El óxido fue preparado por el método de reacción en fase sólida. La muestra fue analizada por difracción de Rayos X y por espectroscopía de Correlaciones Angulares Perturbadas (PAC a diferentes temperaturas. El estudio cristalográfico del material reveló que entre 400 y 420ºC se produce la transición de fase de estructura I4

  14. Determinação das fases na difração dos raios-X usando difração multipla de mais de tres-feixes

    OpenAIRE

    Jose Marcos Sasaki

    1988-01-01

    Resumo: O problema da fase dos feixes de raios-X difratados é um dos maiores problemas da Cristalografia de Raios-X desde a descoberta de Laue e a resolução das primeiras estrutura por Bragg. Neste trabalho é desenvolvido um método teórico, baseado na teoria dinâmica de difração dos raios-X, para análise da intensidade de difração múltipla com o objetivo de obter informações sobre as fases num caso de difração múltipla de N-feixes com N > 3. Faz-se uso de comprimento de onda acima da borda de...

  15. Comparison of the behaviour of rare earth elements in surface waters, overburden groundwaters and bedrock groundwaters in two granitoidic settings, Eastern Sweden

    International Nuclear Information System (INIS)

    Roennback, Pernilla; Astroem, Mats; Gustafsson, Jon-Petter

    2008-01-01

    This work, which was done within the Swedish nuclear waste management program, was carried out in order to increase the understanding of the mobility and fate of rare earth elements (REEs) in natural boreal waters in granitoidic terrain. Two areas were studied, Forsmark and Simpevarp, one of which will be selected as a site for spent nuclear fuel. The highest REE concentrations were found in the overburden groundwaters, in Simpevarp in particular (median ΣREE 52 μg/L), but also in Forsmark (median ΣREE 6.7 μg/L). The fractionation patterns in these waters were characterised by light REE (LREE) enrichment and negative Ce and Eu anomalies. In contrast, the surface waters had relatively low REE concentrations. They were characterised either by an increase in relative concentrations throughout the lanthanide series (Forsmark which has a carbonate-rich till) or flat patterns (Simpevarp with carbonate-poor till), and had negative Ce and Eu anomalies. In the bedrock groundwaters, the concentrations and fractionation patterns of REEs were entirely different from those in the overburden groundwaters. The median La concentrations were low (just above 0.1 μg/L in both areas), only in a few samples were the concentrations of several REEs (and in a couple of rare cases all REEs) above the detection limit, and there was an increase in the relative concentrations throughout the lanthanide series. In contrast to these large spatial variations, the temporal trends were characterised by small (or non existent) variations in REE-fractionation patterns but rather large variations in concentrations. The Visual MINTEQ speciation calculations predicted that all REEs in all waters were closely associated with dissolved organic matter, and not with carbonate. In the hydrochemical data for the overburden groundwater in particular, there was however a strong indication of association with inorganic colloids, which were not included in the speciation model. Overall the results showed

  16. Detección de malas hierbas en girasol en fase temprana mediante imágenes tomadas con un vehículo aéreo no tripulado (UAV

    Directory of Open Access Journals (Sweden)

    J.M. Peña

    2014-12-01

    Full Text Available La discriminación de malas hierbas en fase temprana con técnicas de teledetección requiere imágenes remotas de muy elevada resolución espacial (píxeles <5 cm. Actualmente, sólo los vehículos aéreos no tripulados (UAV pueden generar este tipo de imágenes. El objetivo de este trabajo fue evaluar imágenes UAV tomadas con una cámara visible a diferentes alturas de vuelo (40, 60, 80 y 100 m y cuantificar la influencia de la resolución espacial en la discriminación de malas hierbas en fase temprana en un cultivo de girasol. Se aplicó un algoritmo de clasificación de imágenes basado en objetos, el cual se divide en dos fases principales: 1 detección de líneas de cultivo y 2 clasificación de cultivo, malas hierbas y suelo desnudo. El algoritmo resultó 100% eficaz en la detección de las líneas de cultivo en todos los casos (fase 1, así como en la detección de zonas libres de mala hierba en las imágenes tomadas a 40 y 60 m de altura. En las zonas con presencia de malas hierbas, los mejores resultados se obtuvieron en las imágenes tomadas a baja altura (40 m, con un 71% de marcos de muestreo clasificados correctamente (fase 2. La mayoría de los fallos de clasificación cometidos en todas las imágenes fueron falsos negativos, es decir, malas hierbas no detectadas debido a su pequeño tamaño en el momento de la captura de las imágenes. Por tanto, el siguiente paso sería desarrollar un estudio multitemporal para estudiar la detección de las malas hierbas en estados fenológicos más avanzados. Esto podría facilitar su discriminación en las imágenes y, por tanto, disminuir el porcentaje de falsos negativos en las clasificaciones.

  17. Calculos de estabilidade e divisão de fases por meio de redes neurais artificiais

    OpenAIRE

    Jones Erni Schmitz

    2006-01-01

    Resumo: A simulação de processos é um componente fundamental de uma grande variedade de atividades de Engenharia de Processos, tais como a Otimização Online, o controle em Tempo Real, a Identificação, etc. O cálculo de Equilíbrio de Fases é uma atividade fundamental em qualquer simulação de processos de separação. O elevado tempo computacional deste cálculo provocado pela sua natureza iterativa pode criar incompatibilidades entre a atividade de simulação e as aplicações em tempo real que ela ...

  18. Diagramas de fase CVD para la preparación de películas de iridio

    Directory of Open Access Journals (Sweden)

    Hernández-Pérez, M. A.

    2002-02-01

    Full Text Available Chemical vapor deposition (CVD phase diagrams for the preparation of iridium films were calculated using Gibbs free energy minimization method. Iridium acetylacetonate (Ir(acac3 was used as the precursor compound. Two gaseous mixtures were analyzed: Ir(acac3-O2-Ar and Ir(acac3-Ar. The deposition temperatures were explored from 300 to 800 °C, total pressures from 13.3 to 13.332 Pa and partial pressures of Ir(acac3 gas and O2 gas from 0.001 to 1.000 Pa. The Ir-CVD diagrams predicted that without Oj gas in the gaseous mixture, the solid films consist of two solid phases: Ir+C. In contrast, with addition of O2 to the gaseous mixture, the Ir-CVD diagrams revealed different domains of condensed phases which include IrO2, IrO2+Ir, Ir and Ir+C. These diagrams allow one to establish the total pressures and temperatures required to obtain a given film composition. The results predicted by the Ir-CVD diagrams are in good agreement with those experimentally obtained.

    Se calcularon los diagramas de fase CVD (Chemical Vapor Deposition para la preparación de películas de iridio empleando el método de minimización de la energía libre de Gibbs. Como precursor se utilizó acetilacetonato de iridio (Ir(acac3. Se analizaron las mezclas gaseosas Ir(acac3-O2Ar e Ir(acac3-Ar. Las temperaturas de depósito se exploraron desde 300 hasta 800 °C, las presiones totales de 13,3 a 13.332 Pa y las presiones parciales de los gases Ir(acac3 y O2 desde 0,001 hasta 1.000 Pa. Los diagramas Ir-CVD predicen que sin O2 en la mezcla gaseosa, las películas constan de las fases sólidas Ir+C. En contraste, con adición de O2 los diagramas Ir-CVD revelan diferentes dominios de fases sólidas que incluyen IrO2, IrO2+Ir, Ir e Ir+C. Estos diagramas permiten establecer

  19. FASES DA TEORIA HUMANÍSTICA: ANÁLISE DA APLICABILIDADE EM PESQUISA

    Directory of Open Access Journals (Sweden)

    Ana Luiza Paula de Aguiar Lélis

    2014-01-01

    Full Text Available El objetivo fue analizar la aplicabilidad de las fases de la Teoría Humanística en investigaciones, según un Modelo de Análisis de Teoría. Estudio de análisis crítica de teoría de enfermería con énfasis en la aplicabilidad. Fue efectuada una búsq ueda, en abril y mayo de 2013, en las bases de datos SCOPUS, Cumulative Index of Nursing and Allied Health Literature y en las disponibles en la Biblioteca Virtual de Salud. Fueron utilizados los descriptores: “Teoria de Enfermagem” y “Pesquisa em Enfermagem” y Nursing Theory y Nursing Research , en publicaciones del 2002 hasta mayo de 2013. Siete artículos fueron seleccionados, de los cuales cinco revelaron todas las etapas en su desarrollo, evidenciando la aplicabilidad de la Teoría Humanística como soporte metodológico e n las investigaciones de enfermería.

  20. Leucograma e proteínas de fase aguda de ruminantes domésticos sadios e enfermos

    OpenAIRE

    Simplicio, Kalina Maria de Medeiros Gomes [UNESP

    2011-01-01

    Foi avaliada a importância de proteínas de fase aguda (PFA) como biomarcadores de enfermidades em ruminantes domésticos. Para tal se determinou o proteinograma sérico e leucograma de 15 bovinos sadios e 15 doentes, 15 ovinos sadios e 15 doentes, e 15 caprinos sadios e 15 doentes. Todos foram submetidos a colheitas diárias de sangue durante sete dias, enquanto permaneciam internados no Hospital Veterinário da FCAV-UNESP, Câmpus de Jaboticabal. Em bovinos a haptoglobina teve destaque como bioma...

  1. Estudio del genoma y del transcriptoma en las fases evolutivas de las gammapatías monoclonales

    OpenAIRE

    López Corral, Lucía

    2012-01-01

    [ES] Los estudios epidemiológicos han demostrado que la práctica totalidad de los mielomas múltiples están precedidos por una fase premaligna. En este sentido, la gammapatía monoclonal de significado incierto (GMSI) y el mieloma múltiple quiescente (MMQ) se consideran entidades premalignas y asintomáticas que difieren de forma significativa en la tasa de progresión a MM sintomático. A pesar de su comportamiento clínico radicalmente distinto, las tres entidades comparten aparentemente la m...

  2. Estudio del genoma y del transcriptoma en las fases evolutivas de las gammapatías monoclonales

    OpenAIRE

    López Corral, Lucía

    2013-01-01

    [ES] Los estudios epidemiológicos han demostrado que la práctica totalidad de los mielomas múltiples están precedidos por una fase premaligna. En este sentido, la gammapatía monoclonal de significado incierto (GMSI) y el mieloma múltiple quiescente (MMQ) se consideran entidades premalignas y asintomáticas que difieren de forma significativa en la tasa de progresión a MM sintomático. A pesar de su comportamiento clínico radicalmente distinto, las tres entidades comparten aparentemente la misma...

  3. Utilização de diferentes programas de restrição alimentar na fase de crescimento de matrizes avícolas tipo corte e seus efeitos na fase de produção Broiler breeding performance influenced by feeding programs during the growing period

    Directory of Open Access Journals (Sweden)

    Neventon Santi Vieira

    1995-01-01

    Full Text Available Matrizes avícolas tipo corte necessitam de rigoroso controle de peso nas fases de recria e produção, para que tenham um desenvolvimento adequado e conseqüentemente, espressem seu máximo potencial produtivo. Objetivando avaliar o efeito de diferentes programas de arraçoamento na fase de recria sobre parâmetros produtivos de matrizes avícolas tipo corte, conduziu-se este experimento no Setor de Avicultura do Departamento de Zootecnia da Universidade Federal de Santa Maria/RS. O delineamento experimental foi inteiramente casualizado, constituído de 3 tratamentos com 4 repetições e, a unidade experimental foi de 67 aves. Na 1ª e 2ª semana de idade as aves receberam alimento à vontade, na 3ª e 4ª semana o arraçoamento foi diário controlado. Na fase de recria (5ª a 20ª semana de idade as aves foram submetidas aos tratamentos: T1: 5ª a 14ª semana = "Sip-a-Day"; 15ª a 17ª = 2 dias sim/1 dia não e da 18ª a 20ª semana, arraçoamento diário controlado; T2: 5ª a 8ª semana = "Skip-a-Day", 9ª a 16ª = 48-57-63 h de intervalo entre arraçoamentos. e da 17ª a 20ª semana = 2 dias sim/1 dia não; T3, 5ª a 20ª semana de idade = 48-57-63 h de intervalo entre arraçoamentos. Os resultados obtidos mostram que, o aumento do intervalo de arraçoamento (48-57-63h na fase de crescimento das aves, não afeta negativamente a performance produtiva das aves, podendo ser utilizado durante a fase de recria, tendo ainda por vantagem, a redução com os custos de mão de obra, pois as aves não são arraçoadas nos finais de semana.The body weight of broiler breeders must be rigorously controled during the growing and production periods in order to get on adequate development, and consequently to show his maximum potential of production. An experiment was conducted at the Poultry Section of the Animal Science Department of the Federal University of Santa Maria/RS, to evaluate the effect of different feeding programs during the growing period on

  4. RESOLUCIÓN DEL PROBLEMA DE ENRUTAMIENTO DE VEHÍCULOS CON LIMITACIONES DE CAPACIDAD UTILIZANDO UN PROCEDIMIENTO METAHEURÍSTICO DE DOS FASES RESOLUÇÃO DO PROBLEMA DE ROTEAMENTO DE VEÍCULOS COM LIMITAÇÕES DE CAPACIDADE UTILIZANDO UM PROCEDIMENTO METAHEURÍSTICO DE DUAS FASES SOLVING THE CAPACITATED VEHICLE ROUTING PROBLEM USING A TWOPHASE METAHEURISTIC PROCEDURE

    Directory of Open Access Journals (Sweden)

    Julio Mario Daza

    2009-12-01

    Full Text Available Este artículo presenta un procedimiento alternativo para resolver el problema de enrutamiento de vehículos con limitaciones de capacidad y flota homogénea (CVRP. Se propone un algoritmo metaheurístico que consta de la combinación de dos fases: diseño de rutas y planificación de la flota. La primera fase está compuesta de procedimientos heurísticos y metaheurísticos donde se construye una solución inicial que es mejorada mediante búsqueda tabú obteniendo soluciones no dominadas en tiempo de cálculo polinomial. Para la segunda fase, correspondiente a la planificación (scheduling de la flota, se propone abordar el problema partiendo de una analogía con el problema de programación de máquinas paralelas idénticas. Este procedimiento tiene como función objetivo minimizar el costo fijo causado por la utilización de la capacidad instalada. Esta alternativa se aplicó sobre una instancia generada aleatoriamente y una instancia real arrojando resultados significativos al compararse con las heurísticas evaluadas.Este artigo apresenta um procedimento alternativo para resolver o problema de roteamento de veículos com limitações de capacidade e frota homogênea (CVRP. Propõe-se um algoritmo metaheurístico que consta da combinação de duas fases: desenho de rotas e planejamento da frota. A primeira fase está composta de procedimentos heurísticos e metaheurísticos onde se constrói uma solução inicial que é melhorada mediante busca tabu obtendo soluções não dominadas em tempo de cálculo polinomial. Para a segunda fase, correspondente ao planejamento (scheduling da frota, se propõe abordar o problema partindo de uma analogia com o problema de programação de máquinas paralelas idênticas. Este procedimento tem como função objetivo minimizar o custo fixo causado pela utilização da capacidade instalada. Esta alternativa se aplicou sobre uma instância gerada aleatoriamente e uma instância real dando resultados

  5. Weathering profiles in granitoid rocks of the Sila Massif uplands, Calabria, southern Italy: New insights into their formation processes and rates

    Science.gov (United States)

    Scarciglia, Fabio; Critelli, Salvatore; Borrelli, Luigi; Coniglio, Sabrina; Muto, Francesco; Perri, Francesco

    2016-05-01

    In this paper we characterized several weathering profiles developed on granitoid rocks in the Sila Massif upland (Calabria, southern Italy), integrating detailed macro- and micromorphological observations with physico-mechanical field tests and petrographic, mineralogical and geochemical analyses. We focused our attention on the main weathering and pedogenetic processes, trying to understand apparent discrepancies between weathering grade classes based on field description and geomechanical properties, and two common weathering indices, such as the micropetrographic index (Ip) and the chemical index of alteration (CIA). Our results showed that sericite on plagioclase and biotite chloritization, that represent inherited features formed during late-stage hydrothermal alteration of granitoid rocks, may cause an overestimation of the real degree of weathering of primary mineral grains under meteoric conditions, especially in lower weathering grade classes. Moreover, the frequent identification of Fe-Mn oxides and clay coatings of illuvial origin (rather than or in addition to those formed in situ), both at the macro- and microscale, may also explain an overestimation of the weathering degree with respect to field-based classifications. Finally, some apparent inconsistencies between field geomechanical responses and chemical weathering were interpreted as related to physical weathering processes (cryoclastism and thermoclastism), that lead to rock breakdown even when chemical weathering is not well developed. Hence, our study showed that particular caution is needed for evaluating weathering grades, because traditional field and geochemical-petrographic tools may be biased by inherited hydrothermal alteration, physical weathering and illuvial processes. On the basis of chronological constraints to soil formation obtained from a 42 ka-old volcanic input (mixed to granite parent materials) detected in the soil cover of the Sila Massif upland, a first attempt to estimate

  6. LA VIOLENCIA A TRAVÉS DE LAS FASES DEL AMOR PASIONAL: PORQUE LA PASIÓN TAMBIÉN TIENE UN LADO OBSCURO

    Directory of Open Access Journals (Sweden)

    Rozzana Sánchez Aragón

    2006-06-01

    Full Text Available La pasión ha sido caracterizada por la alegría, sensación de realización, optimismo, éxtasis y profunda idealización del objeto amoroso (Villanueva Orozco, 2004. Sin embargo, autores como Hatfield y Rapson (1993 reconocen un lado más oscuro teñido de desesperanza, ansiedad y vacío. Por su parte, Sánchez Aragón (2004 propone un continuo del amor pasional que va de la atracción al amor desesperado, en donde el matiz negativo se va intensificando básicamente durante el amor obsesivo en donde hay una falta de mutualidad en el sentimiento. Así, la violencia puede surgir y con ello facilitar la presencia de actos dañinos a las personas y a la relación romántica. Con base en esto, el presente trabajo tuvo por objetivos: a identificar las posibles diferencias en términos de atracción, enamoramiento, amor obsesivo y amor desesperado en receptores y ejecutores de violencia en la pareja, y b conocer la posible relación entre la violencia y las fases del continuo del amor pasional. Para ello se trabajó con una muestra de 518 personas residentes de la Ciudad de México a quienes se les aplicó: 1 Escala Multifacética del Amor Pasional (Sánchez Aragón, 2006 y 2 Escala de Violencia en la Pareja (Cienfuegos Martínez, Sánchez Aragón y Rivera Aragón, en prensa. Los resultados muestran efectos diferenciales en las primeras dos fases y correlaciones significativas principalmente entre los factores de violencia y las fases de amor obsesivo y amor desesperado.

  7. Programas preventivos com antibióticos para suínos em fase de creche e efeitos no desempenho, características de carcaça e índices sanitários

    OpenAIRE

    Everson Zotti

    2008-01-01

    O uso de “pulsos” ou “choques” com antibióticos tem sido recomendado e utilizado amplamente em toda cadeia de produção de suínos no Brasil. Neste sentido, o objetivo deste trabalho foi identificar o melhor programa preventivo com antibióticos dispensado na fase de creche, que tenha efeitos consistentes e duradouros até o abate, reduzindo potenciais riscos de perdas pelas principais enfermidades entéricas e respiratórias nas fases de creche, crescimento e terminação. O trabalho foi realizado e...

  8. Fases del kirchnerismo: de la ruptura a la afirmación particularista

    Directory of Open Access Journals (Sweden)

    Francisco J. Cantamutto

    2017-05-01

    Full Text Available El presente artículo analiza el kirchnerismo como proceso político populista. Utilizando la bibliografía especializada, es posible reconstruir la modificación en las alianzas políticas y sociales del gobierno, marcadas por el conflicto con la fracción agropecuaria del bloque en el poder en 2008. Este conflicto produjo un cambio de énfasis en la estrategia política del gobierno, que modificó su discurso y alianzas. Con base en ello se propone una periodización del proceso en dos etapas, donde se pasa de una fase ligada a la ruptura populista del orden institucional previo a una segunda donde se produce una afirmación particularista de la identidad kirchnerista. El artículo analiza en detalle los nuevos rasgos del orden político a partir de 2008.

  9. Interferência de fases de deformação Varisca na estrutura de Torre de Cabedal; sector de Alter-do-Chão – Elvas na Zona de Ossa-Morena

    OpenAIRE

    Moreira, Noel; Dias, Rui; Araújo, António; Pedro, Jorge

    2014-01-01

    O Sector de Alter-do-Chão – Elvas é caracterizado por uma espessa sequência meta-sedimentar escalonada entre o Neoproterozóico (Ediacariano) e o Câmbrico superior. Na região de Vila Boim, surge uma janela estratigráfica onde toda a sequência se encontra exposta (estrutura de Torre de Cabedal) e onde foi possível colocar em evidência duas fases de deformação Varisca principais. A primeira fase de deformação é gerada em andar estrutural superior e caracteriza-se pela génese de dobras deitadas c...

  10. MR cisternography with three-dimensional fast advanced spin-echo (FASE)

    International Nuclear Information System (INIS)

    Ohgi, Kazuyuki; Yamamoto, Hidefumi; Yokote, Hiroyuki

    2000-01-01

    To evaluate the usefulness of MR cisternography (MRC) combined with various postprocessing techniques and three-dimensional (3D) time-of-flight (TOF) MR angiography, MR cisternograms in 212 patients with various cranial nerve symptoms were retrospectively evaluated. MR examinations were performed with a 1.5 T MR imager using a 3D fast advanced spin-echo (FASE) sequence. Maximum intensity projection (MIP) had the advantage of demonstrating fluid-filled structures such as cerebrospinal fluid (CSF)-internal auditory canal (IAC) and Meckel's cave. Minimum intensity projection (Min IP) was especially useful in delineating neurovascular structures (NVS) in wide CSF space. Addition provided the most well-balanced images of NVS, and was superior to Min IP in the depiction of NVS in narrow CSF space. Virtual endoscopy and volume rendering had the potential to provide additional information in the evaluation of the three-dimensional relationships of NVS. Combination of 3D TOF MRA with MRC was helpful in differentiating arteries, veins, and nerves. With the judicious use of various postprocessing techniques and combined MRA, the value of MRC in the evaluation of patients with various cranial nerve symptoms can be further strengthened. (author)

  11. MR cisternography with three-dimensional fast advanced spin-echo (FASE)

    Energy Technology Data Exchange (ETDEWEB)

    Ohgi, Kazuyuki; Yamamoto, Hidefumi; Yokote, Hiroyuki [Japanese Red-Cross Medical Center, Tokyo (Japan)] [and others

    2000-06-01

    To evaluate the usefulness of MR cisternography (MRC) combined with various postprocessing techniques and three-dimensional (3D) time-of-flight (TOF) MR angiography, MR cisternograms in 212 patients with various cranial nerve symptoms were retrospectively evaluated. MR examinations were performed with a 1.5 T MR imager using a 3D fast advanced spin-echo (FASE) sequence. Maximum intensity projection (MIP) had the advantage of demonstrating fluid-filled structures such as cerebrospinal fluid (CSF)-internal auditory canal (IAC) and Meckel's cave. Minimum intensity projection (Min IP) was especially useful in delineating neurovascular structures (NVS) in wide CSF space. Addition provided the most well-balanced images of NVS, and was superior to Min IP in the depiction of NVS in narrow CSF space. Virtual endoscopy and volume rendering had the potential to provide additional information in the evaluation of the three-dimensional relationships of NVS. Combination of 3D TOF MRA with MRC was helpful in differentiating arteries, veins, and nerves. With the judicious use of various postprocessing techniques and combined MRA, the value of MRC in the evaluation of patients with various cranial nerve symptoms can be further strengthened. (author)

  12. Multi-locus phylogenies of the genus Barteria (Passifloraceae) portray complex patterns in the evolution of myrmecophytism.

    Science.gov (United States)

    Peccoud, Jean; Piatscheck, Finn; Yockteng, Roxana; Garcia, Marjorie; Sauve, Mathieu; Djiéto-Lordon, Champlain; Harris, David J; Wieringa, Jan J; Breteler, Frans J; Born, Céline; McKey, Doyle; Blatrix, Rumsaïs

    2013-03-01

    The four species of the central African genus Barteria show variation in habitat and in degree of association with ants. Whereas B. solida, restricted to submontane forests, attracts opportunistic ants to extrafloral nectar, the three other species, found in lowland rainforests (B. fistulosa, B. dewevrei) and in littoral scrub (B. nigritana), possess stem domatia of varying shapes and degrees of specialisation, hosting either non-specific arboreal ants (B. nigritana, some B. dewevrei) or two large species of ants of the genus Tetraponera Smith, 1852 that are specific to some species of Barteria (B. fistulosa, some B. dewevrei). We aimed to investigate whether this variation represents an evolutionary trend toward increasing specialisation of mutualism or the reduction or loss of myrmecophytic traits. For this, we determined phylogenetic relationships within the genus using DNA sequences (primarily nuclear ITS) and microsatellite genotypes (11 loci) on a large sample of individuals, mostly from Cameroon and Gabon. The two types of markers support an initial dichotomy that groups B. dewevrei with B. nigritana and B. fistulosa with B. solida respectively. Within these pairs, species do not appear reciprocally monophyletic. At microsatellite loci, B. nigritana forms a clade embedded within B. dewevrei; and within both B. solida and B. fistulosa, geographical populations show levels of differentiation similar to that observed between populations of B. solida and B. fistulosa. Geographic distance alone does not account for genetic differentiation between species, which indicates reproductive isolation. Divergence in each of the two pairs implies evolutionary transitions in habitat and in myrmecophytism. Specialised mutualism with specific ant species of the genus Tetraponera has been lost in species found in more marginal habitats. Copyright © 2012 Elsevier Inc. All rights reserved.

  13. Proyecto Integral del río Cachi: estudio definitivo, obras 1era. fase (nivel licitación)

    OpenAIRE

    Corporación de Fomento y Desarrollo Económico y Social de Ayacucho

    1984-01-01

    Presenta un informe técnico que contiene el estudio a nivel licitación y que abarca las obras correspondientes a una primera fase de desarrollo del Proyecto integral río Cachi. En este sentido desarrolla los siguientes temas: información básica del proyecto, obras de derivación y trasvase, central hidroeléctrica Lambras, equipamiento electromecánico de la central, líneas de trasmisión, centros de transformación, sistemas de telecomunicaciones, caminos de acceso, programación y costo de las ob...

  14. Eficacia do metodo Meir Schneider de autocuidado em pessoas com distrofias musculares progressivas : ensaio clinico fase II

    OpenAIRE

    Lea Beatriz Teixeira Soares

    1999-01-01

    Resumo: As pessoas com distrofias musculares progressivas vivem o limite do conhecimento médico e aguardam resultados de pesquisa da prevenção, reabilitação e mesmo a cura dos indivíduos portadores. Nesse contexto discute-se a eficácia do método Meir Schneider de autocuidado (self-healing) baseado em ensaio clínico fase II em 12 pessoas com distrofias musculares progressivas, sob tratamento ambulatorial intensivo e não intensivo. Foram atendidos 7 portadores de Distrofia Muscular Duchenne- DM...

  15. Petrography and geochronology (U/Pb-Sm/Nd) the Passagem Granite, Pensamiento Granitoid Complex, Paragua Terrane, SW Amazon Craton, Mato Grosso, Brazil

    International Nuclear Information System (INIS)

    Jesus, Gisely Carmo de; Sousa, Maria Zelia Aguiar de; Ruiz, Amarildo Salina; Matos, Joao Batista de

    2010-01-01

    The Passagem granite includes stocks, plugs and dikes located in the Ricardo Franco hill - Vila Bela da Santissima Trindade region - state of Mato Grosso, central Brazil. The Passagem Granite is included in the Paragua terrane - SW Amazonian Craton. It consists of isotropic monzogranite, sienogranite and more rarely granodiorites with leucocratic dark gray to white color. These rocks range from hypidomorphic inequigranular to xenomorphic texture, fine to medium grained. Biotite is the only primary mafic present as essential phase and characterize an expanded slightly acid sequence formed by a sub-alkaline magmatism of high-potassium calc-alkaline, slightly peraluminous composition from arc magmatic tectonic environment during a post-collisional period. Mechanism of fractional crystallization of plagioclase, biotite, titanite, apatite and zircon associated with simultaneous crustal assimilation are suggested for the evolution of these rocks. The results support the hypothesis of a post-collisional magmatism in the Paragua terrane at 1284 +- 20 Ma corresponding to the crystallization age of the Passagem granite. This paper propose that Passagem Granite represents as an extension in Brazilian terrane of the Pensamiento Granitoid Complex. (author)

  16. Variação do fluxo sanguíneo da artéria central da retina durante as diferentes fases do ciclo menstrual ovulatório Central retinal artery blood flow variation during menstrual cycle

    Directory of Open Access Journals (Sweden)

    Luiz Carlos Viana

    2007-03-01

    Full Text Available OBJETIVO: avaliar a resistência vascular da artéria central da retina, por meio do fluxo Doppler, nas diferentes fases do ciclo menstrual ovulatório. MÉTODOS: estudo observacional, longitudinal e prospectivo com avaliação de 34 mulheres saudáveis, submetidas a estudo dopplerfluxométrico do fundo do olho para avaliação da resistência vascular da artéria central da retina nas posições sentada e deitada, durante quatro fases do ciclo menstrual: fase folicular inicial, fase folicular média, fase periovulatória e fase lútea média. A confirmação da ovulação no ciclo de estudo foi feita pela dosagem de progesterona sérica na fase lútea média. Foram avaliados os índices de pulsatilidade (IP e de resistência, e as velocidades máxima, mínima e média. RESULTADOS: a idade média foi de 29,7 anos. Não foram observadas diferenças entre os índices obtidos para ambos os olhos; assim, utilizamos as médias dos índices para realizar o cálculo estatístico. Quando comparadas às posições de realização do exame, detectou-se um IP maior na posição sentada; assim, as análises foram avaliadas em separado, respeitando-se a posição da paciente. O IP da artéria central da retina, avaliado com a paciente deitada, variou durante o ciclo menstrual, apresentando-se significativamente mais baixo nas fases folicular média (1,5±0,3 e periovulatória (1,5±0,3 quando comparadas às fases folicular precoce (1,7±0,4 e lútea média (1,7±0,4. Quando a avaliação foi feita com a paciente sentada não foram observadas diferenças para as diferentes fases do ciclo. CONCLUSÕES: num ciclo menstrual ovulatório ocorre diminuição da resistência vascular na artéria central da retina e posterior reversão do efeito, como demonstrado pelas variações do IP.PURPOSE: to evaluate the vascular blood flow of the central retinal arteries using dopplervelocimetry in the different phases of the ovulatory menstrual cycle. METHODS: we performed

  17. Cintilografia de perfusão miocárdica e comprometimento cardíaco na fase indeterminada da doença de chagas

    Directory of Open Access Journals (Sweden)

    Amalia Peix

    2013-02-01

    Full Text Available FUNDAMENTO: A cintilografia de perfusão miocárdica (CPM tem sido utilizada na avaliação da cardiopatia chagásica. OBJETIVO: Investigar o valor da CPM com tomografia computadorizada por emissão de fóton único (gated-SPECT para detectar comprometimento cardíaco precoce em pacientes chagásicos na fase indeterminada, que apresentam anomalias de movimento segmentar detectadas por exame de imagem por Doppler tecidual (IDT strain derivada. MÉTODOS: Foram incluídos 40 indivíduos (idade média: 25 ± 2 anos, 50% homens de uma área endêmica da doença de Chagas e com diagnóstico sorológico positivo. Todos foram submetidos à CPM com gated-SPECT de 2 dias (repouso e estresse e ecocardiografia. RESULTADOS: Trinta indivíduos (75% apresentaram resultados normais. Em três casos (8%, a CPM apresentou resultado ligeiramente anormal e em sete foi ambígua. Em todos os casos com defeitos reversíveis, os segmentos afetados foram coincidentes com aqueles com anomalias de movimento. Foi encontrada redução na fração de ejeção ventricular esquerda (FEVE > 5% (ΔLVEF% < -5 pós-estresse em 11 dos 40 indivíduos (28%. Tanto o desvio padrão fasederivado como a largura da banda do histograma mostraram diferença significativa entre o pós-estresse e a fase de repouso. Em ambos os casos, houve ligeira dessincronia em repouso normalizado no pós-estresse. CONCLUSÃO: Uma abordagem estresse-repouso com gated-SPECT é válida para detectar alterações miocárdicas precoces, bem como dessincronia intraventricular na fase indeterminada da doença de Chagas em pacientes com anomalias no movimento segmentar previamente detectadas pela IDT strain derivada.

  18. Providing Meaningful Learning for Students of the Sixth Grade of Middle School: a Study on the Moon Phases. (Breton Title: Propiciando Aprendizagem Significativa Para Alunos do Sexto Ano do Ensino Fundamental: um Estudo sobre as Fases da Lua.) Propiciando el Aprendizaje Significativo Para Alumnos del Sexto Nivel de la Educación General Básica: un Estudio sobre Las Fases de la Luna

    Science.gov (United States)

    Darroz, Luiz Marcelo; Samudio Pérez, Carlos Ariel; da Rosa, Cleci Werner; Heineck, Renato

    2012-07-01

    We relate in this article a didactic experience studying the moon phases with a group of middle school students of a private school of the municipality of Passo Fundo, RS. Based on David Ausubel's Meaningful Learning Theory, we have sought to develop a proposal following a didactic model which simulates the phases of the Moon, as based on the previous conceptions of the students. The signs of learning were evidenced by means of memory registries of the activity. From the obtained results we believe that the proposal achieved its goals, since the students were able to identify, differentiate and transfer the phenomenon of the moon phases to new contexts. Thus, it is concluded that a methodology focused on a meaningful content for the students is fundamental to the construction and genuine grasping of what is being learned. Neste artigo, relata-se uma experiência didática de estudo das fases da Lua com uma turma do 6° ano do Ensino Fundamental, de uma escola privada do município de Passo Fundo, RS. Tendo como fundamentação teórica a Teoria da Aprendizagem Significativa de David Ausubel, buscou-se desenvolver a proposta a partir de um modelo didático que simula as fases da Lua e com base nas concepções prévias dos estudantes. Os indícios da aprendizagem foram constatados através de registros de memórias da atividade. Pelos resultados apresentados, acredita-se que a proposta alcançou seus objetivos, uma vez que os estudantes conseguiram identificar, diferenciar e transferir o fenômeno das fases da Lua para novos contextos. Assim, conclui-se que uma metodologia com enfoque em um conteúdo significativo ao estudante é fundamental para a construção e compreensão genuína do que está sendo aprendido. En este artículo se relata una experiencia didáctica de estudio de las fases de la Luna con una clase de 6º año de la educación general básica de una escuela privada del municipio de Passo Fundo, RS. Teniendo como fundamentación teórica la Teor

  19. Heterose em suínos na fase de aleitamento

    Directory of Open Access Journals (Sweden)

    José Bento Sterman Ferraz

    1991-12-01

    Full Text Available Visando avaliar o ganho de produtividade, advindo da heterose, no peso de suínos em fase de aleitamento, analisaram-se os pesos ao nascimento(PO, 21 dias de idade (P21 e desmama (PD de 746leitões, sendo 201 da raça Landrace, 136 Wessex-Saddleback e 409 mestiços, pelo método dos quadrados mínimos, considerando-se, ainda, os efeitos fixos de época e ano de nascimento, ordem do parto, sexo do leitão e tamanho da leitegada, além de raças paterna e materna e suas interações. Os efeitos não genéticos tiveram influência significativa em quase todas as características. Os mestiços mostraram, em geral, pesos superiores aos puros, com estimativas de heterose de 2,6% para PO, 9,7% para P21 e 13,9% para PD, indicando a importância da herança não aditiva à medida que os leitões ficam menos dependentes de suas mães. Os efeitos de interação entre as raças paterna e materna foram cada vez maiores com o avançar da idade. Os resultados indicam haver ganho de produtividade coma utilização deste tipo de cruzamento.

  20. Evaluación ambiental basado en el análisisdel ciclo de vida (ACV) en la fase de construcción de una edificación en cataluña

    OpenAIRE

    Ortiz, O.; Pasqualino, J.; Castells, F.

    2010-01-01

    Mediante la aplicación de la metodología del Análisis del Ciclo de Vida es posible evaluar el impacto ambiental dela fase de construcción a partir de los materiales de construcción, transporte, energía, y la gestión de residuos. Por lo tanto, un caso de estudio de una construcción en Cataluña ha sido aplicado. Toda la masa de materiales usados durante el ciclo de vida de la fase de construcción fue determinado en 1.88E+03 kg/m2 del cual la estructura representa el 41%, cimientos 25% y cerrami...

  1. Prótesis total. Una innovación para el registro de trayectorias condíleas en la fase de plancha base y rodetes

    OpenAIRE

    Salsench Cabré, Juan; Samsó Manzanedo, Jorge; Nogueras Bayona, Joaquim

    1993-01-01

    Se hace una revisión bibliográfica del registro de trayectorias condíleas en la construcción de prótesis totales. Se presenta un nuevo método sencillo y eficaz, para su registro en la fase de planchas base y rodetes.

  2. Tectonomagmatic evolution of the proto Andean Margin: Geochemical characterization and zircon U-Pb geochronologic constraints from the Ecuadorian Eastern Cordilleran granitoids

    Science.gov (United States)

    Buchwaldt, R.; Toulkeridis, T.

    2013-05-01

    The timing of pan-Pacific Gondwanide Orogeny in the proto-Andes, and its driving mechanisms are still highly debated and relies predominantly upon whole-rock Rb-Sr and K-Ar chronology and rudimentary mineralogy and geochemistry. In order to decipher these uncertainties we have studied the composition, age and provenance of granitoids along the strike of the Eastern Cordillera of Ecuador and related these deep-seated and surface tectonic processes attending the Late Cretaceous-Palaeogene history of the northern Andes. The plutonic rocks constitute a metaluminous to peraluminous (A/CNK ~ 0.8-1.2), calc-alkaline suite. A unimodal and wide compositional range of the intrusives (49-78 wt. % SiO2) is characteristic of this I-type orogenic suites. Mantle-normalized trace element patterns reveal typical subduction-related signature. Chondrite-normalized REE patterns do not show significant HREE fractionation suggesting the absence of high-pressure residual mineralogy in the source and formation in a "normal thickness", garnet-free crust. Slight Eu anomalies, lowering Sr contents, and concave-up REE patterns of samples dioritic in composition indicate a model involving fractionation of plagioclase, amphibole and pyroxene from a basaltic parent. The analyzed zircon crystals are colorless - transparent ranging in size from 50 to 250 μm. In CL images, 95% of the zircons exhibit oscillatory zonation, characteristic of a magmatic origin. This observation is consistent with the REE zircon composition showing a are characteristic steep positive slope from La to Lu with a significantly positive Ce-anomaly and slight negative Eu-anomaly. There is very little variation in Hf isotopic composition with most of the crust maintains near chondritic Zr/Hf ratios of around 35-40. Our results indicate the development of two tectonic episodes; with the first varying between 210-250 Ma and the second approximate 170-180 Ma. These results are consistent with similar events observed throughout

  3. Obtention of the pressed states by canonic transformations in the quantum space phase; Obtencion de estados comprimidos mediante transformaciones canonicas en el espacio fase cuantico

    Energy Technology Data Exchange (ETDEWEB)

    Zuniga Segundo, A. [Instituto Politecnico Nacional, Mexico, D.F. (Mexico)

    2001-10-01

    In this work we introduce squeezed states with real and complex squeezing parameters directly obtained in the coherent-representation of the harmonic oscillator in quantum phase space. By means of the Fourier transform, we recover the usual coordinate states and compare these states with those obtained by another method in the coordinate representation. In addition we also describe numerically its time evolution in quantum phase space and the variances Q and P. [Spanish] En este trabajo presentamos estados comprimidos con parametros de compresion reales y complejos, obtenidos directamente en la representacion de estado coherente del oscilador armonico en el espacio fase cuantico. Por medio de una transformada de Fourier recuperamos los estados en la representacion de coordenadas y los comparamos con aquellos obtenidos por otro metodo. Ademas describimos numericamente sus evoluciones temporales en el espacio fase cuantico y calculamos las varianzas de Q y P.

