WorldWideScience

Sample records for cerro mercado pluton

  1. An empirical calibration for 4He quantification in minerals and rocks by laser fusion and noble gas mass spectrometry using Cerro de Mercado (Durango, Mexico) fluorapatite as a standard

    International Nuclear Information System (INIS)

    An empirical calibration with a natural mineral standard (fluorapatite from Cerro de Mercado, Mexico) is proposed as a method to determine the 4He concentration of mineral and rock samples. The procedure is based on the fusion of several aliquots of the fluorapatite standard with a well-spaced weight distribution in order to obtain a good correlation in coordinates of 4He peak height versus fluorapatite weight. The weight is then converted to moles using the accepted mineral age (31.4 Ma) and appropriate formula. Experimental peak height of 4He for the unknown samples are converted to moles with the regression determined for fluorapatite. The procedure is fast and inexpensive, and both precision and accuracy are always below 10% and usually about 3-5%

  2. Livre mercado

    Directory of Open Access Journals (Sweden)

    Müller, Lúcia Helena Alves

    2003-01-01

    Full Text Available Este artigo é resultado de uma etnografia que foi realizada junto ao mercado de ações brasileiro. Através da análise do funcionamento do pregão da bolsa de valores de São Paulo, das diferentes instituições financeiras que conformam este mercado e das trajetórias dos profissionais neste universo, busco demonstrar como são produzidas as condições sociais para a existência de um espaço de trocas que tem como princípio ordenador e legitimador o modelo teórico do mercado perfeito, formulado pela escola econômica neoclássica

  3. Livre mercado

    OpenAIRE

    Müller, Lúcia Helena Alves

    2003-01-01

    Este artigo é resultado de uma etnografia que foi realizada junto ao mercado de ações brasileiro. Através da análise do funcionamento do pregão da bolsa de valores de São Paulo, das diferentes instituições financeiras que conformam este mercado e das trajetórias dos profissionais neste universo, busco demonstrar como são produzidas as condições sociais para a existência de um espaço de trocas que tem como princípio ordenador e legitimador o modelo teórico do mercado perfeito, formulado pela e...

  4. The Cerro Solo Project

    International Nuclear Information System (INIS)

    The objective of the Cerro Solo Project, which was initiated in 1990, is to perform the assessment of the Co. Solo uranium ore deposit in a sequential manner. The deposit, which is located in the Patagonia Region, Argentine Republic, belongs to the sandstone type, and to the subtype coarse-grained, high energy stream. Uranium occurrences are peneconcordant, lenticular shaped and irregularly distributed in the fluvial sediments of the cretaceous Chubut Group. Resources estimated using up to present data, in tonnes of uranium recoverable at costs up to $80/kg U, are: Reasonable Assured Resources (RAR): 300 tU; Estimated Additional Resources - Category I (EAR-I): 900 tU; Estimated Additional Resources - Category II (EAR-II): 2400 tU. Resources of this ore deposit are significant to the uranium requirements in Argentina. (author). 3 refs, 6 figs

  5. Geothermal drilling in Cerro Prieto

    Energy Technology Data Exchange (ETDEWEB)

    Dominguez A., Bernardo

    1982-08-10

    The number of characteristics of the different wells that have been drilled in the Cerro Prieto geothermal field to date enable one to summarize the basic factors in the applied technology, draw some conclusions, improve systems and procedures, and define some problems that have not yet been satisfactorily solved, although the existing solution is the best now available. For all practical purposes, the 100 wells drilled in the three areas or blocks into which the Cerro Prieto field has been divided have been completed. Both exploratory and production wells have been drilled; problems of partial or total lack of control have made it necessary to abandon some of these wells, since they were unsafe to keep in production or even to be used for observation and/or study. The wells and their type, the type of constructed wells and the accumulative meters that have been drilled for such wells are summarized.

  6. Democracia y mercado

    OpenAIRE

    2013-01-01

    El trabajo parte de una pregunta fundamental: ¿La democracia es funcional a la racionalidad propuesta a las sociedades desde la economía de mercado capitalista?. Darle salida a este interrogante exige asumir dos presupuestos teóricos: 1) no asumir una equiparación lineal y estática entre capitalismo y mercado, es decir, el mercado no se puede reconocer como una condición exclusiva del capitalismo.3 2) Lo que se ha llamado Estado capitalista, ha sufrido transformaciones en su or...

  7. Democracia, mercado y socialismo

    OpenAIRE

    2012-01-01

    El trabajo pretende continuar con la pregunta en torno al papel de la democracia??y su funcionalidad en la econom??a de mercado. Lo nuevo a desarrollar bajo este interrogante, es trasladar la reflexi??n al ??mbito del socialismo y espec??ficamente a lo que se ha denominado el socialismo de mercado. La aspiraci??n es presentar los desarrollos te??ricos en torno al denominado socialismo de mercado, y c??mo desde all?? se ha estructurado un concepto de democracia que adquiere validez desde el re...

  8. Finanzas y mercados

    OpenAIRE

    Muñoz Ballesteros, Michael Jordan

    2014-01-01

    Trabajos relacionados con valoración de activos financieros, gestión de carteras, mercado de capitales, valoración de activos derivados (opciones y futuros) y su utilización como instrumentos de cobertura.

  9. Fluid evolution of Cerro Colorado Porphyry Copper Mine

    Science.gov (United States)

    Tsang, Debbie Pui Wai; Wallis, Simon

    2014-05-01

    The Cerro Colorado porphyry copper deposit is the northernmost currently active copper mine in Chile, producing 90.5kt copper per year. It belongs to one of the Paleocene to early Eocene porphyry copper deposits that are distributed along the western slope of the main Andean Cordillera in Northern Chile (Bouzari & Clark, 2002). Active commercial production began in 1994, and the estimated reserves within the supergene blanket can sustain further 12 years of copper mining. Field studies of the well-exposed geology around the mine site and the access to drilled cores that penetrate into the hypogene zone provide a good opportunity to study the temporal relationship between magmatism, hypogene and supergene ore formation of the region. The geological evolution of Cerro Colorado area can be generalized as follows. The Cretaceous Cerro Empexa Formation, consisting of a sequence of volcanic rocks, mainly andesitic lava and breccia, lahars, some ignimbrite intercalations and dacitic tuff (Charrier, Pinto & Rodrigues, 2007), was intruded by tonalitic to dioritic magma in Middle-Eocene. Magmatic activities generated brecciated rocks accompanying with different alteration zones radiate outward from the intrusion. The mineralized hypogene protore later interacted with ground water, creating the supergene blanket, which is now the principal mining target of Cerro Colorado. Several plutonic lithologies with slight but distinct compositional differences were exposed in the valleys around the mine site. The presence of these several phases of small-scale intrusions suggests the ore genesis may be related to multiple pulses of heating and associated fluid flow. Complementarily, on-site geologists have reported occurrences of early stage biotites vein cutting into phyllitic alteration zone, or across terminal stage quartz-pyrite veins in the drilled cores. These observations are direct evidences of at least two major distinct phases of fluid flow, and imply the ore mineralization

  10. Mercado de Algeciras

    Directory of Open Access Journals (Sweden)

    Torroja, Eduardo

    1962-02-01

    Full Text Available Siguiendo las líneas generales del Anteproyecto aprobado por el Excmo. Ayuntamiento de Algeciras, se proyectó el nuevo Mercado con una planta octogonal inscrita en el polígono que forman las cuatro calles de contorno. De este modo se obtiene una sala de gran utilización para los puestos de venta, sin rincones difíciles de acceso; y la entrada desde los cuatro lados se obtiene fácilmente, descongestionando así la circulación en los alrededores del Mercado. Esta circulación se facilita, también, con los chaflanes que en las esquinas de las calles presentan cuatro lados del octógono, y que, sin perjudicar a los servicios interiores, permite dar mayor amplitud a las aceras, punto importante dadas las aglomeraciones que suelen producirse en los alrededores de estos mercados en las horas de compra.

  11. Deslumbramientos del mercado

    OpenAIRE

    Monique Selim

    2006-01-01

    Con eje en los diferentes aspectos que adopta el actual proceso de mundialización de la lógica del mercado y expansión capitalista, aún en países socialistas, el presente artículo plantea la necesidad de una reflexión antropológica susceptible de articular el surgimiento de nuevas formas de dominación y representación simbólicas. Se discute el aparente efecto de unificación intelectual producido por la hegemonía del mercado respecto de hechos sociales heterogéneos dados en la historia recient...

  12. Los granitos peraluminosos de las Sierras de Vinquis, Cerro Negro y Zapata (Sierras Pampeanas, provincia de Catamarca, Argentina

    Directory of Open Access Journals (Sweden)

    Medina, M. E.

    1992-12-01

    Full Text Available The studied plutons are close to several batholiths of this region, as Sierra de Mazán and other, but with some mineralogical peculiarities. The magmatic cordierite, common in proximate places, is scarce, as sillimanite, while the andalusite is very rare, with few tourmaline. Fluorite and allanite are also typical accasories only in the granites of the Sierra de Zapata. All plutons are peraluminous of potassic tendency, with cortical affinity.The interpretation of the geochemical values distinguishes between granites of different maturity, emplaced under a predominant influence of active margin for Cerro Negro and Vinquis, while the batholith of Zapata has, below these concepts, a marked feature of within plate.The mineralogical associations suggest that the granites of Cerro Negro and Vinquis were emplaced to pressures of 2 kb or less and temperature of 650º C, while the granites of Zapata had done under conditions of lesser pressure, between 1.5 and 2.0 kb and lower temperature, 600-650º C.A grandes rasgos, los plutones estudiados tienen semejanzas con otros del entorno regional, tal como los de la Sierra de Mazán, pero con peculiaridades mineralógicas. La cordierita magmática, que en lugares próximos es muy abundante, es aquí escasa, al igual que la sillimanita, mientras que la andalucita es muy rara y la turmalina poco frecuente. La fluorita y allanita son accesorios comunes y de cierta abundancia sólo en los granitos de la Sierra de Zapata.Todos los plutones son peralumínicos y de tendencia potásica, con neta afinidad cortical. El estudio estadístico de datos geoquímicos seleccionados, permite diferenciar agrupaciones que tienen un reflejo satisfactorio en los plutones caracterizados, por encima de las variaciones de facies. La interpretación de los valores geoquímicos distingue granitos de desigual madurez, emplazados bajo una influencia predominante de margen activo o intraplaca de características continentales, en

  13. Geohydrology of the Cerro Prieto geothermal aquifer

    Energy Technology Data Exchange (ETDEWEB)

    Sanchez R, J.; de la Pena L, A.

    1981-01-01

    The most recent information on the Cerro Prieto geothermal aquifer is summarized, with special emphasis on the initial production zone where the wells completed in the Alpha aquifer are located. These wells produce steam for power plant units 1 and 2. Brief comments also are made on the Beta aquifer, which underlies the Alpha aquifer in the Cerro Prieto I area and which extends to the east to what is known as the Cerro Prieto II and Cerro Prieto III areas. The location of the area studied is shown. The Alpha and Beta aquifers differ in their mineralogy and cementing mineral composition, temperatures, and piezometric levels. The difference in piezometric levels indicates that there is no local communication between the two aquifers. This situation has been verified by a well interference test, using well E-1 as a producer in the Beta aquifer and well M-46 as the observation well in the Alpha aquifer. No interference between them was observed. Information on the geology, geohydrology, and geochemistry of Cerro Prieto is presented.

  14. ESTUDIO ERGONÓMICO DEL PUESTO DE TRABAJO DE RECOLECTOR DE CÍTRICOS EN LA FINCA "HACIENDA EL CERRO", PERTENECIENTE A LA SOCIEDAD; EXPLOTACIONES EL CERRO S.A.

    OpenAIRE

    Guardado-Moro, José Ramón

    2013-01-01

    El objeto del TFM que me ocupa, está basado en el estudio de una empresa agraria, en concreto una empresa dedicada a la producción de cítricos, dicha empresa se denominada EXPLOTACIONES EL CERRO, S.A., cuyo centro de trabajo recibe el nombre de “finca El Cerro”. Dicha finca está compuesta de 150 hectáreas, todas ellas ocupadas por cítricos de diferentes variedades. Cada una de estas variedades tiene una época de recolección diferente, lo que permite a la empresa sacar fruta al mercado d...

  15. Sedimentary rocks Uranium in Cerro Largo Province

    International Nuclear Information System (INIS)

    With the aim of the uranium minerals exploration has been carried out several studies by UTE technicians in Cerro Largo Province from 1968 to 1969. In uranium concentration has been found pyrite, phosphate, iron oxides and manganese in uranium. Furthermore in La Divisa Ore were studied concentration Uranium enrichment has been studied in La Divisa ore

  16. The Study of enclaves and relative age of plutonic bodies in the Alvand Plutonic complex

    International Nuclear Information System (INIS)

    The study of enclaves and field observations indicate that: The Alvand plutonic complex comprise several plutonic phases with sharp contact and different ages. The older plutonic rocks are composed of gabbro, diorite and tonalites. The porphyroid granites were formed at least in two phases and they are younger than gabbros, diorites and tonalites. The hololeucocratic granitoids were also formed in two phases and they are the youngest plutonic phase in the Alvand plutonic complex. The granitic rocks are magmatic and they are not metasomatic in origin. The porphyroid granites (monzogranites and granodiorites) are S-type (Anatexites). According to radiometric ages and relative ages we believe that mafic plutonism have occurred during pre-middle Cretaceous to Paleocene ages and felsic plutonism have occurred during middle Cretaceouc to Paleocene ages

  17. Deslumbramientos del mercado

    Directory of Open Access Journals (Sweden)

    Monique Selim

    2006-07-01

    Full Text Available Con eje en los diferentes aspectos que adopta el actual proceso de mundialización de la lógica del mercado y expansión capitalista, aún en países socialistas, el presente artículo plantea la necesidad de una reflexión antropológica susceptible de articular el surgimiento de nuevas formas de dominación y representación simbólicas. Se discute el aparente efecto de unificación intelectual producido por la hegemonía del mercado respecto de hechos sociales heterogéneos dados en la historia reciente de las sociedades contemporáneas. Así, la renovada atracción que ejercen los nuevos escenarios sociales reconfigurados en virtud de las modalidades específicas de encarnación y operación de los procesos globalizantes, llama al estudio antropológico de las coyunturas. La autora despliega una interpretación del socialismo de mercado, conjunción -siempre en tensión- de un monopolio político estatal y una liberalización del mercado económico. En esta perspectiva se reubica el interés de una antropología del presente en relevar localmente, en este caso en Vietnam del Norte, la conformación de un nuevo mercado de demandas simbólicas, donde la reaparición de las prácticas culturales de comunicación con los antepasados expresa la necesidad de reunificación familiar y reconciliación con los muertos en la "larga guerra".Tendo como eixo os aspectos diferentes que adota o processo atual de mundialização da lógica do mercado e de expansão capitalista, até mesmo nos países socialistas, este artigo propoe a necessidade de uma reflexão antropológica capaz de articular o aparecimento de novas formas de dominação e de representação simbólica. Discute-se o efeito de superfície de unificação intelectual causado pela hegemonia do mercado em fatos sociais diversos em sociedades contemporâneas. Assim, a atração renovada de novos fatos sociais pelos modos específicos de incorporação e operação de processos de globaliza

  18. Mercado Artes y Oficios

    OpenAIRE

    MIGUEL NOGUERA, ROCIO DE

    2015-01-01

    Proyecto de un mercado de las artes y oficios. Los dos aspectos más importantes son la producción y la exposición, ambos vinculados a la venta. La escuela de artes y oficiose está vinculada a la formación de artistas y, a la vez, a la producción. El proyecto se estructura en tres bandas. La primera de ellas está destinada a la exposición de obras y está vinculada directamente a un antiguo gasómetro, hito preexistente, que se usa como sala polivalente. La segunda banda es la centra...

  19. Genesis of Felsic Plutonic Magmas and Their Igneous Enclaves

    DEFF Research Database (Denmark)

    Clemens, John D.; Maas, Roland; Waight, Tod Earle;

    2016-01-01

    -type Pyalong pluton was emplaced, apparently along an east-west-orientated fracture zone. Around 367 Ma, the main I-type Baynton pluton intruded as numerous shallow-dipping sheets. The last plutonic event was the intrusion of the broad, thin, flat-lying, and crosscutting sheet of the I-type Beauvallet pluton...

  20. Accurate Geodetic Coordinates for Observatories on Cerro Tololo and Cerro Pachon

    CERN Document Server

    Mamajek, Eric E

    2012-01-01

    As the 50th anniversary of the Cerro Tololo Inter-American Observatory (CTIO) draws near, the author was surprised to learn that the published latitude and longitude for CTIO in the Astronomical Almanac and iraf observatory database appears to differ from modern GPS-measured geodetic positions by nearly a kilometer. Surely, the position for CTIO could not be in error after five decades? The source of the discrepancy appears to be due to the ~30" difference between the astronomical and geodetic positions -- a systematic effect due to vertical deflection first reported by Harrington, Mintz Blanco, & Blanco (1972). Since the astronomical position is not necessarily the desired quantity for some calculations, and since the number of facilities on Cerro Tololo and neighboring Cerro Pachon has grown considerably over the years, I decided to measure accurate geodetic positions for all of the observatories and some select landmarks on the two peaks using GPS and Google Earth. Both sets of measurements were inter-...

  1. Petrology and radiogeology of the Stripa pluton

    International Nuclear Information System (INIS)

    Both the quartz monzonite and the metavolcanic leptite which it intruded are strongly fractured. Two stages of fracture filling are evident; an earlier stage encompassing quartz, sericite, feldspar, epidote, and chlorite, and a later stage dominated by carbonate minerals. The Stripa quartz monozite is chemically and mineralogically distinct from other plutons in the region. Muscovite is the predominant mica in the quartz monzonite; biotite has been altered to chlorite, hornblende is absent, and accessory minerals are scarce. In contrast, in other plutons in the Stripa region, biotite and hornblende are prominent mafic minerals and accessory minerals are abundant. The Stripa quartz monzonite is also considerably more radioactive than the the leptite and other plutons in the region. Uranium and thorium abundances are both approx. 30 ppM, considerably higher than in normal granitic rocks where the thorium-to-uranium ratio generally exceeds 2. Potassium-argon dating of muscovite from the Stripa quartz monzonite indicates that this rock may be older, at 1691 million years than granitic rock of the neighboring Gusselby and Kloten massifs, whose ages, based on K-Ar dating of biotite, are respectively 1604 and 1640 m.y. Heat flow and heat productivity considerations show that although Stripa quartz monzonite contains high abundances of radioelements, the pluton has little efect on the regional heat flow. If it occurs in a layered plutonic setting, it is not more than 1.5 km thick; otherwise it may comprise a stock, dike, or border phase that is relatively small compared with the large granitic plutons exposed in the region

  2. Petrology and radiogeology of the Stripa pluton

    Energy Technology Data Exchange (ETDEWEB)

    Wollenberg, H.; Flexser, S.; Andersson, L.

    1980-12-01

    Both the quartz monzonite and the metavolcanic leptite which it intruded are strongly fractured. Two stages of fracture filling are evident; an earlier stage encompassing quartz, sericite, feldspar, epidote, and chlorite, and a later stage dominated by carbonate minerals. The Stripa quartz monozite is chemically and mineralogically distinct from other plutons in the region. Muscovite is the predominant mica in the quartz monzonite; biotite has been altered to chlorite, hornblende is absent, and accessory minerals are scarce. In contrast, in other plutons in the Stripa region, biotite and hornblende are prominent mafic minerals and accessory minerals are abundant. The Stripa quartz monzonite is also considerably more radioactive than the the leptite and other plutons in the region. Uranium and thorium abundances are both approx. 30 ppM, considerably higher than in normal granitic rocks where the thorium-to-uranium ratio generally exceeds 2. Potassium-argon dating of muscovite from the Stripa quartz monzonite indicates that this rock may be older, at 1691 million years than granitic rock of the neighboring Gusselby and Kloten massifs, whose ages, based on K-Ar dating of biotite, are respectively 1604 and 1640 m.y. Heat flow and heat productivity considerations show that although Stripa quartz monzonite contains high abundances of radioelements, the pluton has little efect on the regional heat flow. If it occurs in a layered plutonic setting, it is not more than 1.5 km thick; otherwise it may comprise a stock, dike, or border phase that is relatively small compared with the large granitic plutons exposed in the region.

  3. Accurate Geodetic Coordinates for Observatories on Cerro Tololo and Cerro Pachon

    OpenAIRE

    Mamajek, Eric E.

    2012-01-01

    As the 50th anniversary of the Cerro Tololo Inter-American Observatory (CTIO) draws near, the author was surprised to learn that the published latitude and longitude for CTIO in the Astronomical Almanac and iraf observatory database appears to differ from modern GPS-measured geodetic positions by nearly a kilometer. Surely, the position for CTIO could not be in error after five decades? The source of the discrepancy appears to be due to the ~30" difference between the astronomical and geodeti...