  4. Mass changes during hydrothermal alteration/mineralization in the gold-bearing Astaneh granitoid, western Iran

    Science.gov (United States)

    Zahra Afshooni, Seyedeh; Esmaeily, Dariush

    2010-05-01

    The Astaneh granitoid massif, located in western Iran, is a part of Sanandaj-Sirjan structural Zone. This body, mainly consist of granodioritic rocks, is widely affected under hydrothermal alteration and four alteration zones including phyllic (sericitic), chloritic, propylitic and argillic zones could be identified in this area. Four main mineralization- related alteration episodes have been studied in terms of mass transfer and element mobility during the hydrothermal evolution of Astaneh deposit. In order to illustrate these changes quantitatively, isocon plots have been applied. Isocon plots illustrate that Al, Ti, Ga and Tm was relatively immobile during alteration and that mass were essentially conserved during alteration. Phyllic alteration was accompanied by the depletion of Na and Fe and the enrichment of Si and Cu. The loss of Na and Fe reflects the sericitization of alkali feldspar and the destruction of ferromagnesian minerals. The addition of Si is consistent with widespread silicification wich is a major feature of phyllic alteration. All of the HFSE (except in Y), were enriched but all REEs were depleted in this zone. The overall obtained results show that major oxides such as SiO2, Al2O3, Fe2O3, MnO, MgO, CaO, Na2O, K2O, P2O5 and TiO2 and also LOI show dissimilar behaviors in the different zones. All of the LFSE, HFSE and FTSM (except in Cu and Mo) were depleted in argillic alteration but show dissimilar behaviors in the other alteration zones. The results shown strong depletion in REE, in particular LREE, in all of the alteration facies (except in chloritic zone), equivalent fresh rocks. In chloritic zone, compared with HREE, the LREE represent more enrichment.

  5. THE GEOCHEMICAL CHARACTERISTIC OF MAJOR ELEMENT OF GRANITOID OF NATUNA, SINGKEP, BANGKA AND SIBOLGA

    Directory of Open Access Journals (Sweden)

    Ediar Usman

    2017-07-01

    Full Text Available A study of geochemical characteristic of major elelemnt of granitoid in Western Indonesia Region was carried out at Natuna, Bangka, Singkep and Sibolga. The SiO2 contents of the granites are 71.16 to 73.02 wt%, 71.77 to 75.56wt% and 71.16 to 73.02wt% at Natuna, Bangka, and Singkep respectively, which are classified as acid magma. While in Sibolga the SiO2 content from 60.27 to 71.44wt%, which is classified as intermediate to acid magma. Based on Harker Diagram, the granites from Natuna, Bangka and Singkep as a co-genetic. In other hand the Sibolga Granite show as a scatter pattern. Granites of Natuna, Bangka and Singkep have the alkaline-total (Na2O + K2O between 6.03 to 8.51 wt% which are classified as granite and alkali granite regime. K2O content ranges from 3.49 to 5.34 wt% and can be classified as calc-alkaline type. The content of alkaline-total of Sibolga granite between 8.12 to 11.81 wt% and classified as a regime of syenite and granite. The range of K2O is about 5.36 to 6.94wt%, and assumed derived from high-K magma to ultra-potassic types. Granites of Natuna, Bangka and Singkep derived from the plutonic rock types and calc-alkaline magma, while Sibolga granite magma derived from K-high to ultra-potassic as a granite of islands arc. Based on the chemical composition of granite in Western Indonesian Region can be divided into two groups, namely Sibolga granite group is representing the Sumatera Island influenced by tectonic arc system of Sumatera Island. Granites of Bangka and Singkep are representing a granite belt in Western Indonesian Region waters which is influenced by tectonic of back arc.

  6. Diagrama de fases temperatura-campo magnético de cadeias quânticas ferrimagnéticas

    OpenAIRE

    SILVA, Wellington Moreira da

    2015-01-01

    O trabalho consiste no estudo de cadeias quânticas ferrimagnéticas associadas a compostos ferrimagnéticos quase-unidimensionais de spins mistos s − S, com s = 1/2 e S = 1. Estudamos as fases induzidas pela aplicação de um campo magnético, B, e efeitos de temperatura, T; em particular as excitações de baixa energia e as curvas de magnetização em função de B. A modelagem teórica e realizada através do hamiltoniano de Heisenberg com acoplamentos de superexchange antiferromagnéticos, J, entre sít...

  7. Efectivitat de la hipoteràpia en persones amb demència tipus Alzheimer de fase lleu.

    OpenAIRE

    Beà Muro, Laura

    2015-01-01

    La hipoteràpia és més efectiva que un programa convencional d’estimulació cognitiva en el tractament de pacients amb demència tipus Alzheimer de fase lleu no institucionalitzats? En l’actualitat, no existeix cap tractament que detingui l'avanç de la malaltia d'Alzheimer (MA). Les teràpies farmacològiques en persones que pateixen la MA en estadi lleu i moderat es complementen cada vegada amb major freqüència amb tractaments no farmacològics. L'objectiu és el de minimitzar l'impacte neurodeg...

  8. Determination of emplacement mechanism of Zafarghand granitoid Pluton (Southeast of Ardestan by using anisotropy of magnetic susceptibility method (AMS

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    Mahmoud Sadeghian

    2017-03-01

    Full Text Available Zafarghand granitoid pluton with compositional range from gabbro to granite and early to middle Miocene age cropped out about 35 km of SE Ardestan. This pluton intrudedthe Eocene volcanic and volcanosedimentary rocks of the Urumieh - Dokhtar structuralzone. In this research, for the first time, the emplacement mechanism of Zafarghandgranitoidic pluton method has been investigated using of anisotropy of magneticsusceptibility (AMS. Based on field observations, as well as petrography andinterpretations of magnetic parameters, Zafarghand pluton divided into 5 domains (1A,1B, 2, 3, 4 and 5. Domain 1, in turn, is divided into 1A and 1B. Domains 2 and 4 arelithologically, gabbro to quartzdiorite and have been emplaced first. They have playedas feeder zones. Domains 1A, 1B, 3, and 5 are dominantly granodioritic to graniticcomposition and have been emplaced as a big and low dip magmatic flow (or possibly as a sill. The occurrence of gabbro to quartzdiorite as well as grandiorite, granite andtonalite in the margin borders of the body, are all indication of magma mixing. It isshould be noted that during emplacement of the pluton studied, fractionalcrystallization, magma mixing and crustal contamination contributed to its generationand the evolution as well.

  9. Meningoencefalite na fase aguda do sarampo : relato de seis casos

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    EL-FAR FABIANE

    2000-01-01

    Full Text Available Apresentamos 6 casos de meningoencefalite aguda por sarampo, diagnosticados durante epidemia na cidade de São Paulo, em 1997. Os prontuários dos 6 pacientes foram analisados retrospectivamente. O diagnóstico de meningoencefalite baseou-se nas alterações clínicas e liquóricas, e foi confirmado por sorologia específica. Dos 467 pacientes com sarampo atendidos no Instituto de Infectologia Emílio Ribas nesse período, estes 6 evoluíram com alterações neurológicas e liquóricas durante a fase exantemática, sendo a sonolência e rigidez de nuca os achados mais frequentes. Os pacientes tinham entre 2 meses e 28 anos de idade. O exame do líquor mostrou pleocitose em todos. Não houve correlação entre a severidade do quadro clínico e liquórico com a evolução. Em 4 casos foi necessária internação na unidade de terapia intensiva; destes, 2 foram intubados. Apenas 2 pacientes apresentaram alterações na tomografia computadorizada de crânio. Todos tiveram boa evolução, sem sequelas.

  10. Perfil pragmático de crianças surdas em diferentes fases lingüísticas Deaf children's pragmatic profile in different linguistic phases

    Directory of Open Access Journals (Sweden)

    Ida Lichtig

    2008-01-01

    Full Text Available OBJETIVO: O objetivo deste estudo foi verificar a interferência da fase lingüística no perfil comunicativo de crianças surdas. MÉTODOS: Trinta crianças surdas participaram deste estudo, sendo 15 crianças em fase pré-lingüística e 15 em fase lingüística (independente da modalidade comunicativa - língua oral ou língua de sinais, na faixa etária de 41 a 59 meses. Foram analisadas 30 gravações das habilidades comunicativas da criança, em situação de interação com a examinadora. Foi utilizado o Protocolo do Perfil Pragmático das Habilidades Iniciais da Comunicação para identificar quais as habilidades comunicativas ocorridas e qual a sua freqüência de ocorrência. RESULTADOS: Os dois grupos apresentaram basicamente as mesmas habilidades comunicativas; entretanto, o grupo Lingüístico apresentou maior freqüência de ocorr��ncia, principalmente nas habilidades relativas a intenções comunicativas e respostas para comunicação. CONCLUSÕES: Há relação direta entre a complexidade lingüística (independente da modalidade e o perfil comunicativo da criança surda, ou seja, a criança em fase lingüística apresenta maior freqüência de ocorrência no uso das habilidades comunicativas mais complexas e elaboradas.PURPOSE: The aim of this study was to ascertain and to assess the interference of deaf children's linguistic level in their communicative abilities. METHODS:Thirty deaf children participated in this study, 15 in the pre-linguistic phase and 15 in the linguistic phase, independent of the communicative modality used - either oral or sign language. Their age ranged from 41 to 59 months. Thirty videotape recordings of the deaf children's communicative abilities assessment during their interaction with the examiner were analyzed. The Communicative Abilities Pragmatic Profile was used in order to identify the communicative abilities and their frequency of occurrence. RESULTS: Both groups basically presented the same

  11. Estado nutricional e consumo alimentar de mulheres jovens na fase lútea e folicular do ciclo menstrual Nutritional status and food consumption of young women in the luteal and follicular phases of the menstrual cycle

    Directory of Open Access Journals (Sweden)

    Larissa Almenara Silva dos Santos

    2011-04-01

    Full Text Available OBJETIVO: Avaliar o estado nutricional e a ingestão alimentar de mulheres adultas sadias durante o ciclo menstrual. MÉTODOS: Quarenta e cinco voluntárias foram acompanhadas durante três meses. A avaliação do estado nutricional foi baseada no índice de massa corporal, porcentagem de gordura e água corporal. Foram aplicados seis registros alimentares para análise da ingestão dos grupos de alimentos, usando como base o guia alimentar da pirâmide. Para a observação do sintoma "desejos alimentares", foram utilizados três "mapas de sintomas diários". RESULTADOS: Os valores médios de índice de massa corporal e de porcentagem de gordura corporal apresentaram-se normais em ambas as fases, entretanto foi observado maior percentual de mulheres com água corporal acima do padrão na fase lútea (77%. O consumo de alimentos do grupo complementar foi maior na fase lútea. Todos os outros grupos de alimentos, com exceção do grupo de carnes, apresentaram consumo inferior às recomendações, em ambas as fases. A intensidade do sintoma "desejos alimentares" foi leve durante o ciclo menstrual, não sendo observada diferença significativa entre as fases. O sintoma "desejos alimentares" associou-se positivamente com o aumento da ingestão do grupo complementar na fase lútea. CONCLUSÃO: O ciclo menstrual influencia o comportamento alimentar e leva à retenção hídrica, na fase lútea, em mulheres adultas sadias.OBJECTIVE: This study assessed the nutritional status and food intake of healthy young women during the menstrual cycle. METHODS: Forty-five volunteers were followed for three months. Their nutritional status was determined by body mass index, body fat and total body water. Six food recall instruments were used to evaluate food group intake according to the food guide pyramid. Food cravings were detected by three daily symptom charts. RESULTS: The mean body mass index and body fat were normal in both phases; however, there was a higher

  12. Structural control of weathering processes within exhumed granitoids: Compartmentalisation of geophysical properties by faults and fractures

    Science.gov (United States)

    Place, J.; Géraud, Y.; Diraison, M.; Herquel, G.; Edel, J.-B.; Bano, M.; Le Garzic, E.; Walter, B.

    2016-03-01

    In the latter stages of exhumation processes, rocks undergo weathering. Weathering halos have been described in the vicinity of structures such as faults, veins or dykes, with a lateral size gradually narrowing with depth, symmetrically around the structures. In this paper, we describe the geophysical characterisation of such alteration patterns on two granitoid outcrops of the Catalan Coastal Ranges (Spain), each of which is affected by one major fault, as well as minor faults and fractures. Seismic, electric and ground penetrating radar surveys were carried out to map the spatial distribution of P-wave velocity, electrical resistivity and to identify reflectors of electromagnetic waves. The analysis of this multi-method and complementary dataset revealed that, at shallow depth, geophysical properties of the materials are compartmentalised and asymmetric with respect to major and subsidiary faults affecting the rock mass. This compartmentalisation and asymmetry both tend to attenuate with depth, whereas the effect of weathering is more symmetric with respect to the major structure of the outcrops. We interpret such compartmentalisation as resulting from the role of hydraulic and mechanical boundaries played by subsidiary faults, which tend to govern both the chemical and physical alterations involved in weathering. Thus, the smoothly narrowing halo model is not always accurate, as weathering halos can be strongly asymmetrical and present highly irregular contours delimiting sharp contrasts of geophysical properties. These results should be considered when investigating and modelling fluid storage and transfer in top crystalline rock settings for groundwater applications, hydrocarbon or geothermal reservoirs, as well as mineral deposits.

  13. Professor om brexit-åbning: Det bliver sværere i næste fase

    DEFF Research Database (Denmark)

    Wind, Marlene

    2017-01-01

    Professor og centerleder, Marlene Wind, var den 8. december i Vejle Amts Folkeblad, hvor hun kommenterede på udviklingen i Brexit-forhandlingerne i forlængelse af udmeldingen om, at forhandlingerne er klar til den næste fase. Professor Wind kalder dette for et gennembrud, men pointerer også at de...... videre forhandlinger vil være på EU’s præmisser. De videre forhandlinger vil blandt andet handle om en kommende handelsaftale mellem de to parter, til hvilket professor Wind påpeger, at det kan tage mange år, før man har en sådan i hus. Samtidig vurderer Wind også, at nogle leave-vælgere måske vil blive...

  14. ANÁLISE DAS FINALIZAÇÕES NA FASE ELIMINATÓRIA DA COPA DO MUNDO 2014

    Directory of Open Access Journals (Sweden)

    Augusto Caron

    2015-04-01

    Full Text Available O Futebol mudou muito em relação há algumas décadas atrás, vem sendo cada vez mais motivo de estudos para aprimoramentos técnicos, táticos e físicos. Nota-se muitas maneiras diferentes de jogar, devido a culturas, escolas e estilos. Esse estudo contém grande importância para os profissionais do futebol e pesquisadores, pois trata de um tema atual e avaliou partidas com inúmeras peculiaridades táticas e técnicas.Objetivo: O objetivo do presente estudo foi uma análise das finalizações das equipes classificadas para a fase eliminatória da Copa do Mundo 2014 (das oitavas de final até a final

  15. Un procedimiento para separar, a alta temperatura, la fase líquida del clínker de los sólidos a los que impregna

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    Ruiz de Gauna, Ángel

    1979-12-01

    Full Text Available Not avaible

    Según se ha ido profundizando en el conocimiento del mecanismo de formación de los silicatos cálcicos hidráulicamente activos del cemento portland, se ha ido poniendo de relieve la gran importancia que la composición de la fase líquida del clínker tiene, tanto en la temperatura y velocidad de formación de aquéllos, como en sus características hidráulicas incluyéndose en ellas las mecánico-resistentes. En las propiedades tecnológicas del cemento resultante influye también directamente la composición que a alta temperatura tiene la fase líquida, por cuanto de ella depende su aptitud a la cristalización, y la clase y propiedades de los componentes secundarios que cristalizan en el curso del enfriamiento y son de decisiva influencia en propiedades tan importantes como la velocidad de fraguado y estabilidad de volumen.

  16. La violencia a través de las fases del amor pasional: Porque la pasión también tiene un lado obscuro

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    Omar Eduardo Kú Hernández

    2006-01-01

    Full Text Available La pasión ha sido caracterizada por la alegría, sensación de realización, optimismo, éxtasis y profunda idealización del objeto amoroso (Villanueva Orozco, 2004. Sin embargo, autores como Hatfield y Rapson (1993 reconocen un lado más oscuro teñido de desesperanza, ansiedad y vacío. Por su parte, Sánchez Aragón (2004 propone un continuo del amor pasional que va de la atracción al amor desesperado, en donde el matiz negativo se va intensificando básicamente durante el amor obsesivo en donde hay una falta de mutualidad en el sentimiento. Así, la violencia puede surgir y con ello facilitar la presencia de actos dañinos a las personas y a la relación romántica. Con base en esto, el presente trabajo tuvo por objetivos: a identificar las posibles diferencias en términos de atracción, enamoramiento, amor obsesivo y amor desesperado en receptores y ejecutores de violencia en la pareja, y b conocer la posible relación entre la violencia y las fases del continuo del amor pasional. Para ello se trabajó con una muestra de 518 personas residentes de la Ciudad de México a quienes se les aplicó: 1 Escala Multifacética del Amor Pasional (Sánchez Aragón, 2006 y 2 Escala de Violencia en la Pareja (Cienfuegos Martínez, Sánchez Aragón y Rivera Aragón, en prensa. Los resultados muestran efectos diferenciales en las primeras dos fases y correlaciones signi- ficativas principalmente entre los factores de violencia y las fases de amor obsesivo y amor desesperado.

  17. Estudio del Sistema Li2SO4 – Na2SO4. Diagrama de fases y caracterización del LiNaSO4

    Directory of Open Access Journals (Sweden)

    Font-Bardia, M.

    2004-08-01

    Full Text Available An exhaustive study of the phase diagram of binary system Li2SO4-Na2SO4 is presented. Phase diagram was determined using thermo-X-ray diffraction in powder samples and calorimetry ATD. A new phase with formula Li2-xNaxSO4 has been obtained, with 1 ≤ x ≤ 1.22. The crystal structure of β-LiNaSO4 was determined from single-crystal X-ray diffraction. This study shows that the crystals usually become twinned when the growth is by solution; which explains the poor spontaneous polarization. The Raman dispersion of Li2SO4, Na2SO4 and LiNaSO4 compounds is explained from the structural data. The measurements have been made at different heating and cooling rate.Se presenta un estudio exhaustivo del diagrama de fase del sistema binario Li2SO4-Na2SO4. El diagrama de fases se determinó mediante termo-difractometría de rayos-X en muestras de polvo y calorimetría ATD. Se obtiene una nueva fase de fórmula Li2-xNaxSO4, con 1 ≤ x ≤ 1.22. La estructura cristalina de β-LiNaSO4 se determinó por difracción de rayos-X sobre un monocristal. Este estudio muestra que los cristales usualmente se maclan cuando el crecimiento es por solución, lo cual explica la baja polarización espontánea. Se explica la dispersión Raman de los compuestos Li2SO4, Na2SO4 y LiNaSO4, a partir de los datos estructurales. Las medidas experimentales se han efectuado a diferentes velocidades de calentamiento y enfriamiento.

  18. Perspectivas de utilización de los métodos de modulación digital con fase continua en los sistemas de telecomunicaciones modernos

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    Germán Castellanos

    1993-01-01

    Full Text Available Se describen los principales tipos de modulación digital con envolvente constante, que se están desarrollando en sistemas de telecomunicaciones, entre ellos la modulación de fase cuaternaria (QPSK y OQPSK. La modulación de fase continúa que presentan mejores propiedades con respecto a otros tipos digitales. Por ejemplo, mayor fidelidad en radiocanales no lineales (caracterfsticos en la telecomunicación móvil celular y vía satélite, menores niveles de energía fuera de banda, etc. En especial se describen las señales MSK y su variedad con filtración preliminar gaussiana GMSK que se emplean ampliamente en los sitemas de comunicación móbil celular digitales, por poseermenores mayores niveles de energía dentro de la banda de trabajo, fidelidad potencial máxima, mejor compatibilidad electromagnética con otros radiosistemas, etc. Se analizan las principales tendencias de desarrollo de los tipos de modulación digital MSK.

  19. Desempenho do cafeeiro Icatu vermelho sob ação de biorregulador aplicado em fases reprodutivas da cultura

    Directory of Open Access Journals (Sweden)

    Nídia Raquel Costa

    2010-08-01

    Full Text Available Com o objetivo de avaliar o efeito do biorregulador Stimulate® aplicado em diferentes fases da cultura do cafeeiro durante seu ciclo reprodutivo, foi instalado o experimento em uma propriedade comercial localizada no município de Garça - SP, com plantio de café da variedade Icatu vermelho, com idade de 4 anos e espaçamento 4 x 2 m. O delineamento experimental foi o de blocos ao acaso, com 4 repetições, 10 plantas por parcela e 13 tratamentos. Foram marcados 4 ramos plagiotrópicos, de maneira aleatória em 5 plantas, no terço mediano das mesmas, para se proceder as avaliações desejáveis, desde o florescimento até a colheita do café. A aplicação de Stimulate® via foliar durante diferentes fases fenológicas do desenvolvimento reprodutivo do cafeeiro foi promissor para elevar parâmetros qualitativos e quantitativos, como porcentagem de pegamento de frutos após o florescimento, garantindo maior fixação até seu completo desenvolvimento; maior produção de nós nos ramos plagiotrópicos; maior crescimento de frutos e sementes; elevação da produtividade da cultura, além de alterar a maturação dos frutos, acelerando este processo com possibilidade de antecipação da colheita, com maior proporção de frutos tipo cereja, ideal para proporcionar melhor qualidade do café.

  20. Ventajas de los materiales de cambio de fase en la comercialización de productos de la pesca

    OpenAIRE

    Domínguez Alonso, Manuel; García Rodríguez, Carmen; Arias Carrillo, José Maria

    2012-01-01

    Se exponen y discuten las ventajas que se han encontrado en el empleo de los materiales de cambio de fase o PCM, en la comercialización de todos los tipos de productos acuáticos, sobre todo: en el enfriamiento de especies marinas de difícil comercialización, en su transporte hasta puerto, en los de larga duración y en vivo. Se describen los PCM más adecuados y las técnicas de su empleo para las principales aplicaciones que se han visto, facilitando los sistemas de cálculo para su comer...

  1. Resposta de fase aguda e níveis séricos de magnésio em pacientes hospitalizados

    OpenAIRE

    Cunha,D. F. da; Bianco,M. de P.; Lenza,R. da M.; Cunha,S. F. de C. da

    1999-01-01

    OBJETIVO: A resposta de fase aguda (RFA), caracteriza-se por proteólise, com hipotrofia da massa celular corporal, hiperglicemia, retenção hídrica e disfunção renal, fenômenos que potencialmente afetam os níveis de magnésio (Mg++) sérico. O objetivo do estudo foi comparar os níveis séricos de Mg++ entre pacientes hospitalizados, com ou sem RFA. MÉTODOS: Obteve-se um banco de dados do mainframe do Hospital-Escola contendo informações sobre dosagens bioquímicas simultâneas de creatinina, glicos...

  2. Atratividade de diferentes iscas e sua relação com as fases de desenvolvimento ovariano em calliphoridae e sarcophagidae (insecta, diptera Attractiveness of differents baits and its relation with ovarian development fases in Calliphoridae ano Sarcophagidae (Insecta, Diptera

    Directory of Open Access Journals (Sweden)

    José Mario d'Almeida

    1994-01-01

    Full Text Available Attrativeness of differents baits (fish, faeces and banana upon ovarian development fases of Calliphoridae and Sarcophagidae was evaluated. The insects were captured in Distrito Federal (urban area and Rio de Janeiro city (beach, zoological garden, urban area and Tijuca forest. The most frequent species captured were: Calliphoridae - Chrysomya megacephala (Fabricius, 1794 78,9% and Chtysomya puloria (Wiedemann, 1818 5,4% - and Sarcophagidae - Sarcophagula Wulp, 1887 2,3% and Peckya chrysostoma (Wiedemann. 1830 2,2%. Fish was more attractive to females of Calliphoridae flies in intense ovarian vitelogenesis, although banana atracted more flies with mature eggs. Faeces and fish were more atractive for Sarcophagidae in the beggining of vitelogenesis.

  3. Una revisión bibliográfica sobre hidrodecloración catalítica en fase líquida

    OpenAIRE

    Ardila Arias, Alba Nelly; Montes de Correa, Consuelo

    2010-01-01

    Se presenta una visión general de la problemática actual de las emisiones de compuestos organoclorados lige-ros, y las principales características y ventajas de la hidrodecloración catalítica en fase líquida. Se describen los mas importantes catalizadores utilizados en el proceso de hidrodecloración, haciendo énfasis en los de paladio; su naturaleza, actividad y desactivación. Se explica detalladamente el efecto de varios parámetros, tales como: HCl producido, solvente, base y agente reductor...

  4. Morfogénesis de la fase sexual de seis especies mexicanas del género Dryopteris (Dryopteridaceae): Parte II

    OpenAIRE

    Blanca Pérez-García; Aniceto Mendoza; Irma Reyes Jaramillo; Ramón Riba

    2001-01-01

    Se describe y se compara la morfogénesis de la fase sexual de seis especies mexicanas de Dryopteris. Las esporas de todas las especies estudiadas son monoletes y elipsoidales, la perina es plegada, de color pardo claro a pardo obscuro, su superficie es rugosa y de contornos tuberculados. El patrón de germinación es tipo Vittaria y el desarrollo protálico es tipo Aspidium. Los gametangios son del tipo característicos de los helechos leptosporangiados. Se desarrollaron esporofitos en cinco de l...

  5. Petrology and geochemistry of Granitoids at Khanchay-Aliabad region, Tarom sub-zone, East of Zanjan

    Directory of Open Access Journals (Sweden)

    Arefeh Saiedi

    2018-03-01

    Full Text Available Khanchay-Aliabad area as a part of Tarom magmatic belt contains some shallow depth intrusions which are intruded the Eocene volcanic- sedimentary rocks and have very close association with Cu mineralization. The Eocene volcanic- sedimentary rocks include alternation of basalt, basaltic andesite and andesite, various kinds of tuff, tuffaceous sandstone, sandstone, siltstone and occasionally shale. Petrographical studies demonstrate that intrusions are pyroxene quartz monzonite and olivine gabbro in composition. The Khanchay pyroxene quartz monzonite have porphyritic to porphyroidic, hetero-granular to sereitic, ophitic and sub- ophitic textures and composed of plagioclase, clinopyroxene, hornblende, quartz, K-feldspar and biotite. The Aliabad pyroxene quartz monzonite shows porphyritic to porphyroidic textures composing of plagioclase, clinopyroxene and hornblende in the quartz- feldspatic matrix. The Khanchay olivine gabbro is characterized by the presence of coarse grained granular, ophitic and sub- ophitic textures as well as the occurrence of plagioclase, clinopyroxene and olivine. Geochemical studies indicate that the Khanchay- Aliabad pyroxene quartz monzonitic intrusions have SiO2 content varying from 59.58 to 61.34 %. These intrusions have high- K calc- alkaline nature and are classified as I-type metaluminous granitoids. Their similar patterns on spider diagrams are indication of genetic relation of these intrusions. On these diagrams LILEs (Ba, K, Th and Pb enrichment along with negative anomalies of HFSEs (Nb and Ti are observed. Moreover, the Chondrite normalized REE patterns demonstrate LREE enrichment with high ratio of LREE/HREE and Lan/Ybn ratio ranging from 3.08 to 3.72. The overall  field investigation, petrological and geochemical studies as well as  tectonic setting discrimination diagrams confirm that the Khanchay- Aliabad high-K intrusions were formed from a subduction related metasomatized lithospheric mantle in a post

  6. Caracterización térmica de placas de yeso con material de cambio de fase incorporado

    Directory of Open Access Journals (Sweden)

    García, A.

    2010-09-01

    Full Text Available In this research the suitability of including PCM in gypsum boards to multiply their thermal energy storage capacity is demonstrated. So the thermal storage capacity of several constructive materials is evaluated and compared, whose use and application is similar to the gypsum boards: paneling of a wall and partition wall. An experimental facility has been designed and operated for the study of the new compound material, exchanging heat with air. It has been studied the influence of different parameters and system variables (working temperature, air velocity, display of the phase change materials, and location in the building…, to establish a latent heat storage system which –complemented with passive strategies (solar gains, natural ventilation– reduces the acclimatization energy consumption in buildings. So, here we demonstrate that a gypsum board including a 44.5% in weight of phase change materials (PCM is able to store –in a 1.5 cm thick- 5 times the thermal energy of a current gypsum board –with the same thickness–, and the same amount to 11.5 cm brick layer, in the comfort temperature range (20-30 ºC, maintaining the mechanical and physical properties required by the regulations in force.

    En este trabajo se demuestra la idoneidad de incorporar materiales de cambio de fase en placas de yeso para incrementar su capacidad de almacenamiento térmico. Para ello se evalúa y se compara la capacidad de almacenamiento térmico, de diferentes elementos constructivos cuyo uso y aplicación es similar a la de las placas de yeso: trasdosado y tabique separador. Se ha disenado y puesto en funcionamiento una instalación experimental que simula las condiciones de contorno que se producen en una estancia donde estén instalados los diferentes materiales y sistemas constructivos. Se ha estudiado la influencia de diferentes para´metros y variables del sistema (temperatura de trabajo, velocidad del aire, presentación de los

  7. Textures, trace element compositions, and U-Pb ages of titanite from the Mangling granitoid pluton, East Qinling Orogen: Implications for magma mixing and destruction of the North China Craton

    Science.gov (United States)

    Hu, Hao; Li, Jian-Wei; McFarlane, Christopher R. M.; Luo, Yan; McCarron, Travis

    2017-07-01

    The Mangling granitoid pluton, located along the southern margin of the North China Craton, consists mainly of monzogranite with minor amounts of diorite. The monzogranite contains abundant mafic microgranular enclaves (MMEs) and is intruded by numerous mafic dikes, providing an opportunity to study magma mixing and its role in the formation of the granitioid pluton. In this paper, we present in situ analysis of U-Pb isotopes and trace element compositions of titanite from the MMEs and the host monzogranite using Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry to document the role of magma mixing in the formation of the Mangling granitoid pluton. Titanite grains from the MMEs (type 1) are euhedral with patchy zoning, whereas the varieties from the closely associated host monzogranite are euhedral and consist of two types (type 2 and type 3). Type 2 titanite is more abundant and has oscillatory zoning without Fe-Ti oxide inclusions, whereas type 3 grains commonly have Fe-Ti oxide inclusions in the core that is rimmed by inclusion-free overgrowths with weak oscillatory zoning. Titanite from monzogranite without MMEs (type 4) is euhedal and has weak oscillatory zoning, with rare ilmenite inclusions in the core. Titanite from a mafic dike intruding the monzogranite (type 5) is anhedral and has sector zoning. Titanite grains from MMEs and the monzogranite (type 1, 2 and 3) have U-Pb ages that are indistinguishable (149 ± 1 Ma, 148 ± 1 Ma and 148 ± 2 Ma, respectively). These ages agree well with zircon U-Pb ages of 150 ± 1 Ma, 150 ± 1 Ma and 149 ± 1 Ma for the MMEs, host monzogranite, and mafic dike, respectively. The age consistency thus confirms coeval formation of the MMEs, the host monzogranite, and the mafic dikes, demonstrating a mafic magmatic, rather than extraneous or restitic origin for the MMEs. Titanite grains from the MMEs (type 1) and mafic dike (type 5) have much lower Al2O3, REE, Nb/Zr, Y/Zr, and Lu/Hf, but higher (Ce + Nd)/Y and La

  8. Determinación de la composición mineralógica del clínker por microscopía cuantitativa, disolución de fases y difracción de rayos X

    Directory of Open Access Journals (Sweden)

    Triviño, F.

    1983-09-01

    Full Text Available A comparative study has been done about the use of three methods: Microscopic, Dissolution of Phases and X-Ray Diffraction, for the determination of the mineralogical composition of clinker, XRD appears (just as it is shown in this paper as a complicated method which does not guarantee a good determination of C3A. The consecutive dissolution of phases whith methanol and salicylic acid and saccharose is a simple, cheap and reliable alternative method. The dissolution of phases with salicylic acid is a good method to determine the whole of silicates and liquid phase. Optic microscopy (reflected light is a method of determining bi and tricalcium silicates but the results so given are unreliable. Varations which could improve these methods are indicated.

    Se hace un estudio comparativo del empleo de tres métodos, microscópico, disolución de fases y difracción de rayos X, en la determinación de la composición mineralógica del clínker. Se revela DRX (tal y como se desarrolla en este trabajo como un método poco fiable en la determinación del C3A y además es complicada. La disolución sucesiva de fases con metanol-salicílico y sacarosa es una alternativa sencilla, económica y fiable. La disolución de fases con salicílico es un buen método en la determinación total de silicatos y fase líquida. La microscopía óptica de luz reflejada es un método para la determinación de los silicatos bi y tricálcicos, aunque da resultados poco fiables. Se indican variaciones que mejoran los métodos.

  9. Modelación en coordenadas de fase del transformador monofásico con derivación central en el secundario; Modeling in phase-coordinates of the single-phase transformer with center tap in the secondary winding

    Directory of Open Access Journals (Sweden)

    Ignacio - Pérez Abril

    2013-10-01

    Full Text Available Existe un modelo en la literatura para representar el transformador monofásico con derivación central en el secundario. No obstante, dicho modelo representa toda la impedancia del transformador en el secundario, lo que difiere de la realidad. La distribución de la impedancia del transformador entre el primario y ambas secciones del secundario tiene una gran influencia en la magnitud de la corriente de cortocircuito de una fase a la derivación central del secundario. Esta corriente supera ampliamente la corriente de cortocircuito de fase a fase en transformadores con devanados entrelazados. El presente trabajo desarrolla el modelo en coordenadas de fase del transformador monofásico con derivación central en el secundario. El modelo desarrollado se prueba con varios ejemplos que demuestran la conveniencia de emplear el modelo presentado para analizar la carga desigual de ambas secciones del devanado secundario o el cortocircuito de una fase a la derivación central del secundario.There exists a model in the literature to representing the single-phase transformer with center tap in the secondary winding. However, this model represents all the impedance of the transformer in the secondary winding, which differs from practice. The distribution of the impedance between primary and the both sections of the secondary winding has a great influence over the magnitude of the short circuit current from a phase to the center tap. This current is much greater than the phase to phase short circuit current in transformers with interlaced windings. The present paper develops a model in phase coordinates for the single-phase transformer with center tap in the secondary winding. The developed model is tested with several examples that shown the convenience of the use of the presented model to analyze the unequal load in both sections of the secondary or the short circuit from a phase to the center tap of the secondary.

  10. As relações entre o Brasil e os Estados Unidos em perspectiva histórica: problemas das relações bilaterais na fase contemporânea

    Directory of Open Access Journals (Sweden)

    Paulo Roberto Almeida

    2011-02-01

    Full Text Available A presente análise busca realizar uma breve descrição do desenvolvimento histórico das coesções entre Brasil e Estados Unidos e, a partir disso, delinear suas implicações para a fase contemporânea.

  11. Níveis de cálcio e fósforo disponível em rações com fitase para frangos de corte nas fases pré-inicial e inicial Calcium and available phosphorus levels in diets with phytase for broilers in the pre-starter and starter phases

    Directory of Open Access Journals (Sweden)

    Luziane Moreira dos Santos

    2011-11-01

    Full Text Available Dois experimentos independentes, um na fase pré-inicial (1 a 7 dias e outro na fase inicial (8 a 21 dias de idade, foram realizados com frangos de corte para avaliar níveis de cálcio e fósforo disponível (Pdisp em rações suplementadas com 500 unidades de atividade de fitase/kg de ração. Cada experimento constou de um ensaio de desempenho e outro de metabolismo e foi conduzido em esquema fatorial (3 × 4 + 1, sendo três níveis de Pdisp (0,42; 0,37; 0,32% na fase pré-inicial e 0,39; 0,34; 0,29% na fase inicial, quatro níveis de cálcio (0,94; 0,84; 0,74; 0,64% na fase pré-inicial e 0,88; 0,78; 0,68; 0,58% na fase inicial mais uma ração controle. O controle correspondeu à única ração sem fitase e continha 0,47% de Pdisp e 0,94% de cálcio (fase pré-inicial ou 0,44% de Pdisp e 0,88% de cálcio (fase inicial. Nos ensaios de desempenho, aos 7 e aos 21 dias de idade, foram avaliados o consumo de ração, o ganho de peso, a conversão alimentar e o teor de cinzas na tíbia. Nos ensaios de metabolismo, determinaram-se a energia metabolizável aparente corrigida pelo balanço de nitrogênio (EMAn das rações e os coeficientes de digestibilidade da matéria seca (CMMS. Na fase pré-inicial, os níveis de cálcio influenciaram o consumo de ração, a EMAn e o CMMS e, na fase inicial, afetaram o conteúdo de cinzas ósseas, a EMAn e o CMMS. Os níveis de Pdisp influenciaram o teor de cinzas na tíbia, a EMAn e o CMMS na fase pré-inicial e as cinzas ósseas e o CMMS na fase inicial. Adicionando 500 unidades de atividade de fitase/kg de ração, é possível reduzir, respectivamente, os níveis de cálcio e Pdisp para 0,64% e 0,37% na fase pré-inicial e 0,58% e 0,29% na fase inicial, pois essa redução não tem efeito negativo sobre o desempenho e a mineralização óssea dos frangos de corte nessas fases.Two independent experiments, one in pre-starter phase (1 to 7 days and the other in the starter phase (8 to 21 days of age, were

  12. Caracterização reológica das diferentes fases de extrato de inulina de raízes de chicória, obtidas por abaixamento de temperatura Rheological characterization for different phases of inulin extract from chicory roots, obtained through temperature reduction

    Directory of Open Access Journals (Sweden)

    Juliana T. C. Leite

    2004-04-01

    Full Text Available A inulina é um ingrediente funcional, geralmente empregado na indústria alimentícia como substituto do açúcar ou da gordura. Esse ingrediente pode ser encontrado em diversos produtos vegetais, incluindo as raízes de chicória. Por ser um produto com solubilidade variável com a temperatura, a inulina sofre uma separação de fases ao ser resfriada, originando uma fase precipitada, mais viscosa, e uma fase sobrenadante, de menor viscosidade. O estudo das propriedades reológicas das diferentes fases do extrato de inulina é importante para o projeto de equipamentos, como misturadores e bombas. Neste trabalho, foi estudado o comportamento reológico, para três condições distintas de temperatura (25; 40 e 50 ºC, das fases sobrenadante e precipitada do extrato líquido de inulina, extraído de raízes de chicória por difusão em água quente e resfriado a duas temperaturas distintas (8 e -10 ºC, sofrendo separação de fases. A fase precipitada foi analisada em duas condições: pura e com a adição de agentes microencapsulantes. Todos apresentaram um comportamento linear, semelhante ao dos "Plásticos de Bingham", porém, nem todos se ajustaram a esse modelo.Inulin is a functional food ingredient, generally employed as sugar or fat substitute in food systems. This ingredient can be found in several vegetal products, including chicory roots. As the solubility of inulin is susceptible to temperature changes, the product suffers a fractionalization resulting in two phases when cooled, originating a precipitated phase, more viscose, and a liquid phase, of lesser viscosity. The study of rheological properties of different phases of inulin extract is important for equipment designing, such as mixer and bombs. In this work, rheological behavior at three different temperatures (25; 40 and 50 ºC was determined for liquid and precipitated phases of inulin liquid extract, extracted from chicory roots by hot water diffusion and cooled at two

  13. Repeated granitoid intrusions during the Neoproterozoic along the western boundary of the Saharan metacraton, Eastern Hoggar, Tuareg shield, Algeria: An AMS and U-Pb zircon age study

    Science.gov (United States)

    Henry, B.; Liégeois, J. P.; Nouar, O.; Derder, M. E. M.; Bayou, B.; Bruguier, O.; Ouabadi, A.; Belhai, D.; Amenna, M.; Hemmi, A.; Ayache, M.