  4. Multiphase groundwater flow near cooling plutons

    Science.gov (United States)

    Hayba, D.O.; Ingebritsen, S.E.

    1997-01-01

    We investigate groundwater flow near cooling plutons with a computer program that can model multiphase flow, temperatures up to 1200??C, thermal pressurization, and temperature-dependent rock properties. A series of experiments examines the effects of host-rock permeability, size and depth of pluton emplacement, single versus multiple intrusions, the influence of a caprock, and the impact of topographically driven groundwater flow. We also reproduce and evaluate some of the pioneering numerical experiments on flow around plutons. Host-rock permeability is the principal factor influencing fluid circulation and heat transfer in hydrothermal systems. The hottest and most steam-rich systems develop where permeability is of the order of 10-15 m2. Temperatures and life spans of systems decrease with increasing permeability. Conduction-dominated systems, in which permeabilities are ???10-16m2, persist longer but exhibit relatively modest increases in near-surface temperatures relative to ambient conditions. Pluton size, emplacement depth, and initial thermal conditions have less influence on hydrothermal circulation patterns but affect the extent of boiling and duration of hydrothermal systems. Topographically driven groundwater flow can significantly alter hydrothermal circulation; however, a low-permeability caprock effectively decouples the topographically and density-driven systems and stabilizes the mixing interface between them thereby defining a likely ore-forming environment.

  5. Petrology and radiogeology of the Stripa pluton

    Energy Technology Data Exchange (ETDEWEB)

    Wollenberg, Harold; Flexser, Steve; Andersson, Lennart

    1980-12-01

    To better define the character of the rock encompassing the thermomechanical and hydrological experiments at the Stripa mine in central Sweden, and to help determine the size of the Stripa pluton, detailed studies were conducted of the petrology and radiogeology of the quartz monzonite and adjacent rocks. Petrologic studies emphasized optical petrography, with supplementary X-ray diffraction, X-ray fluorescence and microprobe analyses. Radiogeologic investigations were based primarily on surface and underground gamma-ray spectrometric measurements of uranium, thorium and potassium, supplemented by laboratory gamma spectrometric analyses and fission-track radiographic determinations of the locations and abundance of uranium in the rock matrix. Both the quartz monzonite and the metavolcanic leptite which it intruded are strongly fractured. Two stages of fracture filling are evident; an earlier stage encompassing quartz, sericite, feldspar, epidote, and chlorite, and a later stage dominated by carbonate minerals. The Stripa quartz monzonite is chemically and mineralogically distinct from other plutons in the region. Muscovite is the predominant mica in the quartz monzonite; biotite has been altered to chlorite, hornblende is absent, and accessory minerals are scarce. In contrast, in other plutons in the Stripa region biotite and hornblende are prominent mafic minerals and accessory minerals are abundant. The Stripa quartz monzonite is also considerably more radioactive than the leptite and other plutons in the region. Uranium and thorium abundances are both- 30 ppm, considerably higher than in "normal" granitic rocks where the thorium-to-uranium ratio generally exceeds 2. Potassium-argon dating of muscovite from the Stripa quartz monzonite indicates that this rock may be older, at 1691 million years than granitic rock of the neighboring Gusselby and Kloten massifs, whose ages, based on K-Ar dating of biotite, are respectively 1604 and 1640 m.y. Heat flow and heat

  6. Optical atmospheric extinction over Cerro Paranal

    CERN Document Server

    Patat, F; O'Brien, K; Pompei, E; Bensby, T; Carraro, G; Postigo, A de Ugarte; Fox, A; Gavignaud, I; James, G; Korhonen, H; Ledoux, C; Randall, S; Sana, H; Smoker, J; Stefl, S; Szeifert, T

    2010-01-01

    Aims: The present study was conducted to determine the optical extinction curve for Cerro Paranal under typical clear-sky observing conditions, with an accuracy of 0.01 mag/airmass. Methods: The extinction curve of Paranal was obtained through low-resolution spectroscopy of 8 spectrophotometric standard stars observed with FORS1 mounted at the 8.2 m Very Large Telescope, covering a spectral range 3300-8000 A. A total of 600 spectra were collected on more than 40 nights distributed over six months, from October 2008 to March 2009. The average extinction curve was derived using a global fit algorithm, which allowed us to simultaneously combine all the available data. The main atmospheric parameters were retrieved using the LBLRTM radiative transfer code, which was also utilised to study the impact of variability of the main molecular bands of O2, O3, and H2O, and to estimate their column densities. Results: In general, the extinction curve of Paranal appears to conform to those derived for other astronomical si...

  7. Evaluation of geologic characteristics at Cerro Prieto

    Energy Technology Data Exchange (ETDEWEB)

    Howard, J.H.; Halfman, S.E.; Vonder Haar, S.P.

    1981-01-01

    Computerized well-log analysis of Cerro Prieto has led to the identification of a relatively large and irregular low-density volume extending from near the surface in the vicinity of Laguna Volcano to greater depths toward the northeast. This low-density volume is located about a plane of symmetry of a self-potential anomaly and a group of northeast trending active faults. The presence of a volume of relatively high-density rock has been recognized at shallow depths in the initially developed part of the resource. It is believed to be due to minerals deposited by cooled, rising geothermal brine. Storativity calculated from well logs at the south end of the western part of the field shows acceptable comparison with storativity calculated from well tests. The amount of fluid produced from the field during the period 1973-1977 is greater than the amount in situ calculated from the completed interval thicknesses. Because this part of the field is still producing today, fluid must be recharging this part of the field.

  8. Correct nomenclature for the Angadimogar pluton, Kerala, southwestern India

    Indian Academy of Sciences (India)

    H M Rajesh

    2006-04-01

    The proper usage of modal composition and geochemical classification of granitoids is discussed for assigning a proper nomenclature for the Angadimogar pluton,Kerala,southwestern India.This discussion is mainly aimed at addressing questions concerning the nomenclature of Angadimogar pluton (syenite vs. granite).Modal composition and whole-rock XRD data clearly show that the pluton exposed near Angadimogar is a quartz-syenite and its geochemistry is typical of a ferroan, metaluminous,alkali (A-type)granitoid.

  9. Hacer Mercado en una Lógica de Mercado. Las Dimensiones Culturales del Mercado en la Plaza de Mercado de Mesitas del Colegio.

    OpenAIRE

    Hurtado Suaréz, Christian Camilo

    2013-01-01

    Esta investigación desnaturaliza el mercado como concepto económico al abordarlo como fenómeno social. Para ello indagamos ¿Cuáles son las dimensiones culturales del mercado en la plaza de mercado de Mesitas del colegio?; dicha pregunta lleva implícita una postura: lo que entendemos como mercado, el concepto de la ciencia económica, ¿es susceptible de ser analizado en tanto fenómeno social y no solo como fenómeno económico? ¿Qué alcances explicativos tiene introducir otras d...

  10. Herpetofauna del Cerro Guiengola, Istmo de Tehuantepec, Oaxaca

    OpenAIRE

    Cintia Natalia Martín-Regalado; Rosa Ma. Gómez-Ugalde; Ma. Emma Cisneros-Palacios

    2011-01-01

    Este estudio se realizó en el Cerro Guiengola, Tehuantepec, Oaxaca, con el objetivo de contribuir al conocimiento de la herpetofauna en dicha área. Se obtuvieron 602 registros visuales y se recolectaron 103 ejemplares de anfibios y reptiles durante 60 días de trabajo de campo. Se enlistan 40 especies, pertenecientes a 33 géneros y 18 familias. Se determinó la distribución de la herpetofauna en el Cerro Guiengola por microhábitat, tipo de vegetación y altitud. Usando el método de Jaccard se el...

  11. Petrological studies of plutonic rocks of Ecuador

    International Nuclear Information System (INIS)

    The feldspars of many tonalitic plutonic rocks in the coastal regions and West Andean regions are zoned. This leads to the conclusion that they are relatively flat intrusions and to some extent transition rocks in the subvulcanite direction. This is in accordance with the genetic and chronological relationship between plutonites and the surrounding vulcanites of the Basic Igreous Complex (BIC). The composition of representative minerals, e.g. alkali feldspar, plagioclase feldspar, biotite, chlorite, and amphibole has been determined as well as the age of plutonite samples by the K/Ar dating method. (DG)

  12. Report of boring made in the South of Cerro Largo district (Cerro Largo) 1977-1978

    International Nuclear Information System (INIS)

    The present work are within the framework and compiles the data obtained by means of the study of the perforations executed in the District Cerro Largo Sur of the detailed prospection of uranium minerals. This study was carried out by technicians of Geologic ex--Institute of Uruguay (IGU) - at the moment National Direction of Mining and Geology. (DINAMIGE). The works began at the beginning of 1977 and continued until 1978 July; The headquarters of the program of prospection of uranium was carried out by Ing. Hector Goso. In this report the conclusions drawn at the time of the detection of the works in the District already published, as well as the litologicos cuts of all the executed perforations are included

  13. EL CERRO DE POTOSÍ Y EL DIOS PACHACÁMAC THE CERRO DE POTOSÍ AND THE PACHACÁMAC GOD

    OpenAIRE

    Teresa Gisbert

    2010-01-01

    En este trabajo se plantea que el Cerro de Potosí se ocultó a los españoles por ser el santuario más importante de la región, el cual estaba dedicado al dios Pachacámac. Los testimonios que indican que el cerro de Potosí era "Apu" (Cerro o Señor) adorado son abundantes, pero es el cronista Arzans de Orsúa y Vela (año 1736) quien dice que este "Apu" pertenecía a Pachacámac, dios del mundo subterráneo. Una tradición recogida cerca del salar de Uyuni dice lo mismo; finalmente un sacrificio reali...

  14. El Mercado Europeo de Electricidad

    OpenAIRE

    Vélez Alvarez, Luis Guillermo

    2012-01-01

    En este artículo se presenta el proceso de construcción del mercado interior a partir del análisis de las tres Directivas comunitarias que lo han impulsado. Para las dos primeras - Directiva 96/92 EC y Directiva 03/54 EC – se describe la situación del sector anterior a su promulgación, se analiza el contenido de cada una de ellas y, finalmente, se presentan los resultados de su aplicación Por razones obvias, de la tercera Directiva y de los Reglamentos que la acompañan - Directiva 09/72 EC ...

  15. Mercado cultural RE-ciclaje

    OpenAIRE

    Córcoles Martínez, Marta

    2013-01-01

    Proyecto de mercado cultural en la antigua fábrica de Gas Lebón de Valencia. El proyecto se adapta al lugar, reutilizando el antiguo gasómetro que prevalece en la parcela. El programa incluye comercios, dotaciones culturales, espacios de exposición, salas polivalentes, zonas de gestión y administración, almacén, aparcamiento, etc. Dada la baja edificabilidad, el edificio se plantea enterrado o parcialmente enterrado. Puede extenderse a la parcela contigua (actualmente desocupada) siempre que ...

  16. Los cuerpos ígneos neógenos del cerro de Las Minas (35,3°S - 69,9°O, Cordillera Principal de los Andes, SO de Mendoza: geología, petrografía y geoquímica The Neogene igneous bodies of the Cerro de las Minas (35.3°S-69.9°W, Main Cordillera of the Andes, SW of Mendoza: geology, petrography and geochemistry

    Directory of Open Access Journals (Sweden)

    M.J. Pons

    2007-06-01

    Full Text Available El cerro de Las Minas (35,3°S - 69,9°O consiste en cuatro unidades ígneas epizonales: plutón diorítico-tonalítico, plutón granodiorítico, plutón granítico y diques -filones capa andesíticos. Estas unidades forman parte del arco magmático neógeno del SO de Mendoza correspondiente a la Andesita Huincán. Intruyen a rocas sedimentarias jurásicas de las Formaciones Puchenque y Auquilco y las que en las cercanías del contacto con los plutones diorítico y granítico, están modificadas a hornfels, calizas recristalizadas y skarns bandeados con mineralización de Fe. Geoquímicamente, constituyen un conjunto de plutones cogenéticos de amplio rango composicional, metaluminosos, subalcalinos con afinidad calcoalcalina y del tipo I, características que son semejantes a las de otros plutones de márgenes convergentes vinculados a skarns de Fe. Han evolucionado por cristalización fraccionada de sus componentes minerales principales (plagioclasa-piroxeno-anfíbol-magnetita-titanita y mezcla localizada entre los magmas diorítico y granodiorítico. Sus patrones de elementos trazas incompatibles y tierras raras son similares a los observados en las rocas ígneas: a del arco volcánico neógeno (Andesita Huincán, b vinculadas a otros skarns de Fe del SO de Mendoza (Hierro Indio y El Kaiser, c del cerro Nevazón (37,5°S perteneciente al arco volcánico paleógeno del NO de Neuquén y, finalmente, d del arco volcánico cuaternario de un sector de la zona volcánica sur (TSVZ (34,5°-37°S de los Andes, emplazados en una corteza continental relativamente delgada (35-50 km. Esto sugiere que las rocas ígneas del cerro de las Minas se formaron a partir de magmas parentales calcoalcalinos y metaluminosos, derivados de una fuente mantélica similar, con escasez o ausencia de granate residual en la fuente.The cerro de las Minas (35.3°S-69.9°W consists of four epizonal igneous units: diorite-tonalite, granodiorite and granite plutons and andesite

  17. EL CERRO DE POTOSÍ Y EL DIOS PACHACÁMAC THE CERRO DE POTOSÍ AND THE PACHACÁMAC GOD

    Directory of Open Access Journals (Sweden)

    Teresa Gisbert

    2010-06-01

    Full Text Available En este trabajo se plantea que el Cerro de Potosí se ocultó a los españoles por ser el santuario más importante de la región, el cual estaba dedicado al dios Pachacámac. Los testimonios que indican que el cerro de Potosí era "Apu" (Cerro o Señor adorado son abundantes, pero es el cronista Arzans de Orsúa y Vela (año 1736 quien dice que este "Apu" pertenecía a Pachacámac, dios del mundo subterráneo. Una tradición recogida cerca del salar de Uyuni dice lo mismo; finalmente un sacrificio realizado en el siglo XVI a orillas del lago Titicaca en honor a Pachacámac, muestra la presencia de este dios en el Collasuyo. Cuando los incas llegaron a Potosí introdujeron el culto al Sol y cuando llegaron los españoles identificaron el cerro con la Virgen María la cual, a su vez, se identificó con la Pachamama o Madre Tierra.In this essay it is argued that "Cerro de Potosf' was hidden from the Spanish conquerors because it was the region's most important huaca or sanctuary, due to the fact that it was dedicated to the god Pachacámac. Abundant testimonies (colonial documents indicate that "Cerro de Potosf was a worshipped "Apu" (Mountain, Señor or Lord, nevertheless chronicler Orzans de Orsúa y Vela (1736 stated that this "Apu" belonged to Pachacámac, god of the underworld. A tradition collected near the Salar de Uyuni states the same; finally, a sacrifice in honor of Pachacámac that occurred during the 16th century on the shores of Lake Titicaca, shows the presence of this god in the Collasuyo. When the Incas reached Potosí, they introduced worship of the Sun, and when the Spanish conquerors arrived, they identified the "Cerro de Potosf with the Virgin Mary which at the same time was identified with Pachamama or Mother Earth.

  18. A statistical approach to the volcanic-plutonic connection

    Science.gov (United States)

    Schoene, B.; Keller, C.; Samperton, K. M.; Barboni, M.; Husson, J. M.

    2013-12-01

    The geochemical relationship between volcanic and plutonic rocks - whether the two are geochemically identical, or if the choice between eruption or intrusion is correlated with magma chemistry - represents a major unanswered question in igneous petrology. In one endmember scenario, felsic to intermediate plutons represent the unerupted residue from which crystal-poor eruptible melts are extracted. At the other end of the spectrum, it is argued that a nearly the entire volume of magma is evacuated during eruption, and that the probability of eruption versus intrusion is instead largely a function of magma flux. In the first scenario, parental magmas originating at depth experience substantial fractionation during volcanic melt extraction, leading to complementary volcanic and plutonic reservoirs. In the second endmember scenario, volcanic/plutonic fractionation in the middle to upper crust is negligible, predicting no geochemical difference between volcanic and plutonic rocks. A third endmember scenario that is not exclusive from the other two predicts differences between volcanic and plutonic rocks if geochemical characteristics are correlated with the eventual eruptibility of magma. Deciphering the relative importance of each of these models is important for understanding both the long-term geochemical balance of the crust and mantle due to increased erosion and recycling of volcanic rocks and also for understanding magma transport dynamics. We have compared the geochemistry of ~500,000 volcanic and plutonic rocks from a range of tectonic settings by Monte Carlo bootstrap analysis in order to produce maximally representative average compositions. The results indicate that while volcanic and plutonic rocks in general show remarkably similar major element trends, intermediate to felsic plutonic rocks, for a given silica content, display clear enrichments in Sr and Ba and depletions in Zr, Hf, and HREEs relative to their volcanic equivalents. More subtly

  19. Criteria for determining casing depth in Cerro Prieto

    Energy Technology Data Exchange (ETDEWEB)

    Olivas M., H.M.; Vaca S., J.M.E.

    1982-08-10

    On the basis of geological data obtained during drilling and its relation to electric logs, together with the problems that arose when drilling through formations until the production zone was reached, it is possible to establish the most suitable manner to line a well and thus formulate an optimum casings program. The main criteria to be taken into consideration in preparing such a program and its application in the drilling of wells programmed in Cerro Prieto to optimize and economize such drilling and achieve suitable techniques for well completion are presented. The criteria are based on the characteristics of the Cerro Prieto field and on casing design factors, as well as a experience gained during drilling in such a field.

  20. Abordagem comportamental e investimento racional no mercado cambial: o caso do mercado forex

    OpenAIRE

    Campos, Paulo Jorge Fonseca

    2010-01-01

    O mercado Forex é um mercado financeiro muito atractivo. Esta alta atractividade justifica-se pela correlação entre o nível de investimento e a possibilidade de elevados ganhos. Por isso, o nível de risco também é muito elevado. O comportamento do investidor é um dos factores principais para se ter sucesso neste mercado. A impulsividade, geralmente, é o mote para o fracasso, e fracassar neste mercado, normalmente, é sinónimo de grandes perdas financeiras. Ao investir é preci...

  1. The Cerro LOS Calvos and La Banderia chondrites

    Science.gov (United States)

    Whitlock, Randall; Lewis, Charles F.; Clark, James C.; Moore, Carleton B.

    1991-06-01

    The Cerro los Calvos meteorite is a single stone of 68.5 g found in the Nuevo Mercurio strewn field of Zacatecas, (Mexico). It is an unusual H4 chondrite. Its olivine (Fa12.5) and orthopyroxene (Fs 11.7, Wo 0.8) are reduced relative to typical H chondrites. The La Banderia meteorite of 54.3 g from the same vicinity is an LL5 chondrite of shock classification e.

  2. Current state of the hydrothermal geochemistry studies at Cerro Prieto

    Energy Technology Data Exchange (ETDEWEB)

    Fausto L, J.J.; Jimenez S, M.E.; Esquer P, I.

    1981-01-01

    The current state of hydrothermal geochemistry studies being carried out at the field are reported. These studies are based on the results of chemical analysis of water samples collected during 1979 and 1980 at the geothermal wells of the area known as Cerro Prieto I, as well as from those located in the Cerro Prieto II and Cerro Prieto III areas, some of which have only recently started flowing. Data are presented on the chemical variations of the main chemical constituents dissolved in the waters, as well as on the Na/K and Na-K-Ca chemical relations and the temperatures calculated from them and from SiO/sub 2/. Fluid recharge into the reservoir and its direction of flow are interpreted from isotherm contour maps of the field prepared from Na/K and Na-K-Ca geothermometry and from concentration contour maps of some of the main chemical constituents. Well M-43 is discussed as an example of a well affected by well completion problems in its production casing. Its behavior is explained on the basis of the chemical characteristics of the produced water. The chemical changes that have taken place in some of the wells during production are explained by correlating the chemistry with the production mechanisms of the well (steam-water production rates).

  3. Geophysical modeling and structure of Ushuaia Pluton, Fuegian Andes, Argentina

    Science.gov (United States)

    Peroni, Javier Ignacio; Tassone, Alejandro Alberto; Menichetti, Marco; Cerredo, María Elena

    2009-10-01

    Within the area of Ushuaia Bay (Tierra del Fuego, southernmost South America) the deformed Lower Cretaceous sedimentary rocks of Yahgán Formation host the Ushuaia Pluton. The intrusive body is oval in map view; it is compositionally varied with rocks ranging from the ultrabasic to the mesosiliceous realm. The emplacement time is constrained within the Albian-Cenomanian span by new amphibole K/Ar data. Meso- and microstructures of Ushuaia Pluton and its host indicate a synkinematic emplacement with a dominant extensional component. A set of transcurrent and normal faults related to the sinistral strike-slip Beagle Channel Fault System affects the pluton and its host. On the basis of aeromagnetic data combined with field information, a new model is presented for the Ushuaia Pluton. Modeling results fit well with a laccolithic body with an estimated volume of around 111 km 3. The model pluton cross-section displays a central zone with an average thickness of 2000 m which progressively thins toward the margins (˜ 500 m) and a southern root which reaches 5000 m deep. The combined structural and geophysical model supports a transtensive scenario for the Ushuaia Pluton emplacement at Early-Late Cretaceous boundary.

  4. Petrology of the Plutonic Rocks of west-central Alaska

    Science.gov (United States)

    Miller, Thomas P.

    1970-01-01

    A series of plutons in west-central Alaska defines the Hogatza plutonic belt which extends for about 200 miles in an east-west direction from the northeastern Seward Peninsula to the Koyukuk River. The plutonic rocks have an aggregate area of about 1,200 square miles and their composition, distribution, and possible petrogenesis are discussed for the first time in this report. Field, petrographic and chemical data supported by K/Ar age dating indicate the plutonic rocks are divisible into two suites differing in age, location, and composition. The western plutons are mid-Cretaceous (~100 m.y.) in age and consist of a heterogeneous assemblage of monzonite, syenite, quartz monzonite. Associated with these granitic rocks is a group of alkaline sub-silicic rocks that forma belt of intrusive complexes extending for a distance of at least 180 miles from west-central Alaska to the Bering Sea. The complex at Granite Mountain shows a rare example of zoning from an alkaline rim to a quartz-bearing core. The occurrence of a similar complex at Cape Dezhnev on the easternmost tip of Siberia suggests the alkaline province may extend into Siberia. The easternmost plutons are Late Cretaceous (180 m.y.) in age and composed primarily of granodiorite and quartz monzonite similar to calc-alkaline plutons found throughout the North America Cordillera. The plutons are epizonal and intrude deformed but unmetamorphosed Lower Cretaceous andesitic volcanics and volcanic graywacke which constitute the highly mobile Yukon-Koyukuk volcanogenic province of west-central Alaska. No older rocks have been found within the confines of this vast tract; the occurrence of a bounding ophiolite sequence has lead to the suggestion that the province was formed by large-scale rifting and is underlain by oceanic crust. The possibility of no juvenile sialic crust over much of the area suggests that the potassium-rich magma now represented by the alkaline rocks originated in the mantle. The distribution of the

  5. Atmospheric conditions at Cerro Armazones derived from astronomical data

    Science.gov (United States)

    Lakićević, Maša; Kimeswenger, Stefan; Noll, Stefan; Kausch, Wolfgang; Unterguggenberger, Stefanie; Kerber, Florian

    2016-04-01

    Aims: We studied the precipitable water vapour (PWV) content near Cerro Armazones and discuss the potential use of our technique of modelling the telluric absorbtion lines for the investigation of other molecular layers. The site is designated for the European Extremely Large Telescope (E-ELT) and the nearby planned site for the Čerenkov Telescope Array (CTA). Methods: Spectroscopic data from the Bochum Echelle Spectroscopic Observer (BESO) instrument were investigated by using a line-by-line radiative transfer model (LBLRTM) for the Earth's atmosphere with the telluric absorption correction tool molecfit. All observations from the archive in the period from December 2008 to the end of 2014 were investigated. The dataset completely covers the El Niño event registered in the period 2009-2010. Models of the 3D Global Data Assimilation System (GDAS) were used for further comparison. Moreover, we present a direct comparison for those days for which data from a similar study with VLT/X-Shooter and microwave radiometer LHATPRO at Cerro Paranal are available. Results: This analysis shows that the site has systematically lower PWV values, even after accounting for the decrease in PWV expected from the higher altitude of the site with respect to Cerro Paranal, using the average atmosphere found with radiosondes. We found that GDAS data are not a suitable basis for predicting local atmospheric conditions - they usually systematically overestimate the PWV values. The large sample furthermore enabled us to characterize the site with respect to symmetry across the sky and variation with the years and within the seasons. This technique of studying the atmospheric conditions is shown to be a promising step into a possible monitoring equipment for the CTA. Based on archival observations collected at the European Organisation for Astronomical Research in the Southern Hemisphere, Chile and of the Cerro Armazones Observatory facilities of the Ruhr Universität Bochum.Full Table 1

  6. Report of the Cerro Chato ultrabasic geophysical studies

    International Nuclear Information System (INIS)

    This report refers to the obtained results of geophysical practiced during the year 1985 in the area of the ultrabasic of Cerro Chato, located in the area called Puntas del Malbajar in Durazno province. The aim was rehearsed an answer of an ultrabasic behaviour of the geophysical prospecting methods.They were carried out studies in magnetometry, induced polarization, electromagnetism and resistivity measurements in electric vertical sound. As well conclusions as recommendations express that applied geophysical methods allow to make ultrabasic charts or maps.

  7. en el mercado de Estados Unidos

    Directory of Open Access Journals (Sweden)

    Nadima Simón Domínguez

    2004-01-01

    Full Text Available El objetivo de este artículo es analizar el comportamiento de las exportaciones del sector de prendas de vestir (de tejido de punto y de tejido plano en el mercado de Estados Unidos (EUA durante el periodo de 1990 a 2002. Se identifican los principales competidores, las características de ambos mercados y los instrumentos de política comercial utilizados por las empresas estadounidenses para la protección de su industria textil. De igual forma, se hace un análisis de los principales productos de prendas de vestir que nuestro país exportó a EUA clasificándolos por su participación en el mercado de dicho país y por el dinamismo que presentan éstos. También se identifican los factores que inciden en la participación de México en el mercado estadounidense. Se concluye que México incrementó considerablemente sus exportaciones de prendas de vestir a EUA después de la entrada en vigor del TLCAN y de la devaluación del peso mexicano de diciembre de 1994. México es líder en el mercado de aquel país en camisas de algodón y en pantalones de mezclilla, seguido muy de cerca por China. Para mantener la participación de las prendas de vestir de México en dicho mercado, nuestra industria del vestido debe orientarse a la fabricación de paquete completo y de productos de moda con mayor valor agregado.

  8. Survey of lunar plutonic and granulitic lithic fragments

    Science.gov (United States)

    Bickel, C. E.; Warner, J. L.

    1978-01-01

    A catalog of lunar plutonic rocks and granulitic impactites belonging to the ANT suite has been compiled. The coarser-grained, plutonic rocks in the compilation are probably pristine; they belong to two groups, Mg-rich plutonic rocks and anorthosites, with a preponderance of the latter type. The granulitic impactites, however, have bulk and mineral compositions that fall between the two groups defined by the pristine nonmare samples of Warren and Wasson (1977). Thus the granulitic impactites may have originated by metamorphism of mixed impactites in early breccia sheets. The catalog, representative of the lunar crust before the end of heavy bombardment, suggests a crust with over 78 vol. % plagioclase and about equal proportions of material with noritic and troctolitic affinity.

  9. Soberania Alimentar, agroecologia e mercados locais.

    OpenAIRE

    Meirelles, Laércio

    2004-01-01

    A Rede Ecovida tem estimulado a construção de uma Rede Solidária de Produção e Circulação de Produtos Ecológicos nos estados do Paraná, de Santa Catarina e do Rio Grande do Sul, cujas células de comercialização são feiras livres, cooperativas de consumidores, mercados institucionais, pontos de abastecimento popular, pequenas lojas e comerciantes. Essa iniciativa é mais uma demonstração que práticas agroecológicas, associadas a mercados locais, trazem impactos positivos à Soberania Alimentar d...

  10. Mercado laboral y reformas en Bolivia

    OpenAIRE

    Muriel H., Beatriz; Jemio M., Luis Carlos

    2010-01-01

    El estudio presenta un panorama de las reformas sociales y económicas implementadas en Bolivia desde 1985, en su relación e incidencia con el funcionamiento del mercado de trabajo. Inicialmente, se destaca la efectividad de las llamadas Reformas Estructurales, aplicadas durante 1985-2005, en la generación de la estabilidad macroeconómica; en la captación de inversión extranjera directa, en la apertura de mercados y en la disminución de la pobreza (medida por Necesidades Básicas Insatisfechas)...

  11. Periodistas: el acceso al mercado laboral

    OpenAIRE

    2006-01-01

    El presente estudio analiza la situación profesional de los Licenciados en Periodismo en España. Para ello esta investigación sigue la lógica del proceso de acceso al mercado laboral, es decir, se estudia, en primer lugar, la oferta de egresados y las demandas del sector; a continuación, se analiza la forma en la que un titulado en la Licenciatura de Periodismo accede al mercado laboral y el tiempo que tarda en hacerlo; y por último, se examinan los medios de comunicación en lo...

  12. Hydrocarbons emissions from Cerro Prieto Geothermal Power Plant, Mexico

    Science.gov (United States)

    Navarro, Karina; Navarro-González, Rafael; de la Rosa, José; Peralta, Oscar; Castro, Telma; Imaz, Mireya

    2014-05-01

    One of the most important environmental issues related to the use of geothermal fluids to generate electricity is the emission of non-condensable gases to the atmosphere. Mexico has one of the largest geothermal plants in the world. The facility is located at Cerro Prieto, Baja California, roughly 30 km south of Mexicali and the international boundary between Mexico and United States. The Cerro Prieto power plant has 13 units grouped on four individual powerhouses. Gas samples from 9 units of the four powerhouses were collected during 4 campaigns conducted in May-July, 2010, February, 2012, December, 2012, and May, 2013. Gas samples from the stacks were collected in 1000 ml Pyrex round flasks with Teflon stopcocks, and analyzed by gas chromatography-mass spectrometry. Methane was the most abundant aliphatic hydrocarbon, with a concentration that ranged from less than 1% up to 3.5% of the total gas mixture. Normal alkanes represented the second most abundant species, and displayed a decreasing abundance with increasing carbon number in the homologous series. Isoalkanes were also present as isobutane and isopentane. Cycloalkanes occurring as cyclopentane and cyclohexane, were detected only at trace level. Unsaturated hydrocarbons (alkenes and alkynes) were not detected. Benzene was detected at levels ranging from less than 1% up to 3.4% of the total gas mixture. Other aromatic hydrocarbons detected were toluene, and xylenes, and were present at lower concentrations (

  13. Characterization of pottery from Cerro de Las Ventanas, Zacatecas, Mexico

    International Nuclear Information System (INIS)

    With the aim of classifying prehispanic pottery from Cerro de Las Ventanas site, Juchipila, Zacatecas, Mexico, instrumental neutron activation analysis (INAA) was used to analyze ceramic samples at the University of Missouri Research Reactor Center. Thirty-two chemical elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Two multivariate statistical methods, cluster analysis and principal component analysis, were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Mesoamerican ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Malpaso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de Las Ventanas represent a new and unique chemical fingerprint in the region. (orig.)

  14. Characterization of pottery from Cerro de Las Ventanas, Zacatecas, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Lopez-del-Rio, H.; Mireles-Garcia, F. [Unidad Academica de Estudios Nucleares, UAZ, Zacatecas (Mexico); Mendez-Cardona, R.Y. [Unidad Academica de Antropologia, UAZ, Zacatecas (Mexico); Nicolas-Caretta, M. [INAH Delegacion Zacatecas (Mexico); Coordinacion de Ciencias Sociales y Humanidades, UASLP, Fracc. Talleres, SLP (Mexico); Speakman, R.J. [Museum Conservation Inst., Smithsonian Institution, Suitland, MD (United States); Glascock, M.D. [Research Reactor Center, Univ. of Missouri, Columbia, MO (United States)

    2009-09-15

    With the aim of classifying prehispanic pottery from Cerro de Las Ventanas site, Juchipila, Zacatecas, Mexico, instrumental neutron activation analysis (INAA) was used to analyze ceramic samples at the University of Missouri Research Reactor Center. Thirty-two chemical elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Two multivariate statistical methods, cluster analysis and principal component analysis, were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Mesoamerican ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Malpaso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de Las Ventanas represent a new and unique chemical fingerprint in the region. (orig.)

  15. Redes sociales y mercado de trabajo.

    OpenAIRE

    García Faroldi, Livia

    2007-01-01

    Reseña: Requena Santos, F. (1991). Redes sociales y mercado de trabajo. Elementos para una teoría del capital relacional. Madrid: Centro de Investigaciones Sociológicas, Colección Monografías, nº 119.

  16. Redes sociales y mercado de trabajo.

    Directory of Open Access Journals (Sweden)

    García Faroldi, Livia

    2007-12-01

    Full Text Available Reseña: Requena Santos, F. (1991. Redes sociales y mercado de trabajo. Elementos para una teoría del capital relacional. Madrid: Centro de Investigaciones Sociológicas, Colección Monografías, nº 119.

  17. Estrategias de mercado para el frijol centroamericano

    Directory of Open Access Journals (Sweden)

    Lourdes Mart\\u00EDnez

    2004-01-01

    Full Text Available Estrategias de mercado para el frijol centroamericano. En los últimos años, el sub-sector de frijol en Centro América ha sido testigo de varios cambios dinámicos. Si no se encuentran medidas para incrementar la competitividad regional de este sub-sector, los países centroamericanos experimentarán impactos negativos en las áreas sociales y económicas de considerable magnitud, especialmente ahora que Centro América necesita ajustar su economía a los nuevos requerimientos de mercados mas abiertos, como el Tratado Centroamericano de Libre Comercio con USA (TLC. Vendedores de frijoles a nivel intermediario y de consumo final, así como técnicos de oficinas gubernamentales dedicadas al mercadeo de frijoles en Centro América fueron entrevistados para documentar los cambios experimentados, identificar los obstáculos que frenan la viabilidad del sub-sector e identificar las oportunidades de incremento de mercados en el futuro para los productores y vendedores de frijol. Los resultados muestran que para que continúen siendo competitivos, los países centroamericanos deben incrementar la productividad a través del apoyo a las investigaciones para el mejoramiento de variedades de frijol, especialmente aquellas que los consumidores prefieren por características específicas (e.g. color. También es imprescindible el fortalecimiento de los programas de distribución de variedades mejoradas a los productores; las mejoras en la transmisión de información de mercado a los productores; el fortalecimiento de los contactos entre productores, comercializadores a nivel mayorista y supermercados; y una política más específica de apertura de mercados de exportación, especialmente con los Estados Unidos.

  18. Amphiboles of the Khibiny alkaline pluton, Kola Peninsula, Russia

    Science.gov (United States)

    Konopleva, N. G.; Ivanyuk, G. Yu.; Pakhomovsky, Ya. A.; Yakovenchuk, V. N.; Men'shikov, Yu. P.; Korchak, Yu. A.

    2008-12-01

    The rocks of the Khibiny pluton contain 25 amphibole varieties, including edenite, fluoredenite, kaersutite, pargasite, ferropargasite, hastingsite, magnesiohastingsite, katophorite, ferrikatophorite, magnesiokatophorite, magnesioferrikatophorite, magnesioferrifluorkatophorite, ferrimagnesiotaramite, ferrorichterite, potassium ferrorichterite, richterite, potassium richterite, potassium fluorrichterite, arfvedsonite, potassium arfvedsonite, magnesioarfvedsonite, magnesioriebeckite, ferriferronyboite, ferrinyboite, and ferroeckermannite. The composition of rock-forming amphiboles changes symmetrically relative to the Central Ring of the pluton; i.e., amphiboles enriched in K, Ca, Mg, and Si are typical of foyaite near and within the Central Ring. The Fe and Mn contents in amphiboles increase in the direction from marginal part of the pluton to its center. Foyaite of the marginal zone contains ferroeckermannite, richterite, arfvedsonite, and ferrorichterite; edenite is typical of foyaite and hornfels of the Minor Arc. Between the Minor Arc and the Central Ring, foyaite contains ferroeckermannite, arfvedsonite, and richterite; amphiboles in rischorrite, foidolite and hornfels of the Central Ring are (potassium) arfvedsonite, (potassium) richterite, magnesiokatophorite, magnesioarfvedsonite, ferroeckermannite, and ferriferronyboite; amphiboles in foyaite within the Central Ring, in the central part of the pluton, are arfvedsonite, magnesioarfvedsonite, ferriferronyboite, katophorite, and richterite. It is suggested that such zoning formed due to the alteration of foyaite by a foidolite melt intruded into the Main (Central) Ring Fault.

  19. O MARKETING ORIENTADO PELO MERCADO

    Directory of Open Access Journals (Sweden)

    Sandro Deretti

    2005-11-01

    -style-type:export-only; mso-default-props:yes; font-size:10.0pt; mso-ansi-font-size:10.0pt; mso-bidi-font-size:10.0pt;} @page Section1 {size:612.0pt 792.0pt; margin:70.85pt 3.0cm 70.85pt 3.0cm; mso-header-margin:36.0pt; mso-footer-margin:36.0pt; mso-paper-source:0;} div.Section1 {page:Section1;} -->

    Resumo

    A economia globalizada determinou alterações profundas no processo estratégico das empresas, propiciando oportunidades e ameaças em todos os segmentos e exigindo produtos e serviços competitivos. Assim, diante deste cenário extremamente desafiador, a função marketing dentro das empresas assume maior importância no desenvolvimento de vantagens competitivas sustentáveis e na redução das incertezas. Muitos autores consideram que a orientação para o mercado seja a essência da filosofia empresarial que leva ao sucesso nesta luta pelos mercados porque investiga desejos e necessidades do consumidor. Este artigo faz uma contextualização dos principais trabalhos que colaboraram para a estruturação do conceito de marketing e da orientação para o mercado.

     

  20. Progress on the biphase turbine at Cerro Prieto

    Energy Technology Data Exchange (ETDEWEB)

    Cerini, D.; Hays, L.; Studhalter, W. [Douglas Energy Company, Placentia, CA (United States)

    1997-12-31

    The status of a Biphase turbine power plant being installed at the Cerro Prieto geothermal field is presented. The major modules for the power plant are completed except for a back pressure steam turbine. The power plant will be started in April 1997 with the Biphase turbine alone followed by the addition of the steam turbine module two months later. The current power plant performance level is 2780 kWe due to a decline in the well. An increase in power output to 4060 kWe by adding the flow from another well is planned. The addition of five Biphase power plants with a total power output of 21.2 megawatts is described.

  1. Properties of Cerro Prieto rock at simulated in situ conditions

    Energy Technology Data Exchange (ETDEWEB)

    Schatz, J.F.

    1981-01-01

    Rocks from the Cerro Prieto Geothermal Field were tested under simulated in situ conditions in the laboratory to determine their properties and response to pore pressure reduction as would be caused by reservoir production. The primary purpose of the project was to provide information on compaction and creep as they may contribute to surface subsidence. Results show typical compressibilities for reservoir rocks of about 1 x 10/sup -6/ psi/sup -1/ and creep compaction rates of about 1 x 10/sup -9/ sec/sup -1/ when triggered by 1000 psi pore pressure reduction. This creep rate would cause significant porosity reduction if it continued for several years. Therefore it becomes important to learn how to correctly extrapolate such data to long times.

  2. Results from two years of resistivity monitoring at Cerro Prieto

    Energy Technology Data Exchange (ETDEWEB)

    Wilt, M.J.; Goldstein, N.E.

    1981-01-01

    Dipole-dipole resistivity measurements for the combined purposes of reservoir delineation and resistivity monitoring were first made at Cerro Prieto in 1978 and have continued on an annual basis since then. Two 20 km long dipole-dipole lines with permanently emplaced electrodes at one kilometer spacings were established over the field area; one of these lines is remeasured annually. Resistivity measurements are taken using a 25 kW generator capable of up to 80A output and a microprocessor controlled signal averaging receiver; this high power-low noise system is capable of highly accurate measurements even at large transmitter-receiver separations. Standard error calculations for collected data indicate errors less than 5% for all points, but 95% confidence intervals show error limits about 2 to 4 times higher. Analysis of collected data indicate little change in the apparent resistivity of the upper 300 m over the field production zone and that in this section measurements are relatively insensitive to the annual rainfall cycle. Apparent resistivity increases were observed over the older producing zone at Cerro Prieto at depths of 1 km and greater. Large zones of decreasing apparent resistivity were observed flanking the zone of increases on both sides. The increase in apparent resistivity in the production region may be due to an increasing fraction of steam in the reservoir resulting from a production related decline in reservoir pressure. Alternatively the increases may be the result of fresh water influx from the Colorado River. The zone of declining resistivity flanking the area of increase may be due to the movement of saline waters into the reservoir region as a result of the pressure decline. Quantitative modeling of observed changes is impractical owing to the high uncertainty in estimating apparent resistivity changes and the nonuniqueness of models.