    2009-09-01

    The N-S oriented Raghane shear zone (8°30') delineates the western boundary of the Saharan metacraton and is, with the 4°50' shear zone, the most important shear zone in the Tuareg shield. It can be followed on 1000 km in the basement from southern Aïr, Niger to NE Hoggar, Algeria. Large subhorizontal movements have occurred during the Pan-African orogeny and several groups of granitoids intruded during the Neoproterozoic. We report U-Pb zircon datings (laser ICP-MS) showing that three magmatic suites of granitoids emplaced close to the Raghane shear zone at c. 790 Ma, c. 590 and c. 550 Ma. A comprehensive and detailed (158 sites, more than 1000 cores) magnetic fabric study was performed on 8 plutons belonging to the three magmatic suites and distributed on 200 km along the Raghane shear zone. The main minerals in all the target plutons do not show visible preferential magmatic orientation except in narrow shear zones. The AMS study shows that all plutons have a magnetic lineation and foliation compatible with the deformed zones that are zones deformed lately in post-solidus conditions. These structures are related to the nearby mega-shear zones, the Raghane shear zone for most of them. The old c. 793 Ma Touffok granite preserved locally its original structures. The magnetic structures of the c. 593 Ma Ohergehem pluton, intruded in the Aouzegueur terrane, are related to thrust structures generated by the Raghane shear zone while it is not the case of the contemporaneous plutons in the Assodé-Issalane terrane whose structures are only related to the subvertical shear zones. Finally, the c. 550 Ma granite group has magnetic structure related to the N-S oriented Raghane shear zone and its associated NNE-SSW structures when close to them, but NW-SE oriented when further. These NW-SE oriented structures appear to be characteristic of the late Neoproterozoic evolution of the Saharan metacraton and are in relation to the convergence with the Murzuq craton. This

  14. The evolutionary characteristics and study of uranium mineralization conditions of early precambrian basement and old granitoids in Northern Hebei province of China

    International Nuclear Information System (INIS)

    Xia Yuliang; Rong Jiashu; Lin Jinrong; Zheng Maogong; Wen Xiyuan

    1993-05-01

    Based on the systematic studies of petrology, geochemistry and isotope geochronology, the Early Precambrian metamorphic complex in Northern Hebei province of China can be divided into three different series, i.e. granulite series, khondalite series and amphibolitic-felsic rock series. The so called 'magmatic granitoids' in that area are actually some magmagranites with different ages and different geneses, and they are not formed by migmatization. Up to now, the discovered Huaian complex which was formed in 3.5 Ga ago is the oldest nuclear area in the northern margin of North-China Platform. The granulite series, khondalite series and amphibolitic-felsic rock series belong to Early Archaean (>3.0 +- 0.1 Ga), Middle Archaean (>2.7 +- 0.1 Ga) and Later Archaean (>2.4 +- 0.1 Ga) respectively. The geological time scale of the Early Precambrian for Northern Hebei Province has been built. According to the synthetic analyses of various factors there is no prospect of uranium mineralization in the ancient terrain. However, the Mesozoic volcanic basins covering over the Hercynian Period granites would be main goal for looking for large uranium deposits in north part in that area

  15. Pola Sebaran Kelompok Telur Ostrinia furnacalis Guenée (Lepidoptera: Crambidae pada Beberapa Fase Pertumbuhan Tanaman Jagung (Zea mays L.

    Directory of Open Access Journals (Sweden)

    Subiadi Subiadi

    2014-07-01

    Full Text Available A field study was conducted to determine the distribution of egg masses of Ostrinia furnacalis on corn leaves and within corn field. The corn field was divided into three regions: the inner edge closed to other crops and outer edge closed to main road and the middle region. The numbers of egg masses laid were recorded entirely in all corn plants existed (census method. Egg laying period lasted for 34 days, with 11 days from initiation of egg laying to the peak of oviposition and 23 days from the peak to termination of egg laying. The egg masses laid on corn leaves were distributed in aggregation pattern. During eight-opened-leaf to twelve-opened-leaf stages, there were 847 egg masses found, and 80.9% was laid on the sixth-to-ninth leaves. From tasseling to blister stages there were 491 egg masses found of which approximately 80.7% was laid on the seventh-to-11 32.8, and 29.8% of those were found in the inner edge, middle, and outer edge of corn field, respectively. leaves. Egg masses laid within corn field varied, in which 37.4, 32.8, and 29.8% of those were found in the inner edge, middle, and outer edge of corn field, respectively.   Kajian lapang dilaksanakan untuk mengetahui pola sebaran peletakan kelompok telur ngengat Ostrinia furnacalis pada daun tanaman jagung dan penyebarannya pada lahan pertanaman jagung. Lahan penelitian dibagi menjadi tiga kelompok yaitu lahan pinggir dalam berdekatan dengan pertanaman lain, bagian tengah lahan, dan lahan pinggir luar berdekatan dengan jalan raya. Pengamatan kelompok telur dilakukan pada seluruh tanaman jagung (sensus. Periode peletakan telur berlangsung selama 34 hari, dengan periode inisiasi hingga puncak 11 hari dan periode setelah puncak hingga akhir peletakan telur 23 hari. Peletakan telur O. furnacalis pada daun tanaman jagung menyebar secara berkelompok. Pada fase 8 hingga 10 daun telah terbuka sempurna ditemukan sebanyak 847 kelompok telur, 80,9% diantaranya  ditemukan pada daun ke 6–9

  16. Calidad del aire en galpón avícola con ventilación natural durante la fase de pollitos

    Directory of Open Access Journals (Sweden)

    Robinson Osorio H.

    Full Text Available RESUMEN Los pollos de engorde durante la primera fase deben estar protegidos del estrés por frio, especialmente en el inverno, noches y madrugadas frías. Para proteger a los animales, los avicultores han utilizado diferentes estrategias, entre ellas está el uso de varias capas de cortinas para aumentar el nivel de aislamiento térmico y disminuir las pérdidas de calor, disminuyendo también la permeabilidad con el aire externo. En este contexto, es importante dar especial atención a la calidad del aire interno de los galpones avícolas como parte de una producción bajo parámetros de bienestar animal. El presente estudio fue realizado en el municipio de Barbacena, MG, en Brasil, y tuvo como objetivo evaluar la calidad del aire al nivel de los pollos y los trabajadores, específicamente de las concentraciones de amoniaco, dióxido de carbono y monóxido de carbono, en un galpón avícola naturalmente ventilado durante la primera fase de vida de pollos de engorde en el período de inverno, y la influencia del nivel de aislamiento con cortinas laterales sobre las concentraciones de amoniaco. Durante la primera semana experimental, los niveles de amoniaco sobrepasaron los valores aceptables, y se encontró diferencia estadística entre las concentraciones de amoniaco para los diferentes niveles de aislamiento con cortinas laterales.

  17. Transición de fase para modelos diluidos con espines discretos y medidas de Young-Gibbs para el modelo de Ising

    OpenAIRE

    Soprano Loto, Nahuel

    2015-01-01

    Esta tesis contiene dos partes con un tema en común: en cada una de ellas, estudiamos diferentes modelos de mecánica estadística. En la primera parte, estudiamos modelos diluidos de vecinos próximos con espacio de espines finito, donde el grafo subyacente es un subgrafo aleatorio del reticulado d-dimensional. Más precisamente, proporcionamos condiciones suficientes y necesarias para que ocurra co-existencia de fases mediante técnicas de aglomerado aleatorio. En la segunda parte, estudiamos un...

  18. Cuidar de pacientes em fase terminal: a experiência de alunos de medicina

    Directory of Open Access Journals (Sweden)

    Maria Lúcia Araújo Sadala

    2008-03-01

    Full Text Available O objetivo deste estudo foi compreender os significados que alunos de medicina atribuem à experiência de cuidar de pacientes em fase terminal. Os dados foram coletados mediante entrevistas individuais com vinte e quatro estudantes de medicina de uma universidade paulista. As convergências dos depoimentos dos participantes foram agrupadas em três categorias: a deparando-se com o mundo da doença terminal/morte; b relação com o paciente e sua família; c reflexão sobre o cuidar do paciente terminal. Nos depoimentos, os estudantes expressam ansiedade ao cuidar deste tipo de paciente, assim como as dificuldades em lidar com os próprios sentimentos. Consideram-se pouco preparados para relacionar-se com esses pacientes, mas aprenderam com a experiência vivida. Os resultados do estudo apontam para a necessidade de se introduzirem, na formação médica, conteúdos visando desenvolver competências interpessoais e capacidade de reflexão sobre questões de ética e deontologia médica, envolvendo a terminalidade da vida.

  19. Aproximación al control de la fase de vuelo de un dirigible

    Directory of Open Access Journals (Sweden)

    Leonardo Solaque Guzmán

    2008-01-01

    Full Text Available El presente trabajo tiene por objetivo el modelo dinámico de un dirigible (como Karma y UrAn, y la elaboración de un conjunto de leyes de control de velocidad, altitud y dirección cuando el dirigible se desplaza en la fase de vuelo crucero. La primera parte del documento presenta un modelo matemático representativo de las principales dinámicas del dirigible. Luego se muestra una descripción de las principales relaciones de las variables, a partir de un modelado e identificación previos, usados para el planteamiento de modelos reducidos, llamados modelos de control. Una segunda parte está dedicada a la formulación de las estrategias de control, basadas en técnicas PID, GPC y una no Lineal. Estas leyes son planteadas sobre la base del desacople de dinámicas para el vuelo lateral y el vuelo longitudinal. Finalmente se incluyen pruebas de simulación y sobre las estructuras reales.

  20. CFD modelling of an open core downdraft moving bed biomass gasifier; Modelado de un gasificador estratificado de lecho movil de biomasa, utilizando CFD

    Energy Technology Data Exchange (ETDEWEB)

    Rogel-Ramirez, A [Universidad Nacional Autonoma de Mexico, Mexico, D.F. (Mexico)]. E-mail: ARogelR@iingen.unam.mx

    2008-10-15

    This paper contains the description of a bidimensional Computational Fluid Dynamics (CFD), model Developer to simulate the flow and reaction in a stratified downdraft biomass gasifier, whereby Eulerian conservation equations are solved for particle and gas phase components, velocities and specific enthalpies. The model is based on the PHOENICS package and represents a tool which can be used in gasifier analysis and design. Contributions of chemical kinetics and the mixing rate using the EBU approach are considered in the gas phase global homogeneous reactions. The harmonic blending of chemical kinetics and mass transfer effects, determine the global heterogeneous reactions between char and O{sub 2}, CO{sub 2} and H{sub 2}O. The turbulence effect in the gas phase is accounted by the standard {kappa}-{epsilon} approach. The model provides information of the producer gas composition, velocities and temperature at the outlet, and allows different operating parameters and feed properties to be changed. Finally, a comparison with experimental data available in literature was done, which showed satisfactory agreement from a qualitative point of view, though further validation is required. [Spanish] Este estudio describe un modelo numerico bidimensional, basado en Dinamica de Fluidos Computacional (CFD), desarrollado para simular el flujo y las reacciones que ocurren en un gasificador estratificado de flujos paralelos, en el que se resuelven ecuaciones de conservacion Eulerianas para los componentes de la fase gaseosa, la fase solida, velocidades y entalpias especificas. El modelo esta basado en el codigo PHOENICS y representa una herramienta que puede ser utilizada en el analisis y diseno de gasificadores. En las reacciones globales homogeneas se consideran las contribuciones de la cinetica quimica y la rapidez de mezclado, usando el modelo Eddy Brake-UP (EBU). La medida harmonica de la cinetica quimica y la transferencia de masa, determinan las velocidades globales de

  1. Lisina digestível para leitoas em fase de crescimento Digestible lysine for growing gilts

    Directory of Open Access Journals (Sweden)

    Gabriel Cipriano Rocha

    2013-05-01

    Full Text Available Oitenta leitoas (24,2±1,52kg com alto potencial genético para deposição de carne na carcaça foram distribuídas em experimento de blocos ao acaso para avaliar cinco níveis de lisina digestível (Ld (9, 10, 11, 12 e 13g kg-1 durante a fase de crescimento (63 a 103 dias de idade. Os animais foram alojados em pares e alimentados à vontade. No início e ao final do período experimental, as leitoas foram pesadas e submetidas à análise de ultrassom para avaliação da área de olho de lombo (AOL e espessura de toucinho (ET. Os níveis de Ld proporcionaram aumento linear (P0,05 dos níveis de Ld sobre o consumo de ração diário (CRD e ET. Os níveis de 12,0 e 12,5g kg-1 de Ld na dieta, correspondentes, respectivamente, ao consumo de lisina digestível diário (CLdD, de 23,6 e 24,6g, proporcionam os melhores resultados de desempenho e área de olho de lombo de leitoas em fase de crescimento (63 aos 103 dias de idade.Eighty gilts (24.2±1.52kg with high genetic potential for lean gain were used in a randomized complete block design to evaluate five digestible lysine levels (9, 10, 11, 12 and 13g kg-1 during the growing phase (63 to 103 days of age. Gilts were housed in pair and fed their respective diets ad libitum. At the begging and the ending of the experimental period, gilts were weighed and scanned by ultrasound to measure loin area, as well as fat depth. The digestible lysine levels linearly increase (P0.05 of the treatments on the fat depth and feed intake. The digestible lysine levels of 12 and 12.5g kg-1, corresponding to the intake of 23.6 e 24.6g dia-1, provide the best results of performance and loin area of growing gilts (63 to 103 days old.

  2. Fase menstrual na data da cirurgia para câncer de mama: resultados tardios e taxas de sobrevida assintomática Timing of surgery during menstrual cycle, late results and disease-free: survival rates in 130 patients with preast carcinoma

    Directory of Open Access Journals (Sweden)

    Antonio Franco Montoro

    1999-07-01

    Full Text Available Objetivo: verificar se existem diferenças nas taxas de sobrevida para as portadoras de carcinoma de mama, em função da fase do ciclo menstrual vivida pela paciente na data da cirurgia. Pacientes e Métodos: pesquisa retrospectiva de 451 mulheres com câncer de mama, em pré-menopausa, das quais foram selecionados 130 casos com idade entre 26 e 52 anos e acompanhados em seguimento mínimo de 60 meses. Foram operadas 68 na fase folicular e 62 na fase lútea. Foram também analisados os dados referentes ao estádio clínico das neoplasias, ao eventual comprometimento axilar e às determinações quantitativas dos receptores hormonais de estrógenos e de progesterona. Resultados: o seguimento das 130 pacientes demonstrou que 64,6% tiveram sobrevida assintomática após cinco anos e 43% superaram os dez anos. Dividindo os casos em dois subgrupos, segundo o dia da cirurgia executada, as taxas de sobrevida foram diferentes, caindo para 58,8% aos cinco e 36,7% aos dez anos, quando operadas na fase folicular e subindo para 70,9% e 50%, aos 5 e 10 anos respectivamente, durante a fase lútea. Conclusões: neste estudo, as pacientes operadas durante a fase lútea mostraram taxas mais altas de sobrevida do que aquelas operadas na fase folicular. Todavia, os índices foram inferiores aos proporcionados pelos fatores prognósticos clássicos de estado axilar e diâmetro tumoral.Purpose: to offer new data for the conflicting reports which present different prognosis for patients with breast carcinoma, according to the timing of surgery in relation to the menstrual cycle. Patients and Methods: in a retrospective study on 451 premenopausal women with breast cancer, aged between 26 and 52 years, 130 cases were selected and followed for 60 months, at least. Sixty-eight were operated during the follicular phase and 62 in the luteal period, whose findings regarding clinical stages, axillary involvement and estrogen and progesterone hormonal receptor concentrations

  3. U-Pb zircon geochronology, Sr-Nd isotope geochemistry, and petrogenesis of oxidant granitoids at Keybarkuh, southwest of Khaf

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    Ehsan Salati

    2012-10-01

    Full Text Available Keybarkuh area is located 70 km southwest of Khaf, Khorasan Razavi province. The study area is situated in northeastern Lut block. The rock units in the area are Paleozoic metamorphic rocks and Cretaceous to Tertiary subvolcanic intrusions intruded as dike, stock and batholith; their composition varies from granite to diorite. Based on magnetic susceptibility, the intrusive rocks are divided into oxidant and reduced series. In this study, the oxidant intrusions are discussed. These intrusions are mostly high-K to shoshonitic and also meta-aluminous type. Their magma formed in subduction magmatic arc and they belong to I-type granitoid series. Enrichment of Large Ion Lithophile Elements (LILE such as Rb, Cs, K, Ba, and Th relative to High Field Stength Elements (HFSE such as Nb, Zr, and Ti supported the idea. Enrichment of Light Rare Earth Elements (LREE and depletion of Heavy Rare Earth Elements (HREE are also typical of subduction magmatism. Negative anomalies of Eu/Eu* can be attributed to the presence of residual plagioclase in a mantle source and contamination of magma by reduced continental crust. The amount of Nb > 11 ppm, lower ratio of Zr/Nb 0.706, initial 143Nd/144Nd (> 0.512 and εNd (< -3.5 indicate that magma contaminated by reduced continental crust. Hornblende biotite granodiorite porphyry dated using U-Pb zircon geochronology at 43.44 Ma (Middle Eocene. Based on calculated TDM, magma derived from ancient slab with 820 Ma age in the Keybarkuh area, was affected by the highest continental crust contamination during its ascent.

  4. Lunar Phases and Earthly Events: Beliefs from Different Education Levels. (Spanish Title: Fases de la Luna y Acontecimientos Terrestres: Creencia de Distintos Niveles de Instrucción.) As Fases da Lua e os Acontecimentos Terrestres: a Crença de Diferentes Níveis de Instrução

    Science.gov (United States)

    Darroz, Luiz Marcelo; da Rosa, Cleci Teresinha Werner; Alves Vizzotto, Patrick; Becker da Rosa, Álvaro

    2013-12-01

    This article presents the result of a research carried out in the first semester of 2013 with a group of 80 subjects from different education levels. In this research, we sought to investigate the earthly events that this group of people attributes to the phenomenon of lunar phases. For data collection we used semi-structured interviews guided by questions that aimed to keep the focus on subjects of the investigation. Interviews were recorded and transcribed, and the results were compared to scientific studies in the area after being quantitatively and qualitatively analyzed. Research data showed that the Moon and the phenomenon of lunar phases still fascinate and raise the interest of people. However, the lack of knowledge to find correct explanations to the phenomena involving the moon ends up originating a series of beliefs about its influence on earthly events. En este artículo se presenta el resultado de una investigación realizada en el primer semestre de 2013 con a un grupo de 80 individuos de distintos niveles de instrucción. En esta investigación, tratamos de averiguar cuáles son los acontecimientos terrestres que este grupo de personas atribuye al fenómeno las fases lunares. Como instrumento de colecta de datos, se emplearon entrevistas semiestructuradas guiadas por preguntas que trataban de mantener la atención de los entrevistados en el objeto investigado. Las entrevistas fueron grabadas y transcriptas, y los resultados, después de ser analizados cuantitatativa y cualitativamente, fueron confrontados con estudios científicos del área. Los datos de la investigación demuestran que la Luna y de sus fases continúan fascinando y despertando el interés de la población. Sin embargo, la falta de conocimientos para encontrar explicaciones correctas relacionadas a los fenómenos que ocurren con el astro acaba originando una serie de creencias en la población sobre su influencia en los sucesos terrestres. Apresenta-se neste artigo o resultado de uma

  5. Eficácia e tolerância do nitrofurfurilidene (1 na fase crônica da Moléstia de Chagas

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    Newton Neves da Silva

    1974-12-01

    Full Text Available Foram selecionados 25 pacientes chagásicos crônicos que apresentavam sorologia positiva e elevada parasitemia. A 15 deles, durante 120 dias, foi ministrado o Nitrofurfurilidene na dose diária de 8 a 10 mg por quilo de peso. Aos 10 restantes deu-se placebo. No trans e pós-tratamento não se verificaram alterações nas funções hepática, hematopoiética ou renal de caráter iatrogênico. Xenodiagnóstico e provas sorológicas foram realizadas mensalmente. O xenodiagnóstico, nos 15 doentes tratados, aos 60º dias da fase trans-terapêutica, mostrou-se negativo e assim se manteve durante 4 anos, período de tempo que durou a nossa observação. Quanto às reações sorodiagnósticas o mesmo não ocorreu, embora a partir dos 12 meses do término do tratamento o grupo que recebeu a droga tenha passado a apresentar níveis mais baixos de anticorpos. Os A.A. comentam o desacordo entre os achados do xenodiagnóstico e os das provas sorológicas e sugerem uma hipótese para justificá-lo. Concluem que, embora com menos evidência do que nas formas agudas, o Nitrofurfurilidene revela certa eficácia na fase crônica da infecção chagásica.

  6. Proteinograma do soro lácteo de ovelhas da raça Santa Inês em diferentes fases de lactação

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    Vânia F. Lemos

    2013-06-01

    Full Text Available No presente estudo objetivou-se avaliar a influência das fases de lactação sobre o proteinograma do soro lácteo de ovelhas da raça Santa Inês. Foram acompanhadas ovelhas em sistema de criação semi-intensivo com o mesmo manejo higiênico, sanitário e nutricional avaliadas aos 15, 30, 60 e 90 dias após o parto (final da lactação e desmame. Procedeu-se ao exame clínico da glândula mámaria e triagem e cultivo bacteriológico. A triagem do material resultou em 44 amostras de leite de glândulas sadias baseadas no exame negativo simultâneo do CMT e do bacteriológico. Para a obtenção do soro lácteo utilizou-se solução de renina. O soro lácteo foi fracionado em alíquotas e mantido em freezer a -80°C para posterior separação das frações protéicas. Para determinação da proteína total do soro lácteo empregou-se o biureto. A separação das frações protéicas foi realizada utilizando-se eletroforese em gel de poliacrilamida contendo dodecil sulfato de sódio (SDS-PAGE. Foram observadas oito proteínas entre elas lactoferrina, albumina sérica, IgA, IgG ( IgG de cadeia pesada - IgG CP e IgG de cadeia leve - IgG CL, β-lactoglobulina, α-lactoalbumina e as proteínas identificadas como PM 15.000 Da e PM 29.000 Da. Não foi observada diferença significativa nas diferentes fases de lactação nas seguintes proteínas: IgA (P>0,3895, lactoferrina (P>0,1611, PM 29000 (P>0,4879, αlactoalbumina (P>0,0799 e PM 15000 (P>0,4494. Na proteína total (P<0,0022 e nas proteínas albumina (P<0,0377, IgG (P<0,0354 verificou-se variação significativa nos primeiros momentos de observação, na proteína β-lactoglobulina (P<0,0005 verificou-se variação significativa com diminuição dos 15 até 30 dias pós parto com elevação progressiva até a última fase de lactação (90 dias pós parto. A técnica de SDS-PAGE permitiu a quantificação de oito proteínas no soro lácteo de ovelhas sadias. As proteínas identificadas refletem o

  7. Aplicação do Conceito do Ciclo de Vida Organizacional na Definição e Determinação das Fases de uma Organização VarejistaImplementing the concept of Organizational Life Cycle in the definition and Determinations Phases of a Retailers OrganizationAplicación del Concepto del Ciclo de Vida Organizacional en la Definición y Determinación de las Fases de una Organización Minorista

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    BERALDO, Valter

    2004-05-01

    Full Text Available RESUMOO presente artigo aborda a relação entre modelos que analisam as fases do ciclo de vida organizacional e a efetividade organizacional - baseada em uma organização varejista criada no início do século XX, mais precisamente, no dia 29 de novembro de 1913 e que foi reconhecida pela população paulistana, no início dos anos 90, como a loja que tinha a “cara” de São Paulo. A análise dos períodos favoráveis de crescimento e dos períodos críticos possibilitou identificar as características de cada uma das cinco fases identificadas no estudo: crescimento inicial, administrativa, crescimento massificado, expansão e descontrole. Conclui-se pela importância dos conceitos subjacentes que se inserem: na elaboração das fases; na teoria do ciclo de vida organizacional como instrumento que pode contribuir no planejamento estratégico das organizações.ABSTRACTThe present article approaches the relationship among models that analyze the phases of organizational life cycle and the organizational effectiveness, based on a retail organization – created in the beginning of the XX Century, more precisely, on November 29, 1913 and that was recognized by the paulistana population as being the one that most resembled the city. The analysis of the favorable periods of growth and the critical periods has made it possible to identify the characteristics of each one of the five identified phases in the study: initial growth, administrative, mass growth, expansion and lack of control. It is concluded by the importance of underlying concepts that they interfere: in the research when of the phases elaboration; in the theory of organizational life cycle as instrument that can contribute in the strategic planning of the organizations.RESUMENEl presente artículo se refiere a la relación entre modelos que analizan las fases del ciclo de vida organizacional y la efectividad organizacional, basada en una organización minorista creada en el inicio

  8. Piedra lata terrane of Uruguay: Rb-Sr geochronological data of two new paleoproterozoic (transamazonian) granitoids

    International Nuclear Information System (INIS)

    Cingolani, C; Bossi, J; Varela, R; Maldonado, S.; Pineyro, D.; Schipilov, A

    2001-01-01

    The Precambrian basement of Uruguay consists of three major terranes separated and crosscut by wide NE-striking subvertical transcurrent shear zones. The western terrane as a part of the Rio de la Plata Craton is known as the Piedra Alta Terrane (PAT). This is separated from the Nico Perez Terrane by the Sarandi del Yi-Piri olis subvertical shear zone (Bossi et al., 1993). A mafic dykes complex intruded the PAT at 1.8 Ga and was not later deformed. The PAT has equivalent rocks in the igneous-metamorphic basement of Tandilia region and the Martin Garcia Island, Buenos Aires Province, Argentina (Dalla Salda et al., 1988; Cingolani and Dalla Salda, 2000). The PAT shows no evidence of the Neoproterozoic orogenies and is considered a best preserved Paleoproterozoic block (Transamazonian Cycle). It contains three E-W trending belts of volcano-sedimentary rocks with low grade metamorphism. These are from south to north: Pando, San Jose and Andresito belts (Bossi et al., 1996). Associated with them, three granitic-gneissic zones he Ecilda Paullier, Florida and Feliciano- were recognized with magmatic intrusives emplaced at different crustal levels. The San Jose belt is the largest supracrustal unit and contains abundant volcanic and volcaniclastic rocks of low grade metamorphic (Paso Severino Fm.) with sheets of granitic rocks intercalated (Mutti et al., 1996; Bossi et al., 1996). The associated granitic rocks are of large areal extension, mostly granodiorites and tonalites, and minor monzogranite and gabbro (e.g. Cerro Rospide region), including xenoliths from Paso Severino Fm. Towards the north of the San Jose belt an important Florida granitized zone is developed in the central part of the PAT, where the Pintos massif was recognized. The main purpose of this contribution is to offer new Rb-Sr geochronological data from two granitoid units, The Cerro Rospide intrusive in Paso Severino Fm. and Pintos massif included in medium grade migmatic-metamorphic complex and its

  9. Efecto magnetocalórico en materiales con transiciones de fase de segundo orden: Optimización de la capacidad de refrigeración

    OpenAIRE

    Caballero Flores, Rafael

    2011-01-01

    La tesis presenta un estudio del efecto magnetocalórico en materiales con transiciones de fase de segundo orden. Se centra esencialmente en la dependencia con el campo magnético aplicado de la variables termodinámicas relevantes del proceso, estudio de aleaciones basadas en hierro para minimizar los costos de los materiales refrigerantes, y fabricación de composites para minimizar los valores de las intensidades del campo requeridas en el proceso de refrigeración.

  10. Insights into crystal growth rates from a study of orbicular granitoids from western Australia

    Science.gov (United States)

    Zhang, J.; Lee, C. T.

    2017-12-01

    The purpose of this study is to develop new tools for constraining crystal growth rate in geologic systems. Of interest is the growth of crystals in magmatic systems because crystallization changes the rheology of a magma as well as provides surfaces on which bubbles can nucleate. To explore crystal growth in more detail, we conducted a case study of orbicular granitoids from western Australia. The orbicules occur as spheroids dispersed in a granitic matrix. Most orbicules have at least two to three concentric bands, composed of elongate and radially oriented hornblende surrounded by interstitial plagioclase. We show that mineral modes and hence bulk composition at the scale of the band is homogeneous from rim to core. Crystal number density decreases and crystal size increases from rim to core. These observations suggest that the orbicules crystallized rapidly from rim to core. We hypothesize that the orbicules are blobs of hot dioritic liquid injected into a cold granitic magma and subsequently cooled and solidified. Crystals stop growing when the mass transport rate tends to zero due to the low temperature. We estimated cooling timescales based on conductive cooling models, constraining crystal growth rates to be 10-6 to 10-5 m/s. We also show that the oscillatory banding is controlled by disequilibrium crystallization, wherein hornblende preferentially crystallizes, resulting in the diffusive growth of a chemical boundary layer enriched in plagioclase component, which in turns results in crystallization of plagioclase. We show that the correlation between the width of each crystallization couplet (band) with distance from orbicule rim is linear, with the slope corresponding to the square root of the ratio between chemical diffusivity in the growth medium and thermal diffusivity. We estimate chemical diffusivity of 2*10-7 m2/s, which is remarkably fast for silicate liquids but reasonable for diffusion in hot aqueous fluids, suggesting that crystallization

  11. Avaliação eletromiográfica da deglutição dos diferentes tipos clínicos da doença de Parkinson nas fases on e off

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    Douglas Monteiro

    2015-04-01

    Full Text Available OBJETIVO:avaliar os parâmetros eletromiográficos da deglutição dos diferentes tipos clínicos da doença de Parkinson idiopática nas fases on e off.MÉTODOS:foram estudados 20 pacientes com doença de Parkinson, divididos através da Escala Unificada de Avaliação da Doença de Parkinson em três grupos: tremulantes, rígido-acinético e misto. O exame de eletromiografia de superfície foi coletado sobre a musculatura supra-hióidea durante a deglutição de 3 ml e 10 ml de água e iogurte, que foi repetida 5 vezes para cada volume e consistência. Este protocolo foi realizado no antes e após a medicação, período offe on.RESULTADOS:verificou-se que na fase off, o grupo rígido-acinético apresentou as maiores médias de deglutições em partes e duração das eletromiografias de superfície, enquanto que o grupo misto apresentou as menores médias de amplitude. Na fase on, os três grupos tenderam a melhorar ou manter as médias das variáveis estudadas, porém não houve diferença significante entre os tipos clínicos, antes ou depois da Levodopa.CONCLUSÃO:a terapia medicamentosa através da Levodopa não apresenta diferenças consistentes nas eletromiografias de superfície da deglutição dos tipos clínicos da doença de Parkinson.

  12. Ostensiewe illustrasies as mikrostrukturele items in verklarende skoolwoordeboeke gerig op leerders in die junior sekondêre fase

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    Phillip Louw

    2011-10-01

    Full Text Available

    OPSOMMING: 'n Verklarende skoolwoordeboek gerig op leerders in die junior sekondêre fase moet, in die Suid-Afrikaanse konteks, gebruikersgerigte praktyke navolg om op kommunikatiewe en pedagogiese vlak waarde toe te voeg vir beide moedertaal- en niemoedertaalsprekende leerders. Een so 'n praktyk is die opname van ostensiewe illustrasies as mikrostrukturele items om die oordrag van pragmatiese en semantiese data te bevorder. In hierdie artikel word die waarde van ostensiewe illustrasies en hulle relevansie binne 'n verklarende skoolwoordeboek gerig op leerders in die junior sekondêre fase beoordeel, waarna sekere voorbehoude rakende hulle gebruik behan-del word. 'n Besluit om wel ostensiewe illustrasies op te neem, noodsaak verder 'n bespreking van waar om hierdie items in die mikrostruktuur te plaas sowel as 'n bespreking van verskillende tipes illustrasies wat vir opname in die woordeboektipe onder bespreking geskik sal wees. Vervolgens word 'n kritiese evaluering van die hantering van ostensiewe illustrasies in 'n eg Suid-Afrikaanse verklarende skoolwoordeboek gerig op leerders in die junior sekondêre fase gegee en voorstelle gemaak vir 'n verbeterde mikrostrukturele behandeling wat aan die eise van die gebruikersper-spektief voldoen. Laastens word die kwessie van noodsaaklike mediostrukturele ondersteuning vir hierdie datatipe in die vorm van presiese, omvattende kruisverwysings, ter sprake gebring. Hierdie artikel probeer dus om kriteria vir die suksesvolle leksikografiese hantering van ostensiewe illus-trasies aan te bied.


    Sleutelwoorde: BYSKRIFTE, BYVOEGLIKE NAAMWOORD, GROEPILLUSTRASIE, JU-NIOR SÊKONDERE ONDERRIGFASE, KOMMUNIKATIEWE WAARDE, KRUISVERWYSINGS, MIKROSTRUKTURELE ITEMS, OSTENSIEWE ILLUSTRASIES, PEDAGOGIESE WAARDE, SELF-STANDIGE NAAMWOORD, STRUKTUURMERKERS, VERKLARENDE SKOOLWOORDEBOEK, VOORBEELDMATERIAAL, WERKWOORD

    *****

    ABSTRACT: Ostensive Illustrations as Microstructural Items in Explanatory

  13. TRANSICIÓN DE FASE ENTRE FORMAS FCC Y BCC DEL ESTRONCIO Y SUS PROPIEDADES ESTRUCTURALES Y ELECTRONICAS MEDIANTE TEORÍA DEL FUNCIONAL DE LA DENSIDAD (DFT

    Directory of Open Access Journals (Sweden)

    María A. Puerto

    2012-01-01

    Full Text Available Se han realizado cálculos de primeros principios para de terminar las propiedades estructurales y electrónicas del estroncio en sus fases de cristalización Im-3m y Fm-3m dentro del formalismo de la Teoría del Funcional de la Densidad (DFT. Esto se hizo a partir del método de ondas planas aumentadas y linealizadas en la versión de potencial completo (FP-LAPW con la aproximación de gradiente generalizado (GGA. Se encontró que la configuración más estable es la Fm-3m , con una constante de red a 0 = 11,38 bohr , energía de cohesión E o = - 0,107 Ry y módulo de volumen B 0 = 113 GPa . A partir de la densidad de esta dos y la estructura de bandas de energía se evidenció el carácter metálico de este elemento para ambas estructuras cristalinas. Se predice una posible transición de fase estructural de la Fm-3m a la Im-3m bajo una presión de 178 GPa .

  14. Modalidades terapéuticas en la fase latente prolongada del trabajo de parto Therapeutic modalities in the prolonged latent phase of labor

    Directory of Open Access Journals (Sweden)

    Danilo Nápoles Méndez

    2012-05-01

    Full Text Available En el trabajo de parto, la distocia de fase latente constituye una entidad clínica relacionada con el aumento de la morbilidad y mortalidad materna y perinatal. En este artículo se exponen las modalidades de tratamiento para el trastorno de esta fase del trabajo de parto, a fin de que los obstetras posean alternativas terapéuticas que posibiliten una mayor preparación en la toma de decisiones. Asimismo, se describen tanto las formas de terapia conservadora (reposo terapéutico, como las de la activa. Se concluye que el tratamiento activo no invasivo de base etiológica con misoprostol y la terapia activa con oxitocina y rotura artificial de membranas tardía, son modalidades empleadas en obstetricia con resultados satisfactorios.Dystocia of latent phase constitutes a clinical entity related to the increase of maternal and perinatal morbidity and mortality during labor. The treatment modalities for the disorder of this phase of labor are exposed in this work, so that the obstetricians have therapeutic alternatives which facilitate a greater preparation in the decision-making process. The ways for conservative therapy (therapeutic rest and active therapy are also described. It is concluded that the non-invasive active treatment of etiological basis with misoprostol and the active therapy with oxytocin and late artificial rupture of membranes are the modalities used in obstetrics with satisfactory results.

  15. DETERMINAÇÃO DAS DIMENSÕES DE UM BIODIGESTOR EM FUNÇÃO DA PROPORÇÃO GÁS/FASE LÍQUIDA

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    Deyvid da Silva Ribeiro

    2011-03-01

    Full Text Available Devido ao risco de contaminação ambiental através da má manipulação dos excrementos animais produzidos pela pecuária, se faz necessário buscar alternativas eficientes e de baixo custo para resolver este problema. Entre as diversas soluções, FAO (1995 recomenda o Biodigestor como uma alternativa viável e prática. Entre os benefícios gerados pelo o biodigestor podemos citar: produção de biogás, descontaminação biológica e química dos dejetos animais e a geração de biofertilizante (CIPAV, [2004?]; Fregoso et al, 2001; Marchaim, 1992; Botero e Preston, 1986. Por tanto, esse presente trabalho foi realizado com o objetivo de determinar as dimensões de um biodigestor tubular em função da proporção gás/fase líquida desejada. Para esse fim, foram utilizadas as recomendações de Ribeiro (2004, o Raciocínio Lógico-Matemático e os programas EXCEL 2007 e AutoCAD 2009 que foram utilizados para auxiliar nos cálculos e nas simulações de campo. Os modelos encontrados demonstraram 100% de exatidão no que se refere ao dimensionamento e 100% de aplicabilidade em campo para biodigestores com proporções gás/fase líquida menores a 40%.