  3. Isotopic character of Cambro-Ordovician plutonism, southern Victoria Land

    International Nuclear Information System (INIS)

    Previous mapping of granitoid rocks in the Dry Valleys area of southern Victoria Land, Antarctica, identified the calc-alkaline (DV1a), adakitic (DV1b), and monzonitic (DV2) suites. A fourth older suite comprising alkaline gabbro, syenite, and A-type granite occurs in the Mt Dromedary area c. 80 km to the south. U-Pb zircon dating of Bonney Pluton, the largest calc-alkaline DV1a intrusion, indicates emplacement of this regional-scale body at 505 +/- 2 Ma. Pb-loss and inherited zircon were common to Bonney Pluton analyses of this study. U-Pb dating of monazite from Valhalla Pluton, a principal DV1b suite adakitic intrusion, indicates emplacement at 488 +/- 2 Ma. The Bonney Pluton age constrains the peak of calc-alkaline plutonism at 505 Ma and the Valhalla Pluton age records the major pulse of adakitic plutonism that is inferred to mark the final stages of subduction c. 490 Ma along this section of the East Antarctic margin. Nd and Sr isotope data for the calc-alkaline DV1a suite and adakitic DV1b suite define distinct ranges for each suite, supporting their subdivision on the basis of field relationships, petrography, and whole-rock geochemistry. Calc-alkaline DV1a suite granite magmas have eNd(T) = -4.2 to -6.1 and Sri = 0.7071-0.7079, whereas the adakitic DV1b suite rocks have a wider range of eNd(T) = -1.9 to -7.2 and Sri = 0.7065-0.7097. The isotopic data suggest a significant mantle component and subordinate crustal component in the source region of both suites. Time-dependent variations in the isotopic ratios of DV1a and DV1b suites imply a progressive increase in the proportion of more radiogenic material in the source region of the granitoid rocks, either mantle- or crust-derived material. Larger adakitic DV1b plutons are more 'evolved' than equivalent, smaller plutons of the same DV1b suite. Vanda Dikes and monzonitic DV2 suite intrusions are characterised by particularly low Sri = 0.7044-0.7067 and near-constant eNd(T) = -4.8 to -5.3, which indicate a

  4. Miscellaneous investigations series: Bedrock geologic map of the Lone Mountain pluton area, Esmeralda County, Nevada

    International Nuclear Information System (INIS)

    The joint attitudes were measured in the field and plotted on aerial photos at a scale of 1:24,000. The pluton is intensely jointed, primarily as a result of cooling and movement of the magma within a northwest-trending stress field. Foliation, in general, is poorly developed, and quality varies from area to area, but it is best developed close to the contacts with the metasedimentary rocks. A prominent northwest foliation direction was observed that parallels the northwest elongation of the exposed pluton. Faults in the pluton are difficult to identify because of the homogeneity of the rock. Several faults were mapped in the northern part of the area where they have a northeast trend and intersect the northwest-trending lamprophyre dikes with little apparent displacement. A major fault that bounds the northern part of the pluton is downthrown to the north and strikes northeast. This fault offsets the alluvium, the metasedimentary rocks, and the pluton and forms fault scraps as high as 10 m. Aeromagnetic data (US Geological Survey, 1979) suggest the following: (1) the local magnetic highs in the central part of the Lone Mountain pluton are probably related to topographic highs (peaks) where the flight lines are closer to the pluton; (2) a magnetic low in the northeastern part of Lone Mountain coincides with the pluton-country rock contact, which may be very steep; (3) the contours for the southwestern part of the mapped area indicate that the pluton-country rock contact is not as steep as that in the northeastern part and that the pluton probably coalesces at depth with the Weepah pluton, a pluton exposed south of the mapped area; and (4) the contours for the area of the Lone Mountain pluton express a northwest-trending gradient that parallels the northwest elongation of the Lone Mountain pluton and the northwest-trending stress field. 10 refs

  5. Caos en el mercado de commodities

    Directory of Open Access Journals (Sweden)

    Espinosa Méndez Christian

    2010-12-01

    Full Text Available Este artículo aplica seis técnicas y herramientas (análisis gráfico, gráfico de recurrencia, entropía de espacio temporal, coeficiente de Hurst, exponente de Lyapunov y dimensión de correlación, a las series de retornos del cobre, oro, petróleo, plata, zinc, aluminio, plomo y níquel, con el fin de corroborar la existencia de un comportamiento caótico en el mercado de commodities. Se encuentra evidencia de que los mercados financieros se comportan de forma caótica en contra de la hipótesis de aleatoriedad. Se contrasta, igualmente, no-normalidad, no-aleatoriedad y no-linealidad. Los resultados encontrados contradicen algunos de los supuestos básicos de la teoría financiera moderna.

  6. MECANISMOS UTILIZADOS PARA MONITOREAR EL PODER DE MERCADO EN MERCADOS ELÉCTRICOS: REFLEXIONES PARA COLOMBIA

    Directory of Open Access Journals (Sweden)

    Jesús Alonso Botero

    2013-12-01

    Full Text Available El propósito de este trabajo es analizar la viabilidad de la utilización del índice de oferta residual (IOR en el mercado eléctrico mayorista en Colombia, con el fin de promover la competencia. Esto se hace a partir de la revisión de la literatura relacionada con las experiencias internacionales respecto a los mecanismos para monitorear el poder de mercado y del análisis del Documento 118 de la Comisión de Regulación de Energía y Gas (CREG, 2010. La principal conclusión es que el IOR no es un buen mecanismo de control en mercados hidráulicos, mientras que el desarrollo de los mercados de largo plazo ha sido utilizado con gran éxito para mitigar el riesgo de abuso de poder de mercado, seg°n lo muestra la experiencia internacional.

  7. Report of mortmorilloniticas clay in the Medina swamp (Cerro Largo district)

    International Nuclear Information System (INIS)

    This report describes the prospect ion work for the montmorillonitics clay in the region of Medina swamp in Cerro Largo district. The existence of new deposits was detected by cartography and geological study.

  8. Hidrogeologic and geophysical studies into Agro school Melo UTU Cerro Largo province

    International Nuclear Information System (INIS)

    The technical University UTU of Uruguay requested and Hidrogeologic study with the aim to analyze the factibility to discover underground stream waters which supply groundwaters into agro school Ing Agr. Alcides E Pintos Melo, Cerro Largo province.

  9. An overview of the geochemistry of Cerro Prieto geothermal field with emphasis on isotopic changes

    International Nuclear Information System (INIS)

    This paper reviews the global geochemical changes in the Cerro Prieto geothermal reservoir due to exploitation and presents some important conclusions. Distribution of oxygen-18, deuterium, chloride concentrations, enthalpy and geothermometry for the field are presented

  10. Mexican--American cooperative program at the Cerro Prieto Geothermal Field

    Energy Technology Data Exchange (ETDEWEB)

    Witherspoon, P.A.; Espinosa, H.A.; Lippmann, M.J.; Mercado, A.M.; Wollenberg, H.A.

    1978-08-01

    The Cerro Prieto project incorporates studies of the geologic, hydrogeologic, geochemical, and geophysical setting of the geothermal field as well as its structural, reservoir engineering, and subsidence characteristics. A description of the activities involved in each part of this cooperative program is presented. Text of the agreement between the Comision Federal de Electricidad of Mexico and the USERDA for the cooperative study of the Cerro Prieto geothermal field is included.

  11. Evaluation of the physical characteristic of Cerro bend blocks used for radiation therapy

    International Nuclear Information System (INIS)

    In Radiation Therapy, the sparing of normal tissues can be performed using either multi-leaf collimators or Cerro bend blocks. The current work focuses on the physical characteristics of Cerro bend blocks including attenuation coefficient, effective penumbra width and isodose curves undulation in penumbral regions. Materials and Methods: All measurements were performed using a dual energy linac and the Cerro bend blocks designed and fabricated using a commercial Cerro bend material. Data were collected using a calibrated ionization chamber as well as EDR2 films. Results: The results showed that the attenuation coefficient was found to be 0.4475 and 0.4276 cm-1 for photon beams 6 MV and 15 MV, respectively, and a potential air bubble with a diameter greater than 3 mm affects beam attenuation significantly. The optimum Cerro bend block width was found to be around 16 mm. The isodose curves scalloping achieved for secondary collimator jaws, were also similar. Conclusion: If Cerro bend blocks are used as a basic method to protect normal tissues, its physical characteristics will be recommended to be taken into account comprehensively.

  12. Thermophysical properties of americium-containing barium plutonate

    International Nuclear Information System (INIS)

    Polycrystalline specimens of americium-containing barium plutonate have been prepared by mixing the appropriate amounts of (Pu0.91Am0.09)O2 and BaCO3 powders followed by reacting and sintering at 1600 K under the flowing gas atmosphere of dry-air. The sintered specimens had a single phase of orthorhombic perovskite structure and were crack-free. Elastic moduli were determined from longitudinal and shear sound velocities. Debye temperature was also determined from sound velocities and lattice parameter measurements. Thermal conductivity was calculated from measured density at room temperature, literature values of heat capacity and thermal diffusivity measured by laser flash method in vacuum. Thermal conductivity of americium-containing barium plutonate was roughly independent of temperature and registered almost the same magnitude as that of BaPuO3 and BaUO3. (author)

  13. Typomorphism of fluorapatite in the Khibiny alkaline pluton, Kola Peninsula

    Science.gov (United States)

    Konopleva, N. G.; Ivanyuk, G. Yu.; Pakhomovsky, Ya. A.; Yakovenchuk, V. N.; Mikhailova, Yu. A.

    2014-12-01

    The zoning of accessory and rock-forming fluorapatite in the Khibiny pluton is discussed in its content, morphology, and chemical composition. The concentrations of Na, REE, and Si impurities in fluorapatite decrease from the margin and center of the pluton to the Major Ring, composed of melteigiteurtite and rischorrite. Within this structure, the purest apatite is characteristic of the high-grade ore in large deposits, where it occurs free of Na, and REE, as well as Sr in place of Ca. The fractal dimension of fluorapatite aggregates in all textural types of apatite-nepheline rocks (ores) corresponds to the dimension of fractures. Along with mineralogy of apatite-nepheline rocks and zoning of host foidolite, this feature indicates the superimposed character of apatite mineralization.

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

    International Nuclear Information System (INIS)

    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

  15. Pyroxenes of the Khibiny alkaline pluton, Kola Peninsula

    Science.gov (United States)

    Yakovenchuk, V. N.; Ivanyuk, G. Yu.; Pakhomovsky, Ya. A.; Men'shikov, Yu. P.; Konopleva, N. G.; Korchak, Yu. A.

    2008-12-01

    Seven pyroxene varieties were identified in nepheline syenites and foidolites of the Khibiny pluton: enstatite, ferrosilite, diopside, hedenbergite, augite, aegirine-augite, and aegirine. Enstatite and augite are typical of alkaline and ultramafic rocks of dike series. Ferrosilite was found in country quartzitic hornfels. Diopside is a rock-forming mineral in alkaline and ultramafic rocks, alkali gabbroids, hornfels in xenoliths of volcanic and sedimentary rocks and foyaite, melteigite-urtite that assimilate them, and certain hydrothermal pegmatite veins. Hedenbergite was noted in hornfels from xenoliths of volcanic and sedimentary rocks and in a hydrothermal pegmatite vein at Mount Eveslogchorr. Aegirine-augite is the predominant pyroxene in all types of nepheline syenites, phonolites and tinguaites, foidolites, alkaline and ultramafic rocks of dike series, fenitized wall rocks surrounding the pluton, and xenoliths of Devonian volcanic and sedimentary rocks. Aegirine is an abundant primary or, more often, secondary mineral in nepheline syenites, foidolites, and hydrothermal pegmatite veins. It occurs as separate crystals, outer zones of diopside and aegirine-augite crystals, and homoaxial pseudomorphs after Na-Ca amphiboles. Microprobe analyses of 265 pyroxenes samples allowed us to distinguish ten principal trends of isomorphic replacement and corresponding typomorphic features of pyroxenes. Compositional variations in clinopyroxenes along the sampled 35-km profile from the margin of the Khibiny pluton to its center confirm the symmetric zoning of the foyaite pluton relative to semicircular faults of the Minor Arc and the Main (Central) Ring marked by Devonian volcanic and sedimentary rocks, foidolites, and related metasomatic rocks (rischorrite, albitite, and aegirinite). Changes in the composition of pyroxenes are explained mainly by the redistribution of elements between coexisting minerals of foyaites in the process of their intense differentiation under the

  16. Apollo 14 inverted pigeonites - Possible samples of lunar plutonic rocks.

    Science.gov (United States)

    Papike, J. J.; Bence, A. E.

    1972-01-01

    Analysis of 'inverted pigeonites' found in Apollo 14 samples 14082 and 14083 (a polymict breccia, the 'white rock') by a combination of optical, electron probe, and single-crystal X-ray diffraction techniques. These 'inverted pigeonites' are regarded as samples of plutonic rocks that have been blasted out of the Imbrium Basin. It is also concluded that lunar pigeonites will invert to orthopyroxenes, given sufficiently slow cooling histories even in very anhydrous environments.

  17. Indoor - soil gas radon relationshipin the Central Bohemian Plutonic Complex

    OpenAIRE

    I. Fojtíková; J. Miksová; I. Barnet

    2005-01-01

    The relationship of indoor radon measurements and radon in bedrock was studied in the granitoid Central Bohemian Plutonic Complex (CBPC). The indoor data were linked to vectorised geological and radon risk maps using the coordinates of particular dwellings. For each geological unit and rock type it was possible to calculate the statistical characteristics of indoor radon measurements. A clear relationship between indoor radon values and radon in bedrock was confirmed in al...

  18. Paraguay: Mercado de seguros y el desarrollo de un mercado de capitales a largo plazo

    OpenAIRE

    Lorraine Ocampos; Emilio Ortíz Trepowski; Bernardo Navarro A.

    1998-01-01

    En el Paraguay el mercado de seguros está todavía insuficientemente desarrollado, pese a la proliferación de compañías en especial a partir de la década del 90, coincidiendo con la desregulación del sistema financiero. Este mercado ha estado hasta febrero de 1996 regido por una Ley de 1947, que no contribuyó a la modernización del sector, por carecer de controles más dinámicos de solvencia y por impedir la libre determinación de tarifas. Adicionalmente, la normativa de inversión era inadecuad...

  19. K-Ar ages of plutonic rocks in the Lassiter Coast area, Antarctica

    Science.gov (United States)

    Mehnert, Harald H.; Rowley, Peter D.; Schmidt, Dwight L.

    1975-01-01

    Numerous middle Cretaceous stocks and small batholiths intruded Middle and Upper Jurassic sedimentary and volcanic rocks in the Lassiter Coast area of the southern Antarctic Peninsula. To establish the age of the quartz diorite and granodiorite plutonic events, five plutons were dated by the K-Ar method. The results indicate a timespan of about 20 m.y. for the emplacement of the plutons and a minimum age of 120 m.y. for the deformation of the sedimentary (Latady Formation) and volcanic rocks. Three of the more silicic plutons have concordant biotite and hornblende ages of 100 and 106 m.y.; two discordant ages of about 118 m.y. were obtained on the more mafic plutons. Petrographically, chemically, and geochronologically, the plutons of the southern to central Lassiter Coast are similar to the calc-alkaline suite of igneous rocks of the Andes of Patagonia, the Antarctic Peninsula, and eastern Ellsworth Land.

  20. Alternativas para incrementar la liquidez del mercado de energía mayorista colombiano: el caso del mercado no regulado

    OpenAIRE

    García Gómez, Diego Felipe; Mejía Sierra, Diego Fernando

    2013-01-01

    El presente estudio tiene como objetivo la presentación de alternativas que contribuyan a aumentar la liquidez del mercado no regulado de energía eléctrica en Colombia -- Para ello se parte de una revisión general del mercado eléctrico colombiano, posteriormente se introduce el concepto liquidez, haciendo énfasis en la liquidez en mercados eléctricos y se referencian algunos mercados eléctricos desarrollados en Europa, Norte América, Países Nórdicos e Inglaterra -- Se concluye que es necesari...

  1. The mafic dikes from the Panticosa pluton (Pyrenean Axial Zone): petrology and mineral chemistry

    OpenAIRE

    Tierz, Pablo; Lago San José, Marceliano; Galé, Carlos; Arranz, Enrique; Ubide, Teresa; Larrea, Patricia; Sanz, Tomás

    2012-01-01

    The Panticosa pluton is one of multiple granitic plutons cropping out in the Pyrenean Axial Zone, which corresponds to the Palaeozoic core of the Pyrenees. Mafic dikes cut both the Panticosa pluton and its Devonian metasedimentary country rocks. According to their mineralogy and mineral composition, these dikes can be classified into two different groups, with little textural variations: a calc-alkaline group and an alkaline group. The calcalkaline rocks (spessartites and ca...

  2. Uranium and Molybdenum extraction from a Cerro Solo deposit ore

    International Nuclear Information System (INIS)

    Cerro Solo, located in Chubut, Argentina, is a sandstone type uranium-molybdenum deposit. Good recovery of both elements can be achieved by acid leaching of the ore but the presence of molybdenum in pregnant liquors is an inconvenient to uranium separation and purification. A two steps process is developed. A selective alkaline leaching of the ore with sodium hydroxide allows separating and recovering of molybdenum and after solid-liquid separation, the ore is acid leached to recover uranium. Several samples averaging 0,2% uranium and 0,1% molybdenum with variable U/Mo ratio have been used and in both steps, leaching and oxidant reagents concentration, temperature and residence time in a stirred tank leaching have been studied. In alkaline leaching molybdenum recoveries greater than 96% are achieved, with 1% uranium extraction. In acid leaching up to 93% of the uranium is extracted and Mo/U ratio in solvent extraction feed is between 0,013 and 0,025. (author)

  3. Radon and ammonia transects across the Cerro Prieto geothermal field

    Energy Technology Data Exchange (ETDEWEB)

    Semprini, L.; Kruger, P.

    1981-01-01

    Radon and ammonia transects, conducted at the Cerro Prieto geothermal field, involve measurement of concentration gradients at wells along lines of structural significance in the reservoir. Analysis of four transects showed radon concentrations ranging from 0.20 to 3.60 nCi/kg and ammonia concentrations from 17.6 to 59.3 mg/l. The data showed the lower concentrations in wells of lowest enthalpy fluid and the higher concentrations in wells of highest enthalpy fluid. Linear correlation analysis of the radon-enthalpy data indicated a strong relationship, with a marked influence by the two-phase conditions of the produced fluid. It appears that after phase separation in the reservoir, radon achieves radioactive equilibrium between fluid and rock, suggesting that the phase separation occurs well within the reservoir. A two-phase mixing model based on radon-enthalpy relations allows estimation of the fluid phase temperatures in the reservoir. Correlations of ammonia concentration with fluid enthalpy suggests an equilibrium partitioning model in which enrichment of ammonia correlates with higher enthalpy vapor.

  4. Performance of casings in Cerro Prieto production wells

    Energy Technology Data Exchange (ETDEWEB)

    Dominguez A, B.; Vital B, F.; Bermejo M, F.; Sanchez G, G.

    1981-01-01

    A careful evaluation of different production casings used at Cerro Prieto from 1964 to date has shown that the following casings have yielded particularly impressive results: 7 5/8-in. diameter, J-55, 26 lb/ft; 7 5/8-in. diameter, K-55, 45.3 lb/ft; and 5-in. diameter, K-55, 23.2 lb/ft. These casings differ from others of the same diameter but lighter weight which were also used at the field. The results are favorable in spite of severe construction problems, especially the loss of circulation during cementing operations, which we encountered in some of the wells where these casings were used. The use of gravity-fed fine sand as packing material and the arrangement of the production and intermediate casings were important in avoiding damage due to tension-compression stresses and, above all, damage due to internal or external corrosion over time. This situation is clearly evidenced if we compare the damage to the above casings with that experienced by grade N-80 production casings, especially in a corrosive environment.

  5. Detailed microearthquake studies at the Cerro Prieto geothermal field

    Energy Technology Data Exchange (ETDEWEB)

    Majer, E.L. (Lawrence Berkeley Lab., CA); McEvilly, T.V.

    1981-01-01

    There appears to be an increase in seismic activity within the Cerro Prieto production zone since early 1978. The microearthquake activity is now more or less constant at a rate of 2 to 3 events per day. The b-values within the field are significantly higher inside the production zone than are those for events on faults outside of the production region. The earthquakes seem to be controlled by the Hidalgo fault, although slight clustering was observed in the center of the main production region. The earthquakes within the production zone may reflect the reservoir dynamics associated with heat and mass withdrawal. Mechanisms such as volume change, thermal stresses and weakening of materials associated with boiling (i.e., phase changes, dissolution) may all be responsible for the increased seismic activity. Although a small reinjection program has started, the pressure drawdown conditions existing within the field would imply that increased pore pressure resulting from the injection activities is not responsible for the increased seismic activity.

  6. Consumo en mercados alternativos para baja renta

    OpenAIRE

    Peñaloza, Verónica; Denegri Coria, Marianela; Lopes Ferreira de Souza, Lucas; Gerhard, Felipe

    2015-01-01

    Mediante la complementación entre una mirada cuantitativa y el rescate de los significados cualitativos, este trabajo pretende contribuir al conocimiento del consumidor de mercados alternativos. Un hallazgo importante es que la diversión crea un valor agregado importante en el momento de decidir el lugar donde se harán las compras. El comercio a pequeña escala, la atención personalizada y el cultivo del vínculo con el cliente son una enseñanza que se deriva de la observación de la realidad de...