  16. DAR VOZ AOS PROFESSORES DE EDUCAÇÃO FÍSICA: AS HISTÓRIAS DE VIDA SOBRE OS MOMENTOS SIGNIFICATIVOS EM RELAÇÃO AS FASES DA CARREIRA DOCENTE

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    Hugo Norberto Krug

    2013-12-01

    Full Text Available Este estudo objetivou analisar a carreira de professores de Educação Física Escolar de uma cidade do sul do Brasil, numa perspectiva de desenvolvimento profissional e de percurso de formação, identificando os momentos significativos desse mesmo percurso, e, ainda, caracterizando os momentos identificados considerando as fases do percurso profissional docente. A metodologia caracterizou-se como qualitativa com abordagem (autobiográfica onde utilizamos a narrativa oral que foi gravada, transcrita e analisada à luz da identificação dos significados. Participaram dez professoras. Concluímos que os melhores e piores momentos, os problemas sentidos, os momentos de ruptura profissional e a motivação para a carreira podem ocorrer em quaisquer momentos da docência, independentemente da fase do percurso profissional e por diversas razões. Estes traços caracterizadores ajudam a delinear um perfil de carreira que, mesmo não sendo de forma linear entre as professoras, deixam marcas positivas e/ou negativas.

  17. Spinels of Variscan olivine hornblendites related to the Montnegre granitoids revisited (NE Spain): petrogenetic evidence of mafic magma mixing

    Energy Technology Data Exchange (ETDEWEB)

    Galán, G.; Enrique, P.; Butjosa, L.; Fernández-Roig, L.

    2017-07-01

    Olivine hornblendites (cortlandtites) form part of the Montnegre mafic complex related to late-Variscan I-type granitoids in the Catalan Coastal Ranges. Two generations of spinel are present in these hornblendites: Spl1 forms euhedral crystals included in both olivine and Spl2. Spl2 forms euhedral to anhedral crystals associated with phlogopite and fibrous colourless amphibole forming pseudomorphs after olivine. Compositions of Spl1 are picotite-Al chromite (Fe#: 77.78-66.60; Cr#: 30.12-52.22; Fe3+/R3+: 6.99-21.89; 0.10< TiO2%< 0.62). Compositions of Spl2 are pleonaste (Fe#: 37.86-52.12; Cr#: 1.00-15.45; Fe3+/R3+: 0.31-5.21; TiO2% <0.10%). The two types of spinel follow a CrAl trend, mainly due to the substitution (Fe2+)-1Cr-1= MgAl, which is interpreted as the result of mixing between two different mantle-derived melts. The compositions of early Spl1 crystals included in olivine are characteristic of Al-rich basalts. More aluminous Spl2 would result from reaction of olivine with a less evolved, Al and K-rich mantle-derived melt after new refilling of the magma chamber or channel. As a whole, spinels from similar examples of Variscan olivine hronblendites also follow a CrAl trend with high Fe# and starting at higher Cr# than other trends of this type. Cr# heterogeneity in the early spinels from these Variscan hornblendites would be inherited from the variable Al content of the mafic melts involved in their genesis.

  18. Características químicas e avaliação microbiológica de diferentes fases de maturação do biofertilizante Bokashi

    Directory of Open Access Journals (Sweden)

    Flaviane Eva Magrini

    2011-08-01

    Full Text Available O uso de biofertilizantes é uma das alternativas que vêm sendo testada e adotada na agricultura, a fim de reduzir o uso de produtos químicos como forma de reaproveitamento de resíduos da propriedade. O objetivo deste trabalho foi analisar a concentração de N, P, K, Fe, Zn, Mg e Ca e a microbiota fúngica de diferentes fases de maturação do biofertilizante Bokashi. As amostras foram avaliadas aos 15, 30, 60 e 85 dias de maturação. A partir da análise das amostras observou-se que a maioria dos nutrientes avaliados tiveram seu valor mais expressivo aos 60 dias de maturação da compostagem. Os fungos identificados pertencem a diferentes gêneros, destacando-se a presença de Aspergillus sp., Dactylium sp. e Rhizopus sp. na fase final de maturação do composto. Os resultados demonstram que ocorreram variações na concentração dos nutrientes e nas populações de microrganismos do biofertilizante avaliado, demonstrando uma intensa atividade biológica no composto com a liberação de diversos nutrientes para o meio.

  19. Método de cálculo de comportamiento térmico de cerramientos de edificios con materiales de cambio de fase

    OpenAIRE

    Urresti González, Aitor

    2017-01-01

    331 p. El almacenamiento de energía térmica en forma de calor latente puede ser una buena medida para reducirla demanda tanto de refrigeración como de calefacción de los edificios. EL fuerte comportamiento nolineal de este tipo de almacenamiento requiere de un buen análisis previo de las propiedades para unaprovechamiento óptimo. El presente trabajo recoge todo el proceso de selección de un material decambio de fase: desde la medición de propiedades térmicas, pasando por la definición de u...

  20. Fibra na ração de crescimento e seus efeitos no desempenho de poedeiras nas fases de crescimento e postura

    OpenAIRE

    Braz,Nádia de Melo; Freitas,Ednardo Rodrigues; Bezerra,Roseane Madeira; Cruz,Carlos Eduardo Braga; Farias,Nadja Naiara Pereira; Silva,Nemuel Muniz da; Sá,Newton Lima; Xavier,Regina Patrícia de Souza

    2011-01-01

    Objetivou-se com esta pesquisa avaliar os efeitos dos níveis de fibra em detergente neutro (FDN) das rações oferecidas para as aves entre a 7ª e 17ª semanas de idade sobre o desempenho, o desenvolvimento dos sistemas digestório e reprodutor, bem como os efeitos na maturidade sexual, no desempenho e na qualidade dos ovos na fase de postura.Foram distribuídas 1.296 aves em delineamento inteiramente casualizado em esquema fatorial 3 × 2, composto de três níveis de FDN e duas linhagens, com quatr...

  1. Geochronology, geochemistry, and Sr-Nd-Pb-Hf isotopes of the Zhunsujihua granitoid intrusions associated with the molybdenum deposit, northern Inner Mongolia, China: implications for petrogenesis and tectonic setting

    Science.gov (United States)

    Zhang, Xiaojun; Lentz, David R.; Yao, Chunliang; Liu, Rui; Yang, Zhen; Mei, Yanxiong; Fan, Xianwang; Huang, Fei; Qin, Ying; Zhang, Kun; Zhang, Zhenfei

    2018-03-01

    The Zhunsujihua porphyry molybdenum deposit, located in northern Inner Mongolia of China that belongs to Central-Asian Orogenic Belt (CAOB), is the only Mo deposit formed in the late Carboniferous in this area so far. Its mineralization is mainly restricted to the Zhunsujihua granitoid intrusions, which are composed of the main granodiorite (GD) and crosscutting, virtually coeval minor syn-ore leucogranite (LG) and diorite porphyry (DP) dykes. LA-ICP-MS zircon U-Pb dating yields crystallization ages of 300.0 ± 2.0, 299.3 ± 2.0, and 299.0 ± 2.6 Ma for the GD, LG, and DP, respectively. The major and trace element lithogeochemical data show that the GD and LG are metaluminous to weakly peraluminous, high-K calc-alkaline series with I-type granite characteristics, strongly oxidized, with low concentrations of Ba, Nb, Sr, P, and Ti and elevated K and Rb contents, indicating typical arc magmatic features. The LG is a product derived by extensive fractional crystallization of a parental magma similar to the GD as evident from the lower Eu/Eu*, Nb/Ta, Zr/Hf, and T Zr. The moderately altered DP exhibits high concentrations of K, Rb, Cs, LREE, Y, and low Sr/Y, with a positive ɛ Nd (300 Ma), which indicates a mantle or juvenile source associated with an arc setting. The Sr-Nd-Hf isotope data show low I Sr (0.70406-0.70461) and moderate ɛ Nd (300 Ma) (-0.9 to 1.5) for the GD and LG, and relatively high ɛ Hf (300 Ma) values (-3.6 to +11.2) for the GD, suggesting the magma mainly originated from the juvenile lower crust that was derived from depleted mantle, with a minor component of ancient continental crust. Lead isotope data have characteristics of a lower crust source with minor contamination by upper crustal material. Combined with previous research, the Zhunsujihua granitoid intrusions developed in an intracontinental volcanic arc (Uliastai) associated with northward subduction of the Paleo-Asian Ocean plate during late Carboniferous to early Permian; this suggests

  2. Estudo longitudinal do eletrocardiograma na doença de Chagas desde a fase aguda

    Directory of Open Access Journals (Sweden)

    Roberto C. Pedrosa

    1993-09-01

    Full Text Available Vários trabalhos com eletrocardiograma na doença de Chagas têm sido feitos. Alguns referindo-se a grupos selecionados de casos, outros a estudos longitudinais, relatam as características da mortalidade nas diversas fases da doença. Com o objetivo de avaliar o valor do eletrocardiograma como índice de avaliação terapêutica e de seu comportamento na doença de Chagas desde a fase aguda, no presente trabalho, analisou-se evolutivamente o eletrocardiograma de 42 pacientes (18 mulheres e 24 homens procedentes da zona rural do Norte de Minas Gerais; predomínio etário foi nas duas primeiras décadas; todos com comprometimento cardíaco; todos receberam tratamento específico. O acompanhamento dos 42 pacientes foi de 9 anos dos quais 3 pacientes tiveram seguimento de 20 anos. Foram analisados 270 eletrocardiogramas. Nós utilizamos os seguintes critérios para a análise do ECG: código de Minnesota modificado para doença de Chagas; WHO/I. S. F. C. TASK FORCE para condução intraventricular e critérios de Pieretti para área eletricamente inativa. Concluímos que as alterações eletrocardiográficas agravam com a evolução da doença e que o eletrocardiograma não serve de índice de avaliação terapêutica.Several studies have been done to analyse the relationship between the characteristics of the electrocardiogram (ECG and mortality in the several stages of the disease, using different methods like multiple case and longitudinal studies. We anatysed the ECGfrom the acute stage up to twenty years of follow-up (±9 years in 42 patients with Chagas ' disease to determine their evolution and it 's value like an indexfor therapeutic evaluation. The 42 patients (18 female, 24 males were originalty from the North of the State of Minas Gerais (Brazil and the initial stage was mainly in the first two decades of age. All bad cardiac involvementand received fiill specific treatment. We utilized the following criteria for the ECG analyses

  3. Multi-locus phylogenies of the genus Barteria (Passifloraceae) protray complex patterns in the evolution of myrmecophytism.

    NARCIS (Netherlands)

    Peccoud, J.; Piatscheck, F.; Yockteng, R.; Garcia, M.; Sauve, M.; Djieto-Lordon, C.; Harris, D.J.; Wieringa, J.J.; Breteler, F.J.; Born, C.; McKey, D.; Blatrix, R.

    2013-01-01

    The four species of the central African genus Barteria show variation in habitat and in degree of association with ants. Whereas B. solida, restricted to submontane forests, attracts opportunistic ants to extrafloral nectar, the three other species, found in lowland rainforests (B. fistulosa, B.

  4. Quando a fase de equilíbrio pode ser suprimida nos exames de tomografia computadorizada de abdome? What is the real role of the equilibrium phase in abdominal computed tomography?

    Directory of Open Access Journals (Sweden)

    Priscila Silveira Salvadori

    2013-04-01

    Full Text Available OBJETIVO: Avaliar a necessidade de realização da fase de equilíbrio nos exames de tomografia computadorizada de abdome. MATERIAIS E MÉTODOS: Realizou-se estudo retrospectivo, transversal e observacional, avaliando 219 exames consecutivos de tomografia computadorizada de abdome com contraste intravenoso, realizados num período de três meses, com diversas indicações clínicas. Para cada exame foram emitidos dois pareceres, um avaliando o exame sem a fase de equilíbrio (primeira análise e o outro avaliando todas as fases em conjunto (segunda análise. Ao final de cada avaliação, foi estabelecido se houve mudança nos diagnósticos principais e secundários, entre a primeira e a segunda análise. Foi utilizada a extensão do teste exato de Fisher para avaliar a modificação dos diagnósticos principais (p 0,999. Com relação aos diagnósticos secundários, cinco exames (2,3% foram modificados. CONCLUSÃO: Para indicações clínicas como estadiamento tumoral, abdome agudo e pesquisa de coleção abdominal, a fase de equilíbrio não acrescenta contribuição diagnóstica expressiva, podendo ser suprimida dos protocolos de exame.OBJECTIVE: To evaluate the role of the equilibrium phase in abdominal computed tomography. MATERIALS AND METHODS: A retrospective, cross-sectional, observational study reviewed 219 consecutive contrast-enhanced abdominal computed tomography images acquired in a three-month period, for different clinical indications. For each study, two reports were issued - one based on the initial analysis of non-contrast-enhanced, arterial and portal phases only (first analysis, and a second reading of these phases added to the equilibrium phase (second analysis. At the end of both readings, differences between primary and secondary diagnoses were pointed out and recorded, in order to measure the impact of suppressing the equilibrium phase on the clinical outcome for each of the patients. The extension of the exact Fisher

  5. Geochemical criteria for distinguishing magmatic and metasomatic albite-enrichment in granitoids — examples from the Ta-Li granite Yichun (China) and the Sn-W deposit Tikus (Indonesia)

    Science.gov (United States)

    Schwartz, M. O.

    1992-03-01

    Two examples of albite-rich granitoids of different genesis are discussed: the Ta-Li granite at Yichun (China) exhibits dominantly igneous textures, and the sodium-enrichment zone in biotite granite of the Sn-W deposit at Tikus is characterized by metasomatic textures. The Yichun stock shows a magmatic evolution from biotite-muscovite granite to lepidolite granite with an increase of Na2O and F concentrations and a decrease of CaO and Sr concentrations. The composition of the different granite phases is close to pseudoternary minima in the haplogranite-H2O(-Li-F) system. The composition of the F-rich albitization zone at Tikus deviates strongly from the pseudoternary minima and shows a tendency to become monomineralic (nearly pure albitite). CaO and Sr concentrations are increased or remain unchanged with respect to the unaltered biotite granite at Tikus. Albitization produced by fluid-rock interaction in F-rich systems is characterized by that CaO or Sr released by the breakdown of plagioclase in the granite protolith, are fixed in newly formed fluorite or albite, respectively.

  6. Influencia de la fase sigma en la laminación en frío de los aceros inoxidables dúplex

    Directory of Open Access Journals (Sweden)

    Fargas, G.

    2004-04-01

    Full Text Available One of the steps in the industrial rolling process of duplex stainless steels is the annealing heat treatment after hot rolling. If this annealing is performed in a temperature range that favours the precipitation of intermetallic phases, the mechanical properties can be modified considerably. The formation of these precipitates has a detrimental effect on the DSS ductility and toughness, so it will be a drawback for further cold rolling. In the present investigation, the effect of the sigma phase during cold rolling of a duplex stainless steel type EN 1.4462 has been studied. To simulate this process, compression tests up to a thickness reduction similar to that performed at industrial level have been done. The testing samples were studied by optical microscopy, SEM (scanning electronic microscopy and TEM (transmission electronic microscopy. Afterwards, some of the annealing conditions were selected in order to carry out cold rolling, using a laboratory scale machine, with the aim to observe if they offered a similar behaviour as that experienced in the compression tests. The results show that only the annealing condition at 975ºC during 10 minutes allows to produce sheets without rolling defects.

    Una de las etapas en el proceso de fabricación industrial de los aceros inoxidables dúplex laminados es el tratamiento térmico de recocido posterior a la laminación en caliente. Si dicho recocido se efectúa en un rango de temperaturas que favorezca la formación de fases intermetálicas, las propiedades mecánicas del material pueden modificarse notablemente. La presencia en la microestructura bifásica de dichos precipitados provoca efectos muy perjudiciales sobre la ductilidad y la tenacidad del material, pudiendo llegar a hacer inviable la posterior etapa de laminación en frío. En el presente trabajo se ha estudiado el efecto sobre el proceso de laminación en frío de la presencia de fase sigma en un acero dúplex tipo E.N. 1

  7. Geochemistry and petrogenesis of Neoproterozoic Mylliem ...

    Indian Academy of Sciences (India)

    the Mylliem granitoids is depicted by (Ce/Yb)N values, which show a range of 1.39 to 1.65. ... granitoid pluton intrusive into the Shillong Group ..... vs. SiO2 diagram (Frost et al 2001) (figure 6a). MALI of Mylliem granitoids ranges from 4.46.

  8. Rediseño, optimización y producción de fuente fotovoltaica portatil (Fase II

    Directory of Open Access Journals (Sweden)

    Jaime Hernán Rojas Parra

    2010-07-01

    Full Text Available Este artículo presenta los resultados de la investigación institucional desarrollada por la Escuela de Telemática y Electrónica de la Policía Nacional de Colombia en el año 2010, proceso científico y tecnológico que tuvo como objetivo central de estudio el rediseño, optimización y producción de una fuente fotovoltaica portátil (Fase II que permitirá que los operativos o procedimientos en área rural se desarrollen con más precisión y autonomía porque brinda herramientas al personal, garantiza la sostenibilidad de las comunicaciones, así como la de los demás de equipos electrónicos que por su naturaleza son indispensables en este tipo de eventos y que por imperiosa necesidad requieren una fuente generadora de energía eléctrica.

  9. Prioridades de intervención para la fase aguda de las emergencias complejas formuladas por nueve agencias de ayuda humanitaria

    Directory of Open Access Journals (Sweden)

    Carmen Sofía Carrillo Jaimes

    2004-01-01

    Full Text Available Las Emergencias Complejas son un problema de Salud Pública internacional de frecuencia y magnitud crecientes que producen una importante mortalidad y morbilidad especialmente durante su fase aguda. El objetivo de este estudio es identificar y analizar las áreas prioritarias de intervención en la fase aguda de una emergencia compleja formuladas en los manuales operativos de las principales agencias de ayuda, así como el nivel de desarrollo y estructuración de las actividades propuestas en cada área de prioridad. Métodos: Como material de estudio se utilizaron los manuales de intervención elaborados por 9 de las principales agencias de ayuda. Se procedió a un análisis cuantitativo de las 16 prioridades de intervención planteadas así como del nivel de formulación de cada prioridad en base al desarrollo de 73 variables o aspectos de las propuestas formuladas en los manuales. Resultados: El manual de ACNUR recoge el 90% de las 73 variables de desarrollo de las prioridades y el de Oficina de Coordinación de Asuntos Humanitarios de Naciones Unidas el 35% de las 73 variables. ACNUR presenta el mejor desarrollo de las variables no sanitarias, seguido de MSF y USAID. Médicos sin fronteras muestra un grado de desarrollo de las variables sanitarias del 97,3% seguido de ACNUR (94,7%, USAID y UNICEF (92,1%. Conclusiones: Se ha encontrado que ACNUR tiene la propuesta más integral y Oficina de Coordinación de Asuntos Humanitarios de Naciones Unidas la más discreta. Existe una tendencia general a desarrollar y unificar los indicadores de salud, mientras que otros aspectos no se desarrollan.

  10. Purificación y caracterización de alfa-amilasa de penicillium commune producida mediante fermentación en fase sólida

    OpenAIRE

    Espinel, Esperanza; López, Elizabeth

    2010-01-01

    Este estudio reporta la purificación y caracterización parcial de una alfa-amilasa producida por Penicillium commune mediante fermentación en fase sólida, empleandoyuca blanca colombiana (Manihot esculenta Crantz) como soporte. La enzima fue purificada por precipitación fraccionada con sulfato de amonio, cromatografía de intercambio aniónico (DEAE-Sephadex A-50), cromatografía de filtración por gel (Sephadex G-75) y cromatografía de intercambio catiónico (CM-Sephadex C-50) obteniendo una acti...

  11. Anther and pollen development in some species of Poaceae (Poales

    Directory of Open Access Journals (Sweden)

    AT. Nakamura

    Full Text Available Anther and pollen development were studied in Olyra humilis Nees, Sucrea monophylla Soderstr, (Bambusoideae, Axonopus aureus P. Beauv., Paspalum polyphyllum Nees ex Trin. (Panicoideae, Eragrostis solida Nees, and Chloris elata Desv. (Chloridoideae. The objective of this study was to characterise, embryologically, these species of subfamilies which are considered basal, intermediate and derivate, respectively. The species are similar to each other and to other Poaceae. They present the following characters: tetrasporangiate anthers; monocotyledonous-type anther wall development, endothecium showing annular thickenings, secretory tapetum; successive microsporogenesis; isobilateral tetrads; spheroidal, tricellular, monoporate pollen grains with annulus and operculum. Nevertheless, the exine patterns of the species studied are distinct. Olyra humilis and Sucrea monophylla (Bambusoideae show a granulose pattern, whereas in the other species, it is insular. In addition, Axonopus aureus and Paspalum polyphyllum (Panicoideae have a compactly insular spinule pattern, while Chloris elata and Eragrostis solida (Chloridoideae show a sparsely insular spinule pattern. The exine ornamentation may be considered an important feature at the infrafamiliar level.

  12. Fase sexual de los helechos Odontosoria schlechtendalii y Odontosoria scandens (Dennstaedtiaceae

    Directory of Open Access Journals (Sweden)

    Beatriz Granados

    2003-09-01

    Full Text Available Los resultados de los estudios sobre morfogénesis de la fase sexual de Odontosoria schlechtendalii y O. scandens son presentados en este trabajo. En O. schechlechtendalii y O. scandens las esporas son triletes, no clorofílicas, carecen de perina, la exina es lisa, ligeramente granulada a retuculata y la germinación es tipo Vittaria. El patrón de desarrollo protálico es tipo Adiantum. Los gametófitos adultos son cordiforme espatulados, con la probable presencia de anteridiógenos en O. schlechtendalii, ambas especies son glabras. Los organos sexuales son del tipo común de los helechos leptosporangiados. Las primeras hojas aparecen a los 56-92 días de cultivo, cuyo pecíolo y lámina es angostamente dividida, con tricomas bifurcados y estomas anomocíticosThe results of morphogenesis studies of the sexual phase of Odontosoria schlechtendalii and O. scandens are presented in this paper. In O. schlechtendalii and O. scandens the spores are triletes, non-chlorophyllous, and germinación is of the Vittaria-type, devoid of perine, the exine is smoth and sometimes coarsely ridged to reticulate. The development pattern is of the Adiantum-type. The adult gametophyte is cordate-spathulate, with probable presence of anteridiogen in O. schlechtendalii, both species are glabrous. Sex organs are of the common type of the leptosporangiate ferns. The first leaves appeared after 56-92 days of culture, with petiole and plate divide narrow, trichomes bifurcate and stomate anomocytic

  13. Farelo de trigo na alimentação de poedeiras semipesadas na fase de recria Wheat bran in growing phase laying hens feeding

    Directory of Open Access Journals (Sweden)

    Daniel de Magalhães Araujo

    2008-01-01

    Full Text Available O estudo foi conduzido com o objetivo de avaliar os efeitos da inclusão de farelo de trigo (FT na ração sobre o desempenho de frangas semipesadas nas fases de recria 1 (7 a 14 semanas de idade e recria 2 (15 a 19 semanasde idade e seu efeito residual durante a fase inicial de produção de ovos. Foram utilizadas 160 frangas Lohmann Brown distribuídas em delineamento inteiramente casualizado, com quatro níveis de FT na ração: 0 (controle, 10, 20 e 30%, que resultaram em quatro tratamentos, com cinco repetições de oito aves na fase de recria 1. Ao completarem 14 semanas, as aves foram transferidas para gaiolas de arame galvanizado, redistribuídas em seis repetições de seis aves. Utilizaram-se 144 aves e descartaram-se, aleatoriamente, quatro aves por tratamento, constituindo a fase de recria 2. A adição de FT diminuiu linearmente o peso vivo final e o ganho de peso, resultando em reduções de 1,15 e 0,03 g, respectivamente, para cada 1% de inclusão de FT na ração. O consumo de água aumentou de forma quadrática e cresceu, em valores absolutos, com o aumento de 0 a 30% de farelo de trigo. A cada aumento de 1% de FT na ração, a idade das aves ao primeiro ovo elevou aproximadamente 0,6 dia e o peso do ovo em 0,22 g. A inclusão de farelo de trigo na ração reduz a taxa de crescimento de frangas, atrasa o início da postura, mas melhora o peso inicial dos ovos em relação a dietas à base de milho e de farelo de soja.This study aimed to evaluate the effect of the inclusion of the wheat bran (WB in the ration on egg brown chicken (Lohmann Brown performance in the growing phase 1 (7 to 19 week of age and growing phase 2 (15 to 19 week of age and its residual effects on initial egg production. One hundred-sixty chickens were allotted to a completely randomized design with four level of WB in the ration: 0 (control, 10, 20 and 30%, that resulted in four treatments, with five replicates of eight birds in the growing phase 1. At the

  14. Optimal Phase Balancing Planning for Loss Reduction in Distribution Systems using a Specialized Genetic Algorithm Planeamiento Optimo de Balance de Fases para Reducción de Perdidas en Sistemas de Distribución usando un Algoritmo Genético Especializado

    Directory of Open Access Journals (Sweden)

    Mauricio Granada Echeverri

    2012-06-01

    Full Text Available Unbalanced operation of distribution systems deteriorates power quality andincreases investment and operation costs. Feeder reconfiguration and phaseswapping are the two main approaches for load balancing, being the formermore difficult to execute due to the reduced number of sectionalizing switchesavailable in most distribution systems. On the other hand, phase swappingconstitutes a direct, effective and low cost alternative for load balancing. The main contribution of this paper is the proposal of an optimization model anda solution technique for phase balancing planning in distribution systems. Asregards the optimization model, a mixed integer nonlinear programming formulationis proposed. On the other hand, the proposed solution techniqueconsists on a specialized genetic algorithm. To show the effectiveness of theproposed approach, several tests are carried out with two distribution systemsof 37 and 19 buses, this last one with different load models. Results showedthat in addition to the achievement of the primary objective of loss reduction,phase balancing allows obtaining other technical benefits such as improvementof voltage profile and alleviation of congested lines.La operación desbalanceada de los sistemas de distribución deteriora la calidad de la potencia y aumenta los costos de inversión y operación. La reconfiguración de alimentadores y el intercambio de fases son los dos principales enfoques para balance de fases, siendo el primero más difícil de llevar a cabo debido al número reducido de seccionalizadores disponibles en la mayoría de los sistemas de distribución. Por otro lado, el intercambio de fases constituye una alternativa directa, efectiva y de bajo costo para el balance de fases. La contribución principal de este artículo es la propuesta de un modelo de optimización y una técnica de solución para el planeamiento de balance de fases en sistemas de distribución. En cuanto al modelo de optimización, se

  15. Efeito dos teores de cálcio para poedeiras semipesadas durante a fase de pré-postura e no início da postura

    OpenAIRE

    Nunes,Ricardo Vianna; Pozza,Paulo Cezar; Scherer,Carina; Campestrini,Evandro; Rocha,Leonardo Dornelles da; Nunes,Christiane Garcia Vilela; Costa,Fernando Guilherme Perazzo

    2006-01-01

    O fornecimento de diferentes teores de cálcio para poedeiras semipesadas durante a fase de pré-postura e seus efeitos nas quatro semanas subseqüentes foram avaliados neste experimento. Foram utilizadas 288 aves da linhagem Isabrown com 16 semanas de idade, distribuídas em um delineamento inteiramente casualizado, com quatro tratamentos, oito repetições e nove aves por unidade experimental. As rações, à base de milho e farelo de soja, foram formuladas para atender às exigências nutricionais da...

  16. Modelación matemática del transporte neumático del mineral laterítico en fase densa

    Directory of Open Access Journals (Sweden)

    Yoalbys Retirado-Mediaceja

    2007-03-01

    Full Text Available En las empresas cubanas del níquel, el transporte neumático está limitado por el excesivo gasto de energía que alcanza los 18,82 MJ/t. Las causas que originan esta dificultad son: la incorrecta selección de la velocidad del gas transportador, la existencia de los alimentadores sinfín y la infinita variedad de características físicas y aerodinámicas de los materiales a transportar, que conducen a la inexactitud de los proyectos de las instalaciones neumáticas. A partir de los conocimientos existentes para el transporte neumático de sólidos en las fases fluida y densa se deduce un modelo teórico descriptivo, cuyos parámetros (diferencia de velocidad entre el gas y el sólido y velocidad de flotación se obtienen con datos de una instalación experimental. Para obtener los parámetros del modelo se utiliza el método de solución de ecuaciones diferenciales Runge–Kutta cuarto orden, como parte de un procedimiento iterativo que conduce a la minimización del módulo del error promedio entre los valores experimentales y los predichos por el modelo. Con el empleo del modelo se simula la dependencia de las pérdidas de presión, el flujo másico de sólido y la concentración de la mezcla en función del flujo másico de gas de los sistemas de transporte neumático del mineral laterítico. Se confirma la reducción de las pérdidas de presión con el incremento de la velocidad del fluido en zonas inferiores a los 6,12 m/s en el transporte horizontal y 5,21 m/s en el vertical. El transporte en fase densa continua se extiende hasta los 18 m/s, aproximadamente, en ambos casos.

  17. Geochemical and isotopic characterization of the granitic magmatism along the Remígio - Pocinhos shear zone, Borborema Province, NE Brazil

    Science.gov (United States)

    de Lima, Jefferson V.; Guimarães, Ignez de P.; Santos, Lucilene; Amorim, José Victor A.; Farias, Douglas José S.

    2017-04-01

    Two granitoid plutons (Pilõezinhos and Curral de Cima) intruded along the Remígio - Pocinhos shear zone, eastern part of the Borborema Province. The Pilõezinhos and Curral de Cima granites were dated at 566 ± 3 Ma and 618 ± 5 Ma respectively. The granitoids from both plutons have distinct initial 143Nd/144Nd ratios, expressed by εNd(t) values, i.e. the granitoids of Pilõezinhos pluton have lower εNd(t) values (-15.47 to -15.81) and negative εHf (t = 570 Ma) values (-16.0 to -18.6), while the granitoids of the Curral de Cima pluton have εNd(t) values between -1.12 and -5.23. The granitoids of the Curral de Cima pluton are epidote bearing, magnesian calcalkaline I-type granitoids, crystallized under high fO2 conditions. The granitoids of the Pilõezinhos pluton are alkaline, low-fO2, ferroan, ilmenite-series, A2-type granite intrusions. The geochemical and isotopic signatures suggest that the origin of magma of the Curral de Cima granitoids involved mixing/mingling at depth between crustal and mantle magmas, associated to decompression (lateral escape) during the convergent stage of Brasiliano/Pan/African orogeny, which lead the asthenosphere melts to rise into the lower crust. The source of magma of the granitoids of the Pilõezinhos pluton involved a strong crustal component with geochemical and isotopic signatures similar to the orthogneisses of the Serrinha-Pedro Velho Complex, and small mantle component. The emplacement of the Pilõezinhos pluton is associated to an extensional space formed during high-T strike-slip shearing developed by the synchronic movement of the Matinhas sinistral shear zone and Remígio - Pocinhos dextral shear zone.

  18. Climate Management System for mushroom cultivation (CMMC). First phase. Inventory and functional design; Klimaat Managementsysteem Champignonteelt (KMC). 1e fase. Inventarisatie en functioneel ontwerp

    Energy Technology Data Exchange (ETDEWEB)

    Gielen, J.H. [DLV Plant, Horst (Netherlands)

    2011-03-15

    This report describes the feasibility and the opportunities of developing a Climate Management System for Mushroom Cultivation (CMMC) software package, based on which a decision can be made to proceed with the realization of phase 2 of the project, i.e. the actual construction of the CMMC for mushroom cultivation [Dutch] Deze rapportage beschrijft de haalbaarheid en de mogelijkheden van de ontwikkeling van een KMC software pakket, op basis waarvan besloten kan worden tot de realisatie van fase 2 van het project, de daadwerkelijke bouw van de KMC voor de champignonteelt.

  19. Influencia del cobre en la transformación de fase de la aleación Zn - 22 % p Al, durante la homogenización

    OpenAIRE

    Rangel Lara, S.; Bernal, J. L.; Ita de la Torre, A. de

    2011-01-01

    Las aleaciones fueron producidas por fundición y enfriadas en aire quieto a temperatura ambiente, la microestructura dendrítica fue analizada en un trabajo anterior [1]. Muestras de las aleaciones obtenidas fueron sometidas a un tratamiento de homogenización a 375 °C por 120 horas, se observó la modificación de la microestructura a 60, 100 y 120 horas en las aleaciones Zn - 22 % p Al y Zn - 22 % p Al - 2 % p Cu. Las fases presentes en las aleaciones se identificaron por microscopia óptica. Se...

  20. Anther and pollen development in some species of Poaceae (Poales Desenvolvimento da antera e do grão de pólen em espécies de Poaceae (Poales

    Directory of Open Access Journals (Sweden)

    AT. Nakamura

    2010-05-01

    Full Text Available Anther and pollen development were studied in Olyra humilis Nees, Sucrea monophylla Soderstr, (Bambusoideae, Axonopus aureus P. Beauv., Paspalum polyphyllum Nees ex Trin. (Panicoideae, Eragrostis solida Nees, and Chloris elata Desv. (Chloridoideae. The objective of this study was to characterise, embryologically, these species of subfamilies which are considered basal, intermediate and derivate, respectively. The species are similar to each other and to other Poaceae. They present the following characters: tetrasporangiate anthers; monocotyledonous-type anther wall development, endothecium showing annular thickenings, secretory tapetum; successive microsporogenesis; isobilateral tetrads; spheroidal, tricellular, monoporate pollen grains with annulus and operculum. Nevertheless, the exine patterns of the species studied are distinct. Olyra humilis and Sucrea monophylla (Bambusoideae show a granulose pattern, whereas in the other species, it is insular. In addition, Axonopus aureus and Paspalum polyphyllum (Panicoideae have a compactly insular spinule pattern, while Chloris elata and Eragrostis solida (Chloridoideae show a sparsely insular spinule pattern. The exine ornamentation may be considered an important feature at the infrafamiliar level.O desenvolvimento da antera e do grão de pólen de Olyra humilis Nees, Sucrea monophylla Soderstr. (Bambusoideae, Axonopus aureus P. Beauv., Paspalum polyphyllum Nees ex Trin. (Panicoideae, Eragrostis solida Nees and Chloris elata Desv. (Chloridoideae foi estudado visando caracterizar embriologicamente essas espécies de subfamílias consideradas basal, intermediária e derivada, respectivamente. As espécies são similares entre si e entre as demais Poaceae. Apresentam os seguintes caracteres: anteras tetrasporangiadas; desenvolvimento da parede da antera do tipo monocotiledôneo, endotécio com espessamento de parede anelar, tapete secretor; microsporogênese sucessiva; tétrades isobilaterais; grãos de

  1. Cinesioterapia previne ombro doloroso em pacientes hemiplégicos/paréticos na fase sub-aguda do acidente vascular encefálico

    Directory of Open Access Journals (Sweden)

    Horn Agnes Irna

    2003-01-01

    Full Text Available CONTEXTO: Ombro doloroso é freqüente em pacientes com hemiplegia/hemiparesia (H/P por acidente vascular encefálico (AVE, dificultando a recuperação neuromotora gerando incapacidade funcional. OBJETIVO: Estudar tratamento fisioterapêutico para a prevenção da dor no ombro com H/P em pacientes com AVE na fase sub-aguda, e analisar desfechos secundários (força muscular do ombro acometido e movimentos funcionais ativos básicos. MÉTODO: Estudaram-se 21 pacientes (12 homens, 9 mulheres; idades 26 a 87 anos com H/P. O tratamento fisioterapêutico consistiu de 30 minutos diários de cinesioterapia, desde as 48 horas após o AVE até a alta hospitalar. Os pacientes foram avaliados antes e após o tratamento em relação à presença ou ausência de dor no ombro H/P, à força dos diversos grupos musculares do ombro e quanto aos movimentos funcionais de transferência e manutenção postural básica. RESULTADOS: Nenhum paciente apresentava dor no ombro H/P na alta (p<0,001. A força muscular aumentou significativamente em relação à elevação, protusão, abdução e flexão do ombro (p<0,001. Houve melhora dos movimentos funcionais: decúbito dorsal para lateral, decúbito lateral para sentado e manter-se sentado (p<0,001. CONCLUSÃO: A cinesioterapia na fase aguda do AVE preveniu a dor no ombro H/P e favoreceu a recuperação motora.

  2. Modelo predictivo de control en fundiciones de alta precisión: un nuevo enfoque para la fase de predicción

    Directory of Open Access Journals (Sweden)

    Nieves, J.

    2011-08-01

    Full Text Available A Model Predictive Control (MPC is a system which allows us to control a production plant. Thanks to this type of system is possible to make a production that comes close to “zero defects”. In order to achieve its main goal, this kind of systems consists of several phases. One of the most important is the phase that predicts the situation in which the plant is going to be in a given time. Currently, the majority of the research in this field are related to linear MPC, although the process, which the model tries to represent, may not be. Thus, this paper presents several experiments that proof that the forecast phase, usually represented by a single mathematical function, can be represented by machine-learning models.

    Un Modelo Predictivo de Control (MPC es un sistema que permite llevar a cabo el control de una planta de producción. Gracias a este tipo de sistemas es posible realizar una producción que se aproxime al “cero defectos”. Para poder desempeñar su labor fundamental, este tipo de sistemas se compone de varias fases o etapas. Una de las más importantes es la fase que permite predecir la situación en la que se va a encontrar la planta en un momento dado. La mayoría de los avances realizados en este campo han estado ligados a los MPC lineales, a pesar de que el proceso que se intenta representar no lo sea. Así, en este artículo, se presentan varios experimentos que permiten demostrar que la etapa de predicción, habitualmente representada por una única función matemática, puede ser representada mediante modelos de aprendizaje automático.

  3. Fases para el diseño y análisis de la Cadena de Valor en las organizaciones en las organizaciones

    Directory of Open Access Journals (Sweden)

    Emilio García Vega

    2010-07-01

    Full Text Available La generación de valor es un tema fundamental en la gestión de las organizaciones debido a que permite la satisfacción de los consumidores, la dinámica frente a la competencia y la retribución a los dueños o accionistas. Su tratamiento responde tanto al mundo académico como al empresarial; es decir, a docentes, investigadores, ejecutivos y responsables de las empresas, ya sean estas micro, pequeñas, medianas o grandes. Si bien existen diferentes aproximaciones al tema, este trabajo buscará desarrollar un acercamiento desde el punto de vista competitivo y mediante la cadena de valor, debido a que esta puede ser considerada como una herramienta válida para diseñar y analizar cómo las organizaciones generan valor. Asimismo, esta investigación trata de presentar la evolución de la generación de valor, partiendo de los modelos clásicos de McKinsey & Company y de Michael Porter. Luego, se presentan algunos planteamientos y aportes a la cadena de valor de diferentes autores y desde diversos puntos de vista, hasta tener cercanía a la actualidad, de modo que se pueda contar con una serie de ideas adicionales, las cuales el autor considera relevantes para afrontar el diseño y análisis de la mencionada cadena. Finalmente, sobre la base del aporte capital del citado profesor de la Universidad de Harvard, se presenta una serie de recomendaciones para la aplicación estratégica de la cadena de valor en la gestión de las organizaciones actuales, las cuales están organizadas en nueve fases (fases para el diseño y análisis de la cadena de valor.

  4. Isotope geochemistry of brasiliano age, coarsely porphyritic, K-calc-alkalic granitoids and associated K-diorites, northeast Brazil

    International Nuclear Information System (INIS)

    Sial, A.N.; Mariano, G.; Ferreira, V.P.

    1989-01-01

    Several porphyritic, K-calc-alkalic were syntectonically intruded in NE Brazil during the Brasiliano orogeny. They show bi-(qz) diorite and coarsely porphyritic granodiorite to qz monzonite ('Itaporanga-type') in commingling zones on a scale of cm to m irrespective of whether plutons are at the margins of the NE-trending Cachoeirinha-Salgueiro Fold Belt (CSF) or intruded metasediments of the Serido Fold Belt (SFB). The bi(qz) diorites are found in magmatic or stromatic structures and narrow dikes wich intruded the felsic facies. SiO 2 in the porphyritic facies ranges from 61 to 72% with K 2 O usually > Na 2 O. K-diorities exhibit SiO 2 from 50 to 58%, MgO from 2 to 10% and K 2 O from 2 to 5%. Both facies are usually Ba and Sr-enriched, with similar, highly fractionated REE patterns, lacking free of Eu anomaly. Quartz 180 values are considered homogeneous on the scale of these intrusions in the CSF, (8 to 10 per milSMOW). Bi-(qz) diorites exhibit slightly higher 180 (9.5 to 10.5 per milSMOW). In the SFB both facies are lower than 180. The oxygen isotope data for the porphyritic facies are compatible with I-type source with some metasedimentary component of variable proportion. As bi(qz) diorites were formed pre- to post-porphyritic facies intrusion, their high LREE, K and 180 reflect their source rather than the interaction with the potassic felsic magma. Preliminarly sulfur isotope values suggest that porphyritic facies of granitoids in the SBF are lower in 34S than those in the CSF. Rb and Sr isotopes reflect source heterogeneity, complicated by mixing relations. Ages span from 510 to 630 Ma suggesting that the Itaporanga-type association was formed during uplift and cooling of the Pan-African I and onset of the Pan-African II orogenies, recognized in West Africa. (author) [pt

  5. Exigências de treonina para frangos de corte machos nas fases de 1 a 20, 24 a 38 e 44 a 56 dias de idade Threonine requirement of male broiler chicks from 1 to 20, 24 to 38 and 44 to 56 days of age

    Directory of Open Access Journals (Sweden)

    Anel Atencio

    2004-08-01

    Full Text Available Três experimentos foram realizados com o objetivo de determinar a exigência de treonina e a relação treonina:lisina digestível para frangos machos, Avian Farm, nas fases de 1 a 20, 24 a 38 e 44 a 56 dias de idade. Os experimentos foram conduzidos em delineamento inteiramente casualizado, com cinco níveis de treonina digestível, seis repetições e 20 aves por boxe nas fases de 1 a 20 e 24 a 38 dias de idade e 16 aves por boxe na fase de 44 a 56 dias de idade. Os níveis de treonina digestível utilizados nas diferentes fases foram: de 1 a 20 dias de idade, 0,684 a 0,870% (incremento de 0,047%; de 24 a 38 dias de idade, 0,637 a 0,807% (incremento de 0,043%; e de 44 a 56 dias de idade, 0,565 a 0,715% (incremento de 0,037%. No final de cada experimento, foram avaliadas as características de desempenho e a qualidade de carcaça. Houve efeito quadrático para consumo de ração e ganho de peso na fase de 1 a 20 dias de idade. A exigência de treonina digestível (total na fase de 1 a 20 dias de idade foi de 0,777% (0,890% total, correspondente a uma relação treonina:lisina de 67%, de acordo com os resultados de ganho de peso e com o modelo descontínuo. Não houve efeito dos níveis de treonina sobre as características de desempenho, sugerindo que o nível de treonina digestível (total de 0,637 (0,731% total, correspondente a uma relação de 60%, foi suficiente para atender às exigências das aves na fase de 24 a 38 dias de idade, no entanto níveis mais baixos devem ser estudados para determinação do valor exato da exigência. Observou-se efeito linear dos níveis de treonina digestível sobre o rendimento de perna na fase de 24 a 38 dias de idade. Não houve efeito dos níveis de treonina sobre as características de desempenho e rendimento de cortes nobres na fase de 44 a 56 dias de idade, sugerindo que o nível de treonina digestível (total de 0,565% (0,650% total, correspondente a uma relação de 60%, foi suficiente para

  6. Tentativa de tratamento específico, por meio da ticlopidina, de pacientes com doença de Chagas em fase crônica

    Directory of Open Access Journals (Sweden)

    Rassi Anis

    2000-01-01

    Full Text Available Em investigação experimental, a ticlopidina mostrou ser ativa no sentido de diminuir a parasitemia e a mortalidade quando avaliada a infecção de camundongos pelo Trypanosoma cruzi. Por isso, este fármaco foi administrado a 12 pacientes com doença de Chagas, em fase crônica. Houve utilização de 150, 200 ou 250mg, durante 90 dias, conforme se tratasse de crianças, adolescentes ou adultos, respectivamente. Ficou documentado cabal insucesso sob os pontos de vista parasitológico e sorológico.

  7. Síntesis de TiO2, fase anatasa, por el método solgel: estudio del efecto de la presencia de AcacH en el sistema

    Directory of Open Access Journals (Sweden)

    Yasser Ochoa

    2010-01-01

    Full Text Available El dióxido de titanio, TiO2, es un semiconductor tipo n sensible a la luz que absorbe radiación electromagnética en la región del UV, es anfótero y muy estable químicamente. Por las características mencionadas es el fotocatalizador más empleado y actualmente se utiliza para degradar moléculas orgánicas durante la purificación del agua. En este trabajo se utilizó el método Sol-Gel para sintetizar dióxido de titanio, proceso que permitió obtener materiales amorfos y policristalinos de forma sencilla. Se estudió el efecto de la presencia de un acomplejante, acetilacetona, y de los tratamientos térmicos realizados a las muestras sobre las características del producto final, poniendo especial atención a la fase cristalina presente en el sólido, para el presente caso anatasa. Los polvos cerámicos obtenidos se caracterizaron empleando diferentes técnicas, principalmente espectroscopía infrarroja con transformada de Fourier (FTIR, difracción de rayos X (DRX y microscopía de transmisión (MET. Los resultados indican que utilizando AcacH se pueden obtener partículas nanométricas (< 20 nm de TiO2 fase anatasa, muy bien cristalizado a 450ºC.

  8. ESTUDIO CINÉTICO DE LA HIDRODECLORACIÓN CATALÍTICA DE CLOROFENOLES EN FASE ACUOSA

    Directory of Open Access Journals (Sweden)

    Elena Diaz

    2011-01-01

    Full Text Available En este trabajo se estudió la hidrodecloración catalítica de 2-clorofenol, 4-clorofenol y 2,4-diclorofenol en fase acuosa empleando un catalizador comercial de Pd/Al2O3 (0,5 % w/w, en condiciones suaves de operación (30oC, 1 bar. La conversión de los reactivos resultó completa en tiempos cortos de reacción. Analizando la evolución de la concentración frente al tiempo de cada uno de los reactivos, intermedios y productos de reacción, se estableció un esquema de reacción serie-paralelo para cada una de las reacciones de hidrodecloración. Se desarrollo un modelo cinético de primer orden respecto al clorofenol de partida que se validó mediante el adecuado ajuste de los resultados experimentales. La posición de los átomos de cloro en la molécula orgánica y el número de los mismos influyeron significativamente tanto en la reactividad de los clorofenoles ensayados como en la velocidad de decloración. Así, la velocidad de decloración siguió el siguiente orden: 4-clorofenol > 2-clorofenol > 2,4-diclorofenol.

  9. El uso de placebo en ensayos clínicos de fase III en Brasil

    Directory of Open Access Journals (Sweden)

    Gustavo Butzge Rubenich

    2015-01-01

    Full Text Available El Consejo Federal de Medicina de Brasil (CFM –órgano normativo y fiscalizador del ejercicio ético de la medicina– prohibió, en 2008, la participación de médicos brasileños en investigaciones que utilizaran placebo para enfermedades con tratamiento eficaz y efectivo, en contraposición a la Declaración de Helsinki, que permite su uso en condiciones metodológicamente justificadas. Con el objetivo de verificar si la normativa ética del CFM modificó el uso de placebo en ensayos clínicos de fase III en Brasil, se analizaron varias características de sus registros en el ClinicalTrials.gov, en los períodos de 2003 a 2007 y de 2009 a 2013. Se concluye que: a la normativa promulgada por el CFM en 2008 fue ineficaz y prevaleció la posición adoptada por la Declaración de Helsinki; b el patrocinio de ensayos con placebo por parte de la industria farmacéutica multinacional fue significativo; c predominaron las investigaciones de fármacos para enfermedades crónicas, y fueron poco significativas para las enfermedades postergadas, de importancia para Brasil.

  10. Migration of fluids as a tool to evaluate the feasibility of the implantation of geological radioactive wastes repositories (RARN) in granitoid rocks: tests on granites submitted to natural deformation vs. not deformed

    International Nuclear Information System (INIS)

    Lopes, Nilo Henrique Balzani; Barbosa, Pedro Henrique Silva; Santos, Alanna Leite dos; Amorim, Lucas Eustáquio Dias; Freitas, Mônica Elizetti de; Rios, Francisco Javier

    2017-01-01

    Fluid composition and migration studies in granitoid rocks subjected to deformation events are a factor that should be considered in the selection of geologically favorable areas for RANR construction, and may be an excellent complement to engineering barrier designs. The research objective was to develop an academic approach, comparing the behavior of deformed and non-deformed granites, not being related to any CNEN project of deploying repositories. It is concluded that in the choice of suitable sites for the construction of repositories, granite bodies that are submitted to metamorphic / deformation / hydrothermal events or that are very fractured should be disregarded. The domes of granite batholith that have undergone hydraulic billing should also be discarded. It has been found that, because of the warming caused by radioactive decay reactions, there is a real possibility that the release of potentially abrasive fluids contained in the minerals can reach and corrode the walls of the repositories and / or packaging

  11. Características clínicas da fase aguda da infecção experimental de felinos pelo vírus da imunodeficiência felina

    Directory of Open Access Journals (Sweden)

    M.S. Zanutto

    2011-03-01

    Full Text Available A infecção dos felinos pelo Vírus da Imunodeficiência Felina (FIV resulta no desenvolvimento da síndrome de imunodeficiência dos felinos. Gengivite, perda de peso, linfadenomegalia generalizada, anemia, insuficiência renal crônica, complicações neurológicas, diarréia crônica e infecções bacterianas são encontradas frequentemente. A fase aguda da infecção pode ser assintomática, retardando o estabelecimento do diagnóstico e a implantação de medidas profiláticas para restringir o contágio e a transmissão do agente aos felinos suscetíveis. Com a finalidade de estudar as características clínicas da fase aguda da infecção, dez felinos jovens, sem definição racial, com oito meses de idade foram inoculados por via endovenosa com 1mL de sangue venoso de um gato portador do FIV subtipo B. A confirmação da infecção foi obtida através de teste sorológico em quatro e oito semanas pós-inoculação (p.i. e por nested-PCR. Foram realizados hemogramas semanais, exame ultrassonográfico do abdômen quinzenais e exame oftalmológico mensal, durante doze semanas p.i. Discreta tendência a linfopenia na segunda semana p.i. e a neutropenia entre a quinta e sétima semana p.i., febre intermitente em alguns gatos, linfadenomegalia e hepato-esplenomegalia entre a quarta e a 12ª semana p.i. foram as alterações clínicas observadas. Apenas um gato apresentou uveíte unilateral direita. A fase aguda da infecção transcorreu com alterações clínicas inespecíficas. A linfadenomegalia e a hepato-esplenomegalia observadas no decorrer da infecção, refletindo hiperplasia linfóide, sugerem a necessidade de se realizar o teste sorológico para o FIV, em todos os gatos que se apresentarem com essas alterações, o que permitirá o diagnóstico precoce da infecção e a adoção de medidas profiláticas no sentido de minimizar a propagação da infecção.

  12. Estructura y textura de la fase Al3CaZn en una chapa laminada de la aleación superplástica Al-5 % Ca-5 % Zn

    Directory of Open Access Journals (Sweden)

    Pérez-Pardo, M. T.

    1998-05-01

    Full Text Available The structure of the intermetallic phase Al3CaZn present in the superplastic sheet alloy Al-5 % Ca-5 % Zn has been determined by means of x-ray diffraction (XRD and electrón diffraction (TEM. Also, the texture of this phase has been studied by means of pole figures and the orientation distribution function (ODF. The Al-5 % Ca-5 % Zn alloy is formed by a fine grained aluminum matrix (d ≈ 2-3 μm and 20 % vol. of Al3CaZn in the form of round-shaped particles with 0.2-0.5 μm diameter. This alloy undergoes superplastic behavior in a wide range of strain rates and temperatures. It has been found in this work that the structure of the second phase is body-centered tetragonal, with lattice parameters a = b = 0.422 nm and c = 1.131 nm. The texture of the alloy is formed by the fiber <001>, i.e., the crystallites are oriented preferentially with the c-axis perpendicular to the rolling plane. The texture sharpens after severe annealings.

    En este trabajo se ha determinado la estructura de la fase Al3CaZn, presente en una chapa laminada de la aleación Al-5 % Ca-5 % Zn, mediante técnicas de difracción de rayos X (DRX y difracción de electrones (MET. Además, se ha estudiado su textura mediante figuras de polos y la función de distribución de orientaciones (FDO. La aleación Al-5 % Ca-5 % Zn objeto de este estudio consta de una matriz de aluminio de grano fino (d ≈ 2-3 μm y un 20 % vol. de la fase Al3CaZn. Esta segunda fase está presente en el material de partida en forma de partículas esferoidales de 0,2 - 0,5 μm de diámetro. La aleación presenta un comportamiento superplástico en un amplio intervalo tanto de velocidades de deformación como de temperaturas. Se ha encontrado que la fase Al3CaZn posee una estructura tetragonal centrada, con parámetros de red a = b= 0,422 nm y c = 1,131 nm. Presenta, además, una textura de fibra <001>, en la

  13. Estimación de la característica de Inductancia de fase del Motor de Reluctancia Conmutada MFR 132.1 Estimation of phase inductance profile of MFR 132.1 switched reluctance motor

    Directory of Open Access Journals (Sweden)

    Javier Quintana Santos

    2011-06-01

    Full Text Available En el presente trabajo se enuncia la idea fundamental en la que se basan todos los métodos empleados para la estimación de los parámetros de fase de los motores de reluctancia conmutada. Se describe, además, un algoritmo de división con punto decimal fijo en lenguaje VHDL. El algoritmo descrito se utiliza posteriormente para la estimación de la inductancia de fase del motor de reluctancia conmutada MFR 132.1, mediante el empleo de la técnica invasiva de modulación de amplitud con señales de tensión pulsantes de tres estados. Se diseñó y construyó una instalación experimental sobre la base de un FPGA de Actel, de la familia ProASIC 3 modelo A3P250, para el procesamiento de las señales. Finalmente se exponen y comentan las características de inductancia de fase del motor de reluctancia MFR 132.1, obtenidas.  In the present work is enunciated the fundamental idea of all the methods used for the estimation of phase parameters in the switched reluctance motors. The fixed point division algorithm employed to estimate the inactive phase inductance profile of the MFR 132.1 switched reluctance motor, is described in VHDL programming language. The algorithm implements the intrusive estimation technique of amplitude modulation with three states pulsating signals. The structure of the experimental set up for the digital signal processing, which is based on the Actel FPGA ProAsic 3 A3P250 development kit, is depicted. Finally, the inactive phase’s inductance profiles, which were experimentally obtained, are shown for different voltage values in the Direct Current converter link.

  14. Fase gametofítica del helecho Microgramma nitida (Polypodiaceae

    Directory of Open Access Journals (Sweden)

    Ma. del Rosario Ramírez

    1998-09-01

    Full Text Available Se describe la fase gametofítica del helecho Microgramma nitid con esporas de Veracruz, México (siembra promedio 40 esporas/ cm². La morfogénesis se caracteriza por: germinación tipo Vittaria, un filamento inicial de seis células protálicas; gametofitos jóvenes espatulados que se transforman en gametofitos adultos cordiformes-alargados, con márgenes ondulados y tricomas unicelulares-capitados en los margenes y en las superficies; aparición de una célula meristemática obcónica apical, que es reemplazada rápidamente por un meristemo pluricelular. Los anteridios y arquegonios son del tipo usual de las Polypodiaceae s.str. El desarrollo protálico es del tipo Drynaria. Ocho meses después de la siembra apareció la primera hoja del esporofito; ésta es espatulada, con márgenes lisos y una hilera de células aclorofílicas, tricomas pluricelulares, bifurcados y estomas anomocíticos. Las células epidérmicas de la hoja del esporofito tienen paredes laterales onduladas en las superficies dorsal y ventral.The development of the gametophytic phase of Microgramma nitida is described based on spore samples that was obtained of fertil specimens gathered on Veracruz State, Mexico. The spore sowing density was 40 spores/cm2 ; it is characterized by Vittaria-type germination of the spore, a germinal filament of six cells; young gametophytes are naked, spathulated and later are transformed in cordate-elongated adult gametophytes with wavy borders; marginal, superficial capitated, unicellular hairs; the meristematic cell is wedge-shaped and is quickly replaced by a pluricellular meristem. The antheridia and archegonia are of the usual Polypodiaceae s. str.type. Prothallial development is thus of the Drynaria-type. The first leaf of the sporophyte appeared eight months after spore sowing. The leaf is spathulated, with smooth borders and the margin has a row of cells without chlorophyll; bifurcated and pluricellular hairs; anomocytic stomata; the

  15. Shelters in Denmark for Battered Women

    DEFF Research Database (Denmark)

    Koch-Nielsen, Inger; Caceres, Lucia

    The first Danish crises centres were part of the women’s move-ment back into the 1970’s and were originally based mainly upon female volunteers, who saw the volunteering as part of their engagement in the movement. The centres were created upon and ran according to the principles of sister solida...

  16. Spatiotemporal evolution of magmatic pulses and regional metamorphism during a Cretaceous flare-up event: Constraints from the Ryoke belt (Mikawa area, central Japan)

    Science.gov (United States)

    Takatsuka, Kota; Kawakami, Tetsuo; Skrzypek, Etienne; Sakata, Shuhei; Obayashi, Hideyuki; Hirata, Takafumi

    2018-05-01

    The spatiotemporal relationship between granitoid intrusions and low-pressure/temperature type regional metamorphism in the Ryoke belt (Mikawa area) is investigated to understand the tectono-thermal evolution of the upper- to middle-crust during a Cretaceous flare-up event at the Eurasian active continental margin. Three plutono-metamorphic stages are recognized; (1) 99-84 Ma: intrusion of granitoids (99-95 Ma pulse) into the upper crust and high-T regional metamorphism reaching sillimanite-grade (97.0 ± 4.4 Ma to 88.5 ± 2.5 Ma) in the middle crust, (2) 81-75 Ma: intrusion of gneissose granitoids (81-75 Ma Ma pulse) into the middle crust at 19-24 km depth, and (3) 75-69 Ma: voluminous intrusions of massive to weakly-foliated granitoids (75-69 Ma pulse) at 9-13 km depth and formation of contact metamorphic aureoles. Cooling of the highest-grade metamorphic zone below the wet solidus of granitic rocks is estimated at 88.5 ± 2.5 Ma. At ca. 75 Ma, the upper-middle crustal section underwent northward tilting, resulting in the exhumation of regional metamorphic zones to 9-13 km depth. Although the highest-grade metamorphic rocks and the 99-95 Ma pulse granitoids preserve similar U-Pb zircon ages, the absence of spatial association suggests that the regional metamorphic zones were mainly produced by a transient thermal anomaly in the mantle and thermal conduction through the crust, supplemented by localized advection due to granitoid intrusions. The successive emplacement of granitoids into shallow, deep and shallow levels of the crust was probably controlled by the combination of change in thermal structure of the crust and tectonics during granitoid intrusions.

  17. Sustancias húmicas en la disminución del estrés en gallinas ponedoras durante la fase posmuda

    Directory of Open Access Journals (Sweden)

    Rosa Angélica Sanmiguel-Plazas

    2015-01-01

    Se tomaron muestras sanguíneas los días 8,30 y 60, para evaluar hematocritos y relación heterófilos/linfocitos (H/L, y se registró la inmovilidad tónica (IT los días 30 y 60.Se evidenció que los días 30 y 60, los grupos suplementados con SH incrementaron la concentración de hematocrito y disminuyeron la relación H/L y el tiempo de IT (p<0,05. Los resultados obtenidos indican que las SH provenientes de la biotransformación de cachaza, hojas y vinaza de la producción de azúcar se comportan como agentes mitigadores de estrés en la fase temprana y media de la posmuda en gallinas ponedoras Hy Line Brown.

  18. CONTROL Y VIGILANCIA EN FRONTERAS. PAPEL DE SANIDAD EXTERIOR DURANTE LAS FASES DE CONTENCIÓN DE LA PANDEMIA (H1 N1 2009

    Directory of Open Access Journals (Sweden)

    Miguel Dávila Cornejo

    2010-01-01

    Full Text Available Los controles sanitarios en fronteras, establecidos con el objetivo de retrasar la entrada del virus pandémico en España, constituyen una de las actividades propias de las fases de contención de la enfermedad. Su puesta en práctica como estrategia de salud pública en respuesta a epidemias es responsabilidad de la Dirección General de Salud Pública y Sanidad Exterior del Ministerio de Sanidad y Política Social, a través de la Subdirección General de Sanidad Exterior, y para ello se requiere una actuación coordinada con otros organismos implicados. Este trabajo tiene como finalidad describir las actuaciones realizadas en los aeropuertos internacionales durante dichas fases, así como evaluar su efectividad en la consecución del objetivo para el que fueron diseñadas. En este sentido, se establece una hipótesis que trata de explicar cómo las medidas adoptadas por Sanidad Exterior y la colaboración con los Servicios de Vigilancia Epidemiológica de las Comunidades Autónomas podrían haber contribuido a retrasar la propagación del virus en nuestro país. Se destaca la necesidad de consolidar los sistemas de vigilancia en fronteras potenciando dicha colaboración, así como la importancia de diseñar una estrategia clara de comunicación a la población en estos escenarios, que debe acompañar a la implementación de las demás medidas para evitar situaciones de incertidumbre.

  19. Migrantes por amor? Ciclo de vida, gênero e a decisão de migrar em diferentes fases da vida

    Directory of Open Access Journals (Sweden)

    Viviane Assunção

    2016-05-01

    interlocutoras de uma pesquisa etnográfica realizada entre 2012 e 2013, a idade é um importante fator a ser considerado para ponderar os riscos, vantagens e desvantagens da migração. Além da faixa etária, outros marcadores do curso de vida, como ter filhas/os, o nascimento das/os netas/os e a idade destes indivíduos também são considerados em suas decisões. O artigo também traz as considerações das interlocutoras da pesquisa sobre o amor, que, segundo elas, difere a cada fase da vida. Mais do que o amor por seus companheiros holandeses, elas evidenciam e reificam a idealização do amor materno.

  20. Experimental numerical study utilizing CFD in a stratified gasifier operating with biomass; Estudio numerico experimental de un gasificador estratificado que opera con biomasa, utilizando CFD

    Energy Technology Data Exchange (ETDEWEB)

    Rogel Ramirez, Alejandro

    2007-07-01

    The central idea behind this work is the developing of a numeric-experimental model, useful to optimize the biomass stratified gasifier design. Firstly, model validation will be carried up by comparison with reference experimental data available. This study describes a 1-D + 2-D numerical model used to simulate the gasification of pine wood pellets in a stratified downdraft gasifier whereby Eulerian conservation equations are solved for particle and gas phase components, velocities and specific enthalpies. The model takes into account the biomass particle process such as heating up, drying, primary pyrolysis of biomass, secondary pyrolysis of tar, homogeneous reactions and heterogeneous combustion/gasification reactions, and particle size change. This CFD model can be used to predict temperature profiles, gas composition, producer gas lower heating value, and carbon conversion efficiency, and the reactor performance when operating parameters and feed properties are changed. The standard {kappa}-{epsilon} and RNG {kappa}-{epsilon} models were used to simulate the turbulent flow conditions. [Spanish] La idea central del presente trabajo es el desarrollo de un modelo numerico- experimental, para optimizar el diseno de gasificadores estratificados de biomasa. Primeramente, el modelo sera validado utilizando datos experimentales disponibles en la literatura. Este estudio describe un modelo numerico 1-D+2-D, utilizado para simular la gasificacion de 'pelets' de madera de pino en un gasificador estratificado de flujos paralelos, en el que se resuelven ecuaciones de conservacion Eulerianas para los componentes de la fase gaseosa, la fase solida, velocidades y entalpias especificas. El modelo considera procesos como: calentamiento, secado de la biomasa, pirolisis primaria de la madera, pirolisis secundaria de los alquitranes, reacciones homogeneas, reacciones heterogeneas de combustion/gasificacion y cambio en el tamano de la particula. Este modelo CFD puede ser

  1. Petrogenesis of the middle Jurassic appinite and coeval granitoids in the Eastern Hebei area of North China Craton

    Science.gov (United States)

    Fan, Wenbo; Jiang, Neng; Xu, Xiyang; Hu, Jun; Zong, Keqing

    2017-05-01

    An integrated study of zircon U-Pb ages and Hf-O isotopic compositions, whole rock elemental and Sr-Nd isotope geochemistry was conducted on three lithologically diverse middle Jurassic plutons from the Eastern Hebei area of the North China Craton (NCC), in order to reveal both their petrogenesis and possible tectonic affinity. The three plutons have consistent magmatic zircon U-Pb ages from 167 ± 1 Ma to 173 ± 1 Ma. The Nianziyu pluton has typical characteristics of appinite with low SiO2 (43.7-52.6%), high Ca, Mg, Fe and H2O contents. It possesses subduction-related trace element patterns, enriched Nd-Hf isotopic signatures as well as elevated zircon δ18O values (6.2-7.2‰), arguing for an enriched mantle source metasomatized by fluids related to subduction. The Shuihutong monzogranites have high silica (SiO2 = 75.4-75.9%) and alkali contents, low Ca contents and striking negative Ba, Sr and Eu anomalies. Samples from the pluton have more evolved Nd-Hf isotopic values and are considered to be most likely derived from anatexis of ancient lower continental crust. Hybridization between mantle- and ancient lower crust-derived magmas is proposed for the mafic microgranular enclave-bearing Baijiadian granitoids, which are characterized by variable εNd (t) and εHf(t) values. Integrated with the regional geologic history, we suggest that the formation of the three middle Jurassic plutons were related to the subduction of the Paleo-Pacific ocean plate beneath the NCC. Their petrogenetic differences reflect complex magmatic processes in subduction settings involving melting of multiple sources, possible partly facilitated by fluid metasomatism and water-rich magma injection, accompanied with various degrees of magma mixing. The appearance of middle Jurassic appinitic rocks leads us to propose that the NCC destruction and lithosphere thinning were facilitated and controlled by the weakening of the lithospheric mantle after hydration because of the subduction of the

  2. Microextracción en fase sólida de compuestos volátiles en albahaca (Ocimum basilicum L. Microextracción en fase sólida de compuestos volátiles en albahaca (Ocimum basilicum L.

    Directory of Open Access Journals (Sweden)

    Isaac Andrade-González

    2012-02-01

    Full Text Available Volatile compounds of basil (Ocimum basilicum L. were extracted with solid phase microextraction(SPME and analyzed with gas chromatography-mass spectrometry (GC-MS. TwoSPME fiber coatings, Polydimethylsiloxane/Divinylbenzene (PDMS/DVB, 65 μm and Carbowax/Divinylbenzene (CW/DVB, 65 μm were evaluated in order to compare the extraction ofcomponents. Among the 25 volatile compounds detected were phenylpropanoids, monoterpenes,sesquiterpenes, esters, and aldehydes. There were significant (P Los compuestos volátiles de la albahaca (Ocimum basilicum L. fueron extraídos mediante la microextracción en fase sólida (SPME y analizados con cromatografía de gases-espectrometría de masas (GC-MS. Se evaluaron dos fibras, Polidimetilsiloxano/Divinilbenceno (PDMS/DVB, 65 μm y Carbowax/Divinilbenceno (CW/DVB, 65 μm, para comparar la extracción de componentes. Entre los 25 compuestos volátiles recuperados en la albahaca, se identificaron fenilpropanoides, monoterpenos, sesquiterpenos, ésteres, y aldehídos. Hubieron diferencias significativas (P Cuantitativamente, el componente más importante fue el cinamato de metilo, seguido por el linalol.

  3. VALIDACIÓN DE UN MÉTODO PARA EL ANÁLISIS DE RESIDUALIDAD DE PLAGUICIDAS EN AGUACATE HASS

    Directory of Open Access Journals (Sweden)

    SANTIAGO BENAVIDES

    2014-07-01

    Full Text Available El aguacate es una fruta que se caracteriza por su alto contenido de grasas, siendo la variedad Hass la de mayor cantidad de pigmentos y componentes fenólicos, lo que la convierte en una matriz compleja para el análisis de residuos de plaguicidas. Se validó un método para el análisis simultáneo de residualidad de tres plaguicidas en aguacate fresco de la variedad Hass. Se aplicó la técnica QuEChERS siguiendo una modificación del protocolo AOAC 2007.1; para la preparación de las muestras se empleó acetonitrilo acidificado, MgSO4 y CH3COONa y se limpiaron por extracción en fase solida dispersiva con una mixtura de sorbentes: amina primaria secundaria (PSA, octadecilo (C18 y carbón grafitado negro GCB. Los plaguicidas fueron analizados por GC-μECD. En el análisis de linealidad se obtuvieron correlaciones de 0,9908; 0,9968 y 0,9965 para dimetoato, malatión y deltametrina respectivamente y se cumplieron las pruebas de significancia. El efecto matriz provoca una mejora en la sensibilidad de la curva de calibración producto de la concentración de la muestra en la extracción. Se lograron límites de cuantificación de 0,02mg/kg para los tres compuestos con estimaciones de incertidumbre menores al 50%. Se cumplieron los criterios de precisión y exactitud, logrando una validación exitosa.

  4. Estudio del Efecto de Suspensiones Biológicas sobre la Formación de Fases Acuosas en Sistemas de Extracción que Utilizan Polietilenglicol (PEG) y Fosfato-Edición Única

    OpenAIRE

    Luisa Fernanda Cueto Gómez

    1999-01-01

    Los procesos de extracción líquido-líquido de dos fases acuosas representan una alternativa conveniente para recuperar macromoléculas (P. Ej. proteínas) presentes en suspensiones biológicas, debido a que dichos sistemas propician condiciones de operación amigables y que permiten mantener la estabilidad de las proteínas.

  5. Sistemas dinámicos en la interacción emocional madre-hijo: primera fase

    Directory of Open Access Journals (Sweden)

    Jaime Castro Martínez

    2013-03-01

    Full Text Available Los avances en psicología de las emociones y psicología del desarrollo han exigido nuevos cambios tanto de orden teórico como metodológico para describir y explicar la variabilidad de las res-puestas infantiles a los cambios que tienen lugar en la dinámica socio-emocional con la madre. Producto de estas variaciones, aparece la integración de los sistemas dinámicos a las descrip- ciones de los teóricos del desarrollo emocional bajo supuestos psicobiológicos y sociobiológicos. Esta investigación indaga el posible uso de modelos de sistemas dinámicos en la generación de patrones de organización durante la interrelación socio- emocional madre-hijo, bajo cambios en los estados emocionales de la madre y bajo modificaciones debidas al desarrollo infantil. Los hallazgos de esta primera fase muestran algunas diferencias en las dinámicas socio-emocionales en cada uno de los estados emocionales maternos, al igual que regu- laridades en la variación por estado emocional. La investigación sugiere ampliar el marco teórico hacia modelos de componentes emocionales y modelos neurobiológicos, y la inclusión de modelos matemáticos de predicción y de análisis de series de tiempos.

  6. Sr-Nd isotope systematics of xenoliths in Cenozoic volcanic rocks from SW Japan

    International Nuclear Information System (INIS)

    Kagami, Hiroo; Iwata, Masatoshi; Iizumi, Shigeru; Nureki, Terukazu.

    1993-01-01

    Based on new and previously published Sr and Nd isotope data, we examined the petrogenetic relationship between deep crust- and upper mantle-derived xenoliths contained in Cenozoic volcanic rocks and Cretaceous-Paleogene granitoid rocks in SW Japan. The deep crust- and upper mantle-derived mafic to ultramafic xenoliths contained in Cenozoic volcanic rocks from SW Japan have comparable initial Sr and Nd isotope ratios to the Cretaceous-Paleogene granitoid rocks in their respective districts. This may suggest that these xenoliths were genetically related to the Cretaceous-Paleogene granitoid rocks in SW Japan, and that regional variations in Sr and Nd isotope ratios observed in the granitoid rocks are attributed to differences in the geochemistry of the magma sources. (author)

  7. Materiales ultrablandos: diagrama de fase de una suspensión coloidal de polímeros estrella

    Directory of Open Access Journals (Sweden)

    Gregorio Alejandro Vejar Delgado

    2013-06-01

    Full Text Available La determinación experimental y predicción teórica de diagrama de fases para las sustancias es un aspecto de la mayor importancia en la ciencia de materiales. La cristalización y fusión a pesar de ser fenómenos cotidianos y de estar dentro de la agenda de estudio de la mecánica estadística desde sus inicios, aún no provee una teoría que las explique de primeros principios. La dificultad principal se debe a que estas transiciones se presentan en sistemas concentrados convirtiéndose en un problema colectivo de muchos cuerpos. Es en este contexto que la prescripción de criterios fenomenológicos que permitan la localización de las líneas de transición es altamente valorada por la comunidad científica. Motivados por ello, en esta comunicación se presentan resultados obtenidos con el criterio de Löwen, mediante simulaciones computacionales, para una suspensión coloidal de partículas ultra suaves conformada por polímeros estrella.

  8. Método para obtenção de metáfases mitóticas de ostras para o estudo do cariótipo

    Directory of Open Access Journals (Sweden)

    Rafael Alves

    2010-04-01

    Full Text Available http://dx.doi.org/10.5007/2175-7925.2010v23n1p111 Atualmente a maricultura está em expansão no litoral de Santa Catarina e Florianópolis é a maior cidade produtora de ostras do Brasil, sendo cultivada a ostra japonesa Crassostrea gigas (Thunberg, 1793. Sobre as ostras nativas há necessidade de muitos tipos de estudo, incluindo aqueles que auxiliem a elucidar a complexa questão sobre o número de espécies brasileiras do gênero Crassostrea. Os estudos taxonômicos de ostras têm se baseado, quase que exclusivamente, na morfologia das conchas de indivíduos recentes e fósseis, a qual nem sempre tem sido suficiente para diferenciar as espécies. Informações citogenéticas podem ser importantes, como características adicionais, para auxiliar na taxonomia. O objetivo deste trabalho foi experimentar e adequar metodologias tradicionalmente empregadas em citogenética animal para a obtenção de metáfases mitóticas para o estudo do cariótipo de ostras. Foram utilizados espécimes coletados na Praia da Ponta do Sambaqui – Florianópolis/SC/Brasil. O método mais eficaz foi a utilização de brânquias obtidas de animais tratados por 12h em solução de colchicina a 0,005% em água do mar, com tratamento hipotônico de 30min em solução de água deionizada 1:1. Apresenta-se um método que permite obter metáfases em quantidades maiores, com número pequeno de cromossomos sobrepostos e morfologia cromossômica bem definida para análise.

  9. Metallogenetic systems associated with granitoid magmatism in the Amazonian Craton: An overview of the present level of understanding and exploration significance

    Science.gov (United States)

    Bettencourt, Jorge Silva; Juliani, Caetano; Xavier, Roberto P.; Monteiro, Lena V. S.; Bastos Neto, Artur C.; Klein, Evandro L.; Assis, Rafael R.; Leite, Washington Barbosa, Jr.; Moreto, Carolina P. N.; Fernandes, Carlos Marcello Dias; Pereira, Vitor Paulo

    2016-07-01

    The Amazonian Craton hosts world-class metallogenic provinces with a wide range of styles of primary precious, rare, base metal, and placer deposits. This paper provides a synthesis of the geological database with regard to granitoid magmatic suites, spatio temporal distribution, tectonic settings, and the nature of selected mineral deposits. The Archean Carajás Mineral Province comprises greenstone belts (3.04-2.97 Ga), metavolcanic-sedimentary units (2.76-2.74 Ga), granitoids (3.07-2.84 Ga) formed in a magmatic arc and syn-collisional setting, post-orogenic A2-type granites as well as gabbros (ca. 2.74 Ga), and anorogenic granites (1.88 Ga). Archean iron oxide-Cu-Au (IOCG) deposits were synchronous or later than bimodal magmatism (2.74-2.70 Ga). Paleoproterozoic IOCG deposits, emplaced at shallow-crustal levels, are enriched with Nb-Y-Sn-Be-U. The latter, as well as Sn-W and Au-EGP deposits are coeval with ca. 1.88 Ga A2-type granites. The Tapajós Mineral Province includes a low-grade meta-volcano-sedimentary sequence (2.01 Ga), tonalites to granites (2.0-1.87 Ga), two calc-alkaline volcanic sequences (2.0-1.95 Ga to 1.89-1.87 Ga) and A-type rhyolites and granites (1.88 Ga). The calc-alkaline volcanic rocks host epithermal Au and base metal mineralization, whereas Cu-Au and Cu-Mo ± Au porphyry-type mineralization is associated with sub-volcanic felsic rocks, formed in two continental magmatic arcs related to an accretionary event, resulting from an Andean-type northwards subduction. The Alta Floresta Gold Province consists of Paleoproterozoic plutono-volcanic sequences (1.98-1.75 Ga), generated in ocean-ocean orogenies. Disseminated and vein-type Au ± Cu and Au + base metal deposits are hosted by calc-alkaline I-type granitic intrusions (1.98 Ga, 1.90 Ga, and 1.87 Ga) and quartz-feldspar porphyries (ca. 1.77 Ga). Timing of the gold deposits has been constrained between 1.78 Ga and 1.77 Ga and linked to post-collisional Juruena arc felsic magmatism (e.g., Col

  10. O eletrocardiograma na fase crônica da doença de Chagas experimental no cão

    Directory of Open Access Journals (Sweden)

    J. Pellegrino

    1946-03-01

    Full Text Available O Autor estudou o eletrocardiograma de 6 cães adultos antes e após a inoculação, nestes animais, de uma amostra de Schizotrypanum cruzi obtida de um caso humano de miocardite chagásica com bloqueio aurículo-ventricular total. A fase aguda da moléstia nos cães foi seguida por frequentes exames de sangue a fresco, entre lãmina e lamínula, para a pesquisa do flagelado. Os traçados eletrocardiográficos foram obtidos antes da inoculação e até 320 dias após a mesma. Além das derivações periféricas, em alguns cães, registrou também as derivações precordiais. A interpretação dos eletrocardiogramas seriados foi feita levando-se em conta a variabilidade dos traçados em série observada em cães normais. Em todos os 6 cães estudados houve uma diminuição muito acentuada da voltagem dos complexos ventriculares, denotando lesão miocárdica. A diminuição da voltagem de QRs já se evidencia na fase aguda e de transição da moléstia, tornando-se máxima logo no inicio da fase crônica. Em dois cães, paralelamente com a diminuição da voltagem, houve uma rotação do eixo elétrico para a esquerda. Em um cão foram observadas extrasístoles ventriculares e, em dois, extrasístoles auriculares. Somente em um cão observou alterações significativas da onda P. constituidas por alargamento e entalhe da mesma. O Autor salienta e discute o fato de não ter encontrado alterações na condução (não houve aumento de Pr e somente em um caso houve alargamento significativo de QRS. As pesquizas ainda continuam sendo apenas parciais os resultados apresentados. Agradecemos ao Prof. AMERICANO FREIRE pelas sugestões e ao Sr. KURT BENSEMANN pela constante assistencia técnica.The Author has studied the electrocardiograms of 6 adult dogs, before and after the inoculation of a Schizotrypanum cruzi strain in these animals, which has been obtained from a human case of Chagas' myocarditis with complete aurriculoventricular block. The acute

  11. Clasificación y selección de materiales de cambio de fase según sus características para su aplicación en sistemas de almacenamiento de energía térmica

    Directory of Open Access Journals (Sweden)

    Oliver, A.