  7. Los cuerpos ígneos neógenos del cerro de Las Minas (35,3°S - 69,9°O, Cordillera Principal de los Andes, SO de Mendoza: geología, petrografía y geoquímica

    Directory of Open Access Journals (Sweden)

    M.J. Pons

    2007-06-01

    Full Text Available El cerro de Las Minas (35,3°S - 69,9°O consiste en cuatro unidades ígneas epizonales: plutón diorítico-tonalítico, plutón granodiorítico, plutón granítico y diques -filones capa andesíticos. Estas unidades forman parte del arco magmático neógeno del SO de Mendoza correspondiente a la Andesita Huincán. Intruyen a rocas sedimentarias jurásicas de las Formaciones Puchenque y Auquilco y las que en las cercanías del contacto con los plutones diorítico y granítico, están modificadas a hornfels, calizas recristalizadas y skarns bandeados con mineralización de Fe. Geoquímicamente, constituyen un conjunto de plutones cogenéticos de amplio rango composicional, metaluminosos, subalcalinos con afinidad calcoalcalina y del tipo I, características que son semejantes a las de otros plutones de márgenes convergentes vinculados a skarns de Fe. Han evolucionado por cristalización fraccionada de sus componentes minerales principales (plagioclasa-piroxeno-anfíbol-magnetita-titanita y mezcla localizada entre los magmas diorítico y granodiorítico. Sus patrones de elementos trazas incompatibles y tierras raras son similares a los observados en las rocas ígneas: a del arco volcánico neógeno (Andesita Huincán, b vinculadas a otros skarns de Fe del SO de Mendoza (Hierro Indio y El Kaiser, c del cerro Nevazón (37,5°S perteneciente al arco volcánico paleógeno del NO de Neuquén y, finalmente, d del arco volcánico cuaternario de un sector de la zona volcánica sur (TSVZ (34,5°-37°S de los Andes, emplazados en una corteza continental relativamente delgada (35-50 km. Esto sugiere que las rocas ígneas del cerro de las Minas se formaron a partir de magmas parentales calcoalcalinos y metaluminosos, derivados de una fuente mantélica similar, con escasez o ausencia de granate residual en la fuente.

  8. Sheeted and bulbous pluton intrusion mechanisms of a small granitoid from southeastern Australia: implications for dyke-to-pluton transformation during emplacement

    Science.gov (United States)

    Fowler, T. J.

    1994-06-01

    The small late syn-tectonic Carboniferous Davys Creek Granite (DCG) of southeastern Australia consists of microgranitic intrusive bodies of diverse geometry and structure. These bodies include: (1) subvertical concordant sheets; (2) bulbous peneconcordant plutons with apophyses and discordant lobes; and (3) subvertical dykes and stocks. The sequence of changing intrusive style is broadly 1-2-3. Transition from 1 to 2 was probably a response to rising magma pressures or declining tectonic stresses. The λ parameter of Emerman and Marrett (1990), which discriminates between stable sheet-like and potential stock/pluton/batholith emplacement modes, adequately predicts the transitions between sheet and pluton emplacements for the DCG. Ductile dyking along actively forming foliations appears to have been an important early intrusive mechanism. A transition from sheet to bulbous pluton intrusion style is suggested to have been in response to magma pressure increases.

  9. Albitization and the gold-bearing Roodepoort pluton, Pietersburg granite-greenstone terrane, South Africa

    International Nuclear Information System (INIS)

    The gold bearing Roodepoort pluton in the Pietersburg granite-greenstone terrane of South Africa consists primarily of undeformed albite with lesser amounts of quartz, ankerite, magnesite, and pyrite. The pluton intruded a major N-70 degrees trending shear zone, the Knight's Pietersburg line. The present mineralogy of the pluton and its gold content are essentially secondary, formed by open system hydrothermal alteration. However, relic minerals indicate that the pluton originally had a granodioritic composition. This composition, as well as its initial 87Sr/86Sr ratio, are similar to those of the 2 660 Ma Turfloop batholith and are consistent with the possibility that the Roodepoort pluton is an altered phase of the batholith. Sr isotopic data also suggest that hydrothermal alteration occured shortly after the magmatic crystallization of the pluton. Some alteration along the Knight's Pietersburg line occured about 2 680 Ma ago. It is proposed that the emplacement of the Roodepoort pluton, the hydrothermal alteration and the gold mineralization are related to the Limpopo Orogeny. A second phase of open system hydrothermal alteration occured in shear zones along the margins of and within the Roodepoort pluton, apparently about 2 320 Ma ago. 5 figs., 5 tabs., 27 refs

  10. Guidelines to classification and nomenclature of Arabian felsic plutonic rocks

    Science.gov (United States)

    Ramsay, C.R.; Stoeser, D.B.; Drysdall, A.R.

    1986-01-01

    Well-defined procedures for classifying the felsic plutonic rocks of the Arabian Shield on the basis of petrographic, chemical and lithostratigraphic criteria and mineral-resource potential have been adopted and developed in the Saudi Arabian Deputy Ministry for Mineral Resources over the past decade. A number of problems with conventional classification schemes have been identified and resolved; others, notably those arising from difficulties in identifying precise mineral compositions, continue to present difficulties. The petrographic nomenclature used is essentially that recommended by the International Union of Geological Sciences. Problems that have arisen include the definition of: (1) rocks with sodic, zoned or perthitic feldspar, (2) trondhjemites, and (3) alkali granites. Chemical classification has been largely based on relative molar amounts of alumina, lime and alkalis, and the use of conventional variation diagrams, but pilot studies utilizing univariate and multivariate statistical techniques have been made. The classification used in Saudi Arabia for stratigraphic purposes is a hierarchy of formation-rank units, suites and super-suites as defined in the Saudi Arabian stratigraphic code. For genetic and petrological studies, a grouping as 'associations' of similar and genetically related lithologies is commonly used. In order to indicate mineral-resource potential, the felsic plutons are classed as common, precursor, specialized or mineralized, in order of increasing exploration significance. ?? 1986.

  11. U/Pb Zircon Ages of Plutons from the Central Appalachians and GIS-Based Assessment of Plutons with Comments on Their Regional Tectonic Significance

    OpenAIRE

    Wilson, John Robert

    2001-01-01

    The rocks of the Appalachian orogen are world-class examples of collisional and extensional tectonics, where multiple episodes of mountain building and rifting from the pre-Cambrian to the present are preserved in the geologic record. These orogenic events produced plutonic rocks, which can be used as probes of the thermal state of the source region. SIMS (secondary ion mass spectrometry) U/Pb ages of zircons were obtained for ten plutons (Leatherwood, Rich Acres, Melrose, Buckingham, Diana ...

  12. SOCIALISMO ENTRE GLOBALIZACIÓN Y MERCADO

    Directory of Open Access Journals (Sweden)

    Mario González Arencibia

    2011-12-01

    Full Text Available Desde finales del siglo XX, el término “globalización” ha venido multiplicando su presencia tanto en el lenguaje cotidiano como en la jerga especializada de las distintas disciplinas sociales, de tal modo que a la fecha actual son ya innumerables los documentos y los discursos en los cuales dicho término es ampliamente empleado. Ello es resultado de que, en la palabra “globalización” parecen resumirse las principales transformaciones que se están produciendo desde el siglo pasado, entre las cuales ha sido trascendente el derrumbe del socialismo como sistema mundial. Asociado a esto también han sido variados los criterios acerca de las posibilidades de la práctica de mercado y de la conexión a la globalización de los antiguos y actuales países socialistas.

  13. A AMAZONIA E O MERCADO DE CARBONO

    OpenAIRE

    Lamarca Junior, Mariano Rua; Chalita, Marie Anne Najm; Godoy, Amalia Maria Goldberg; Silva, Cesar Roberto Leite da

    2008-01-01

    A Amazônia tem um destacado papel na crise ambiental global uma vez que, no Brasil, há mais emissões de carbono por o desmatamento e queimadas do que pela queima de combustíveis de origem fóssil. Para discutir a problemática e a importância da inserção da Amazônia no mercado de carbono, parte-se dos processos de ocupação e uso dos recursos naturais da floresta e das contradições na formulação das políticas para a região. Com base nos conceitos de direitos de propriedade, direitos econômicos e...

  14. The age and constitution of Cerro Campanario, a mafic stratovolcano in the Andes of Central Chile

    OpenAIRE

    Wes Hildreth; Brad Singer; Estanislao Godoy; Francisco Munizaga

    1998-01-01

    ABSTRACT Cerro Campanario, a towering landmark on the continental divide near Paso Pehuenche, is a glacially eroded remnant of a mafic stratovolcano that is much younger than previously supposed. Consisting of fairly uniform basaltic andesite, rich in olivine and plagioclase, the 10-15 km³ edifice grew rapidly near the end of the middle Pleistocene, about 150-160 ka, as indicated by 40Ar/39Ar and unspiked K-Ar analyses of its lavas.La edad y formación del cerro Campanario, un estratovolcán má...

  15. El higo y sus posibilidades de mercado

    Directory of Open Access Journals (Sweden)

    Sonia Barboza Flores

    2008-04-01

    Full Text Available Este proyecto tuvo como objetivo general “promover la diversificación agrícola del país mediante la generación de tecnologías para la producción e industrialización del cultivo del higo (Ficus carica, así como el establecimiento de nuevas alternativas de mercados y comercialización del producto, con el fin de mejorar las condiciones de vida de los productores”. Como parte de este se procuró el cumplimiento de objetivos específicos como el de “contar con información sobre el estado de la oferta y de la demanda de higo en el país, así como el comportamiento de los precios y de los canales de comercialización existentes” y, también, “ recopilar información sobre la opinión de los consumidores con respecto a las características sensoriales de los productos elaborados a base de higo por el Centro de Investigación en Gestión Agroindustrial, así como medir la eventual intención de compra”.Para estos efectos, se evaluaron distintos factores relacionados con la producción nacional y el uso actual del fruto en su estado fresco y procesado. Además, tomando como base el desarrollo de dos nuevos productos procesados, se hace una evaluación de estos para determinar la aceptación del producto en un mercado regional y para determinar los posibles ajustes que deban hacerse en la formulación del producto.

  16. Age and intrusive relations of the Lamarck granodiorite and associated mafic plutons, Sierra Nevada, California

    Energy Technology Data Exchange (ETDEWEB)

    Joye, J.L.; Bachl, C.A.; Miller, J.S.; Glazner, A.F. (Univ. of North Carolina, Chapel Hill, NC (United States). Dept. of Geology); Frost, T.P. (Geological Survey, Spokane, WA (United States)); Coleman, D.S. (Massachusetts Inst. of Tech., Cambridge, MA (United States). Dept. of Earth, Atmospheric and Planetary Sciences)

    1993-04-01

    The compositionally zoned Late Cretaceous Lamarck granodiorite, west of Bishop, hosts numerous mafic intrusions ranging from hornblende gabbro to mafic granodiorite. Frost and Mahood (1987) suggested from field relations that the Lamarck and the associated mafic plutons were co-intrusive. Contact relations between the Lamarck host and the mafic intrusions are variable (sharp to diffuse) and in places suggest commingling. In order to constrain the intrusive relationships between the Lamarck and its associated mafic plutons, the authors have analyzed feldspars from the Mt. Gilbert pluton and the Lamarck granodiorite to see if feldspar compositions in the Mt. Gilbert overlap those in the Lamarck host and determined U-Pb zircon ages for the Mt. Gilbert and Lake Sabrina plutons to see if they have the same age as the Lamarck granodiorite. Feldspars from the Lamarck granodiorite are normally zoned and range compositionally from An[sub 38--32]; those in the Mt. Gilbert diorite are also normally zoned but range compositionally from An[sub 49--41] and do not overlap the Lamarck host. Four to five zircon fractions from each pluton were handpicked and dated using U-Pb methods. The Mt. Gilbert mafic diorite has a concordant age of 92.5 Ma and the Lake Sabrina diorite has a concordant age of 91.5 Ma. Ages for the two plutons overlap within error, but multiple fractions from each suggest that the Lake Sabrina pluton is slightly younger than the Mt. Gilbert pluton. These data and field relationships indicate: (1) plagioclase phenocrysts in the Mt. Gilbert pluton were not derived from the Lamarck granodiorite despite their textural similarity; but (2) the Lamarck granodiorite and its associated mafic plutons are co-intrusive as supported by the close agreement of the ages with the crystallization age obtained by Stern and others for the Lamarck granodiorite.

  17. Metodologia de desenvolvimento de novos produtos orientados para o mercado

    OpenAIRE

    Sousa, Carlos Eduardo Rodrigues de

    2012-01-01

    O desenvolvimento de novos produtos orientados para o mercado/cliente visa, na sua essência, identificar, compreender e analisar quais os ativos num produto que o cliente mais valoriza. Através de metodologias de orientação para o mercado, é possível identificar informação de valor sobre o mercado alvo, e, com base nesta informação, aplicar melhorias nas características e propriedades do novo produto desde o seu desenvolvimento. Tudo isto permitirá desenvolver novos produtos co...

  18. Evaluation of the Cerro Solo nuclear ore, province of Chubut. The Cerro Solo project within the frame of uranium exploration in Argentina. Pt. 1

    International Nuclear Information System (INIS)

    The Cerro Solo ore deposit was selected by the CNEA to invest in an assessment project because of their promising grade and amount of known and potential resources, significant to Argentina's uranium requirements. The deposit, which is located in the central region of the Chubut Province, belongs to the sandstone type and is hosted by the cretaceous Chubut Group. Technical studies carried out forecast an important growth of nuclear capacity to meet Argentina's energy requirements in the first two decades of of the the next century. To be in position to confront the challenge presented by increasing uranium resources to fuel the nuclear powers plants it is very important, as a first step, to improve the geological knowledge of uranium favorability in the country. The preliminary results of the Cerro Solo project indicate that the eastern slope of the Pichinan hills is a promising area for development of uranium resources, increasing the favorability of the San Jorge Basin in order to allow contributing to meet future uranium requirements. The Cerro Solo Project was planned in a sequential manner, as a multidisciplinary effort which includes studies on: geologic setting of mineralization, resource estimates, costs of mining and milling methods, economic analysis and environmental impact research. Among the mining methods, studies include the alternative of the in-situ leaching technology, which is becoming a low producing cost interesting possibility. (Author)

  19. Melt segregation evidence from a young pluton, Takidani Granodiorite (Japan)

    Science.gov (United States)

    Hartung, Eva; Caricchi, Luca; Floess, David; Wallis, Simon; Harayama, Satoru; Chiaradia, Massimo; Kouzmanov, Kalin

    2016-04-01

    We are presenting new petrological data from one of the youngest exposed plutons in the world, the Takidani Granodiorite (Japan), which has been suggested as a source for large volume ignimbrites (> 300km3). Takidani Granodiorite (1.54 Ma ± 0.23 Ma) is located within the active Norikura Volcanic Chain in the Northen Japan Alps and has been previously linked to large andesitic (1.76 Ma ± 0.17 Ma) and rhyolitic eruptions (1.75 Ma ± 0.17 Ma). The pluton is vertically zoned and consists of granites (67 to 68 wt.% SiO2) in the lower section, granodiorites (65 to 66 wt.% SiO2) in the middle section, a chemically more evolved fine-grained porphyritic unit (67 to 71 wt.% SiO2) near the roof and a marginal granodiorite at the roof (67 to 68 wt.% SiO2). The porphyritic texture of the more evolved unit near the roof indicates rapid crystallisation, which could be the result of the late intrusion of this unit at the roof of the magmatic system. However, no sharp contact is found between the underlying granodiorite and the porphyritic unit. Instead, a gradual change in rock fabric, whole-rock chemistry and mineralogy is observed suggesting that melt was extracted from the granodiorite. Electron microprobe analyses of plagioclases show three main crystal populations (Type I, II and III) with distinct anorthite and Fe contents. Type I plagioclase (An30‑40) occurs dominantly within the marginal granodiorite at the roof. Type II plagioclase (An40‑45) are common in the granodiorite and porphyritic unit. Type III plagioclase (An45‑50) is predominantly present in the granite. All plagioclase populations share a common sodic rim (An22) across the different units. Takidani Granodiorite rocks are compared to crystallisation experiments from similar magmatic suites. Emplacement conditions of the Takidani Granodiorite are obtained from the latter as well as barometry, thermometry and hygrometry indicating that magmas were ultimately emplaced at around 200 MPa, 850° C to 875° C

  20. Forecast of environmental impact in the evaluation of Cerro Solo nuclear mine

    International Nuclear Information System (INIS)

    This work presents a project for the study of the environmental impact of the Cerro Solo uranium mine. The survey is to be carried out performing different kinds of studies: mineralization, tectonics, hydrogeology, preliminary studies on different exploitation methods, costs, reserves estimation, economical studies and preliminary studies on possible environmental impacts. (author). 24 refs., 1 fig., 1 tab

  1. O mercado voluntário de carbono

    OpenAIRE

    Silva, Carlos Filipe Araújo da

    2012-01-01

    O objecto desta dissertação é caracterizar, em termos económicos, o problema que está subjacente à instituição dos mercados das licenças de carbono e a natureza económica deste tipo de solução para esse problema, dando-se, depois, uma atenção especial ao Mercado Voluntário. Para este tipo de mercado descreve-se o seu funcionamento e apresenta-se um projecto elaborado para uma federação de organizações de produtores florestais que poderia ser submetido a esse tipo de mercado....

  2. Rb-Sr isochronous age of Vepor pluton granitoids

    International Nuclear Information System (INIS)

    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 87Sr/86Sr 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)

  3. Cretaceous plutonic rocks in the Donner Lake-Cisco Grove area, northern Sierra Nevada, California

    Science.gov (United States)

    Kulow, Matthew J.; Hanson, Richard E.; Girty, Gary H.; Girty, Melissa S.; Harwood, David S.

    1998-01-01

    The northernmost occurrences of extensive, glaciated exposures of the Sierra Nevada batholith occur in the Donner Lake-Cisco Grove area of the northern Sierra Nevada. The plutonic rocks in this area, which are termed here the Castle Valley plutonic assemblage, crop out over an area of 225 km2 and for the most part are shown as a single undifferentiated mass on previously published geological maps. In the present work, the plutonic assemblage is divided into eight separate intrusive units or lithodemes, two of which each consist of two separate plutons. Compositions are dominantly granodiorite and tonalite, but diorite and granite form small plutons in places. Spectacular examples of comb layering and orbicular texture occur in the diorites. U-Pb zircon ages have been obtained for all but one of the main units and range from ~120 to 114 Ma, indicating that the entire assemblage was emplaced in a narrow time frame in the Early Cretaceous. This is consistent with abundant field evidence that many of the individual phases were intruded penecontemporaneously. The timing of emplacement correlates with onset of major Cretaceous plutonism in the main part of the Sierra Nevada batholith farther south. The emplacement ages also are similar to isotopic ages for gold-quartz mineralization in the Sierran foothills west of the study area, suggesting a direct genetic relationship between the voluminous Early Cretaceous plutonism and hydrothermal gold mineralization.

  4. Why are plutons dry? Outgassing mechanisms of crustal magmatic bodies

    Science.gov (United States)

    parmigiani, andrea; Huber, Christian; Bachmann, Olivier; Leclaire, Sébastien

    2016-04-01

    Magma bodies crystallizing to completion within the crust (i.e., forming plutons) typically undergo significant amounts of second boiling (i.e. cooling and crystallization of dominantly anhydrous minerals lead to volatile saturation and bubble nucleation/growth). The low water content ( 6 wt % H2O for evolved compositions in subduction zones), testify that outgassing from crystalline mushy reservoirs must be an efficient and widespread process. Understanding this outgassing mechanism is key to understand how volatiles are transferred from mantle depths to the surface. From the hydrodynamics point of view, the mass balance of exsolved volatiles in these plutonic bodies is controlled by the difference between the rate of degassing (formation of bubbles by 2nd boiling) and outgassing (transport of gas out of the magma body). In this study, we use pore-scale multiphase modeling to constrain these rates as function of the crystal and volatile contents in the magma. Because second boiling is a slow process, one can consider equilibrium degassing as a valid assumption. Outgassing, on the other end, is controlled by the competition between buoyancy, capillary and viscous forces. Our numerical simulations are used to determine the most efficient setting for gas to escape its magmatic trap. The high viscosity of interstitial melts and capillary forces (due to the non-wetting nature of the gas phase with most of the mineral phases in magmatic systems) strongly limits gas transport until vertically extensive gas channels are generated. We show that channels can readily form in volatile-rich coarse-grained mush zones in the upper crust, and allow efficient outgassing at crystallinities around 50-75 vol%, when millimetric bubbles can still win capillary resistive forces.

  5. Eruptive Variations During the Emplacement of Cerro Pinto, an Ambitious Rhyolite Dome, Puebla, Mexico

    Science.gov (United States)

    Zimmer, B.; Riggs, N.; Carrasco-Nunez, G.

    2006-12-01

    Cerro Pinto is a rhyolite dome complex located in the eastern Trans-Mexican Volcanic Belt. The complex is composed of four tuff rings and four domes that were emplaced in three distinct eruptive stages marked by changes in vent location and eruptive character. Each of these stages contained eruptive sequences that follow simple rhyolite-dome models, in which a pyroclastic phase is followed immediately by effusive dome emplacement. However, some aspects of the eruptive history, such as the occurrence of explosive reactivation and dome destruction through a lateral blast are uncommon in small rhyolitic structures and are more commonly associated with polygenetic structures, such as stratovolcanoes or calderas. In these larger structures, new pulses of magma often initiate reactivation, but at Cerro Pinto the story is different. Major and trace element geochemistry suggest that Cerro Pinto was sourced by a small, isolated magma chamber, unassociated with any surrounding silicic centers and did not experience any change in chemical composition over the course of the eruption. Based on these data and field observations, it is inferred that Cerro Pinto's eruptive variations were not the result of the influx of a new magma batch, but were the result of both phreatomagmatic interactions and the presence of a small magma chamber that was zoned with respect to volatiles. Both of these factors are commonly encountered in volcanologic studies, but documentation of their influence on smaller structures is under represented. Rhyolite domes have long been considered relatively simple volcanic structures with only localized hazard implications. However, the eruptive variations displayed by Cerro Pinto suggest that isolated rhyolite dome evolutions can be much more complex with the potential for explosive reactivation and dome collapse; events that must be taken into consideration when making hazard assessments.

  6. An Archean Geomagnetic Reversal in the Kaap Valley Pluton, South Africa

    Science.gov (United States)

    Layer; Kroner; McWilliams

    1996-08-16

    The Kaap Valley pluton in South Africa is a tonalite intrusion associated with the Archean Barberton Greenstone Belt. Antipodal paleomagnetic directions determined from the central and marginal parts of the pluton record a geomagnetic reversal that occurred as the pluton cooled. The age of the reversal is constrained by an 40Ar/39Ar plateau age from hornblende at 3214 +/- 4 million years, making it the oldest known reversal. The data presented here suggest that Earth has had a reversing, perhaps dipolar, magnetic field since at least 3.2 billion years ago. PMID:8688075

  7. Oster pluton (Central Karelia) - the ancient massif of two-feldspar granites of Baltic Shield

    International Nuclear Information System (INIS)

    Geochronological study of two-feldspar granites forming the Oster pluton in the Central Karelia was performed using the methods of U-Pb- and Sm-Nd-dating. U-Pb isotope data for zircons from granite of the Oster pluton correspond to the age of 2876±21 mln. years, whereas Sm-Nd isotope data obtained for three samples of the garnet correspond to the age varying from 3.0 to 3.5 bln. years. The ancient age of granites of the Oster pluton is explained by the presence of a sufficiently powerful crust in the region by that moment

  8. Custos sociais: Onde para o mercado?

    Directory of Open Access Journals (Sweden)

    Vítor Neves

    2012-12-01

    Full Text Available Os mercados constituem um poderoso mecanismo de coordenação económica. Ainda assim, as suas limitações não podem nem devem ser ignoradas. Os custos da mais diversa ordem com origem na atividade das empresas no quadro do capitalismo e externalizados, isto é, transferidos para outros agentes ou para a sociedade como um todo sem repercussão no mecanismo de preços, são um exemplo particularmente relevante dessas limitações. Neste artigo põem‑se em confronto as diferentes conceções sobre os custos sociais existentes na literatura económica, desde a identificação do problema como uma “falha do mercado” até à conceção mais heterodoxa (e também menos conhecida de K. William Kapp, segundo a qual os custos sociais são um problema intrínseco e inevitável no contexto institucional do capitalismo. Num primeiro momento discute‑se a natureza do problema. Em seguida, apresentam‑se, se bem que de forma muito sumária, duas linhas fundamentais de fratura entre a abordagem convencional dominante e a abordagem heterodoxa de Kapp: o conceito de eficiência adotado e o modo como é vista a questão da valoração dos custos sociais.

  9. El mercado de los economistas y el mercado de los sociólogos

    Directory of Open Access Journals (Sweden)

    Rème Pétronille

    2005-12-01

    Full Text Available Este artículo explora la posible ‘fertilización cruzada’ entre la sociología y la economía recurriendo a trabajos sociológicos recientes sobre las relaciones de mercado. Muestra que la principal diferencia entre estas dos disciplinas reside en el tipo de organización social que suponen sus modelos respectivos, y la atribuye a que los investigadores de ambos campos tienen aspiraciones distintas: mientras que los sociólogos tratan de explicar el funcionamiento real del mercado, los economistas –al menos los neoclásicos– teorizan cómo debería funcionar para que sea ‘eficiente’. Concluye que es difícil esperar dicha ‘fertilización cruzada’ (Schumpeter 1954 a menos que los trabajos recientes de economistas como Kirman desaten una tormenta en la disciplina económica.

  10. Chronology and cooling history of the Tianmenshan pluton in South Jiangxi Province and their geological significance

    Institute of Scientific and Technical Information of China (English)

    ZENG Qingtao; MAO Jianren; HU Qing; ZHAO Xilin; YE Haimin

    2008-01-01

    Geochronological studies on the crust-derived Tianmenshan pluton were undertaken by SHRIMP zircon U-Pb dating and Ar-Ar dating of biotite, muscovite and K-feldspar, giving a petrogenetic age of 167 Ma. Owing to the closure systems in different minerals, the cooling history of the pluton can be determined with an age-temperature diagram. The late hydrothermal event has been recognized, which is related probably with mineralization. In terms of the comparative geochronological and petrologic records, it is concluded that there are some constrains on tectonic evolution and that the formation of the Tianmenshan pluton proceeded in a transition period from lndosinian post-orogeny extension to strong compressive tectonics. And the timing of the hydrothermal event matches the compressive climax of the Yanshanian orogeny. The temporal gap between granite emplacement and wolframite mineralization could last 10-20 Ma owing to the low cooling rate of the pluton.

  11. Iron variation within a granitic pluton as determined by near-infrared reflectance

    Science.gov (United States)

    Baird, A. K.

    1984-01-01

    One-hundred fifty-one previously chemically analyzed samples of tonalite from the Lakeview Mountains pluton, southern California batholith, were analyzed for their iron content using near-infrared spectrophotometry. Compared to the earlier analyses of the same sample set by X-ray fluorescence spectrography, the infrared data have higher analytical variance but clearly define patterns of compositional zonation in the pluton which are closely similar to those patterns obtained from X-ray data; petrogenetic interpretations for the pluton would be the same from either data set. Infrared spectral data can be obtained directly in the field with relatively simple instruments and field measurements can be made to average local heterogeneities that often mask significant plutonic variations.

  12. Typochemistry of rinkite and products of its alteration in the Khibiny Alkaline pluton, Kola Peninsula

    Science.gov (United States)

    Konopleva, N. G.; Ivanyuk, G. Yu.; Pakhomovsky, Ya. A.; Yakovenchuk, V. N.; Mikhailova, Yu. A.; Selivanova, E. A.

    2015-12-01

    The occurrence, morphology, and composition of rinkite are considered against the background of zoning in the Khibiny pluton. Accessory rinkite is mostly characteristic of foyaite in the outer part of pluton, occurs somewhat less frequently in foyaite and rischorrite in the central part of pluton, even more sparsely in foidolites and apatite-nepheline rocks, and sporadically in fenitized xenoliths of the Lovozero Formation. The largest, up to economic, accumulations of rinkite are related to the pegmatite and hydrothermal veins, which occur in nepheline syenite on both sides of the Main foidolite ring. The composition of rinkite varies throughout the pluton. The Ca, Na, and F contents in accessory rinkite and amorphous products of its alteration progressively increase from foyaite and fenitized basalt of the Lovozero Formation to foidolite, rischorrite, apatite-nepheline rocks, and pegmatite-hydrothermal veins.

  13. Tertiary plutonic rocks of southern Serbia Vardar Zone as dimension stone

    Directory of Open Access Journals (Sweden)

    Kurešević Lidja

    2014-01-01

    Full Text Available Three granitoid plutons of south-Serbian part of the Vardar Zone, of Tertiary age were studied in order to establish their potential for utilization as dimension stone. These rocks vary in composition from quartzmonconite to quartzdiorite. Field study aimed at establishing the geological factors - presence of fractures, harmful minerals, alterations, jointing type and fabric homogeneity in order to determine the possibility of obtaining large size blocks of stone from the plutons. Laboratory examinations comprised petrological analyses and testing of technical properties. Stone from these plutons has shown favourable results in both field and laboratory examinations. Evaluation of the rock based on obtained laboratory testing results is performed according to technical requirements of the Serbian standard B.B3.200. It has shown that rocks from these plutons can be used as dimension stone for the production of slabs for the exterior and interior paving and cladding. [Projekat Ministarstva nauke Republike Srbije, br. OI176016

  14. Volcanic-plutonic parity and the differentiation of the continental crust.

    Science.gov (United States)

    Keller, C Brenhin; Schoene, Blair; Barboni, Melanie; Samperton, Kyle M; Husson, Jon M

    2015-07-16

    The continental crust is central to the biological and geological history of Earth. However, crustal heterogeneity has prevented a thorough geochemical comparison of its primary igneous building blocks-volcanic and plutonic rocks-and the processes by which they differentiate to felsic compositions. Our analysis of a comprehensive global data set of volcanic and plutonic whole-rock geochemistry shows that differentiation trends from primitive basaltic to felsic compositions for volcanic versus plutonic samples are generally indistinguishable in subduction-zone settings, but are divergent in continental rifts. Offsets in major- and trace-element differentiation patterns in rift settings suggest higher water content in plutonic magmas and reduced eruptibility of hydrous silicate magmas relative to dry rift volcanics. In both tectonic settings, our results indicate that fractional crystallization, rather than crustal melting, is predominantly responsible for the production of intermediate and felsic magmas, emphasizing the role of mafic cumulates as a residue of crustal differentiation. PMID:26178961

  15. Consideration of the ultramafic intrusive rocks in Arroyo Las Palmas (ex Cerro Chato - Las Canias) Durazno. R. O. del Uruguay

    International Nuclear Information System (INIS)

    This work is about the ultramafic rocks which its chemistry composition fluctuate since the basic to the ultra basic field and appear in the nascent of the Las Palmas stream near Las Canias and Cerro Chato district.

  16. Petrology and Geochemistry of Neoproterozoic Arc Plutons Beneath the Atlantic Coastal Plain, SRS, SC

    Energy Technology Data Exchange (ETDEWEB)

    Maryak, M.

    1998-10-21

    In this report is presented first a brief review of the regional geologic setting of the Savannah River Site, descriptions of the plutonic rock units sampled here, whole rock geochemical data on the plutonic igneous rocks, and finally, a discussion of how the crystalline basement rocks of the Savannah River Site formed and how they may correlate with other terranes exposed in the Piedmont of the Carolinas, Georgia, and Virginia.

  17. Colour masks in digital image analysis: a technique for modal analyses of quartz saturated plutonic rocks

    OpenAIRE

    Elliott, B.A.

    1999-01-01

    Mineral modes can be calculated quickly and accurately by using colour masks in scanned digital images of stained, quartz saturated plutonic rocks. The image analysis method for determining modal compositions is as accurate as manual point counting, and remarkably faster. A comparison of the manual point counting and pixel resolution methods, and a step by step procedure for calculating mineral modes in quartz saturated plutonic rocks are provided to make modal composition calculations fast, ...

  18. Multidisciplinary study of Santa Eulália Plutonic Complex (Central Portugal): Preliminary insight.

    OpenAIRE

    Sant’Ovaia, Helena; Lopes, José Carrilho; Nogueira, Pedro

    2011-01-01

    Multidisciplinary study of Santa Eulalia Plutonic Complex (Central Portugal): Preliminary insight H. SANT’OVAIA1*, J. CARRILHO LOPES2 AND P. NOGUEIRA2 1DGAOT, Centro de Geologia, FCUP, Portugal (*correspondence: ) 2Dep. Geo., Univ. Évora, Centro de Geologia UL, Portugal The Santa Eulália Plutonic Complex (SEPC) is a late- Variscan calcalkaline granitic body that occupies an area of 400 km2 and is located in the Variscan Iberian sector. The host ...

  19. Colour masks in digital image analysis: a technique for modal analyses of quartz saturated plutonic rocks

    Directory of Open Access Journals (Sweden)

    Elliott, B.A.

    1999-12-01

    Full Text Available Mineral modes can be calculated quickly and accurately by using colour masks in scanned digital images of stained, quartz saturated plutonic rocks. The image analysis method for determining modal compositions is as accurate as manual point counting, and remarkably faster. A comparison of the manual point counting and pixel resolution methods, and a step by step procedure for calculating mineral modes in quartz saturated plutonic rocks are provided to make modal composition calculations fast, accurate, and efficient.

  20. Using micro-scale evidence to understand regional-scale hydrothermal alteration of plutonic rocks

    OpenAIRE

    Plümper, O.; King, H. E.; Putnis, A.

    2009-01-01

    Subsolidus re-equilibration of plutonic feldspars induced by hydrothermal fluids provides a valuable record of fluid-rock interactions that affect large volumes of the Earth's continental crust (Taylor, 1977). The effect of hydrothermal fluids has important implications for the interpretation of the present plutonic mineralogy and geochemistry. However, crustal hydrothermal activity is usually not accounted for unless stages of replacement can be identified or new minerals that are characteri...

  1. Different meanings for cummingtonite-hornblende association in plutonic rocks (Iberian Massif, Portugal)

    OpenAIRE

    Solá, A. R.; Moita, P.; Santos, J. F.; Neiva, A.M.R.; Ribeiro, M. L.

    2010-01-01

    Cummingtonite-grunerite series is frequently related with metamorphism or volcanic environments but rarely described as belonging to a plutonic assemblage [1]. Recently, in Iberian Massif (Portugal), there have been several references [2,3,4,5] of this Fe-Mg amphibole intimately associated with Ca amphiboles (mainly hornblende) on plutonic rocks. Different textural relations between two amphibole types have been argued to for a primary (igneous) or subsolidus metamorphic origin for Fe-Mg amph...

  2. Coeval Shoshonitic-ultrapotassic dyke emplacements within the Kestanbol Pluton, Ezine – Biga Peninsula (NW Anatolia)

    OpenAIRE

    Akal, Cüneyt

    2013-01-01

    The Biga Peninsula, in the north-western part of Western Anatolia, is part of the Sakarya Zone of the Western Pontides and the tectonically overlying Ezine group. The basement rocks are intruded by the early Miocene Kestanbol Pluton and early to middle Miocene calc-alkaline to shoshonitic-ultrapotassic volcanic successions related to postcollisional continental extension. The Kestanbol Pluton mainly comprises monzonite and granodiorite and is cut by shoshonitic-ultrapotassic tephriphonolite d...

  3. Uranium-Lead Zircon Ages and Sr, Nd, and Pb Isotope Geochemistry of Selected Plutonic Rocks from Western Idaho

    Science.gov (United States)

    Unruh, Daniel M.; Lund, Karen; Kuntz, Mel A.; Snee, Lawrence W.

    2008-01-01

    Across the Salmon River suture in western Idaho, where allochthonous Permian to Cretaceous oceanic rocks are juxtaposed against Proterozoic North American rocks, a wide variety of plutonic rocks are exposed. Available data indicate much variation in composition, source, and structural state of these plutons. The plutonic rocks were long described as the western border zone of the Cretaceous Idaho batholith but limited pre-existing age data indicate more complicated origins. Because the affinity and age of the plutonic rocks cannot be reliably determined from field relations, TIMS U-Pb dating in conjunction with Sr, Nd, and Pb isotopic studies of selected plutons across the suture in western Idaho were undertaken. The data indicate three general groups of plutons including (1) those that intruded the island arc terranes during the Triassic and Jurassic, those that intruded near the western edge of oceanic rocks along the suture in the Early Cretaceous, and the plutons of the Idaho batholith that intruded Proterozoic North American rocks in the Late Cretaceous. Plutons that intruded Proterozoic North American rocks commonly include xenocrystic zircons and in several cases, ages could not be determined. The least radiogenic Sr and most radiogenic Nd are found among the Blue Mountains superterrane island arc samples. Suture-zone plutons have isotopic characteristics that span the range between Idaho batholith and island arc samples but mostly follow island arc signatures. Plutons of the Idaho batholith have the most radiogenic initial Pb and Sr ratios and the least radiogenic Nd of the samples analyzed.

  4. Panorama Pluton : a composite gabbro-monzodiorite early Ross Orogeny intrusion in southern Victoria Land, Antarctica

    International Nuclear Information System (INIS)

    The Koettlitz Glacier Alkaline Province of the Walcott Glacier to Radian Glacier area of the Transantarctic Mountains contains a diverse suite of intrusions ranging from gabbro and diorite to granite, nepheline syenite, and carbonatite. Most of the plutons are alkaline (A-type), although the Panorama Pluton is mafic, comprising both hypersthene normative gabbroic and quartz normative monzodioritic lithologies. The pluton has a composite nature, determined by whole-rock geochemical trends and Nd-Sr isotope data that reflect distinctive source regions for the different components. U-Pb geochronology of zircon and titanite indicates the Panorama Pluton was intruded during the early stages of the Neoproterozoic-early Paleozoic Ross Orogeny at 535 ± 9 Ma, and that it is coeval with the geochemically similar Dromedary Mafic Complex which crops out 10 km to the southeast. The Panorama Pluton is a volumetrically minor mafic component of the Koettlitz Glacier Alkaline Province, which predates, by at least 15 m.y., the dominant calc-alkaline suites that occur along-strike in the Dry Valleys area to the north, and the central Transantarctic Mountains to the south. The Panorama Pluton magmas, and other Koettlitz Glacier Alkaline Province lithologies, are interpreted to have formed in an extensional or transtensional jog that predates the onset of widespread Ross Orogeny subduction. (author). 48 refs., 7 figs., 3 tabs

  5. Geological, geochemical and isotopic characteristics of the Archaean Kaap Valley pluton, Barberton mountain land, South Africa

    International Nuclear Information System (INIS)

    The Kaap Valley pluton consists predominantly of a homogeneous weakly foliated, hornblende-bearing tonalite. It is among the oldest granitoid bodies yet recognized in the environs of the Barberton greenstone belt, yielding 207Pb/206Pb mineral ages of about 3300 Ma and a Rb-Sr whole rock isochron age of about 3500 Ma. The Kaap Valley pluton is distinctive in many respects. Whereas all other gneiss plutons in the area are characterized by a trondhjemitic bulk composition with mafic mineralogies dominated by biotite, the Kaap Valley pluton is tonalitic in bulk composition with hornblende (plus minus minor biotite) as its major mafic phase. In this paper, the results of a detailed geological, geochemical and Pb-isotopic study of the Kaap Valley pluton are presented. Questions relating to the origin of the body are considered, with an emphasis on the formation of a tonalitic magma which is more mafic than those typically encountered in the region. Although exposure does not permit a detailed structural study of the gneiss pluton consideration is given to its mode of emplacement

  6. Case history report on East Mesa and Cerro Prieto geothermal fields

    Energy Technology Data Exchange (ETDEWEB)

    Davis, DG.; Sanyal, S.K.

    1979-06-01

    Well log analysis as applied to the geothermal industry is one of the areas of technology in great need of further development. One means of improving log analysis technology is to study case histories of the past uses of log analysis as applied to specific fields. The project described in this report involved case history studies on two well-known geothermal areas in North America: the East Mesa field in California and the Cerro Prieto field in Mexico. Since there was considerably more pertinent material available on East Mesa, a major part of the effort on this project was devoted to studying the East Mesa field. One particular problem that first came to attention when studying the Cerro Prieto data was the difficulty in determining actual formation temperature at the time of logging. Since the temperature can have a significant effect on well log readings, an accurate temperature determination was considered to be important.

  7. New mammalian records in the Parque Nacional Cerros de Amotape, northwestern Peru

    OpenAIRE

    Cindy M. Hurtado; Víctor Pacheco

    2015-01-01

    The Pacific Tropical Rainforest and Equatorial Dry Forest are found only in southern Ecuador and northern Peru, and are among the most poorly known ecosystems of South America. Even though these forests are protected in Parque Nacional Cerros de Amotape (PNCA), they are threatened by fragmentation because of farming and agriculture. The aim of this study was to determine the medium and large mammalian species richness, using transect census, camera trapping, and specimen bone collection. Nine...