    2012-03-01

    Full Text Available Thermal energy storage has been linked to Architecture since ancient times, in large massive buildings through sensible heat. Latent heat storage —through phase change materials (PCMs is another way of thermal storage, which has aroused great interest in recent decades. These materials, maintain constant temperature during the phase change while the material stores or releases energy. Their energy density storage is higher than any other. Its use is linked to renewable energy to adjust the supply periods to demand. In this paper we study the different phase change materials, classifying them and analyzing their physical, chemical, mechanical, thermal properties; availability, pricing, durability, and their compatibility with other materials. Their uses and most interesting applications are discussed.

    El almacenamiento térmico ha estado ligado a la edificación desde la Antigüedad, en las grandes construcciones masivas, mediante el calor sensible. Otra forma de almacenamiento térmico, que ha suscitado gran interés en las últimas décadas, es en forma de calor latente, mediante materiales de cambio de fase. Estos materiales mantienen constante la temperatura durante el cambio de fase mientras que el material almacena o cede energía. Este hecho supone una mayor densidad energética en comparación con cualquier otro. Su uso está ligado al de las energías renovables para ajustar los periodos de suministro a los de demanda. En este trabajo se estudian los diferentes materiales de cambio de fase, clasificándolos en diferentes grupos y analizando sus características físicas, químicas, propiedades mecánicas, térmicas, así como su compatibilidad con otros materiales, disponibilidad, precios, durabilidad… Se analizan sus usos y aplicaciones más interesantes en general.

  12. FASE INTESTINAL DE Trichinella spiralis EN MODELO MURINO

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    MARÍA ALEJANDRA MORENO GARCÍA

    2009-01-01

    Full Text Available RESUMEN Trichinella spiralis se encuentra principalmente en el hombre, rata, cerdo, perro; puede infectar a cualquier carnívoro u omnívoro. Cuando la carne o sus derivados están contaminados con larvas infectantes (LI de T. spiralis y son ingeridas éstas pasan al estómago, donde sus cápsulas son disueltas por acción de los jugos gástricos, las larvas son liberadas en pocas horas, después pasan a la porción proximal del intestino delgado, donde se lleva a cabo su desarrollo. El objetivo del presente trabajo fue evaluar la fase intestinal de T. spiralis en un modelo murino. Un lote de 45 ratas Long Evans, se infectaron con aproximadamente 500 LI, y fueron sacrificadas tres diarias por 15 días. Se tomó un segmento de duodeno, yeyuno e íleon y se fijaron en formol al 10% para posteriormente ser procesados en parafina y teñido con hematoxilina-eosina. El resto del intestino delgado fue fraccionado, se incubó a 37 ºC por dos horas y el sobrenadante se observó al microscopio de luz. Se encontró que el implante se lleva a cabo a nivel de yeyuno e íleon, que las hembras adultas dan origen aproximadamente 60-80 larvas recién nacidas (LRN, parto vivíparo en un tercio distal y subse-cuentemente son destruidas. Los machos adultos tienen espermatozoides no ciliados. Palabras clave: larvas infectantes, adultos, larvas recién nacidas. ABSTRACT Trichinella spiralis is a parasitic disease in man, rat, pig, but can infect any carnivorous or omnivorous. When the meat or their derivates are contaminated with infective larvae (il of T. spiralis pass to the stomach, their capsules are dissolved by the stomach juice, the larvaes are liberated in few hours, and then they pass to the near portion of the slim intestine in which they develop. The objective of the present work was to evaluate the intestine phase of T. spiralis in a murine model. Fourtyfive Long Evans rats were infected with 500 li approximately, then 3 rats were sacrificed everyday

  13. Argamassas com incorporação de Materiais de Mudança de Fase (PCM): Caracterização física, mecânica e durabilidade

    OpenAIRE

    Cunha,Sandra; Aguiar,José; Ferreira,Victor; Tadeu,António

    2015-01-01

    O despertar da consciência ambiental pela sociedade, tem levantado problemas até então ignorados tais como os consumos energéticos. Numa sociedade com um elevado ritmo de crescimento e padrões de conforto cada vez maiores, surge a necessidade de minimizar os elevados consumos energéticos, tirando partido de fontes de energia renováveis. As argamassas com incorporação de materiais de mudança de fase (PCM) possuem a capacidade de regular a temperatura no interior dos edifícios, contribuindo des...

  14. Passionflower supplementation in diets of Japanese qualis at rearing and laying periods Efeitos da utilização de passiflora em rações de codornas japonesas nas fases de recria e postura

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    Janaina Della Torre da Silva

    2010-07-01

    dietas (0, 125, 250 e 375, e 0, 250, 500 e 750 mg de passiflora/kg de ração nas fases de recria e postura, respectivamente, 8 repetições e 6 aves por parcela. A fase de recria iniciou-se aos 28 dias de idade das aves e teve duração de 15 dias. Nesta fase foram avaliados o consumo diário de ração, o ganho diário de peso, a conversão alimentar, a viabilidade, o tempo em imobilidade tônica, a intensidade de ferimentos, o comportamento, a relação heterófilo/linfócito e concentração plasmática de corticosterona. A fase de postura teve início quando as aves atingiram 43 dias de idade e seu término encerrou-se aos 140 dias de idade das aves; foi constituída de seis ciclos de 14 dias, nos quais foram avaliados o consumo de ração, a conversão alimentar, a produção e qualidade de ovos, a viabilidade, o tempo em imobilidade tônica, a intensidade de ferimentos, o comportamento, a relação herófilo/linfócito, a concentração plasmática de corticosterona e a resposta imunológica. Na fase de recria, o uso de passiflora na dieta de codornas influenciou os parâmetros comportamentais, tornando as aves mais calmas, principalmente na dosagem de 375 mg/kg de ração. Já na fase de postura, foi eficaz na redução do estresse das codornas, e os resultados mais promissores foram observados quando aplicadas as maiores dosagens do fitoterápico. A dosagem de 750 mg/kg de ração, no entanto, diminui a produção de ovos, embora não tenha influência na qualidade dos ovos nem a resposta imunológica das aves.

  15. Vivenciando a inexorabilidade do tempo e as suas mudanças com perdas e possibilidades: a mulher na fase do climatério Vivenciando la inexorabilidad del tiempo y sus cambios con pérdidas y posibilidades: la mujer en la fase del climaterio Living the inexorability of time and its changes with losses and possibilities: the woman in climacterium

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    Josefa Vieira de Lima

    2001-12-01

    Full Text Available Este estudo versa sobre a experiência da mulher na fase do climatério. O Interacionismo Simbólico e a Teoria Fundamentada nos Dados foram as abordagens teóricas e metodológicas que nortearam o estudo tendo em vista os seguintes objetivos: compreender como a experiência do climatério é definida pela mulher; quais os processos psicossociais de interação vividos pela mulher e desenvolver um modelo teórico representativo da vivência da mulher na fase do climatério. As estratégias utilizadas para a obtenção dos dados foram a observação e a entrevista. Tomamos como sujeito da investigação a mulher na faixa etária de 45 a 60 anos, perfazendo um total de 30 mulheres. Através deste estudo foi possível descobrir que a experiência do climatério pode ser constituída por dois fenômenos: REJEITANDO AS MUDANÇAS, no qual o climatério é caracterizado pela mulher como um momento de perda e BUSCANDO SUPERAR AS MUDANÇAS, que representa um momento na construção de novos conceitos, com possibilidades de renovação. A partir desses fenômenos identificamos a categoria central: VIVENCIANDO A INEXORABILIDADE DO TEMPO E SUAS MUDANÇAS COM PERDAS E POSSIBILIDADES, que é fundamental para o modelo teórico representativo da experiência da mulher na fase do climatério.Este estudio trata de la experiencia de la mujer en el período del climaterio. El Interaccionismo Simbólico y la Teoria Fundamentada en los Datos fueron los abordajes teórico y metodológico que nortearon el estudio teniendo en cuenta el alcance de los siguientes objetivos: comprender como la experiencia del climaterio es definida por la mujer; cuales son los procesos psicosociales de interacción vividos por la mujer y desenvolver un modelo teórico representativo dela vivencia de la mujer en la fase del climaterio. Las estrategias utilizadas para la obtención de los datos fueron la observación y la entrevista. Tomé como sujetos de la investigación la mujer en la

  16. Efek Beauveria bassiana pada Anopheles maculatus Fase Aquatik di Laboratorium

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    Bina Ikawati

    2017-07-01

    Full Text Available AbstractBeauveria bassiana can be used both as for controlling agricultural insect and protecting health. Thisstudy aims to examine the effects of aquatic phase of B. bassiana on An. maculatus in the laboratory.Samples were eggs and larvae of An. maculatus reared from Banjarnegara colony. Eggs and instarlarvae II, III and IV and their control which consisted of 10 larvae/eggs were replicated six times andcontacted to B. bassiana spores for 15 minutes and then transferred to aquades to be maintained forobservation, in every 24 hours as long as 192 hours (8 days. Probit analysis found that applicationof B. bassiana caused damage of external coat of eggs and inhibited >60% of unhatched eggs. Lethaldosage was dosage spores of 1,713x107 (16 days, whereas the lethal dose required to make 50% ofunperached eggs is a dose of spore concentration of 1,361x107 (11.6 days. Higher concentrationswill be needed to know the faster effects B bassiana on An. maculatus larvae or eggs.Key words: Beauveria bassiana, Anopheles maculatus, aquatic phase, laboratory AbstrakBeauveria bassiana dapat digunakan baik sebagai pengendali serangga pertanian maupun kesehatan.Penelitian ini bertujuan mengkaji efek B. bassiana terhadap An. maculatus pada fase akuatik dilaboratorium. Sampel uji berupa telur dan larva An. maculatus dari koloni Banjarnegara. Telur danlarva instar II,III dan IV serta kontrol masing-masing sebanyak 10 ekor/butir dengan replikasi 6 kalidikontakkan dengan spora B. bassiana selama 15 menit dan selanjutnya dipindahkan ke aquadesuntuk dipelihara untuk dilakukan pengamatan, pengamatan dengan mikroskop compound terutamapada larva yang lemah/mati setiap 24 jam selama 192 jam (8 hari. Analisis probit membuktikanbahwa aplikasi B. bassiana pada telur menimbulkan efek kerusakan pada lapisan luar telur diketahuidari pengamatan dengan mikroskop serta mampu menghambat >60% telur tidak menetas. Simulasidengan análisis probit menunjukkan lethal dose yang dibutuhkan

  17. U-Pb (LA-ICPMS) zircon ages and Nd isotopes for granitoids of the Tamboril-Santa Quiteria Complex, Ceara Central Domain: implication for neoproterozoic syncollisional magmatism in north Borborema Province, Brazil

    Energy Technology Data Exchange (ETDEWEB)

    Costa, Felipe Grandjean da; Araujo, Carlos Eduardo Ganade de; Vasconcelos, Antonio Maurilio, E-mail: felipe.costa@cprm.gov.br, E-mail: caegeo@gmail.com, E-mail: maurilio.vasconcelos@cprm.gov.br [Servico Geologico do Brasil (CPRM), Fortaleza, CE (Brazil); Amaral, Wagner da Silva, E-mail: wamaral@ufc.br [Universidade Federal do Ceara (UFC), Fortaleza, CE (Brazil). Departamento de Geologia; Rodrigues, Joseneusa Brilhante, E-mail: joseneusa.rodrigues@cprm.gov.br [Servico Geologico do Brasil (CPRM), Brasilia, DF (Brazil)

    2013-06-15

    The Tamboril-Santa Quiteria Complex (TSQC) is one of the largest Neoproterozoic plutonic manifestations in the north Borborema Province (NE Brazil). It represents an anatectic/igneous association characterized by a number of magmatic pulses that occurred in the 650-610 Ma interval. In this paper, we present U-Pb (LA-MC-ICP-MS) zircon ages and Nd isotopes for quartz monzonite and quartz diorites of the southern part of TSQC. The quartz monzonite belong to a hybrid granitoid association, including monzonite, syenites and quartz syenites, all with abundant mafic magmatic enclaves. A quartz monzonite sample yielded a U-Pb zircon age of 634 {+-} 10 Ma and a TDM age of 2.69 Ga. The quartz diorites are much more homogeneous in composition and yielded a U-Pb zircon age of 618 {+-} 23 Ma and a TDM age of 2.19 Ga. The presence of coeval mantle-derived magmatism and diatexites (crustal anatexis) post-dating high-pressure metamorphism (ca. 650 Ma), and together with high-temperature metamorphism (ca. 630-610 Ma), suggests that this large magmatic manifestation evolved in a collisional setting, probably related to slab break off during the Western Gondwana amalgamation. (author)

  18. Resultados del tratamiento con implantes dentales osteointegrados en la fase quirúrgica

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    Oviedo Pérez Pérez

    Full Text Available Objetivo: evaluar los resultados del tratamiento con implantes dentales osteointegrados en la fase quirúrgica. Métodos: se realizó un estudio longitudinal y prospectivo en 802 pacientes en quienes se colocaron 2 165 implantes, en la Clínica Estomatológica Provincial Docente de Santiago de Cuba y la Facultad de Estomatología de La Habana en el decenio 20002009. Se evaluaron las variables: técnica quirúrgica, longitud y diámetro de los implantes, complicaciones intraoperatorias y complicaciones postoperatorias, los resultados del tratamiento se evaluaron en supervivencia y fracaso. Resultados: se logró la supervivencia de los implantes en 705 pacientes para el 87,9 % y se produjo el fracaso en 97 pacientes para el 12,1 %. Se colocaron 2 165 implantes, se logró efectividad de 2 055 para el 94,9 % y fracasaron 110 que representan el 5,08 %. No existen diferencias significativas de los resultados de acuerdo a la técnica quirúrgica empleada. Los implantes que más fracasaron fueron los de 10 mm, para el 34,9 % y 8 mm con el 13,1 %. La efectividad se incrementa a medida que aumenta el diámetro. En las complicaciones intraoperatorias el fracaso fue mayor en relación con la perforación de la tabla ósea con el 92,9 %, inestabilidad con el 86 % y la dehiscencia ósea con el 57,4 %. En el postoperatorio fue notable que en el 100 % de los casos con dolor existió fracaso de los implantes. Conclusiones: en la etapa quirúrgica existe una fuerte asociación de los resultados con la longitud, diámetro de los implantes y la presencia de complicaciones intraoperatorias y postoperatorias.

  19. El xeroderma pigmentoso en su fase de proliferación cutánea tumoral

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    Ernesto Melardo Taño Espinosa

    2012-03-01

    Full Text Available El xeroderma pigmentoso es una enfermedad dermatológica rara, autosómica recesiva, y su etiología está relacionada con el déficit congénito de una endonucleasa que impide la reparación de ADN de las células de la piel que mutan por la incidencia de los rayos ultravioletas. La enfermedad transcurre por 3 etapas clínicas evolutivas y morfológicas. Si no están totalmente protegidos de la luz solar, los enfermos sufren un envejecimiento acelerado de la piel, y desarrollan inevitablemente lesiones oculares y dérmicas que pueden conducir a múltiples lesiones cancerosas. No existe actualmente ningún tratamiento curativo. El diagnóstico precoz y la protección frente a la radiación ultravioleta son los factores imprescindibles en el tratamiento de los pacientes afectados. Se describe la evolución clínica de una niña de 10 años con xeroderma pigmentoso, la cual presenta una fase muy avanzada de la enfermedad, con importante crecimiento de carcinomas cutáneos. El objetivo de la presente publicación es presentar un caso clínico poco frecuente de xeroderma pigmentoso, y al mismo tiempo, realizar una revisión bibliográfica con el fin de orientar el diagnóstico precoz y el tratamiento oportuno en este tipo de casos.

  20. Reação de fase aguda e sua relação com o desempenho de cavalos em competição de longa distância

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    L.A. Amaral

    2015-04-01

    Full Text Available O exercício físico é um dos estímulos fisiológicos mais estressantes que um animal pode sofrer e, dependendo de sua intensidade, sugere-se que possa gerar uma reação mediada por proteínas de fase aguda (PFA. O objetivo deste estudo foi caracterizar a reação de fase aguda e sua relação com o desempenho de cavalos submetidos a uma competição de longa distância. O experimento foi desenvolvido durante a Marcha de Resistência anual promovida pela Associação Brasileira de Criadores de Cavalos Crioulos (ABCCC, composta por um percurso de 750km percorrido durante 15 dias. Foram avaliados 23 equinos, os quais foram divididos em dois grupos, sendo o grupo 1 composto pelos 10 primeiros colocados na competição e o grupo 2 formado pelos 13 animais que concluíram a competição em colocações inferiores ou foram desclassificados antes de terminar a prova. Efetuaram-se coletas sanguíneas em repouso (dia 0 e no último dia de competição, e foi realizado o teste de eletroforese em gel de poliacrilamida contendo dodecil sulfato de sódio (SDS-PAGE para identificar as proteínas (albumina, haptoglobina, ceruloplasmina, transferrina, imunoglobulina G, imunoglobulina A, glicoproteína ácida e proteína de peso molecular de 23kDa. Os resultados demonstraram que o exercício físico imposto influenciou de forma significativa (P<0,0001 as concentrações séricas de haptoglobina, ceruloplasmina, imunoglobulina A, glicoproteína ácida e proteína de peso molecular de 23kDa. Quando comparados os resultados dos grupos estudados, observou-se que a concentração de haptoglobina após a competição foi superior no grupo de animais com baixo desempenho (grupo 2. Conclui-se que a competição de longa duração é capaz de gerar reação de fase aguda e que o monitoramento da concentração de haptoglobina pode ser um sinalizador de processo inflamatório e baixo desempenho.

  1. PROCESSO DE GERAÇÃO DE BIOGÁS A PARTIR DO REAPROVEITAMENTO DA GLICERINA – FASE PESADA E LIXO ORGÂNICO DOMICILIAR

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    Caroline Klinger

    2016-06-01

    Full Text Available Diante dos problemas ambientais enfrentados atualmente em relação ao destino de resíduos orgânicos e industriais, o presente projeto visa à produção de biogás a partir do reaproveitamento do lixo orgânico domiciliar e da glicerina fase pesada (subproduto originado a partir da produção de biodiesel. Até pouco tempo, o biogás era simplesmente conhecido como um subproduto obtido a partir da decomposição anaeróbia de lixo. No entanto, o acelerado desenvolvimento econômico dos últimos anos e a alta acentuada do preço dos combustíveis convencionais têm encorajado as investigações na produção de energia a partir de novas fontes renováveis e economicamente atrativas. Para tanto, utilizando-se um biodigestor anaeróbio, realizaram-se testes com diferentes quantidades de lixo orgânico e glicerina fase pesada com o intuito de avaliar a condição mais propícia para a produção de biogás. Além disso, tem-se por objetivo propor uma aplicação em escala maior que a até então executada em laboratório utilizando esterco oriundo da criação de suínos, uma vez que os resíduos de origem animal constituem elevada proporção da biomassa, e sua utilização em sistemas de reciclagem é de extrema importância sob aspectos econômicos e ambientais tornando-o uma excelente matéria prima na produção de biogás. Após a análise do biogás gerado, tanto a partir do lixo orgânico quanto do esterco de suínos, verificou-se que os processos utilizados foram satisfatórios.  

  2. Estudio definitivo de la derivación a Lima de las aguas de la cuenca alta del río Mantaro (Primera fase): informe final

    OpenAIRE

    Ministerio de Vivienda y Construcción; Proyecto Transvase Mantaro; Binnie & Partners

    1981-01-01

    Contiene la primera fase del estudio final de derivación de agua a Lima desde la cuenca superior del Río Mantaro, abarcando tópicos tales como los costos del control de la contaminación en el Río Mantaro y la medida en que podría utilizarse el agua subterránea en los valles de los Ríos Rímac, Chillón y Lurín. Este estudio tiene como objetivo principal la preparación de un Plan Integral que comprenda un plan de desarrollo que satisfaga la demanda de agua para uso urbano y agrícola en la Gra...

  3. Caracterización de una pantalla LCoS con polarimetría de Stokes promedio y aplicación a la simulación de elementos de fase

    OpenAIRE

    Martínez Guardiola, Francisco Javier; Márquez Ruiz, Andrés; Gallego Rico, Sergi; Ortuño Sánchez, Manuel; Francés Monllor, Jorge; Pascual Villalobos, Inmaculada; Beléndez Vázquez, Augusto

    2015-01-01

    Recientemente demostramos una técnica de caracterización, la polarimetría de Stokes promedio, que permite obtener tanto el retardo en función del voltaje como la amplitud del flicker que presentan muchas pantallas de cristal líquido sobre silicio de alineación paralela (PA-LCoS). En este trabajo mostramos que conociendo ambas magnitudes podemos simular y diseñar elementos ópticos de fase multinivel para ser enviados a la pantalla PALCoS, con una muy buena capacidad predictiva. Financiado p...

  4. Termografia infravermelha da superfície ocular como indicador de estresse em suínos na fase de creche

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    Lina Fernanda Pulido-Rodríguez

    Full Text Available RESUMO: Desmama é uma fase crítica na vida do suíno devido a separação materna e a introdução de uma dieta seca. A termografia infravermelha medida na região ocular se mostra como um indicador confiável para a condição de estresse pontual de suínos. O objetivo deste estudo foi determinar a relação entre medidas de termografia infravermelha da superfície ocular e de cortisol em situações de estresse em leitões na pós desmama. Foram avaliados 66 leitões, uma vez por semana, durante sete semanas, em dois períodos do dia (7h e 15h com medidas de temperatura superficial ocular, temperatura superficial do dorso e amostras de saliva para determinação de cortisol salivar. A análise estatística contemplou os efeitos fixos de semana e período do dia e sua interação e correlações de Pearson para relação entre termografia ocular, temperatura superficial e cortisol a 5% de significância. Cortisol salivar não diferiu entre os períodos, mas foi superior nas três primeiras semanas após o desmame (P<0,05. Nas duas primeiras semanas após a desmama o cortisol apresentou correlação alta e positiva (P<0,05 com a temperatura ocular máxima (0,89 e a temperatura superficial do dorso (0,80. As duas temperaturas superficiais apresentaram uma associação moderada positiva (r=0,41; P<0,0001 durante todo o período experimental. Este estudo destaca que a temperatura de superfície ocular obtida por meio da termografia infravermelha pode ser um indicador de temperatura de superfície corporal e estado de bem-estar de leitões em fase de creche, além de ser um método não invasivo e de rápida mensuração. Entretanto, mais pesquisas são necessárias para aprofundar a relação entre temperatura ocular e cortisol durante estresse crônico.

  5. IDENTIFICACIÓN DE UNA NUEVA FASE EN LA ESTRUCTURA CRISTALINA DEL COMPUESTO CUATERNARIO Cu2ZnSnSe4 DURANTE LA ETAPA INCORPORACIÓN DEL ZnSe

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    Anderon Dussán Cuenca

    Full Text Available En este trabajo se presenta un estudio de las propiedades estructurales de películas delgadas del compuesto Cu2ZnSnSe4 variando tanto la masa (M X como la temperatura del sustrato al cual fue evaporado (Ts el compuesto binario ZnSe. Todas las muestras fueron depositadas por el método de co-evaporación en tres etapas y manteniendo constante los demás parámetros. A partir de las medidas de difracción de Rayos x fue posible establecer con el incremento de la Ts la presencia de fases binarias asociadas al compuesto cuaternario durante el proceso de crecimiento del material. Se encontró que alrededor del pico principal, 2θ = 27,1°, predominan las fases binarias y la presencia del ZnSe que se forma durante la subsecuente etapa de selenización del material. Una especie de bifurcación en el pico principal (2θ = 27,1° fue observado para la transición entre M ZnSe = 0,153 g a 0,171 g. Medidas de difracción de rayos x fueron realizadas al compuesto binarios puro, observándose una correspondencia con los picos encontrados alrededor del pico principal del compuesto. Un estudio a través de espectroscopia Raman evidenció corrimientos raman asociados a los compuestos binarios observados por XRD. A partir de la ecuación de Scherrer se encontró que los tamaños de los cristalitos variaban entre 80 y 90 nm.

  6. Avaliação de provas de fase aguda em crianças e adolescentes com artrite idiopática juvenil e sua correlação com atividade da doença Acute phase reactants evaluation in children and adolescents with juvenile idiopathic arthritis and its correlation with disease activity

    Directory of Open Access Journals (Sweden)

    Aline Alencar M. F. Nicácio

    2009-06-01

    Full Text Available OBJETIVO:Analisar a relação entre as provas de fase aguda e a atividade clínica da artrite idiopática juvenil e avaliar a concordância entre velocidade de hemossedimentação e proteína C reativa (VHS e PCR na fase aguda da doença. MÉTODOS: Foi realizado estudo retrospectivo tipo coorte a partir da análise de prontuários de 30 crianças e adolescentes que preenchiam os critérios diagnósticos para artrite idiopática juvenil, estavam em atendimento em ambulatório de Reumatologia Pediátrica e haviam realizado as provas de fase aguda (VHS e PCR. RESULTADOS: Dos 30 pacientes, 21 (70% eram do sexo feminino e 19 (63,3% apresentavam o subtipo oligoarticular da doença. A média de idade de início dos sintomas foi 65,6 meses, a idade de diagnóstico de 85,3 e o tempo de evolução, 57,2 meses. As provas de fase aguda mostraram associação positiva com a atividade de doença. A anemia não teve relação com a atividade de doença. A concordância entre as duas provas de fase aguda foi superior a 80%. CONCLUSÕES: As provas de fase aguda mantêm relação positiva com a atividade da doença e o seu uso concomitante aumenta a especificidade.OBJECTIVE:To analyze the relationship between the acute phase reactants and the disease activity of Juvenile Idiopathic Arthritis (JIA and to evaluate the agreement between erythrocyte sedimentation rate and C-reactive protein during the acute phase of the disease. METHODS: a cohort retrospective study has been conducted based on the analysis of 30 children and adolescents who fulfilled the diagnostic criteria of JIA. All of them were in current follow-up at the pediatric rheumatology outpatient clinic and had acute phase reactants blood tests performed. RESULTS: Studied population comprised 30 patients: 21 (70% of them were females and 19 (63.3% presented oligoarticular subtype. The mean age at disease onset was 65.6 months; the age at diagnosis was 85.3 months and the follow-up had 57.2 months of

  7. Influência da levodopa sobre a fase oral da deglutição em pacientes com Doença de Parkinson Influence of levodopa on the oral phase of swallowing in patients with Parkinson's disease

    Directory of Open Access Journals (Sweden)

    Renata Mancopes

    2013-01-01

    Full Text Available Este estudo objetiva realizar levantamento bibliográfico para verificar a possível influência da Levodopa sobre a fase oral da deglutição de indivíduos com Doença de Parkinson. Foi realizado levantamento bibliográfico em periódicos indexados no Science Direct, periódicos Capes, LILACS, SciELO, MedLine e Scopus e livros. Para busca foram utilizados os termos disfagia, medicamentos, levodopa, Parkinson, dysphagia, drugs, swallowing disorders, Parkinson's disease, disfagia, las drogas e enfermedad de parkinson. Foram identificados 16 artigos internacionais e 25 nacionais, após a leitura de todos os artigos identificados foram selecionados 32, utilizaram-se ainda quatro livros e um resumo de anais de congresso. Para tal seleção utilizou-se como critério de inclusão aqueles artigos que considerassem o comprometimento causado pela Doença de Parkinson, especialmente na fase oral da deglutição, bem como os efeitos da levodopa sobre a mesma, e como critério de exclusão a influência do fármaco na fase faríngea, pois geralmente ele parece ter maior efeito na fase oral. Existe discordância na literatura quanto aos possíveis efeitos da Levodopa na deglutição. Quando estes ocorrem, geralmente afetam a fase oral desta função, uma vez que as dificuldades que o portador da Doença de Parkinson já apresenta são maximizadas pela xerostomia decorrente da administração deste fármaco. Em virtude da grande diversidade dos resultados dos estudos encontrados, faz-se necessária a realização de estudos controlados para uma elucidação mais detalhada dos efeitos da Levodopa na deglutição.The purpose of this study is to conduct a literature review in order to verify the possible influence of Levodopa on the oral phase of deglutition in individuals with Parkinson disease. The survey was conducted in journals indexed in Science Direct, Capes periodicals, LILACS, SciELO, MedLine and Scopus, as well as in books. For this survey, the terms

  8. Two-phase southward subduction of the Mongol-Okhotsk oceanic plate constrained by Permian-Jurassic granitoids in the Erguna and Xing'an massifs (NE China)

    Science.gov (United States)

    Liu, Huichuan; Li, Yinglei; He, Hongyun; Huangfu, Pengpeng; Liu, Yongzheng

    2018-04-01

    Geodynamics of the Mongol-Okhotsk oceanic plate southward subduction are still pending problems. This paper presents new zircon LA-ICP-MS U-Pb age and whole-rock geochemical data for the middle Permian to Middle Jurassic granitoids in the western Erguna and central Xing'an massifs. 267-264 Ma, 241 Ma and 173 Ma I-type granites, and 216 Ma A-type granites were identified in the Erguna and Xing'an massifs (NE China). The I-type granites were produced by partial melting of the lower mafic crust. The 216 Ma A-type granites were derived from partial melting of crustal materials with tonalitic to granodioritic compositions. The 267-264 Ma and 241 Ma I-type granites were generated in an Andean-type arc setting, wheras the 216 Ma A-type and 173 Ma granites were formed in supra subduction extensional setting. We summarized previous age data of the middle Permian to Middle Jurassic magmtaic rocks in the Erguna and Xing'an Massifs and identified two isolated phases of magmatic activity including the ca. 267-225 Ma and ca. 215-165 Ma periods, with a significant magmatic gap at ca. 225-215 Ma. These middle Permian to Middle Jurassic magmatic rocks are closely related to the southward subduction of the Mongol-Okhotsk ocean. A two-stage tectonic evolutionary model was proposed to account for these geological observations in the Erguna and Xing'an massifs, involving Permian to Middle Triassic continuous southward subduction of the Mongol-Okhotsk oceanic plate and Late Triassic to Jurassic slab-rollback and supra subduction extension.

  9. Fluencia a alta temperatura de policristales con tamaño de grano nanométrico de YTZP dopados con diferentes cantidades de fase vítrea

    Directory of Open Access Journals (Sweden)

    Lorenzo-Martín, C.

    2004-04-01

    Full Text Available Nano-sized YTZP (Yttria Tetragonal Zirconia Polycrystals samples with different amounts of a glassy phase have been crept in a range of temperature between 1150ºC-1200ºC. A macroscopic characterization of the mechanical behaviour as well as the microstructural analysis by Transmission electron Microscopy (TEM of both the as-received and deformed samples have been carried out. The glassy phase accounts for a significant softening while the deformation parameters values (n, Q are not altered with respect to those measured in non-doped specimens of the same material with the same average grain size.Grain boundary sliding has been proved to be the deformation mechanism.

    Muestras de YTZP (policristales de óxido de circonio dopados con itria con tamaños de grano nanométrico y diferentes cantidades de fase vítrea han sido sometidas a experiencias de fluencia en un rango de temperatura entre 1150ºC y 1200ºC, con objeto de estudiar el comportamiento mecánico de dichos materiales. Para conocer los mecanismos de deformación puestos en juego se ha realizado el estudio microestructural de las muestras deformadas y no deformadas mediante Microscopía Electrónica de Transmisión (MET. Se ha demostrado que la presencia de fase vítrea da lugar a un significativo descenso de la resistencia a la fluencia. No obstante, los parámetros característicos de la deformación (n y Q no se ven alterados, obteniéndose como mecanismo de deformación el deslizamiento de las fronteras de grano.

  10. Utilização da farinha pré-gelatinizada de milho na alimentação de leitões na fase de creche. Digestibilidade e desempenho

    Directory of Open Access Journals (Sweden)

    Moreira Ivan

    2001-01-01

    Full Text Available Foram realizados dois experimentos, um de digestibilidade (Experimento I e outro de desempenho (Experimento II. No experimento de digestibilidade, foram utilizados 16 leitões mestiços, machos castrados, desmamados aos 2l dias de idade e com 6,0kg de peso vivo inicial médio, alojados em gaiolas de metabolismo, contendo dois animais por unidade experimental. O alimento estudado foi a farinha pré-gelatinizada de milho (FPGM. Os coeficientes de digestibilidade CD da matéria seca, da proteína bruta e da energia bruta foram, respectivamente, de 89,2; 78,7 e 90,2%. Os teores de matéria seca digestível, proteína digestível, energia digestível e absorção de água foram, respectivamente, de 81,8%; 6,5%; 3682 kcal/kg e 500%. No experimento de desempenho, foram utilizados 96 leitões mestiços, sendo metade machos castrados e metade fêmeas, desmamados aos 21 dias de idade, em um delineamento em blocos casualizados, com quatro tratamentos, seis repetições e quatro leitões por unidade experimental, conduzido para verificar os efeitos de níveis crescentes de substituição (0; 33; 66; 100% do milho comum pela FPGM sobre o desempenho de leitões na fase de creche (21-63 dias de idade. Concluiu-se que a FPGM substituiu o milho comum até o nível de 23,7% em rações fareladas, compostas de milho, farelo de soja e núcleo comercial, para leitões na fase de 21 a 63 dias de idade.

  11. Syn-collisional felsic magmatism and continental crust growth: A case study from the North Qilian Orogenic Belt at the northern margin of the Tibetan Plateau

    Science.gov (United States)

    Chen, Shuo; Niu, Yaoling; Xue, Qiqi

    2018-05-01

    The abundant syn-collisional granitoids produced and preserved at the northern Tibetan Plateau margin provide a prime case for studying the felsic magmatism as well as continental crust growth in response to continental collision. Here we present the results from a systematic study of the syn-collisional granitoids and their mafic magmatic enclaves (MMEs) in the Laohushan (LHS) and Machangshan (MCS) plutons from the North Qilian Orogenic Belt (NQOB). Two types of MMEs from the LHS pluton exhibit identical crystallization age ( 430 Ma) and bulk-rock isotopic compositions to their host granitoids, indicating their genetic link. The phase equilibrium constraints and pressure estimates for amphiboles from the LHS pluton together with the whole rock data suggest that the two types of MMEs represent two evolution products of the same hydrous andesitic magmas. In combination with the data on NQOB syn-collisional granitoids elsewhere, we suggest that the syn-collisional granitoids in the NQOB are material evidence of melting of ocean crust and sediment. The remarkable compositional similarity between the LHS granitoids and the model bulk continental crust in terms of major elements, trace elements, and some key element ratios indicates that the syn-collisional magmatism in the NQOB contributes to net continental crust growth, and that the way of continental crust growth in the Phanerozoic through syn-collisional felsic magmatism (production and preservation) is a straightforward process without the need of petrologically and physically complex processes.

  12. Use of petrophysical data for siting of deep geological repository of radioactive waste

    Science.gov (United States)

    Petrenko, Liliana; Shestopalov, Vyacheslav

    2017-11-01

    The paper is devoted to analyzing the petrophysical properties and petrographical characteristics of Volyn region with the view to choosing the least permeable and so the most suitable geological formation for the radioactive waste disposal. On a basis of the petrophysical estimations of the granitoids properties the argumentation of permeability has been developed for the petrotypes of Volyn region. Also method of classification of the petrotypes with their relative rate of suitability for radioactive waste disposal was developed. As a result of studying the perspectives were shown of the zhytomyr and korosten types of the granitoids as host rock for the radioactive waste disposal. According to the results of investigations performed by Swedish researchers a comparative analysis of rocks based on the age of formation, composition, structural features and some petrophysical properties of granitoids as host rocks for repository of radioactive waste was performed. Detail comparison the data of the granitoids of the Forsmark site in Sweden and the data of the granitoids of the Volyn megablock can be one of the next steps in researching the host rocks for the development of the RW disposal system in Ukraine.

  13. Use of petrophysical data for siting of deep geological repository of radioactive waste

    Directory of Open Access Journals (Sweden)

    Petrenko Liliana

    2017-01-01

    Full Text Available The paper is devoted to analyzing the petrophysical properties and petrographical characteristics of Volyn region with the view to choosing the least permeable and so the most suitable geological formation for the radioactive waste disposal. On a basis of the petrophysical estimations of the granitoids properties the argumentation of permeability has been developed for the petrotypes of Volyn region. Also method of classification of the petrotypes with their relative rate of suitability for radioactive waste disposal was developed. As a result of studying the perspectives were shown of the zhytomyr and korosten types of the granitoids as host rock for the radioactive waste disposal. According to the results of investigations performed by Swedish researchers a comparative analysis of rocks based on the age of formation, composition, structural features and some petrophysical properties of granitoids as host rocks for repository of radioactive waste was performed. Detail comparison the data of the granitoids of the Forsmark site in Sweden and the data of the granitoids of the Volyn megablock can be one of the next steps in researching the host rocks for the development of the RW disposal system in Ukraine.