  8. Study of the atmospheric conditions at Cerro Armazones using astronomical data

    OpenAIRE

    Lakicevic, Masha; Kimeswenger, Stefan; Noll, Stefan; Kausch, Wolfgang; Unterguggenberger, Stefanie; Kerber, Florian

    2016-01-01

    Aims: We studied the precipitable water vapour (PWV) content near Cerro Armazones and discuss the potential use of our technique of modelling the telluric absorbtion lines for the investigation of other molecular layers. The site is designated for the European Extremely Large Telescope (E-ELT) and the nearby planned site for the Cherenkov Telescope Array (CTA). Methods: Spectroscopic data from the Bochum Echelle Spectroscopic Observer (BESO) instrument were investigated by using line-by-line ...

  9. The age and constitution of Cerro Campanario, a mafic stratovolcano in the Andes of central Chile

    Science.gov (United States)

    Hildreth, W.; Singer, B.; Godoy, E.; Munizaga, F.

    1998-01-01

    Cerro Campanario, a towering landmark on the continental divide near Paso Pehuenche, is a glacially eroded remnant of a mafic stratovolcano that is much younger than previously supposed. Consisting of fairly uniform basaltic andesite, rich in olivine and plagioclase, the 10-15 km3 edifice grew rapidly near the end of the middle Pleistocene, about 150-160 ka, as indicated by 40Ar/39Ar and unspiked K-Ar analyses of its lavas.

  10. El bronce final y la Edad del Hierro en "Cerro del Berrueco" (Ávila-Salamanca

    Directory of Open Access Journals (Sweden)

    J. Francisco FABIÁN GARCÍA

    2009-10-01

    Full Text Available El Cerro del Berrueco es un monte-isla enclavado en las inmediaciones del Sistema Central y, más concretamente, de las Sierras de Gredos y Béjar, en el sector Sur-Occidental de la Meseta Norte. Corresponde una parte de él a la provincia de Avila y otra, más extensa, a la de Salamanca.

  11. Light pollution at high zenith angles, as measured at Cerro Tololo Inter-American Observatory

    CERN Document Server

    Krisciunas, Kevin; Sanhueza, Pedro; Smith, Malcolm G

    2010-01-01

    On the basis of measurements of the V-band sky brightness obtained at Cerro Tololo Inter-American Observatory in December 2006 and December 2008 we confirm the functional form of the basic model of Garstang (1989, 1991). At high zenith angles we measure an enhancement of a factor of two over Garstang's later model when there is no marine cloud layer over La Serena/Coquimbo. No corresponding enhancement is found in the B-band.

  12. Works carried out in the south of Cerro Largo district. Uranium prospection programme. Preliminary report

    International Nuclear Information System (INIS)

    During the carried out work of radimetric preliminary Investigation in the northeast of the uraniferous country were detected radimetric anonalias which are associated to the formation San Gregorio and Tres Islas. Later the works of prospection ratified those anomalies to which they defined in the environs other anomalies. The studies of revision of these conducted anomalies they took to conclude the necessity to carry out a detailed study of the area to that district was denominated Cerro Largo Sur

  13. Titulación de la propiedad y mercado inmobiliario

    Directory of Open Access Journals (Sweden)

    Julio Calderón Cockburn

    2010-01-01

    Full Text Available En este estudio se analiza la relación entre la tenencia de títulos de propiedad (registrados y los mercados inmobiliarios en aquellas zonas de la ciudad cuyo origen fue informal o ilegal. Al hacerlo se plantean cuestionamientos a los presupuestos internacionales y se encuentran paradojas en el funcionamiento del mercado de suelo popular. La metodología es cuantitativa y cualitativa. Las conclusiones muestran que en los asentamientos no consolidados la tenencia de un título de propiedad contribuye a conferir un mayor valor a los predios en relación con los que no están titulados. No obstante, el título de propiedad no necesariamente induce al predominio de los mercados inmobiliarios formales; más bien se mantienen las tendencias que apuntan a las transacciones informales en cuanto a alquileres, compras y ventas.

  14. Estado, mercado de tierra urbana e inundaciones en ciudades argentinas

    Directory of Open Access Journals (Sweden)

    Clichevsky Nora

    2006-10-01

    Full Text Available En este trabajo se presentan los resultados de una investigación sobre las relaciones que se establecen entre los mercados de tierra urbana y las inundaciones en ciudades argentinas, en el marco más amplio de la vulnerabilidad urbana. Se pretende despejar incógnitas acerca del papel jugado por el Estado como regulador del mercado en áreas urbanas con vulnerabilidad natural a la inundación y como constructor de defensas contra las inundaciones y acerca de los impactos que han tenido las inundaciones y las obras de defensa contra ellas sobre el mercado de tierra y, por lo tanto, sobre el acceso al suelo urbano por parte de los distintos sectores de la población.

  15. Evolution of the Cerro Prieto geothermal system as interpreted from vitrinite reflectance under isothermal conditions

    Energy Technology Data Exchange (ETDEWEB)

    Barker, C.E. (US Geological Survey, Denver, CO); Pawlewicz, M.J.; Bostick, N.H.; Elders, W.A.

    1981-01-01

    Temperature estimates from reflectance data in the Cerro Prieto system correlate with modern temperature logs and temperature estimates from fluid inclusion and oxygen isotope geothermometry indicating that the temperature in the central portion of the Cerro Prieto System is now at its historical maximum. Isoreflectance lines formed by contouring vitrinite reflectance data for a given isothermal surface define an imaginary surface that indicates an apparent duration of heating in the system. The 250/sup 0/C isothermal surface has a complex dome-like form suggesting a localized heat source that has caused shallow heating in the central portion of this system. Isoreflectance lines relative to this 250/sup 0/C isothermal surface define a zone of low reflectance roughly corresponding to the crest of the isothermal surface. Comparison of these two surfaces suggest that the shallow heating in the central portion of Cerro Prieto is young relative to the heating (to 250/sup 0/C) on the system margins. Laboratory and theoretical models of hydrothermal convection cells suggest that the form of the observed 250/sup 0/C isothermal surface and the reflectance surface derived relative to it results from the convective rise of thermal fluids under the influence of a regional hydrodynamic gradient that induces a shift of the hydrothermal heating effects to the southwest.

  16. Relationship between water chemistry and sediment mineralogy in the Cerro Prieto geothermal field: a preliminary report

    Energy Technology Data Exchange (ETDEWEB)

    Valette-Silver, J.N. (Univ. de Perpignan, France); Thompson, J.M.; Ball, J.W.

    1981-01-01

    The chemical compositions of waters collected from the Cerro Prieto geothermal production wells and hydrothermal emanations are different. Compared to the Cerro Prieto well waters, the surficial waters generally contain significantly less potassium, slightly less calcium and chloride, and significantly more magnesium and sulfate. In comparison to the unaltered sediments, the changes in the mineralogy of the altered sediments appear to be controlled by the type of emanation (well, spring, mud pot, geyser, fumarole, or cold pool). However, an increase in quartz and potassium feldspar percentages seems to be characteristic of the majority of the sediments in contact with geothermal fluids. Preliminary attempts to model the chemical processes occurring in the Cerro Prieto geothermal field using chemical equilibrium calculations are reported. For this purpose the chemical compositions of thermal waters (well and surficial emanation) were used as input data to make calculations with SOLMNEQ and WATEQ2 computer programs. Then the theoretical mineral composition of altered sediments was predicted and compared to the mineralogy actually observed in the solid samples.

  17. Mineral potential of felsic plutonic rocks in the north-central Arabian Shield, Kingdom of Saudi Arabia

    Science.gov (United States)

    Moore, W.J.

    1985-01-01

    Fourteen plutons of Late Proterozoie age potentially favorable for rare-element mineralization have been identified in a geochemical and petrographic assessment of felsic plutonic rocks in the north-central Arabian Shield (lat 23°00'-25°00' N., long 40°00'-45°00' E.). The plutons are highly fractionated, leucocratic granitoids assigned to a major magmatic pulse that spanned the later stages of the Hijaz orogeny (about 610 Ma to about 550 Ma). Most of the targeted plutons are small or not deeply eroded. Two rock types are dominant: subsolvus, muscovite-bearing monzogranite or syenogranite; and hypersolvus, mieroeline perthite granite commonly containing sodic pyriboles. Enrichment in varied suites of the granitophile elements (Sn-W-NbTa-Zr-Y-Th-U) is characteristic. The plutons occupy the central part of a broad arcuate belt of geochemically specialized plutons that conforms generally to the eastern limit of exposed Proterozoic basement.

  18. Magnetic properties of ilmenite-hematite single crystals from the Ecstall pluton near Prince Rupert, British Columbia

    DEFF Research Database (Denmark)

    Brownlee, Sarah J.; Feinberg, Joshua M.; Kasama, Takeshi;

    2011-01-01

    Ecstall pluton experienced considerable mineralogical changes as younger Eocene plutons, such as the ∼58 Ma Quottoon Pluton, were emplaced along its margins. We investigated changes in the rock magnetic properties associated with this reheating event by examining isolated grains of intergrown ilmenite and......Paleomagnetic studies of the 91 Ma Ecstall pluton and other Cretaceous plutons of British Columbia imply large northward tectonic movements (>2000 km) may have occurred during the tectonic evolution of western North America. However, more recent studies have shown that the eastern edge of the...... hematite, the primary paleomagnetic recorder in the Ecstall pluton. Measurements of hysteresis properties, low-temperature remanence, and room temperature isothermal remanent magnetization acquisition and observations from magnetic force microscopy and off-axis electron holography indicate that samples...

  19. Diagnóstico del mercado de trabajo en Uruguay

    OpenAIRE

    Carmen Pagés-Serra

    2005-01-01

    En los últimos 15 años, la economía uruguaya sufrió grandes transformaciones y fuertes choques externos, los cuales tuvieron importantes repercusiones en el mercado laboral. Más allá de los devastadores efectos de la reciente crisis económica sobre el empleo, desempleo e ingresos de los uruguayos, el mercado de trabajo uruguayo evidencia síntomas que delatan problemas de corte estructural, tales como alta duración del desempleo y elevadas y persistentes tasas de desempleo juvenil y femenino. ...

  20. Bio-sociodiversidade: preservação e mercado

    OpenAIRE

    Mauro Leonel

    2000-01-01

    VÁRIOS estudos vêm revelando possibilidades de aproveitamento de conhecimentos indígenas e de outras culturas tradicionais, entre eles, medicamentos, cosméticos, novos materiais, alimentos, sementes e conservantes como produtos de mercado. A prática do mercado vem sendo a de apropriar-se desses bens culturais, registrá-los após adaptações e devolvê-los como mercadorias protegidas por patentes, inclusive aos países onde tais conhecimentos foram desenvolvidos, geralmente ao sul do Equador. Fren...

  1. Diferenciación de productos y poder de mercado

    OpenAIRE

    Coloma, Germán

    1998-01-01

    El siguiente trabajo presenta un modelo de análisis del poder de mercado en un contexto de diferenciación de productos simétrica. Cada variedad posee un componente homogéneo y otro idiosincrático que los consumidores valoran separadamente. Según el modo en el cual las empresas influyan sobre sus precios, se distinguen cuatro hipótesis de comportamiento (competencia pura, competencia monopolística, oligopolio de Cournot y colusión), se evalúa el poder de mercado local y global que las mismas i...

  2. Diferenciación de Productos y Poder de Mercado

    OpenAIRE

    Coloma, Germán

    1997-01-01

    El presente trabajo presenta un modelo de análisis del poder de mercado en un contexto de diferenciación de productos simétrica. Cada variedad posee un componente homogéneo y otro idiosincrático que los consumidores valoran separadamente. Según el modo en el cual las empresas influyan sobre sus precios, se distinguen cuatro hipótesis de comportamiento (competencia pura, competencia monopolística, oligopolio de Cournot y colusión), se evalúa el poder de mercado local y global que las mismas im...

  3. ¿Qué tan verde es tu mercado?

    OpenAIRE

    Wilmar R. Olaya-González; Luz Adriana Gómez-Rodríguez

    2011-01-01

    El mercado de lo verde y lo ecológico es una tendencia indiscutible en nuestro mundo globalizado, que busca de alguna manera resarcir el daño infringido sobre el medio ambiente. Más allá de simple altruismo, la ecología se ha convertido en una moda, de la cual unos y otros toman ventaja a su mejor acomodo, haciendo del mercado de productos y servicios su tribuna; eco-diseño, planes de responsabilidad social y ambiental, campañas por el reciclaje y consumo de productos "más amigables" con el m...

  4. O MERCADO DE SEMENTES DE MILHETO NO BRASIL

    OpenAIRE

    TRDEZINI, CÍCERO ANTÔNIO DE OLIVEIRA; SOUZA, JUAN DIEGO FERELLI; JÚLIO, JÚLIO CÉSAR DE PAIVA; UTIMA, ANGÉLICA YABUSAME; Kobayashi, Juliana Bonamingo

    2006-01-01

    O objetivo desse trabalho é discutir o padrão competitivo do mercado de sementes de milheto no Brasil. Para tanto, será avaliada a competitividade desse negócio, usando a metodologia das cinco forças competitivas de Porter, com base em opiniões dos entrevistados de todos os elos da cadeia, além de consulta a fontes secundárias. Trata-se de um mercado que, em função do lançamento de novas variedades nestes últimos anos, pode ser visto como bastante promissor e com expectativas de crescimento. ...

  5. Prueba de racionalidad para el mercado de capitales mexicano

    OpenAIRE

    Rodríguez Mejía, Josué de Israel

    2005-01-01

    A pesar de la amplia noción de eficiencia de mercado numerosos autores sugieren que los precios de los activos no están racionalmente relacionados a la realidad económica. En esta investigación ofrecemos una amplia revisión de la literatura que aborda la falta de eficiencia en el mercado de capitales y sus posibles explicaciones, haciendo énfasis en las investigaciones que presentan evidencia de que el precio de los activos es mas volátil de lo que deberían ser si estos r...

  6. Migración y Mercado Laboral en Chile

    OpenAIRE

    Dante Contreras; Jaime Ruiz-Tagle; Paulina Sepúlveda

    2013-01-01

    Los últimos procesos migratorios que ha vivido Chile han despertado el interés respecto a los efectos de la inmigración sobre la economía del país. El objetivo de este trabajo es caracterizar y analizar los efectos de la inmigración sobre el mercado laboral en Chile y la situación de los migrantes en el mercado laboral local. Utilizando los datos de la encuesta CASEN 2006 y 2009, y los datos de Extranjería del Ministerio del Interior y del Ministerio de Relaciones Exteriores, encontramos que ...

  7. Mercados emisores y competencia multicultural del profesional de turismo

    OpenAIRE

    Orlando Cedeño-Almaguer

    2012-01-01

    Se abordó la necesidad de diversificar el mercado turístico cubano en función de hacerlo más competitivo frente a la diversidad sociocultural de sus mercados emisores, superando las estrecha opción de sol y playa, sobre la base de nuevas alternativas que contemplen las riquezas paisajísticas y culturales del país, así como las variadas expectativas de los visitantes. La solución a esta situación está vinculada con la calidad del desempeño del profesional de turismo, el cual se sustenta en ...

  8. Is there a geochemical link between volcanic and plutonic rocks in the Organ Mountains caldera?

    Science.gov (United States)

    Memeti, V.; Davidson, J.

    2013-12-01

    Results from separate volcanic and plutonic studies have led to inconsistent conclusions regarding the origins and thus links between volcanic and plutonic systems in continental arcs and the magmatic processes and time scales responsible for their compositional variations. Some have suggested that there is a geochemical and geochronological disconnect between volcanic and plutonic rocks and hence have questioned the existence of magma mush columns beneath active volcanoes. Investigating contemporary volcanic and plutonic rocks that are spatially connected is thus critical in exploring these issues. The ca. 36 Ma Organ Mountains caldera in New Mexico, USA, represents such a system exposing contemporaneous volcanic and plutonic rocks juxtaposed at the surface due to tilting during extensional tectonics along the Rio Grande Rift. Detailed geologic and structural mapping [1] and 40Ar/39Ar ages of both volcanics and plutons [2] demonstrate the spatial and temporal connection of both rock types with active magmatism over >2.5 myr. Three caldera-forming ignimbrites erupted within 600 kyr [2] from this system with a total erupted volume of 500-1,000 km3 as well as less voluminous pre- and post-caldera trachyte and andesite lavas. The ignimbrite sequence ranges from a crystal-poor, high-SiO2 rhyolite at the base to a more crystal-rich, low-SiO2 rhyolite at the top. Compositional zoning with quartz-monzonite at the base grading to syenite and alaskite at the top is also found in the Organ Needle pluton, the main intrusion, which is interpreted to be the source for the ignimbrites [1]. Other contemporaneous and slightly younger plutons have dioritic to leucogranitic compositions. We examined both volcanic and plutonic rocks with petrography and their textural variations with color cathodoluminescence, and used whole rock element and Sr, Nd and Pb isotope geochemistry to constrain magma compositions and origins. Electron microprobe analyses on feldspars have been completed to

  9. Subduction polarity of the prototethys: insights from the Yirba pluton of the western Kunlun range, NW China

    OpenAIRE

    C. Yuan; M. Sun; Xiao, WJ; Zhou, H.; Hou, QL; Li, JL

    2003-01-01

    The Yirba (128 km) pluton is an early Paleozoic dioritic intrusion of western Kunlun orogenic belt, northwest China as an important element when reconstructing the evolution history of this belt. Due to the scarcity of field data and methodological difference in studying this pluton, however, no consensus for its age, source and tectonic setting has been adopted. In this paper, we present new geochronological and geochemical data for the Yirba pluton, aiming to better understand its age, sour...

  10. Poder de mercado e dominância no mercado dos vedantes de cortiça

    OpenAIRE

    Soares, Rita Carolina Almeida

    2013-01-01

    A base deste relatório foi o estágio curricular desenvolvido na Amorim Cork Composites, uma das empresas do Grupo Amorim. Relativamente ao Grupo Amorim muitas são as afirmações de que este Grupo é dominante no mercado da cortiça mas, não existem estudos realizados que o comprovem. Daqui surgiu, então, a ideia de realizar um estudo para o mercado dos vedantes de cortiça, entre 2008 e 2012, sobre a concentração de mercado e dominância. Neste estudo é utilizada uma medida alternativa ao ín...

  11. Seguimiento al marco institucional del mercado de valores en Colombia. Los segundos mercados como instrumento de desarrollo de las pequeñas y medianas empresas

    Directory of Open Access Journals (Sweden)

    Constanza Blanco Barón

    2009-08-01

    Full Text Available Los segundos mercados de valores, mercados balcón o mercados paralelos, se han estructurado como mercados transitorios, de aclimatación al mercado de valores, para que las pequeñas y medianas empresas puedan optar por nuevas fuentes de financiamiento, dando solución a las dificultades y mayor costo que tienen estas empresas para su acceso al mercado. Este artículo muestra que en varios países del mundo, incluida Colombia, se establecieron segundos mercados diseñados según un modelo de segmentación vertical, que determinan requisitos de registro e información menos exigentes para la emisión en oferta pública, para abaratar los costos de emisión y negociación, y que estos modelos, no solamente fracasaron en tanto no cumplieron con lo esperado en cuanto a aumentar los recursos para financiar empresas pequeñas y medianas, sino que disminuyeron los estándares de protección a los inversionistas. En su lugar, se han venido desarrollando en el mundo terceros mercados, también llamados nuevos mercados, en el ámbito de la autorregulación, basados en el logro de estándares de gobierno corporativo y que sigue patrones de organización y procedimientos cercanos al mercado tecnológico nasdaq de estados unidos.

  12. La implementación de un mercado de futuros en el sector ganadero argentino

    OpenAIRE

    Dopchiz, Mariana Y.

    2008-01-01

    El presente trabajo de investigación tiene por objeto analizar las dificultades que presenta el sector ganadero argentino para implementar un mercado de futuros. Para alcanzar dicho fin, en primera instancia se exponen las condiciones teóricas necesarias para el eficaz funcionamiento del mercado ganadero, que posibiliten implementar un mercado de futuros. Luego, se presentan tres experiencias internacionales con mercados de futuros en carne exitosos y, seguidamente, se desarrollan los motivos...

  13. Huacas olvidadas y cerros santos: Apuntes metodológicos sobre la cartografía sagrada en los Andes del sur de Bolivia

    OpenAIRE

    Pablo Cruz

    2009-01-01

    A través de la articulación de fuentes coloniales tempranas con los registros arqueológicos y etnográficos locales, hemos identificado varios cerros sacralizados y huacas prehispánicas de las regiones de Potosí y Chuquisaca (Bolivia). A partir de tres casos: los cerros Potosí y Porco, el cerro Quiquijana y el cerro Poder de Dios, se exploran y analizan las dimensiones religiosas y políticas del culto a las montañas en los Andes surandinos.A combination of early colonial sources and local arch...