  14. K-Ar age and tectonic setting of brannerite-mineralized Futagojima granodiorite, Koshiki Islands, Southern Kyushu

    International Nuclear Information System (INIS)

    Ishihara, Shunso; Shibata, Ken; Terashima, Shigeru

    1984-01-01

    Futagojima granodiorite, which was previously thought to be a part of Cretaceous Ryoke granitoids, is turned out to be upper Miocene granitoids (7.5 Ma). The granodiorite contains magnetite and is depleted in lithophile components. This is characteristics of magnetite-series granitoids in the Green Tuff terrains. All the Miocene granitoids in Koshiki Islands are relatively mafic consisting of hornblende-bearing facies such as quartz diorite, tonalite and granodiorite; thus belonging to I-type magnetite series. These rocks are considered to have generated at depth and formed along a rift zone during Miocene time (13 - 7 Ma). Thus, Koshiki Islands may represent an aborted rift at margin of the Danjo basin. Miocene granitoids of Koshiki Islands are small stocks but magmatic-hydrothermal ore deposits are only seen in Futagojima. This localization of mineralization is explained by a high degree of magmatic fractionation, which is only observed in Futagojima and by a low rate of erosion to preserve the mineralized horizons. Mineralization here is unique having brannerite-magnetite and chalcopyrite-molybdenite-quartz assemblages. No gold and silver were detected from the vein-type deposit. (author)

  15. The Archaean Granny Smith gold deposit, western Australia: age and Pb-isotope tracer studies

    International Nuclear Information System (INIS)

    Ojala, V.J.; McNaughton, N.J.; Groves, D.I.; Ridley, J.R.; Fanning, C.M.

    1997-01-01

    The Granny Smith gold deposits are situated within a greenstone sequence in the Laverton-Leonora area of the Northeastern Goldfields Province of the Archaean Yilgarn Block, Western Australia. The greenstone sequence (U-Pb zircon age of 2677±6 Ma, felsic pyroclastic rock) was intruded by the Granny Smith Granodiorite at 2665±4 Ma. Gold mineralisation is located along a reactivated N-S Stricking, thrust which wraps around the granitoid intrusion, and within the granitoid intrusion. Initial lead-isotope compositions of the Granny Smith Granodiorite and ore-fluid Pb, estimated from K-feldspar and galena and lead tellurides, respectively, are slightly different. Calculations based on Pb isotope data for the host rocks, and the U-Pb zircon age of the Granny Smith Granodiorite, suggest that ore-fluid Pb was derived from a source with a similar initial lead-isotopic composition to the source of the Granny Smith Granodiorite but about 30 million years after the intrusion of the granitoid. The Pb-isotope data for granitoids of the Northeastern Goldfields fall in a distinct field different to that of the granitoids of the Norseman area and those from Kambalda to Menzies. (authors)

  16. Proteinograma sérico, com ênfase em proteínas de fase aguda, de bovinos sadios e bovinos portadores de enfermidade aguda de ocorrência natural

    OpenAIRE

    Simplício,K.M.M.G.; Sousa,F.C.; Fagliari,J.J.; Silva,P.C.

    2013-01-01

    Nas últimas décadas, as proteínas de fase aguda (PFAs) tornaram-se biomarcadores de escolha em medicina humana para identificação e monitoração de doenças. Não há razão para imaginar que tais pesquisas clínicas não sejam igualmente úteis na medicina veterinária. Com o objetivo de verificar a importância das PFAs como biomarcadores de doenças inflamatórias em bovinos, determinou-se o proteinograma sérico, por meio da técnica de eletroforese SDS-PAGE, com interesse especial nas PFAs. Foram util...

  17. Estudo imunobiológico de estoques de Trypanosoma cruzi isolados de pacientes na fase aguda da doença de Chagas

    Directory of Open Access Journals (Sweden)

    T.L. Kipnis

    1983-12-01

    Full Text Available Estoques de tripanossomas isolados de pacientes na fase aguda da doença de Chagas foram injetados em grupos de camundongos albinos não isogênicos nas doses de 10³, 10(4 e 10(5 parasitas/camundongos. O curso da infecção foi seguido por três meses. A pctrasitemia foi em geral baixa, com picos recorrentes, na maioria das vezes os animais evoluiam para cronicidade. Somente um estoque induziu alto índice de mortalidade. Os parasitas e as lesões apesar de detectadas no pico da parasitemia e restritos ao coração estavam ausentes aos três meses. Nesta época os perfis de Igs apresentaram diferenças marcantes. Grupos de animais que foram inoculados com estes estoques foram desafiados com doses letais da cepa Y ou CL. Em alguns casos obteve-se uma parasitemia, mas patente.

  18. Uji Klinik Fase II Ramuan Jamu sebagai Pelindung Fungsi Hati

    Directory of Open Access Journals (Sweden)

    zuraida - zulkarnain

    2017-07-01

    Full Text Available AbstractThe human liver is susceptible to interference due to its complex function. The development ofhepatoprotective from jamu formula is still needed as to produce more effective, cheaper andsafer hepatoprotective. The result of previous study showed that the hepatoprotective from jamuformula was safe and efficacious. This phase 2 trial was conducted to evaluate the efficacy andsafety of hepatoprotective from jamu formula which consists of Curcuma longa rhizomes, Curcumaxanthorrhiza rhizomes, and Taraxacum officinale leaves. The design was open label randomizedclinical trial with silimarin as a comparison for 42 days intervention. Two hundreds of humansubjects participated in this study. The trial held in 2015 and involved 50 physician members ofSaintifikasi Jamu Network at several regencies in Indonesia. The parameters for assessing efficacywere SGPT, SGOT and as for safety were routine blood, urea, and creatinine. Clinical symptoms andpossible side effects were also observed. The results showed that the jamu formula can reduce theaverage value of SGPT and SGOT equal to silimarin. Jamu formula can relieve clinical symptomsarising from liver function disruption, and it is safe, it does not alter kidney function, hemoglobin,leukocyte count and platelet count in its use for 42 days.Keywords: hepatoprotective, Saintifikasi Jamu, Curcuma longa, Curcuma AbstrakHati mudah mengalami gangguan disebabkan fungsinya yang kompleks. Saat ini masih diperlukanpengembangan ramuan jamu untuk melindungi dan memperbaiki sel-sel hati (hepatoprotektor yanglebih efektif, murah dan aman. Hasil penelitian observasi klinik terdahulu menunjukkan bahwaformula jamu untuk hepatoprotektor aman dan berkhasiat sehingga dilanjutkan dengan uji klinik fase2. Tujuan uji ini untuk menilai khasiat dan keamanan ramuan jamu sebagai hepatoprotektor dengankomposisi rimpang temulawak, rimpang kunyit, dan daun jombang. Rancangan uji adalah open labelrandomised clinical trial dengan

  19. Respuestas del clima de América del Sur a las fases de ENSO

    Directory of Open Access Journals (Sweden)

    1998-01-01

    impulsions de El Niño. Les régions du centre du Brésil semblent aussi ne pas dépendre du phénomène. Durant les années classées comme normales, on n’observe pas de dépendance des contrôles climatiques qui agissent au cours des phases extrêmes de l’Oscillation du Sud. Ceci montre que l’on doit approfondir l’étude des autres causes de variation de la circulation tropicale responsables des anomalies de précipitation. Las fases altas de ENSO, El Niño (EN, y las fases bajas, Anti-Niño (AN, se relacionan diferentemente con los regímenes de lluvias en América del Sur. Para establecer el carácter de estas relaciones, se ha analizado la precipitación anual de estaciones típicas, considerando tres subpoblaciones: totales anuales de años EN, totales de años AN, y el resto o años “normales”. Precediendo a veranos australes con fenómenos EN, la precipitación invernal en Chile Central y los Andes de Argentina es abundante. Durante los veranos con episodios EN en el Pacífico tropical, suelen afectar sequías el Noreste de Brasil especialmente en el otoño o verano precedente. De diciembre a marzo de años EN, llueve copiosamente a lo largo de la costa oeste de América del Sur comprendida entre la Bahía de Tumaco y Pacasmayo. En el interior de la Sierra y el Altiplano peruano boliviano tienen lugar sequías. En las tierras bajas de Bolivia, Paraguay, y el sureste de Brasil hay fuertes lluvias anormales durante el verano y otoño austral. En medio del otoño hay precipitaciones intensas en las tierras bajas del Río de la Plata y el sur de Brasil. El segmento norte y la cuenca inferior del Amazonas tienen menos pluviosidad durante EN y niveles mayores durante AN. La cuenca interior del Amazonas reacciona inversamente, ya que tiene pluviosidad excesiva durante algunos EN. Las regiones de Venezuela y Colombia bajo la influencia del Caribe y el Atlántico experimentan anomalías negativas de lluvias durante EN y alta pluviosidad en AN. Algunas regiones de la

  20. Migration of fluids as a tool to evaluate the feasibility of the implantation of geological radioactive wastes repositories (RARN) in granitoid rocks: tests on granites submitted to natural deformation vs. not deformed; A migração de fluidos como ferramenta de avaliação da viabilidade da implantação de repositórios de rejeitos radioativos geológicos (RARN) em rochas granitoides: testes em granitos submetidos a deformação natural vs. não deformados

    Energy Technology Data Exchange (ETDEWEB)

    Lopes, Nilo Henrique Balzani; Barbosa, Pedro Henrique Silva; Santos, Alanna Leite dos; Amorim, Lucas Eustáquio Dias; Freitas, Mônica Elizetti de; Rios, Francisco Javier, E-mail: javier@cdtn.br [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN/CNEN-MG), Belo Horizonte, MG (Brazil). Lab. de Caracterização Mineralógica e Metalogênese

    2017-07-01

    Fluid composition and migration studies in granitoid rocks subjected to deformation events are a factor that should be considered in the selection of geologically favorable areas for RANR construction, and may be an excellent complement to engineering barrier designs. The research objective was to develop an academic approach, comparing the behavior of deformed and non-deformed granites, not being related to any CNEN project of deploying repositories. It is concluded that in the choice of suitable sites for the construction of repositories, granite bodies that are submitted to metamorphic / deformation / hydrothermal events or that are very fractured should be disregarded. The domes of granite batholith that have undergone hydraulic billing should also be discarded. It has been found that, because of the warming caused by radioactive decay reactions, there is a real possibility that the release of potentially abrasive fluids contained in the minerals can reach and corrode the walls of the repositories and / or packaging.

  1. Prueba del software: más que una fase en el ciclo de vida/Software testing: more than a stage in the life cycle

    Directory of Open Access Journals (Sweden)

    Edgar Serna

    2011-12-01

    Full Text Available La prueba de software es probablemente la parte menos comprendida del ciclo de vida del desarrollo de software. En este trabajo, mediante una propuesta metodológica de cuatro fases, se muestra por qué es difícil detectar y eliminar errores, por qué es complejo el proceso de realizar pruebas y por qué es necesario prestarle más atención.Software testing probably is the least understood part of the software testing life cycle. In this work, by means of a methodological proposal of four stages, is showed why is complex the process of carrying out the testing software, why is necessary to pay it more attention and why is so difficult to detect and delete the mistakes.

  2. DESARROLLO Y OPTIMIZACIÓN DE UNA METODOLOGÍA MULTIRESIDUO POR MÉTODO SIMPLEX PARA EL ANÁLISIS DE PLAGUICIDAS EN MIEL DE ABEJAS

    Directory of Open Access Journals (Sweden)

    Danny Rodriguez

    2014-07-01

    Full Text Available La aplicación de plaguicidas en cultivos cercanos a las zonas de producción apícola puede afectarla supervivencia de las abejas y la calidad de los productos derivados de la colmena, por lo cual es de gran importancia realizar estudios de residualidad de estos agroquímicos en mieles yen otros productos apícolas. Para esto es indispensable desarrollar metodologías que permitan el análisis de estos contaminantes en productos apícolas. Este trabajo muestra los resultados en el desarrollo y optimización de una metodología multiresiduo para el análisis de 30 plaguicidas, incluyendo plaguicidas organoclorados, organofosforados y piretroides en miel de abejas. El método consistió en una extracción líquido-líquido, seguida de un paso de limpieza en fase solida usando una columna cargada con silica gel/florisil. El análisis de los plaguicidas fue realizado por cromatografía de gases con detectores de nitrógeno fósforo (NPD y microcaptura electrónica (µ-ECD.La optimización de las variables experimentales presentes en los pasos de pre-tratamiento, extracción y limpieza se realizó mediante el empleo del método simplex modificado. Con este fin, se escogieron 14 variables las cuales se optimizaron en 21 experimentos. Los resultados mostraron que los porcentajes de recuperación obtenidos para la mayoría de los plaguicidas se encuentran entre el 78.8% y el 114.5%, con coeficientes de variación inferiores al 20%.

  3. Níveis de fósforo disponível e cálcio em rações suplementadas com fitase para frangos de corte nas fases de crescimento e final Calcium and available phosphorus levels in diets supplemented with phytase for broilers in the growing and finishing phases

    Directory of Open Access Journals (Sweden)

    Luziane Moreira dos Santos

    2011-11-01

    Full Text Available Avaliaram-se os níveis de cálcio e fósforo disponível (Pdisp em rações com fitase para frangos de corte da linhagem Cobb nas fases de crescimento (22 a 35 dias e final (36 a 42 dias. Utilizou-se um esquema fatorial 3 × 4 + 1, composto de três níveis de Pdisp (0,36; 0,31; 0,26% na fase de crescimento e 0,33; 0,28; 0,23% na final, quatro níveis de cálcio (0,82; 0,72; 0,62; 0,52% para a fase de crescimento e 0,76; 0,66; 0,56; 0,46% para a final e um nível de suplementação da fitase (500 ftu/kg. As rações controle não foram suplementadas com fitase e continham, respectivamente, os seguintes níveis de Pdisp e cálcio: 0,41 e 0,82% (fase de crescimento e 0,38 e 0,76% (final. Nos ensaios de desempenho, aos 35 e 42 dias de idade, avaliaram-se o consumo de ração, o ganho de peso, a conversão alimentar e o teor de cinzas na tíbia. Nos ensaios de metabolismo, foram determinados os valores energéticos das rações (EMAn e os coeficientes de metabolizabilidade da matéria seca (CMMS. Na fase de crescimento, a redução do cálcio e Pdisp para 0,52 e 0,26%, respectivamente, não comprometeu o desempenho, a mineralização óssea, a EMAn e o CMMS. Na fase final, a redução do cálcio e fósforo disponível para 0,56 e 0,28%, respectivamente, não comprometeu o desempenho, a EMAn e o CMMS e melhorou a mineralização óssea. Os níveis de cálcio e fósforo disponível em rações para frangos de corte podem ser reduzidos para 0,52 e 0,26% na fase de crescimento e 0,56 e 0,28% na fase final desde que essa redução seja combinada com a suplementação de fitase no nível de 500 ftu/kg de ração.Calcium and available phosphorus (aP levels in diets with phytase for Cobb broilers in the growing (22 to 35 days and finishing phases (36 to 42 days of age were evaluated. A 3 × 4 + 1 factorial scheme, with three aP levels (0.36, 0.31, 0.26% in the growing phase and 0.33, 0.28, 0.23% in the finishing phase, four calcium levels (0.82, 0.72, 0

  4. EVALUACIÓN DE TRES NIVELES DE NITRÓGENO EN MEDIO DE CULTIVO, EN LAS FASES DE ENRAIZAMIENTO in vitro Y ADAPTACIÓN A SUSTRATO DE Rubus glaucus (BENTH)

    OpenAIRE

    Vaca, Ivonne; Landazuri, Pablo

    2013-01-01

    El presente trabajo fue desarrollado en el Cantón Rumiñahui, provincia de Pichincha, Ecuador. El objetivo fue evaluar tres concentraciones nitrógeno de las sales Murashige y Skooog (MS) en el medio de cultivo, en las fases de enraizamiento in vitro y adaptación a sustrato de Rubus glaucus. La dosis de 4,88mMde nitrógeno en elmedio presentó el mayor número de raíces con un promedio de 3,72 raíces por planta, mayor longitud de raíz con 1,8cm de largo, mayor porcentaje de enraizamiento ...

  5. Geochemical evidence for Paleozoic crustal growth and tectonic conversion in the Northern Beishan Orogenic Belt, southern Central Asian Orogenic Belt

    Science.gov (United States)

    Yuan, Yu; Zong, Keqing; He, Zhenyu; Klemd, Reiner; Jiang, Hongying; Zhang, Wen; Liu, Yongsheng; Hu, Zhaochu; Zhang, Zeming

    2018-03-01

    The Beishan Orogenic Belt is located in the central southernmost part of the Central Asian Orogenic Belt (CAOB), which plays a key role in understanding the formation and evolution of the CAOB. Granitoids are the documents of crustal and tectonic evolution in orogenic belts. However, little is known regarding the petrogenesis and geodynamic setting of the widely distributed Paleozoic granitoids in the Northern Beishan Orogenic Belt (NBOB). The present study reveals significant differences concerning the petrogenesis and tectonic setting of early and late Paleozoic granitoids from the NBOB. The early Paleozoic granitoids from the 446-430 Ma Hongliuxia granite complex of the Mazongshan unit and the 466-428 Ma Shibanjing complex of the Hanshan unit show classic I-type granite affinities as revealed by the relative enrichment of LILEs and LREEs, pronounced depletions of Nb, Ta and Ti and the abundant presence of hornblende. Furthermore, they are characterized by strongly variable zircon εHf(t) values between - 16.7 and + 12.8 and evolved plagioclase Sr isotopic compositions of 0.7145-0.7253, indicating the involvement of both juvenile and ancient continental crust in the magma source. Thus, we propose that the early Paleozoic granitoids in the NBOB were generated in a subduction-related continental arc setting. In contrast, the late Paleozoic 330-281 Ma granitoids from the Shuangjingzi complex of the Hanshan unit exhibit positive zircon εHf(t) values between + 5.8 and + 13.2 and relatively depleted plagioclase Sr isotopic compositions of 0.7037-0.7072, indicating that they were mainly formed by remelting of juvenile crust. Thus, an intra-plate extensional setting is proposed to have occurred during formation of the late Paleozoic granitoids. Therefore, between the early and late Paleozoic, the magma sources of the NBOB granitoids converted from the reworking of both juvenile and ancient crusts during a subduction-induced compressional setting to the remelting of

  6. Aspectos éticos de la fase terminal Ethical aspects of terminal phase care

    Directory of Open Access Journals (Sweden)

    Oscar Velásquez

    1993-02-01

    Full Text Available

    Partiendo de una definición de la ética en general, de la ética médica y de la bioética, el autor discute estos conceptos en cuanto se relacionan con la atención del paciente en fase terminal, así como los temas de la muerte, el sufrimiento y los sentimientos que despierta el saberse moribundo. Hace énfasis en las relaciones médico-paciente y médico-familla y en los valores éticos de la igualdad y la reciprocidad. Plantea cómo a menudo el médico carece de una actitud correcta frente al paciente terminal y propone guías para el trabajo médico en tales circunstancias. Destaca la necesidad de respetar en todo momento la autonomía y la dignidad del enfermo y de saber usar con sabiduría los recursos tecnológicos disponibles.

     

    The author starts with definitions of ethics, medical ethics and bioethics and discusses their relationship with terminal patient care; also discussed are the subjects of death, suffering and the feelings that appear with the selfawareness of being near-death. Emphasis Is given on both patient-physician and family-physician relationships and on the values of equality and reciprocity. Guidelines are proposed for the approach and medical care of terminal patients and their families; they deal mainly with the need to respect autonomy and dignity and with the wise use of technological advances presently available.

     

  7. Ser Irmão de uma Pessoa Surda: Relatos da Infância à Fase Adulta

    Directory of Open Access Journals (Sweden)

    Juliana Archiza YAMASHIRO

    Full Text Available RESUMO: o objetivo do presente estudo foi analisar a experiência de irmãos de pessoas surdas acerca de sua história de vida e das implicações da deficiência nos relacionamentos fraternos. Tratou-se de um estudo exploratório, de abordagem qualitativa, que contou com a participação de cinco irmãos de pessoas surdas com idade entre 31 a 44 anos. Para a coleta de dados foram utilizados os seguintes instrumentos: questionário de identificação e roteiro de entrevista em profundidade. Os dados obtidos foram analisados a partir do modelo de produções de sentido das práticas discursivas. Os principais resultados apontaram que a dificuldade de comunicação entre os participantes e seus irmãos surdos repercutiu em questões nos relacionamentos desde a infância até a fase adulta. Considera-se que as questões inerentes à deficiência trouxeram consequências a todos os membros da família, em especial nos quesitos relacionamentos e comunicação e que disponibilizar atenção especializada aos pais e irmãos destas pessoas auxiliaria no manejo das situações vinculadas à deficiência e fortalecimento dos vínculos familiares.

  8. Barren Miocene granitoids in the Central Andean metallogenic belt, Chile: Geochemistry and Nd-Hf and U-Pb isotope systematics

    International Nuclear Information System (INIS)

    Deckart, Katja; Godoy, Estanislao; Bertens, Alfredo; Jerez, Daniela; Saeed, Ayesha

    2010-01-01

    Four Middle-to-Late Miocene barren plutonic complexes that occur between the giant porphyry copper deposits of the central Chilean Andes were selected for U-Pb LA-ICPMS geochronology and Hf-isotope systematics on single zircon grains. Major and trace elements and Sr-Nd-Hf isotope whole rock geochemical studies were undertaken to compare with slightly younger or coeval barren and fertile intrusive rocks between 32 o and 34 o S. The studied granitoids yield resolvable crystallization ages of 11.3±0.1 Ma (Cerro Meson Alto massif), 10.3±0.2 Ma (La Gloria pluton), 14.9±0.2 Ma/14.9±0.1 Ma (Yerba Loca stock) and 11.2±0.1 Ma/14.7±0.1 Ma (San Francisco Batholith). Major and trace elements discard an adakitic signature as suggested for coeval porphyric intrusions at 32 o S, slightly younger mineralized porphyries at Rio Blanco-Los Bronces deposit and other Cenozoic adakites. Volcanic host rocks are less fractionated than the intrusive rock units. The same observation can be made for the unmineralized northern plutons compared to the southern ones. Initial Sr-Nd isotope data show insignificant variation (0.703761-0.704118 and 0.512758- 0.512882), plotting in the mantle array. Trace element enrichment can be explained by addition of subducted-slab fluids and/or terrigenous sediments to the mantle wedge prior to and/or slight crustal input during magma ascent. Zircon grains separated from these barren intrusives share a similar initial εHf-data variation for the younger age group (10-12 Ma; 7.04-9.54) and show a more scattered range for the older one (14-15 Ma; 8.50-15.34); both sets plot between the DM and CHUR evolution lines. There is evidence that magma evolution was slightly distinct through time from older to younger barren magmatism, compared to a few fertile porphyritic rocks from Rio Blanco-Los Bronces porphyry copper deposit. It is suggested that chronological inconsistencies within these complexes might be related to differential shortening across the NE

  9. SHRIMP U-Pb zircon dating of Archean core complex formatio and pancratonic strike-slip deformation in the East Pilbara Granite-Greenstone Terrain

    NARCIS (Netherlands)

    Zegers, T.E.; Nelson, D.R.; Wijbrans, J.R.; White, S.H.

    2001-01-01

    Sensitive high-resolution ion microprobe (SHRIMP) U-Pb dating of zircons from granitic rocks in the East Pilbara Granite-Greenstone Terrain has provided time constraints for main tectonic events in the Shaw Granitoid Complex and has shown that deformation was intricately related to granitoid

  10. Estrutura da comunidade das larvas de Chironomidae (Insecta: Diptera, em diferentes substratos artificiais e fases hídricas, no trecho superior do rio Paraná, Estado do Paraná, Brasil = Community structure of Chironomidae larvae (Insecta: Diptera, in different artificial substrates and during distinct hydrological phases, in the upper stretch of the Paraná river, Paraná State, Brazil

    Directory of Open Access Journals (Sweden)

    Adriana Felix dos Anjos

    2010-04-01

    Full Text Available Este estudo teve como objetivo verificar a influência das fases hídricas sobre a composição, a densidade e a dominância das larvas de Chironomidae em diferentes tipos de substratos artificiais. As coletas foram realizadas quinzenalmente, entre os meses de agosto de2004 e dezembro de 2005. A análise de agrupamento revelou diferenças na composição e densidade das morfoespécies entre as fases hídricas e, de acordo com o índice de dominância de Kownacki, Cricotopus sp. foi dominante ou subdominante em todos os substratos e fases hídricas.Na fase de águas baixas, a maior similaridade foi observada entre os substratos de mesma forma. Nesse período, os maiores valores de riqueza e densidade das larvas foram registrados nos substratos em forma de X. Na fase de águas altas, o aumento no nível do rio Paraná influenciou na redução da densidade média das larvas e somente nos substratos de madeira em forma de X e PVC em forma de tubo, cujos materiais favoreceram a melhor fixação das larvas, foramregistrados maiores valores de densidade.This study investigated the influence of hydrological phases on species composition, density and dominance of Chironomidae larvae indifferent types of artificial substrates. Samplings were undertaken fortnightly, between August 2004 and December 2005. Cluster analysis evidenced differences in the species composition and density of Chironomidae morphospecies among hydrological phases; according to the Kownacki dominance index, Cricotopus sp. was dominant or subdominant in all substrates and hydrological phases. During the low water phase, the greatest similarity was observed among the substrateswith the same shape. In this period, the highest values of species richness and density of larvae were registered in X-shaped substrates. During the high water phase, the rise in the level of the Paraná River influenced on the reduction of mean larvae density, and only in wooden X-shaped and tube-shaped PVC

  11. El final del Mesolítico y los inicios del neolítico en la Península Ibérica : cronología y fases

    Directory of Open Access Journals (Sweden)

    Alday Ruiz, Alfonso

    2009-01-01

    Full Text Available El análisis racional de la serie radiocronológica C14 correspondiente al Neolítico y su inmediato Mesolítico geométrico permite establecer una secuencia cronocultural bien definida. Desde esta base se defiende unos inicios prematuros del Neolítico peninsular, en el segundo cuarto del VI milenio cal BC plenamente coincidente con el final del Mesolítico. Desde ese punto y hasta el fin del milenio delimitamos tres fases para el Neolítico antiguo: la de arranque con posibilidad de "movimientos pioneros", la intermedia de formación de los dominios cerámicos, y la final de diversificación.

  12. Características de carcaça de bovinos zebu e cruzados holandês-zebu (F1) nas fases de recria e terminação

    OpenAIRE

    Alves,Dorismar David; Paulino,Mário Fonseca; Backes,Alfredo Acosta; Valadares Filho,Sebastião de Campos; Rennó,Luciana Navajas

    2004-01-01

    Foram avaliadas as características de carcaça de bovinos Indubrasil e cruzados F1 Holandês-Gir e F1 Holandês-Guzerá, nas fases de recria e terminação. Foram determinados os rendimentos de carcaça e porcentagens dos cortes básicos, comprimento de carcaça, espessura de gordura subcutânea, área de olho de lombo, proporções de músculo, gordura e ossos. Os grupos genéticos não influenciaram os rendimentos de carcaça quente, em relação ao peso vivo e ao peso corporal vazio, e dos cortes básicos, di...

  13. Fluid geochemistry associated associated to rocks: preliminary tests om minerals of granite rocks potentially hostess of radioactive waste repository; Geoquimica de fluidos associados a rochas: testes preliminares em minerais de rochas granitoides potencialmente hospedeiras de repositorios de rejeitos radioativos

    Energy Technology Data Exchange (ETDEWEB)

    Amorim, Lucas E.D.; Rios, Francisco J.; Oliveira, Lucilia A.R. de; Alves, James V.; Fuzikawa, Kazuo; Garcia, Luiz; Ribeiro, Yuri, E-mail: LDAmorim@cdtn.b [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN/CNEN-MG), Belo Horizonte, MG (Brazil); Matos, Evandro C. de [Industrias Nucleares do Brasil S.A. (INB), Caetite, BA (Brazil)

    2009-07-01

    Fluid inclusions (FI) are micro cavities present on crystals and imprison the mineralizer fluids, and are formed during or posterior to the mineral formation. Those kind of studies are very important for orientation of the engineer barrier projects for this purpose, in order to avoid that the solutions present in the mineral FI can affect the repository walls. This work proposes the development of FI micro compositional studies in the the hostess minerals viewing the contribution for a better understanding of the solution composition present in the metamorphosis granitoid rocks. So, micro thermometric, microchemical and characterization of the material confined in the FI, and the hostess minerals. Great part of the found FI are present in the quartz and plagioclase crystals. The obtained data on the mineral compositions and their inclusions will allow to formulate hypothesis on the process which could occurs at the repository walls, decurrens from of the corrosive character (or not) of the fluids present in the FI, and propose measurements to avoid them

  14. Ação do prebiótico sobre as proteínas de fase aguda de pacientes com neoplasia hematológica Action of prebiotics on proteins in the acute phase of hematologic neoplasia

    Directory of Open Access Journals (Sweden)

    Telma Búrigo

    2007-06-01

    Full Text Available Os pacientes com neoplasias hematológicas são submetidos a tratamento quimioterápico que induz uma intensa alteração na integridade da mucosa intestinal, favorecendo um aumento da sua morbi-mortalidade. O presente trabalho foi desenvolvido na Unidade de Transplante de Medula Óssea do Centro de Pesquisas Oncológicas em Florianópolis - SC e teve como objetivo estudar a ação do prebiótico na resposta de proteína da fase aguda de pacientes com neoplasias hematológicas submetidos à quimioterapia. Foi realizado um estudo clínico randomizado duplo cego envolvendo 25 pacientes divididos em dois grupos que receberam por 15 dias: 12g de FOS (n=14 ou placebo (maltodextrina (n=11. Todas as variáveis foram determinadas antes e após a suplementação. Foram avaliados os níveis séricos das proteínas de fase aguda negativas (albumina e pré-albumina e a proteína de fase aguda positiva, proteína C reativa (PCR. Verificaram-se a presença de diarréia e de constipação, bem como a quantidade de bifidobactérias e valores de pH fecal. A redução dos níveis séricos de proteínas de fase aguda negativas (albumina e pré-albumina comprovam o intenso catabolismo protéico, priorizando a síntese de proteína de fase aguda positiva (PCR. O grupo suplementado apresentou um aumento significante na quantidade de bifidobactérias e o pH fecal não foi alterado em ambos os grupos. Os níveis séricos de PCR foram estatisticamente superiores no grupo controle, indicando a ocorrência de processos inflamatórios e maior demanda metabólica, sugerindo que a quantidade de bifidobactérias pode ter favorecido a redução deste quadro no grupo suplementado, confirmado pela correlação negativa entre estas variáveis.Patients with hematologic neoplasias are submitted to chemotherapeutic treatment that induces intense alterations in the integrity of the intestinal mucous membrane, favoring an increase in the morbimortality rate. The current work was

  15. Turnover de carbono nos tecidos de frangos de corte em diferentes fases de crescimento

    Directory of Open Access Journals (Sweden)

    Carlos Ducatti

    2014-01-01

    Full Text Available Este trabalho objetivou determinar o turnover do carbono no Pectoralis major, quilha, tíbia e fígado de frangos de corte em seus diferentes períodos de crescimento, utilizando a técnica dos isótopos estáveis. Foram utilizados 216 pintos de corte, machos, Cobb. O delineamento experimental foi inteiramente casualizado e consistiu de sete tratamentos com dias de substituição das dietas distintos: 0; 7; 14; 21; 28; 35; 42 dias de idade. Para mensurar o turnover do carbono nos tecidos em determinado intervalo de tempo, foi utilizado o modelo sigmoidal de regressão de Boltzmann ou função exponencial do tempo. Os valores de meias-vidas foram: 2,5; 2,8; 2,9; 4,9; 5,1; 5,5 e 6,0 dias para músculo peitoral; 2,7; 2,9; 3,1; 4,6; 5,3; 4,1 e 8,0 dias para quilha; 4,4; 3,6; 5,4; 5,8; 4,3; 5,2 e 6,3 dias para tíbia e 1,3; 1,9; 1,4; 1,5; 1,9; 1,7 e 2,1 dias para fígado, nos tratamentos T1, T2, T3, T4, T5, T6 e T7, respectivamente. Pode-se concluir que a tíbia possui metabolismo lento e pode indicar o sinal isotópico das dietas iniciais da criação dos frangos de corte; e o fígado, metabolismo rápido, indicado para refletir a dieta próxima da fase de avaliação.

  16. Estabilidade de fases em blendas de policarbonato-poliestireno avaliada por micro-FTIR, análise térmica e microscopia eletrônica de varredura Phase stability of polycarbonate-polystyrene blends evaluated by micro-FTIR, thermal analyses and scanning electron microscopy

    Directory of Open Access Journals (Sweden)

    Rodrigo L. Oréfice

    2004-06-01

    Full Text Available Nos últimos anos tem-se verificado uma acentuada desaceleração no desenvolvimento de novos homopolímeros, e nota-se um crescente interesse no estudo e desenvolvimento de processos que misturam os polímeros já existentes, dando origem às blendas poliméricas. Neste trabalho, blendas de poliestireno e policarbonato foram preparadas por extrusão em diferentes proporções. O processo de separação de fases foi estudado através da combinação de ferramentas analíticas como microscopias de infravermelho (micro-FTIR, óptica, eletrônica de varredura, e análise térmica. Resultados obtidos a partir das microscopias eletrônica e óptica permitiram definir as correlações entre morfologia e grau de estabilidade das fases do sistema. A composição e proporção relativas das fases das blendas foram determinadas usando microscopia de infravermelho. Tais resultados foram utilizados no cálculo do parâmetro de interação polímero-polímero de Flory-Huggins.In the last decade, a progressive reduction on the development of new homopolymers could be observed, while processes, such as blending, that combine commercially available polymers were emphasized. In this work, polycarbonate-polystyrene blends were extruded in compositions from 0% to 100% of polycarbonate in weight. The phase separation process was studied by combining a series of analytical techniques such as scanning electron, optical and infrared microscopy (micro-FTIR. Electron and optical microscopy allowed the determination of a correlation between phase morphology and the degree of phase stability of the system. The composition of the phases and information on phase stability were determined by using micro-FTIR. The Flory-Huggins interaction parameter could also be calculated from the micro-FTIR data.

  17. Aleaciones cuasicristalinas Al93Fe3Cr2Ti2

    Directory of Open Access Journals (Sweden)

    García-Escorial, Asunción

    2015-12-01

    solución solida sobresaturada, tanto en la matriz como en los cuasicristales, y posteriormente los cuasicristales se transforman en las fases de equilibrio del sistema: α-Al, Al13Fe4, Al13Cr2 y Al3Ti.

  18. Determinação de residuos de herbicidas em aguas utilizando extração em fase solida seguida de separaçaõ por cromatografia liquida e alta eficiencia

    OpenAIRE

    Glaucia Maria Ferreira Pinto

    1999-01-01

    Resumo: O sucesso da produção agrícola depende da aplicação de substâncias químicas, os pesticidas, que controlam as pestes. Se por um lado a aplicação de pesticidas é indispensável, por outro lado, pode ser muito perigosa para o meio ambiente e à saúde humana. Os pesticidas podem ser transportados para fontes de água causando contaminações. No mundo, tem crescido a preocupação com a qualidade das águas e devido a isto, torna-se necessário o desenvolvimento de métodos para analisar estes cont...

  19. Níveis de cloro para codornas japonesas na fase de postura Chlorine levels for Japanese quails during the egg-laying period

    Directory of Open Access Journals (Sweden)

    Roseane Madeira Bezerra

    2011-11-01

    Full Text Available Com o objetivo de avaliar os efeitos de quatro níveis de cloro sobre o desempenho e a qualidade de ovos de codornas japonesas na fase de produção, 288 codornas com 17 semanas de idade foram distribuídas em delineamento inteiramente casualizado, com seis tratamentos, oito repetições e seis aves por unidade experimental. Os níveis de cloro avaliados foram 0,07; 0,12; 0,17; 0,22; 0,27 e 0,32% e os parâmetros de desempenho e qualidade dos ovos foram: consumos de ração e água, porcentagem de postura, peso e massa de ovos, conversão alimentar, umidade das excretas, coeficientes de digestibilidade da matéria seca (CDMS, nitrogênio (CDN e energia bruta (CDEB, energia metabolizável aparente (EMA e aparente corrigida (EMAn, unidade Haugh, porcentagens de albúmen, gema e casca. Os níveis de cloro não influenciaram significativamente nenhuma dessas variáveis, entretanto, a gravidade específica aumentou linearmente com o acréscimo de cloro na ração. Pode-se recomendar que rações para codornas japonesas na fase de produção sejam formuladas com níveis de cloro de até 0,32%.In order to evaluate the effects of chlorine levels on performance and egg quality of Japanese quails during the production phase, 288 quails with seventeen weeks of age were distributed in a completely randomized design with six treatments, eight replicates and six birds experimental unit. Chlorine levels were: 0.07, 0.12, 0.17, 0.22, 0.27 and 0.32%. Performance and egg quality parameters evaluated were: feed intake (g/bird/day, water consumption (mL/bird/day, production (%, egg weight (g, egg mass (g/bird/day, feed conversion (g/g, moisture of excreta, digestibility of dry matter, coefficient of nitrogen, coefficient of gross energy, apparent metabolizable energy, corrected apparent metabolizable energy, Haugh unit, percentages of albumen, yolk and shell. Chlorine levels did not significantly influence any of those variables; however, the specific gravity

  20. Structural analysis and magmatism characterization of the Major Gercino shear zone, Santa Catarina State, Brazil

    International Nuclear Information System (INIS)

    Passarelli, Claudia Regina

    1996-01-01

    This work describes the geometric and kinematic characteristics of the Major Gercino Shear Zone (MGSZ) in the Canelinha-Garcia area. This shear zone is one of the major lineaments that affect all southern Brazilian precambrian terrains. In Santa Catarina State, it separates, along its whole extension, the supracrustal rocks of the Brusque belt (northern part) from the Granitoid belt (southern). This zone is characterized by a regional NE trend and a dextral sense of movement where ductile-brittle structures predominate. The MGSZ is composed of two mylonitic belts separated by granitoid rocks probably associated to the development of the shear zone. Both shear zones show cataclastic to ultra mylonitic rocks, but mylonites and protomylonites conditions at high strain rate. The calc-alkaline granitoids present in the area can be grouped in two granitoid associations with meta to peraluminous affinities. The Rolador Granitoid Association is characterized by grayish porphyritic biotite-monzogranites and the Fernandes Granitoid Association by coarsed-grained to porphyritic pinkish amphibole-syenogranites. The U-Pb and Rb-Sr ages range from 670 to 590 Ma with the Sr 87 / Sr 86 initial ratios suggesting a crustal contribution in the generation of these rocks. The importance of the pure shear component is also emphasized by the results of the Fry method. Many z axes of the strain ellipses are at high angle to the shear foliation. Symmetric porphyroclasts also corroborate this hypothesis. The micaceous minerals formed during the shear development indicate K-Ar ages around 555 ± 15 Ma. Brittle reactivations of the shear zone have been placed by K-Ar in fine-fraction materials at Triassic time (215 ± 15 Ma.)

  1. ESTUDIO DE LAS PROPIEDADES ESTRUCTURALES Y ELECTRÓNICAS DE LA FASE (P 4(2/mnm DEL MnO2

    Directory of Open Access Journals (Sweden)

    Wilmer Y. Córdoba

    2012-01-01

    Full Text Available Se reportan cálculos de primeros principios de las propiedades electrónicas del MnO 2 , el cual posee propiedades magnéticas debido a su configuración electrónica , por lo cual es apto para diversas aplicaciones a nivel tecnológico e industrial. Se calculan las propiedades estructurales y electrónicas en su fase P4(2/mnm, usando el formalismo de la Teoría de la Funcional de la Densidad (DFT con la aproximación LDA+U para tratar los efectos de la correlación fuerte y el método de ondas planas aumentadas y linealizadas (FP - LAPW, el cual se implementa en el software Wien2k . L os parámetros estructurales enco ntrados son: la constante de red , la energía de cohesión Además, se realizó un estudio detallado de las propiedades electrónicas por medio de la densidad de estados (DOS para obtener las características conductoras del material encontrando que este posee propiedades distintas de espín indicando que el material se comporta como de tipo Hall Metall .

  2. Mini-implantes ortodônticos como auxiliares da fase de retração anterior Orthodontic mini-implants assisting the anterior retraction phase

    Directory of Open Access Journals (Sweden)

    Carlo Marassi

    2008-10-01

    Full Text Available INTRODUÇÃO: os mini-implantes ortodônticos se estabeleceram como um importante método de ancoragem e vêm auxiliando os ortodontistas nas várias etapas do tratamento ortodôntico, eliminando, em grande parte, a necessidade de colaboração dos pacientes e tornando os resultados mais previsíveis. OBJETIVO: este artigo descreve os principais aspectos do uso dos mini-implantes como auxiliares da fase de retração anterior, trazendo considerações sobre suas indicações, quantidade de movimentação dos dentes anteriores, os vetores de força de retração, o controle vertical, o posicionamento dos mini-implantes, os tipos de apoio na região anterior e a força a ser utilizada. São citados os sítios de instalação mais usados para a retração anterior e abordados fatores que deverão ser controlados durante o fechamento de espaço. Por fim, são citadas algumas considerações clínicas sobre o uso dos mini-implantes nessa importante fase do tratamento ortodôntico.INTRODUCTION: The use of orthodontic mini-implants has settled as an important anchorage method and is aiding the orthodontists in the several stages of the treatment, largely eliminating the need of patients' compliance, and turning the results more predictable. AIM: This article describes the main aspects of the use of mini-implants as auxiliaries on the retraction phase of the anterior teeth, bringing considerations about their indications, amount of movement of the anterior teeth, the vectors of retraction force, the vertical control and evaluation of the incisors vestibulolingual tipping, the positioning of the mini-implants, the support types in the anterior area and the force to be applied. The placement sites best used for the anterior retraction are mentioned, and the factors that should be controlled during the space closure are approached. Lastly, some clinical considerations on the use of mini-implants in such important phase of the orthodontic treatment are

  3. Effects of water deficit in two phenological stages on production of japanese cucumber cultived in greenhouse Efeito do déficit hídrico em duas fases fenológicas sobre a produção do pepino-japonês cultivado em ambiente protegido

    Directory of Open Access Journals (Sweden)

    Eduardo C. Oliveira

    2011-01-01

    Full Text Available The experiment was performed in the experimental area of the Engineering Department Federal University of Lavras, Minas Gerais State, Brazil. It aimed at identifying the adequate irrigation management of the greenhouse-cultivated Japanese cucumber (Cucumis sativus L.. complete randomized design, with four levels of soil water potential (15; 30; 60 e 120 kPa at two phenological phases (vegetative and reproductive, and 5 replications. Overall, the results showed decrease of yield according to increase of soil water potentials. During the reproductive stage, Japanese cucumber plants were more sensitive to water deficit, resulting in further decrease in yield compared to applied water deficit during the vegetative stage of the culture.O experimento foi realizado na área experimental do Departamento de Engenharia da Universidade Federal de Lavras, em Lavras - MG, e teve como objetivo identificar um manejo adequado da irrigação para a produção do pepino-japonês (Cucumis sativus L. cultivado em ambiente protegido. Foi utilizado um delineamento inteiramente casualizado, envolvendo, como tratamentos, quatro níveis de potencial de água no solo (15; 30; 60 e 120 kPa em duas fases fenológicas da cultura (vegetativa e reprodutiva, com 5 repetições. De forma geral, os resultados mostraram decréscimo da produtividade de acordo com o incremento do potencial de água no solo; as plantas do pepineiro-japonês, quando na fase reprodutiva, mostraram-se mais sensíveis ao déficit hídrico, redundando em maiores quedas de produtividade em comparação com o déficit hídrico aplicado durante a fase vegetativa da cultura.

  4. Fluid inclusion study of radioactive granite and cherty cataclasite in the Southeastern part of Nanded district, Maharashtra: implications for the uranium mineralisation

    International Nuclear Information System (INIS)

    Banerjee, Rahul; Shivkumar, K.; Thomas, Tresa; Thomas, Jugina; Pandian, M.S.

    2013-01-01

    Southeastern part of Nanded district, Maharashtra exposes Palaeoproterozoic granitoids, representing the younger phase of Peninsular Gneissic Complex (PGC), mark the northeastern extension of Eastern Dharwar Craton. These granitoids are predominantly pink/grey granites, which are traversed by younger phosphatic cherty cataclasites close to the Deccan Trap capping. They are also affected by profuse pegmatitic/quartzo-feldspathic, quartz and epidote venations, especially close to fault/shear zones. A number of N-S to NNE-SSW, NE-SW, NW-SE and E-W trending lineaments marked by faults/fractures/shear zones and dykes are delineated in this granitic terrain. Among these, NE-SW and NNE-SSW faults/shear zones affecting granitoids and cherty cataclasites in Shahpur-Sujayatpur and Thadisaoli area have recorded significant uranium anomalies (Granitoids: upto 1% U 3 O 8 and 0.20% ThO 2 ; Cherty cataclasites upto 0.11% U 3 O 8 and <0.005% ThO 2 ) and enrichment in rare metal and rare earth element content (Nb-77ppm, Y-111 ppm, Zr-432ppm; n=9 and total REE-1167ppm; n=3). Presence of discrete uranium/thorium minerals (uraninite, b-uranophane and thorite) and high content of resistates viz., apatite, zircon, allanite, sphene, cerianite, monazite and ilmenite are responsible for radioactivity in granitoids while phosphatic material accounts for radioactivity in cherty cataclasites

  5. Oxygen reduction using platinum electrocatalysts prepared by liquid phase photo-deposition; Reduccion de oxigeno mediante electrocatalizadores de platino preparados por foto-deposicion en fase liquida

    Energy Technology Data Exchange (ETDEWEB)

    Ruiz-Camacho, B.; Perez-Galindo, J. A.; Valenzuela, M. A.; Gonzalez-Huerta, R. G. [Instituto Politecnico Nacional, ESIQIE, Mexico D.F. (Mexico)]. E-mail: rosgonzalez_h@yahoo.com.mx

    2009-09-15

    This work presents the synthesis and characterization of nanometric-sized Pt/C electrochemical catalysts using impregnation and liquid phase photo-deposition methods. Two platinum precursors were used, C{sub 10}H{sub 14}O{sub 4}Pt (Pt acetylacetonate, Pt(acac){sub 2}) and H{sub 2}PtCl{sub 6} (hexachloroplatinic acid) to study the effect on the particle size and the electrocatalytic behavior in the oxygen reduction reaction. The characterization of the catalysts was done using x-ray diffraction, hydrogen chemisorption and transmission electron microscopy. The electrochemical study was conducted with cyclic voltamperometry and rotary disc electrode (RDE) techniques. Pt (E-tek) was used as a reference catalyst. The peaks of the platinum were identified based on the x-ray diffraction results, and correspond to crystalline phases (111) and (200), whose intensity was greater when using H{sub 2}PtCl{sub 6} versus Pt(acac){sub 2}. The hydrogen chemisorption and transmission electron microscopy tests found that the larger-sized particle (1-5 nm) and greater metallic dispersion was obtained using Pt(acac){sub 2} as a platinum precursor and liquid phase photo-deposition. It was also found that this material presented the best electrochemical response, showing a open-circuit potential of 0.96 V and over-potential of 0.05 V with respect to H{sub 2}PtCl{sub 6} and of 0.22 V with respect to the catalyst obtained using impregnation. [Spanish] En este trabajo se presenta la sintesis y caracterizacion electroquimica de catalizadores de tamano nanometrico de Pt/C empleando los metodos de impregnacion y foto-deposicion en fase liquida. Se utilizaron dos precursores del platino C{sub 10}H{sub 14}O{sub 4}Pt (acetil-acetonato de Pt, Pt(acac){sub 2}) y H2PtCl6 (acido hexacloroplatinico), para estudiar el efecto que tienen sobre el tamano de particula y el comportamiento electrocatalitico en la reaccion de reduccion de oxigeno. La caracterizacion de los catalizadores se realizo mediante

  6. Distributional patterns of the South American species of Hyalella (Amphipoda: Hyalellidae)

    OpenAIRE

    De los Ríos-Escalante, Patricio; Morrone, Juan J; Rivera, Reinaldo

    2012-01-01

    Distributional patterns of the South American species of the freshwater amphipod genus Hyalella were analysed using a panbiogeographic approach. Five generalized tracks were found: (1) northern Andes to Lake Titicaca (H. dielaii, H. meinerti, H. dybowskii, H.jelskii, H. lubominsky, and H. pauperocavae; (2) lake Titicaca (H. armata, H. cuprea, H. latinamus, H. lucifugax, H. montforti, H. neveulemairei, H. robusta, H. tiwanaku, H. simplex simplex, and H. solida); (3) central Andes (H. fossamanc...

  7. Review article: RE-SiAlONa¤b- composites. Formation, thermal stability, phase relationships, reaction densification Artigo revisão: compósitos TR a¤b SiAlON. Formação, estabilidade térmica, relações de fases, densificação por reação

    Directory of Open Access Journals (Sweden)

    V. A. Izhevskiy

    1999-02-01

    Full Text Available In view of the considerable progress that has been made over the last several years on the fundamental understanding of phase relationships, microstructural design, and tailoring of properties for specific applications of rare-earth doped SiAlONs, a clear review of current understanding of the basic regularities lying behind the processes that take place during sintering of SiAlONs is timely. Alternative secondary phase development, mechanism and full reversibility of thea«btransformation in relation with the phase assemblage evolution are elucidated. Reaction sintering of multicomponent SiAlONs is considered with regard of wetting behavior of silicate liquid phases formed on heating. Regularities of SiAlON’s behavior and stability are tentatively explained in terms of RE-element ionic radii and acid/base reaction principle.Em vista do considerável progresso obtido nos últimos anos quanto à relação entre fases, o design microestrutural e a otimização de propriedades para aplicações específicas de SiAlONs dopados com elementos de terras-raras, se faz necessário uma clara revisão dos mecanismos envolvidos nos processos que ocorrem durante a sinterização dos SiAlONs. O desenvolvimento de segundas fases alternativas, os mecanismos e a completa reversibilidade da transformaçãoa«b, em relação ao conjunto das fases são elucidados. Sinterização por reação de SiAlONs multi-componentes é analisada em relação à molhabilidade da fase líquida a base de silicato formada no aquecimento. Propõe-se uma explicação para a regularidade e estabilidade do comportamento dos SiAlONs em termos do raio iônico dos elementos de terras-raras e do princípio de reação ácido/base.

  8. Pseudotachylitic breccia from the Dhala impact structure, north-central India: Texture, mineralogy and geochemical characterization

    Science.gov (United States)

    Pati, J. K.; Reimold, W. U.; Greshake, A.; Schmitt, R. T.; Koeberl, C.; Pati, P.; Prakash, K.

    2015-05-01

    Pseudotachylitic breccia (PTB) occurs in a drill core from the crater floor of the 11 km diameter, Proterozoic Dhala impact structure, India. PTBs were intersected in late Archean granitoids between 348.15 m and 502.55 m depth in the MCB-10 drill core from the center of the Dhala structure. The breccias comprise both cataclastic-matrix as well as melt breccias. The presence of microlites and vesicles in the groundmass and a widely observed flow fabric in the PTB support the presence of melt in the groundmass of some samples. Clasts in PTB are derived from the Archean granitoid basement. PTB matrix, the matrix of impact melt breccia also occurring between 256.50 m and 502.55 m depth, and the target granitoids vary in terms of silica, total alkali, magnesium and iron oxide contents. Chondrite-normalized REE patterns of PTB and target granitoids are similar, but the elemental abundances in the PTB are lower. The restricted size of PTB as veins and pods of up to 2.5 cm width, their occurrence at varied depths over a core length of 150 m, the clast population, and the chemical relationships between PTB and their host rocks all suggest the derivation of these breccias locally from the fractured basement granitoids involving in-situ melting. We favor that this took place due to rapid decompression during the collapse and modification stage of impact cratering, with, locally, additional energy input from frictional heating. Locally, amphibolite and dioritic mylonite occur in the host granitoids and their admixture could have contributed to the comparatively more mafic composition of PTB. Alteration of these crater floor rocks could have involved preferential reduction of silica and alkali element abundances, possibly due to impact-induced hydrothermal activity at crater floor level. This process, too, could have resulted in more mafic compositions.

  9. Structural analysis and magmatism characterization of the Major Gercino shear zone, Santa Catarina State, Brazil; Analise estrutural e caracterizacao do magmatismo da zona de cisalhamento Major Gercino, SC

    Energy Technology Data Exchange (ETDEWEB)

    Passarelli, Claudia Regina

    1996-12-31

    This work describes the geometric and kinematic characteristics of the Major Gercino Shear Zone (MGSZ) in the Canelinha-Garcia area. This shear zone is one of the major lineaments that affect all southern Brazilian precambrian terrains. In Santa Catarina State, it separates, along its whole extension, the supracrustal rocks of the Brusque belt (northern part) from the Granitoid belt (southern). This zone is characterized by a regional NE trend and a dextral sense of movement where ductile-brittle structures predominate. The MGSZ is composed of two mylonitic belts separated by granitoid rocks probably associated to the development of the shear zone. Both shear zones show cataclastic to ultra mylonitic rocks, but mylonites and protomylonites conditions at high strain rate. The calc-alkaline granitoids present in the area can be grouped in two granitoid associations with meta to peraluminous affinities. The Rolador Granitoid Association is characterized by grayish porphyritic biotite-monzogranites and the Fernandes Granitoid Association by coarsed-grained to porphyritic pinkish amphibole-syenogranites. The U-Pb and Rb-Sr ages range from 670 to 590 Ma with the Sr{sup 87} / Sr{sup 86} initial ratios suggesting a crustal contribution in the generation of these rocks. The importance of the pure shear component is also emphasized by the results of the Fry method. Many z axes of the strain ellipses are at high angle to the shear foliation. Symmetric porphyroclasts also corroborate this hypothesis. The micaceous minerals formed during the shear development indicate K-Ar ages around 555 {+-} 15 Ma. Brittle reactivations of the shear zone have been placed by K-Ar in fine-fraction materials at Triassic time (215 {+-} 15 Ma.) 220 refs., 107 figs., 18 tabs., 4 maps

  10. Purificação de três diferentes beta-galactosidades microbianas por partição em sistemas de duas fases aquosas Purification of three different microbial beta-galactosidases by partitioning in aqueous two-phase systems

    Directory of Open Access Journals (Sweden)

    Maria Estela SILVA

    1997-12-01

    Full Text Available Este trabalho tratou da investigação do efeito do peso molecular de polietilenoglicol (PEG sobre a partição de enzimas beta-galactosidases de diferentes origens microbianas: Escherichia coli, Klueveromyces lactis e Aspergillus orizae em sistemas de duas fases aquosas (SDFA.Foi observado que os melhores sistemas para purificação da enzima de E. coli foram os formados por PEG 4000, 6000 e 8000/fosfato, fornecendo os mais elevados fatores de purificação da enzima. As enzimas de Klueveromyces lactis e Aspergillus orizae não foram eficientemente purificadas nestes sistemas sendo insensíveis à alterações do peso molecular do PEG. Portanto, um outro sistema de duas fases aquosas foi desenvolvido contendo um ligante específico, p-aminofenil 1-tio-beta-D-galactopiranosídeo (APGP, acoplado ao PEG para purificar a enzima de Klueveromyces lactis. Uma etapa simples de partição no SDFA formado por 6% APGP-PEG4000 + 12% dextrana T505.000 foi capaz de recuperar 83% da enzima na fase superior do sistema e de aumentar 1,6 vezes o fator de purificação.This work investigated the effect of the molecular weight of polyethyleneglycol (PEG upon the partition coefficient of beta-galactosidases from three different microorganisms: Escherichia coli, Klueveromyces lactis and Aspergillus orizae. It was found that PEG 6,000 and PEG 8,000/phosphate were the best systems for achieving the highest purification factors of E. coli beta-galactosidase. However, the other two yeast beta-galactosidases were not efficiently separated from their contaminants in any of the PEG/salt systems. In order to improve the separation of Klueveromyces lactis beta-galactosidase from the main protein contaminants, the biospecific ligand p-aminophenyl 1-thio-beta-D-galactopyranoside (APGP was attached to activated PEG 4000. The affinity PEG having APGP bound to its backbone was synthesized in two steps. The partitioning of Klueveromyces lactis beta-galactosidase in aqueous two

  11. La fase principal de las tormentas geomagnéticas y la anomalía geomagnética del Atlántico Sur

    Directory of Open Access Journals (Sweden)

    María Andrea Van Zele

    2012-12-01

    Full Text Available El objetivo de este estudio es determinar en qué condiciones se produce y cuánto perdura el rápido crecimiento de la variación de intensidad del campo magnético durante la fase principal de una tormenta geomagnética (dB, y si depende de la intensidad del campo principal donde ésta se registra. Para ello se comparan variaciones de tormentas calculadas dentro y fuera de la Anomalía Geomagnética del Atlántico Sur (SAMA, donde el campo geomagnético principal es mínimo. Con los registros del observatorio de Vassouras (latitud baja, Brasil se calculan las variaciones de tormenta correspondientes a la zona de la Anomalía. Los registros del observatorio de Kourou (KOU a la misma longitud geográfica y latitud geomagnética conjugada, y los de Kakadu (Australia y Kanoya (Japón, a 180° de longitud y algo mayor latitud, se utilizan para la comparación. Se seleccionan tormentas geomagnéticas registradas entre los años 2000 y 2009 que presentan una fase principal bien definida según el índice Dst, independientemente de su intensidad y de al menos media hora de duración. Se establece que a las características generales de las variaciones de tormentas registradas en la SAMA son compartidas con las registradas fuera de la región; b por lo general, el decrecimiento rápido de la componente norte X es mayor en VSS, pero no es independiente de la hora de inicio ni la época del año; c por lo general la variación de tormenta del campo total (dB es mayor en VSS, pero no es independiente de la hora de inicio ni la época del año. Puede concluirse que allí donde el campo magnético total es aproximadamente la mitad del que correspondiente al campo dipolar, el rápido crecimiento de la intensidad de la fase principal de una tormenta geomagnética (dB no tiene un comportamiento unívoco, asociado a la intensidad del campo principal.The aim of this study is to determine whether the rapid growth of the magnetic field intensity during the main

  12. Aplicação de metodos de otimização para o calculo do equilibrio quimico e de fases combinados para processos com gas de sintese

    OpenAIRE

    Consuelo Cristina Gomes Silva

    2008-01-01

    Resumo: Essa pesquisa consiste em aplicar métodos de otimização global para o cálculo do equilíbrio químico e de fases combinados para misturas com gás de síntese. O gás de síntese tem grande interesse industrial, pelas inúmeras possibilidades de produção de diversos compostos químicos. Dessa forma, é fundamental conhecer as condições termodinâmicas que favoreçam a obtenção de determinado produto. A aplicação de métodos de otimização global é de grande interesse para a determinação do equilíb...

  13. Estado de mistura e dispersão da fase borrachosa em blendas PVC/NBR Phase separation and rubber phase dispersion in PVC/NBR blends

    Directory of Open Access Journals (Sweden)

    Fábio R. Passador

    2006-01-01

    Full Text Available Termoplásticos modificados com elastômeros têm despertado grande interesse de pesquisadores e de indústrias devido à atraente relação custo/benefício e a possibilidade de aumento significativo da tenacidade sob impacto de polímeros frágeis com a incorporação de uma fase borrachosa dispersa. Este artigo mostra a relação entre o estado de mistura e a dispersão da fase borrachosa em blendas de poli (cloreto de vinila (PVC com borracha nitrílica (NBR. O estado de mistura de blendas poliméricas é um fator muito importante a ser considerado no desenvolvimento destes tipos de materiais, uma vez que determina o nível de mistura molecular das blendas. A característica estrutural do PVC é responsável pela morfologia das blendas PVC/NBR, sendo que há uma otimização de propriedades mecânicas quando as partículas de borracha formam a morfologia "pseudo-network", ou seja, quando as partículas de borracha estão randomicamente dispersas entre as partículas primárias do PVC.Thermoplastics modified with elastomers have attracted great interest of researchers and industries due to the low cost/benefit relationship and the possibility of significant increase in the toughness of brittle polymers through the incorporation of a dispersed rubber phase. This article shows the relationship between the interaction between phases and rubber phase dispersion in poly (vinyl chloride/nitrile rubber blends. The interaction between components in polymer blends is an important factor to be considered in the development of this kind of materials because it determines the level of the mixture at the molecular level. The particulate nature of PVC and the degree of nitrile groups in the NBR are responsible to the PVC/NBR blends morphologies leading to an optimization of the mechanical properties when the rubber particles form a pseudo-network morphology with the rubber particles randomly dispersed in between the PVC primary particles.

  14. Una revisión de metodologías seguras en cada fase del ciclo de vida del desarrollo de software

    Directory of Open Access Journals (Sweden)

    César Marulanda L.

    2012-06-01

    Full Text Available El desarrollo de software seguro es un asunto de alta importancia en las compañías, debido a que la mayoría de ellas dependen altamente de sus aplicaciones para su operación normal. Es por esto que se hace necesario implementar efectivamente metodologías de desarrollo seguro que sean aplicadas en cada fase del ciclo de vida: requisitos, diseño, desarrollo y pruebas. Es importante tener presente la seguridad desde las etapas más tempranas del proceso de desarrollo y no dejarla en un segundo plano. Además, se requiere investigar el estado del arte en desarrollo de aplicaciones seguras y así escoger metodologías de acuerdo con las necesidades de cada aplicación y los requisitos de los interesados en el producto final. El objetivo de este artículo es recopilar una serie de metodologías y herramientas existentes que se puedan implementar, añadiendo seguridad en toda la aplicación y desarrollando no sólo software de alta calidad sino también de alta seguridad.

  15. Análisis de fase mediante "Gated-SPECT" de perfusión miocárdica para valorar el sincronismo mecánico del ventrículo izquierdo realizado con dos programas distintos de procesamiento

    Directory of Open Access Journals (Sweden)

    Víctor Marín Oyaga

    2016-01-01

    Full Text Available Introducción y objetivos: El análisis de fase mediante Gated- SPECT de perfusión mio - cárdica ( GS-PMI es una nueva herramienta para medir la asincronía ventricular izquierda con importantes aplicaciones clínicas futuras en resincronización e insuficiencia cardiaca. Se puede medir mediante dos programas ( ECTb o QGS C-S . El objetivo es demostrar su factibilidad y verificar si existen diferencias entre ambos. Metodología: Estudio analítico, observacional y retrospectivo en pacientes con GS-PMI normales. Los parámetros obtenidos fueron: la desviación estándar de la fase (DE y el ancho de banda de histograma (AH . La evaluación de la diferencia entre los grupos se realizó usando pruebas para muestras independientes después de analizar la distribución de datos. Nivel de significación p<0,05. Se utilizó SPSS IBM V.21 ®. Resultados: Total pacientes: 193 (104 hombres. Edad media: 64 años (24-89.61/193 procesados con QGS C-S y 132/193 con ECT b. Postestrés: la media de la DE fue 6º±3,7º, con mediana de 5º y rango intercuartílico ( IR :3.6º. La media de AH fue 22,7º±10º, con mediana de 18º y IR :11.5º. Postreposo: la media de la DE fue 5,76º±4,82º y la mediana 4,5º con IR : 3.1º. La media de AH fue 21.67º± 14.06º y la mediana 18º, IR :12º. Entre ambos programas se encontraron diferencias significativas en la DE en postestrés (p=0,001 y postreposo (p=0,019, sin diferencias en el AH postestrés (p=0,31 y postreposo (p=0,18. Conclusión : Realizar el análisis fase de análisis por GS-PMI es factible. Sin embargo, la DE mostró diferencias significativas entre los dos programas. Aunque los valores mostrados podrían ser utilizados como valores normales, se recomienda que estos se obtengan y utilicen para cada programa por separado.

  16. Anaerobic biodigestion of pigs feces in the initial, growing and finishing stages fed with diets formulated with corn or sorghum Biodigestão anaeróbia de dejetos de suínos nas diferentes fases alimentados com dietas formuladas com milho ou sorgo

    Directory of Open Access Journals (Sweden)

    Adélia P. Miranda

    2012-02-01

    Full Text Available The objective of this study was to evaluate the quality and the production of biogas and biofertilizer obtained from biodigester supplied with pig feces in the initial, growing and finishing stages, fed with diets formulated based on corn or sorghum. Twenty bench biodigesters were used with hydraulic retention time of 30 days and daily loads that contained 4 to 6% of total solids (TS and 3.6 to 5.2% of volatile solids (VS. In the effluent of the biodigesters, mean levels of TS were observed ranging between 1.6 and 2.0% and of VS between 1.2 and 1.6%. The mean reductions of TS were 57.7 to 64.7% and of VS from 61.7 to 69.0%, and there was only difference in the finishing phase, in which the major averages reductions were produced by the biodigesters supplied with feces from animals fed with diets based on corn. In biodigesters supplied with feces from animals in the initial and growing stages fed with diets based on corn, were observed higher average productions of biogas and the greatest average potentials of biogas production. The average potentials obtained were 0.033; 0.181; 0.685; 0.788 and 1.132 m³ per kg of affluent, manure, TS added, VS added and VS reduced, respectively. No differences were found on the average content of methane in the biogas between diets and stages. The average concentrations of nutrients N, P, K, Ca, Mg, Na, Fe, Mn, Zn and Cu in the biodigester affluent and effluent, ranged between diets and stages.Objetivou-se avaliar a produção e a qualidade do biogás e do biofertilizante obtidos em biodigestores abastecidos com dejetos de suínos, nas fases inicial, crescimento e terminação, alimentados com dietas formuladas à base de milho ou sorgo. Foram utilizados 20 biodigestores de bancada, com tempo de retenção hidráulica de 30 dias, e cargas diárias que continham 4,0 a 6,0% de sólidos totais (ST e 3,6 a 5,2% de sólidos voláteis (SV. Nos efluentes dos biodigestores, foram verificados teores médios de ST

  17. New Phase in the System Uranium-Molybdenum-Silicon; Nouvelle phase dans le systeme uranium-molybdene-silicium; Novaya faza v sisteme uran-molibden'-kremnij; Una fase nueva en el sistema uranio-molibdeno-silicio

    Energy Technology Data Exchange (ETDEWEB)

    Sikirica, M.; Ban, Z. [Rudjer Bokovic Institute, Zagreb, Yugoslavia (Croatia)

    1963-11-15

    During the investigation of the ternary system uranium-molybdenum-silicon, a new phase with the composition U{sub 4}Mo{sub 5}-Si{sub 3} was formed. Structure determination exclusively based on the powder data showed that the particular phase belongs to the hexagonal system. Space group P6/mmc or one of the sub-groups is indicated. Unit cell dimensions were found to be a = 5.37{sub 0}A, c = 8 . 58{sub 2}A. A comparison of calculated and observed intensities shows close resemblance to the structure of the Laves phases of the C14-type. (author) [French] Au cours de recherches sur le systeme ternaire uranium-molybdene-silicium, on a constate la formation d'une nouvelle phase, de composition U{sub 4}Mo{sub 5}Si{sub 3}. Une determination de la structure, exclusivement fondee sur des donnees relatives a la poudre, a revele que cette phase particuliere appartenait au systeme hexagonal. Les auteurs indiquent un groupe spatial P6/mmc ou un des sous-groupes. Les dimensions d'une maille individuelle sont donnees par a = 5,37{sub 0}A, c = 8,58{sub 2}A. La comparaison entre l'intensite calculee et Tintensite observee montre une ressemblance etroite avec la structure des phases de Laves du type C-14. (author) [Spanish] En-el curso del estudio del sistema temario uranio-molibdeno-silicio, los autores observaron la formacion de una fase cuya composicion responde a la formula U{sub 4}Mo{sub 5}Si{sub 3}. La determinacion de la estructura, basada exclusivamente en los datos referentes al material en polvo, demuestra que esa fase pertenece al sistema hexagonal. Se senalo la existencia de un grupo especial P6/mmc y se comprobo que las dimensiones de la celda elemental son a = 5,37{sub 0}A, c = 8,58{sub 2}A. La comparacion de las intensidades calculadas con las observadas indica que existe una analogia estrecha con la estructura de la fase de Laves del tipo C 14. (author) [Russian] Pri izuchenii trojnoj sistemy uran - molibden - kremnij obrazovalas' novaya faza sostava U{sub 4}Mo{sub 5

  18. Caracterización de la población del corregimiento de Salgar (Atlántico, Colombia) como fase preliminar para la implementación de un Modelo de Atención Primaria en Salud, 2014

    OpenAIRE

    Hernando Baquero-Latorre; Ana Liliana Ríos-García

    2015-01-01

    Objetivo:Caracterizar la población del corregimiento de Salgar (Atlántico) como fase pre-liminar para la implementación de un Modelo de Atención Primaria en Salud. Materiales y método: Investigación descriptiva transversal de ámbito comunitario. Fuente primaria, se recolectó con tarjeta familiar en el lugar de residencia. Se realizaron intervenciones en salud con docentes y estudiantes de medicina y enfermería, con base en riesgos identificados.Resultados:Se caracterizó a 418 familias, 7...

  19. Caracterización de la población del corregimiento de Salgar (Atlántico, Colombia) como fase preliminar para la implementación de un Modelo de Atención Primaria en Salud, 2014

    OpenAIRE

    Baquero-Latorre, Hernando; Ríos-García, Ana Liliana

    2015-01-01

    Objetivo: Caracterizar la población del corregimiento de Salgar (Atlántico) como fase preliminar para la implementación de un Modelo de Atención Primaria en Salud. Materiales y método: Investigación descriptiva transversal de ámbito comunitario. Fuente primaria, se recolectó con tarjeta familiar en el lugar de residencia. Se realizaron intervenciones en salud con docentes y estudiantes de medicina y enfermería, con base en riesgos identificados. Resultados: Se caracterizó a 418 familias, 78.9...

  20. Inquietudes e tensionamentos: pistas para a compreensão do futuro do rádio comercial em sua fase de convergência

    Directory of Open Access Journals (Sweden)

    Luiz Artur Ferraretto

    2015-12-01

    Full Text Available Este artigo busca amparo teórico na economia política da comunicação para analisar as perspectivas do rádio comercial brasileiro em sua fase de convergência. Objetiva demonstrar o equívoco da sobrevalorização da tecnologia neste processo, assumindo tal prática como algo comum entre a classe empresarial. Para tanto, parte de proposições anteriores para a redefinição do conceito de rádio, considerando uma concepção plural para o meio, a linguagem específica empregada, a expansão em direção a outras mídias e a sua caracterização como uma criação cultural coletivamente desenvolvida. Trabalha, neste quadro teórico e conceitual, as estações comerciais na contemporaneidade por quatro pontos de vista tidos aqui como complementares: (1 o tecnológico; (2 o empresarial; (3 o profissional e de conteúdos; e (4 o do público.

  1. Natural Afsluitdijk. Phase 1. Report Marketing Research Afsluitdijk; Natuurlijk Afsluitdijk. Fase 1 rapport Marktverkenning Afsluitdijk

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2008-07-15

    An overview is given of sketches and ideas for an integral vision on the Afsluitdijk, Netherlands with regard to safety, sustainability and innovation. Chapter 2 sheds a light on the original idea and explains the elaborated vision. Chapter 3 contains the integral vision, discussing the development process, the design models and the elaboration of the various functions, including their synergy. Chapter 4 addresses the feasibility of the vision. Chapter 5 examines the effects and the stakeholders. Chapter 6 provides the legal and administrative frameworks and chapter 7 provides a preliminary analysis of the shaping of the public-private process. Finally, chapter 8 provides a state of the art at the end of phase 1 of the marketing research Afsluitdijk. [Dutch] Dit rapport van het consortium 'Natuurlijk Afsluitdijk' bevat schetsen en ideeen voor een integrale visie op de Afsluitdijk t.a.v. veiligheid, duurzaamheid en innovatie. Het Consortium Natuurlijk Afsluitdijk bestaat uit de volgende partijen: Wubbo Ockels B.V.; Haskoning Nederland B.V.; Cooperatieve Centrale Raiffeisen-Boerenleenbank B.A. (Rabobank); Van Oord Dredging and Marine Contractors B.V.; Koninklijke BAM Groep N.V. (BAM); Raadgevend Ingenieursbureau Lievense B.V.; Eneco Milieu B.V. Hoofdstuk 2 belicht het oorspronkelijke idee en geeft de uitgewerkte visie weer. Hoofdstuk 3 is de 'Integrale visie', waarbij zowel het ontwikkelproces, de ontwerpmodellen en de uitwerking van de verschillende functies, inclusief hun synergie worden weergegeven. In hoofdstuk 4 komt de haalbaarheid aan de orde. In hoofdstuk 5 komen de effecten en stakeholders aan de orde. In hoofdstuk 6 de wettelijke en bestuurlijke kaders en in hoofdstuk 7 wordt een eerste analyse gegeven van de vormgeving van het publiekprivate proces. Hoofdstuk 8 tenslotte geeft de stand van zaken aan het einde van fase 1 van de Marktverkenning Afsluitdijk.

  2. Gas exchange alteration caused by water deficit during the bean reproductive stage Alterações das trocas gasosas na fase reprodutiva e produtividade do feijão sob déficit hídrico

    Directory of Open Access Journals (Sweden)

    Lauricio Endres

    2010-01-01

    Full Text Available The purpose of the present study was to analyze gas exchanges in leaves and the parameters of productivity of beans (Phaseolus vulgaris, L. submitted to two water deficiency periods during which three water regimes were employed: W1 (1,0 ETo during the entire plant cycle; W2 (1,0 ETo up to the flowering period and irrigation interruption from the 37 to the 51st day following sowing, and W3 (in addition to the reproductive phase, water deficit was also applied during the vegetative stage. Photosynthesis was one of the main physiological factors affected by water deficit. This was not only caused by the stomata closure, but also by carboxilation reduction due to metabolic damage. This effect was, however, offset 24 h after rehydration. During flowering, the water deficit caused crop productivity to drop significantly, reducing the number of pods and the number of seeds per pod, independently of the water deficit during the vegetative stage. The weight of 100 seeds however, was the same regardless of treatment. These results suggest that the water deficit caused the reduction of photo-assimilates, which affected grain productivity. Nevertheless, once properly formed, seeds developed totally; a strategy of the plant to produce less seeds under stress, but viable to perpetuate the species.Neste trabalho, se analisaram as trocas gasosas das folhas e parâmetros de produtividade de feijão (Phaseolus vulgaris, L. submetido a dois períodos de deficiência hídrica e se empregaram três regimes hídricos, a saber: W1 (1,0 ETo durante todo o ciclo da cultura; W2 (1,0 ETo até a floração e suspensão da irrigação do 37 ao 51º dia após a semeadura (DAS, correspondendo à fase de floração e W3 (além da fase reprodutiva também se aplicou um déficit hídrico durante a fase vegetativa. A fotossíntese foi um dos principais fatores fisiológicos afetados pelo déficit hídrico devido não só ao fechamento estomático, mas, também, à redução da

  3. Life cycle assessment. Specific indicators for Italy in impact evaluation; Life cycle assessment: sviluppo di indicatori specific per l'Italia per la fase di valutazione d'impatto

    Energy Technology Data Exchange (ETDEWEB)

    Masoni, P [ENEA, Centro Ricerche Casaccia, S. Maria di Galeria, RM (Italy). Dipt. Energia; Scimia, E [Bologna Univ., Bologna (Italy)

    1999-07-01

    After a brief recall and a short description of the LCA (life cycle assessment) methodology, the work is focused on the impact assessment step, discussing the state of the art and a critical identification of environmental indicators, of normalization and weighting principles for the different environmental categories specific for Italy. The application methodology to a case study concerning the production of butter by the Consorzio Granterre of Modena (Italy) is also described. [Italian] Il lavoro analizza la fase centrale della metodologia denominata valutazione d'impatto, resentando una rassegna dello stato dell'arte e un'individuazione critica dei possibili indicatori ambientali, di criteri di normalizzazione e di attribuzione di pesi ai diversi temi ambientali specific per l'Italia. Viene descritta l'applicazione ad un caso concreto relativo alla produzione del burro nel consorzio Granterre di Modena.

  4. Separação de fases induzida por meio de reação química no sistema éter diglicidílico do bisfenol A e piperidina com poli(metacrilato de metila Phase separation induced by chemical reaction in the system of diglycidyl ether of bisphenol A and piperidine with poly(methyl methacrylate

    Directory of Open Access Journals (Sweden)

    Filiberto González Garcia

    2003-12-01

    Full Text Available O comportamento da separação de fases e da gelificação do sistema epoxídico, constituído pelo éter diglicidílico do bisfenol A (DGEBA e a piperidina, modificado com poli(metacrilato de metila (PMMA, foi estudado na faixa de temperatura de 60 °C - 120 °C. A concentração de PMMA e a temperatura de cura causam mudanças significativas na morfologia gerada. A massa molecular de PMMA provoca ligeiras mudanças para a observação da separação de fases e não afeta a velocidade da reação. O sistema modificado com PMMA mostra o efeito de retardação cinético e a velocidade de separação de fases é maior que a velocidade de polimerização.The phase separation and gelification behavior of epoxy system based on diglycidyl ether of bisphenol-A (DGEBA and piperidine modified with poly(methyl methacrylate (PMMA were studied in the range between 60 °C and 120 °C. The morphology is influenced by the PMMA content in the blend and also by the cure temperature. The molecular weight of PMMA provokes slight changes on cloud point and does not affect the reaction rate. The systems modified by PMMA exhibited kinetic retardation effect but the cloud point rate was higher than the polymerization rate.

  5. Celda de combustible: análisis teórico del rendimiento eléctrico de hidrógeno almacenado en fase sólida

    Directory of Open Access Journals (Sweden)

    I. A. Vértiz-Maldonado

    2012-01-01

    Full Text Available En este trabajo se presenta una metodología para determinar el efecto del almacenamiento de hidrógeno en una estructura de fase sólida formada por hidruro de magnesio (acumulación de hidrógeno. Se realiza un análisis comparativo del porcentaje teórico que es capaz de almacenar en peso este hidruro que es del 7.59%, mientras que el obtenido en un experimento de hidruración es de 5.955% en peso. Lo anterior se llevó acabo con el fin de determinar el rendimiento de energía acum