  14. Burn Severities, Fire Intensities, and Impacts to Major Vegation Types from the Cerro Grande Fire

    International Nuclear Information System (INIS)

    The Cerro Grande Fire resulted in major impacts and changes to the ecosystems that were burned. To partially document these effects, we estimated the acreage of major vegetation types that were burned at selected burn severity levels and fire intensity levels. To accomplish this, we adopted independently developed burn severity and fire intensity maps, in combination with a land cover map developed for habitat management purposes, as a basis for the analysis. To provide a measure of confidence in the acreage estimates, the accuracies of these maps were also assessed. In addition, two other maps of comparable quality were assessed for accuracy: one that was developed for mapping fuel risk and a second map that resulted from a preliminary application of an evolutionary computation software system, called GENIE. According to the burn severity map and the fire intensity map, the Cerro Grande Fire is estimated to have covered 42,885.4 acres and 42,854.7 acres, respectively. Of this, 57.0 percent was burned at low severity and 34.7 percent was burned at high severity. Similarly, 40.0 percent of the Cerro Grande Fire burned at high fire intensity, greater than 70 percent mortality, while 33.1 percent burned at moderately low intensity, 10 to 40 percent mortality. The most frequently burned cover types over the entire Cerro Grande Fire were ponderosa pine forest and mixed conifer forest, at approximately 43 percent each. However, portions of the fire that burned on Los Alamos National Laboratory (LANL) property were predominantly in ponderosa pine forests, whereas the Cerro Grande Fire burned primarily in mixed conifer forests on lands managed by other agencies. Some of the polygons of burn severities and fire intensities were extensive. The two largest burn severity polygons were 10,111 acres and 10,903 acres and these were burned at low severity. The next two largest polygons were 8999 acres (14 square miles) and 1551 acres (2.4 square miles) and both of these polygons

  15. Granite intrusion by externally induced growth and deformation of the magma reservoir, the example of the Plasenzuela pluton, Spain

    Science.gov (United States)

    Castro, Antonio; Fernández, Carlos

    1998-09-01

    The Plasenzuela pluton in the Central Extremadura batholith in the southern Iberian Massif, is an example of permissive emplacement in relation to the tectonic development of extensional fractures in the upper continental crust. Paradoxically, this pluton has a concordant structural pattern which is classically attributed to diapirism or ballooning. This pattern consists of the following elements: (a) nearly elliptical shape in the horizontal section; (b) conformity of the pre-existing aureole structures to the shape of the pluton contacts; and (c) development of a crenulation cleavage, parallel to the contacts, in the vicinity of the pluton walls. All these features have been interpreted in many plutons as resulting from the pushing-aside of the country rock structures due to the expansion of the pluton. However, the detailed structural relationships in the aureole do not favour a forceful emplacement mechanism. By contrast, these relationships constitute prime evidence of permissive intrusion in extensional fractures. According to this interpretation, the concordant shape of the pluton was acquired by syn-plutonic opening of a mixed tensional-shear fracture, parallel to the main foliation in the host rocks, and by folding of the fracture walls together with the previous anisotropy of the country rocks. This is a growth-deformation process that can operate at local conditions in the upper continental crust giving rise to concordant syn-tectonic plutons.

  16. Mercado laboral en Chile: Nota técnica sectorial

    OpenAIRE

    Graciana Rucci

    2011-01-01

    La presente nota técnica presenta un panorama del mercado laboral chileno y su contexto a nivel nacional. Esta nota incluye un diagnóstico del sector, la programación del BID para el período 2010-2014 y una matriz de resultados.

  17. La nueva pobreza en el mercado de trabajo

    OpenAIRE

    Climent Sanjuán, Víctor

    2015-01-01

    El presente trabajo tiene por objeto analizar una nueva realidad laboral, distante de las propias de los años 80 y 90 del siglo pasado, que está configurando un nuevo modelo de pobreza dentro del mercado de trabajo

  18. A HIPÃTESE CONJUNTA DO CAPM E MERCADO EFICIENTE

    Directory of Open Access Journals (Sweden)

    César Martins Guimarães

    2006-05-01

    Full Text Available O CAPM é utilizado para testar a eficiência de mercados desde o final dos anos 1960. O objetivo deste trabalho foi testar a hipótese conjunta do CAPM e da eficiência do mercado brasileiro de ações nos cinco anos compreendidos entre abril de 2000 e março de 2005, através da análise do desempenho de fundos mútuos de ações. O Alfa de Jensen foi escolhido como medida de retorno extraordinário dos fundos de ações, por considerar o ajuste do resultado em relação exposição da carteira ao risco sistemático. Os dados apontaram que não há evidências de ineficiência de mercado para o período analisado, assumindo-se ser o IBX e o Ibovespa índices representativos da carteira de mercado e o CDI de um dia uma taxa representativa do ativo livre de risco.

  19. A HIPÓTESE CONJUNTA DO CAPM E MERCADO EFICIENTE

    Directory of Open Access Journals (Sweden)

    César Martins Guimarães

    2006-05-01

    Full Text Available O CAPM é utilizado para testar a eficiência de mercados desde o final dos anos 1960. O objetivo deste trabalho foi testar a hipótese conjunta do CAPM e da eficiência do mercado brasileiro de ações nos cinco anos compreendidos entre abril de 2000 e março de 2005, através da análise do desempenho de fundos mútuos de ações. O Alfa de Jensen foi escolhido como medida de retorno extraordinário dos fundos de ações, por considerar o ajuste do resultado em relação � exposição da carteira ao risco sistemático. Os dados apontaram que não há evidências de ineficiência de mercado para o período analisado, assumindo-se ser o IBX e o Ibovespa índices representativos da carteira de mercado e o CDI de um dia uma taxa representativa do ativo livre de risco.

  20. Los componentes de la orientación al mercado : un estudio exploratorio en el mercado del seguro en Europa y Estados Unidos

    OpenAIRE

    Lado, Nora

    1999-01-01

    A pesar de la importancia creciente del estudio de la orientación hacia el mercado de las empresas (OM) todavía son escasas las investigaciones que comparan resultados entre diferentes mercados, especialmente Europa y Estados Unidos. Esta carencia limita la comprensión de la OM como una estrategia competitiva válida en el ámbito de los mercados globales. La presente investigación tiene como objetivo explorar en qué medidad son extensibles al mercado americano resultados previos obtenidos en e...

  1. Physical Properties and Distribution of Intrusive Rocks (Plutons) in the Great Basin

    Science.gov (United States)

    Ponce, D. A.; Watt, J. T.; Glen, J. M.

    2010-12-01

    The distribution of intrusive rocks throughout the Great Basin is important because many plutons are associated with base and precious metal mineral deposits, and may provide insights on regional magmatism and tectonism. Combined information on their physical properties and geophysical signatures will allow improvements on their inferred horizontal extent and facilitate modeling their subsurface structure. Physical property measurements of over 1700 plutonic rock samples in the Great Basin, excluding those in the Sierra Nevada, show an average grain density of about 2670 and a range of about 2260 to 3200 kg/m3; show an average saturated bulk density of about 2630 and a range of about 2290 to 3050 kg/m3; an average magnetic susceptibility of about 0.007 and range from essentially non-magnetic to 0.126 SI-units (equivalent to just over 3 per cent magnetite). As a comparison, over 6,000 granitic samples in the Sierra Nevada (Sikora et al., 1991) have an average grain density of about 2690 and a range of about 2420 to 2780 kg/m3; an average magnetic susceptibility of about 0.006 and range from essentially non-magnetic to 0.016 SI-units (equivalent to about 0.4 per cent magnetite). Remanent magnetizations were measured for selected plutons, for example the remanent magnetization of the Ibapah pluton in the Deep Creek Range, Utah is relatively low and has a Koenigsberger ratio (the ratio between remanent and induced magnetization) of about 0.1. In Nevada, previous pluton extents (Grauch et al., 1988; Grauch , 1996) have been only slightly modified. For example, the Cretaceous to Jurassic stock at Blue Mountain, north-central Nevada (Wilden, 1964) is now mapped as a diorite dike swarm (Wyld, 2002) and thought to be mid-Miocene and related to the inception of the Yellowstone Hotspot (Ponce et al, 2010). Magnetic and gravity data indicate that a possible pluton (or other magnetic basement rock), the top of which could be at moderate crustal depths, is skewed from the

  2. Areas to explore surrounding the Cerro Prieto geothermal field, BC; Areas para exploracion en los alrededores del campo geotermico de Cerro Prieto, BC

    Energy Technology Data Exchange (ETDEWEB)

    Aguilar Dumas, Alvaro [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia General de Cerro Prieto, Mexicali, Baja California (Mexico)]. E-mail: alvaro.aguilar@cfe.gob.mx

    2009-07-15

    Exploration plays an important role in tapping underground natural resources-whether water, oil, natural gas or minerals. Exploratory data allow us to learn reservoir conditions, increasing probable reserves and reservoir life span. Around the Cerro Prieto geothermal field, BC, and in the Mexicali Valley in general, exploration had almost stopped but recently was resumed by the Studies Division of Comision Federal de ELectricidad (CFE)'s Gerencia de Proyectos Geotermoelectricos. The division sent technical personnel to structurally map the northern and eastern portions of Laguna Salada. The paper offers a general outline of the main zones undergoing exploratory studies-studies perhaps culminating in siting exploratory wells to locate more geothermal resources (and ultimately producing them using binary power plants). CFE also wants to site injection wells west of the current production zone, and this is covered, as well. All activities are meant to increase the productive lifespan of the geothermal reservoir. [Spanish] Cuando se trata de la explotacion de recursos naturales del subsuelo, sea agua, gas, petroleo o minerales, la exploracion juega un papel muy importante, ya que permite conocer las condiciones del yacimiento que pudieran llevar a incrementar las reservas de los recursos explotados y extender su vida util. En las zonas aledanas al campo geotermico de Cerro Prieto, BC, y en general en el Valle de Mexicali, la exploracion estaba practicamente detenida habiendose reactivado a raiz de que la Subgerencia de Estudios de la Gerencia de Proyectos Geotermoelectricos de la Comision Federal de Electricidad (CFE) envio personal para realizar mapeos estructurales en las porciones norte y oriente de la Laguna Salada. Este trabajo presenta un panorama general de las areas prioritarias para realizar estudios exploratorios y poder programar, con mas bases, pozos exploratorios enfocados a localizar mas recursos geotermicos, inclusive para generar energia por medio

  3. Basic aspects of the Cerro Prieto reservoir water recharge; Aspectos basicos de la recarga de agua al reservorio de Cerro Prieto

    Energy Technology Data Exchange (ETDEWEB)

    Mercado, Sergio [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

    1991-12-31

    The Cerro Prieto geothermal field, located 30 km South of Mexicali City, Baja California, has at present an installed capacity of 620 MW in geothermal power plants, that operating with endogenous steam, make use of the underground energy by means of deep wells, from which about 80 million cubic meters per year of high enthalpy water and steam mixture are extracted. During the exploitation physical an chemical changes in the hydrothermal fluids discharged by the wells have been detected, which shows, among other things, an elevated water recharge, located towards the West area of the field and a low recharge in the part of the east zone area. For this reason the hot brine waste re-injection is recommended, (previously treated to eliminate the silica excess) to thermally an hydraulically recharge the reservoir in that part of the field. [Espanol] El campo geotermico de Cerro Prieto, situado a 30 km al sur de la ciudad de Mexicali, Baja California, cuenta actualmente, despues de 18 anos en explotacion, con 620 MW de capacidad instalada en plantas geotermoelectricas que, operando con vapor endogeno, aprovechan la energia del subsuelo mediante pozos profundos de los que se extraen alrededor de 80 millones de metros cubicos por ano de una mezcla de agua vapor de elevada entalpia. Durante la explotacion se han percibido cambios fisicos y quimicos en los fluidos hidrotermales descargados por los pozos, lo que indica, entre otras cosas, una recarga elevada de agua localizada hacia el poniente del campo y una recarga baja en una zona de la parte oriental. Por ello se recomienda la reinyeccion de salmuera geotermica caliente de desecho (previamente tratada para eliminar el exceso de silice) para recargar termica e hidraulicamente el reservorio en esa parte del campo.

  4. Hydraulic model and steam flow numerical simulation of the Cerro Prieto geothermal field, Mexico, pipeline network

    International Nuclear Information System (INIS)

    The development of a hydraulic model and numerical simulation results of the Cerro Prieto geothermal field (CPGF) steam pipeline network are presented. Cerro Prieto is the largest water-dominant geothermal field in the world and its transportation network has 162 producing wells, connected through a network of pipelines that feeds 13 power-generating plants with an installed capacity of 720 MWe. The network is about 125 km long and has parallel high- and low-pressure networks. Prior to this study, it was suspected that steam flow stagnated or reversed from its planned direction in some segments of the network. Yet, the network complexity and extension complicated the analysis of steam transport for adequate delivery to the power plants. Thus, a hydraulic model of the steam transportation system was developed and implemented numerically using an existing simulator, which allowed the overall analysis of the network in order to quantify the pressure and energy losses as well as the steam flow direction in every part of the network. Numerical results of the high-pressure network were obtained which show that the mean relative differences between measured and simulated pressures and flowrates are less than 10%, which is considered satisfactory. Analysis of results led to the detection of areas of opportunity and to the recommendation of changes for improving steam transport. A main contribution of the present work is having simulated satisfactorily the longest (to our knowledge), and probably the most complex, steam pipeline network in the world. - Highlights: • Extensive literature review of flow models of geothermal steam gathering networks. • Hydraulic model of the Cerro Prieto geothermal field steam network. • Selection and validation of the employed pressure-drop model. • Numerical flow simulation of the world's largest geothermal steam gathering network. • Detailed network pressure drop analysis and mapping of steam flow distribution

  5. Archaeological fieldwork in the Bronze Age site of Cerro de la Encina (Monachil, Granada

    Directory of Open Access Journals (Sweden)

    Aranda Jiménez, Gonzalo

    2005-06-01

    Full Text Available New archaeological fieldwork has been carried out from November 2003 to May 2004 in the Bronze Age site of Cerro de la Encina, due to the interest of the regional government of Andalusia in displaying the settlement for visitors. The aim of this fieldwork has been the systematic excavation of a large settlement area partially known thanks to the excavations developed at the beginning of 1980s. A first toccupation period belonging to the Argaric Culture has been documented, highlighting specially the funerary ritual characterized by individual inhumations located below dwellings. After a gap in the occupation of the settlement a new social group belonging to the Late Bronze Age Culture of Southeast of Spain inhabits the Cerro de la Encina.

    El interés de la Consejería de Cultura de la Junta de Andalucía por la musealización del yacimiento del Cerro de la Encina ha motivado el desarrollo de nuevas investigaciones arqueológicas cuya primera fase se ha desarrollado entre Noviembre de 2003 y Mayo de 2004. Los trabajos han consistido en la excavación sistemática de un área de poblado de grandes dimensiones parcialmente conocida por las investigaciones realizadas a principios de los años 80. Los resultados han sido del máximo interés documentándose un primer momento de ocupación perteneciente a la Cultura de El Argar en el que destaca su espectacular registro funerario integrado dentro de las áreas de habitación. Tras un periodo de abandono del yacimiento se produce una nueva ocupación correspondiente a una comunidad del Bronce Final del Sureste.

  6. Mercados futuro e à vista de câmbio no Brasil: o rabo abana o cachorro

    OpenAIRE

    André Ventura; Márcio Garcia

    2012-01-01

    Com base na nova literatura de microestrutura de mercados, comparamos os dois principais mercados cambiais no Brasil - o mercado à vista e o mercado futuro de curta maturidade - buscando identificar em qual dos mercados se dá a formação da taxa de câmbio. Analisa-se o funcionamento do mercado cambial no seu nível micro, isto é, nas suas instituições e nas assimetrias entre seus participantes, através da abordagem da microestrutura de mercados. Utiliza-se uma base de dados inédita que contém 1...

  7. Two-dimensional modeling of apparent resistivity pseudosections in the Cerro Prieto region

    Energy Technology Data Exchange (ETDEWEB)

    Vega, R.; Martinez, M.

    1981-01-01

    Using a finite-difference program (Dey, 1976) for two-dimensional modeling of apparent resistivity pseudosections obtained by different measuring arrays, four apparent resistivity pseudosections obtained at Cerro Prieto with a Schlumberger array by CFE personnel were modeled (Razo, 1978). Using geologic (Puente and de la Pena, 1978) and lithologic (Diaz, et al., 1981) data from the geothermal region, models were obtained which show clearly that, for the actual resistivity present in the zone, the information contained in the measured pseudosections is primarily due to the near-surface structure and does not show either the presence of the geothermal reservoir or the granitic basement which underlies it.

  8. Geo archaeology in Cerro Lutz site, paleoenvironmental and palaeo geographic implications. Province of Entre Rios, Argentina

    International Nuclear Information System (INIS)

    The aim of this paper is to present the geo morphological evolution of the Cerro Lutz archaeological site located in the Lower Par ana Delta, Argentina River (Gualeguaychu Department). This is to add information to the paleogeographic and paleoenvironmental scheme during the occupation of site and add data to refine the regional evolution of deltaic advance against the Parana River.The geomorphology of the delta is composed of landforms resulting from fluvial modeling, coastal ( wave and tidal ) and to a lesser extent wind.They have different relative ages and dating from the late Pleistocene to the present

  9. Uranium prospecting in Cerro Partido Region-Encruzilhada do Sul Basin-RS, Brazil

    International Nuclear Information System (INIS)

    The Cerro Partido residual basin is a shallow (85 meters) and small (25km2) sedimentary basin, a remainder of the erosive cicle, enclosed in the pre-cambrian granitic rocks of the Rio Grande do Sul Shield. Grades of 0.2+ U3O8 were found in its upper-paleozoic sandstones and shales drilles for uranium. The small size and thicknesses of these concentrations prevent their economic mining. However, the different levels of the shield exposed by tectonics, the intrusive granitic, riolitic and syenitic rocks, the anomalous uranium contents in sedimentary and crystalline rocks recommend further investigations on the shield area

  10. Inestabilidad de laderas en el barrio cerros de marín, maracaibo, estado zulia, venezuela

    OpenAIRE

    Katty Montiel; Yendry González Bravo; Crismar Loaiza Arellano; Edith Gouveia Muñetón

    2008-01-01

    Se propone la aplicación de técnicas que permitan establecer una zonificación de amenaza geomorfológica para el barrio Cerros de Marín del municipio Maracaibo, expresada en términos de inestabilidad y propensión al colapso de laderas. Se efectuó un estudio de las condiciones biofísicas como litología, procesos morfogenéticos, precipitaciones y el efecto de las actividades humanas, basado en el método heurístico de Van Westen. Mediante la teledetección, inspección de campo y ...

  11. Reconstruction of mid-crustal pluton assembly and evolution using trace elements in augite: Sausfjellet pluton, Bindal batholith, north-central Norway.

    Science.gov (United States)

    Coint, Nolwenn; Barnes, Calvin; Yoshinobu, Aaron; Prestvik, Tore; Barnes, Melanie

    2013-04-01

    The Sausfjellet pluton is a 445 Ma gabbroic to monzonitic body of 7 Km in diameter emplaced in two stages at ~700 MPa pressure. Stage 1 is a coarse pyroxene hornblende gabbro. Stage 2 intrudes a steep contact between marbles on the east and pelitic migmatites on the west. Stage 2 displays a gradational transition from hornblende biotite two-pyroxene diorite to hornblende biotite three-pyroxene quartz monzonite. This transition is accompanied by a decrease in the An content of normally-zoned plagioclase from An61 to An27. Much of the pluton consists of cumulate rocks, as illustrated by the presence of anorthosite and pyroxene-rich layers. In the western part of the intrusion, hosted by metapelitic rocks, incompatible element concentrations and bulk-rock ^18O increase to levels that cannot be explained by fractional crystallization. These increases were originally explained by AFC processes, but because of the cumulative nature of the rocks, it is difficult to assess magmatic processes using bulk rock compositions. Therefore, we analyzed trace element contents and core-to-rim zoning in augite as a proxy to track changes in melt composition. Augite is normally zoned, with lower incompatible element abundances in the cores than in the rims, consistent with evolution of the melt by fractional crystallization. However, instead of plotting along a single differentiation trend, augite compositions define two trends, which is inconsistent with a closed system. The most mafic rocks define a trend with lower REE contents and smaller (negative) Eu anomalies compared to those from the more evolved part of the pluton, although the two trends overlap in Zr content. The two trends correspond to the central, more mafic zone that intrudes marble and the western, more evolved zone that intrudes metapelites. The trend associated with the western zone consists of the same samples that show bulk-rock ^18O enrichment, and is best explained as resulting from assimilation of the host

  12. SITE CHARACTERISTICS OF THE SUMMIT OF CERRO CHAJNANTOR AT THE 5640 M ALTITUDE

    Directory of Open Access Journals (Sweden)

    K. Motohara

    2011-01-01

    Full Text Available Instituto de Astronomía de la Universidad de Tokio está promoviendo el proyecto TAO (University of Tokyo Atacama Observatory; Yoshii et al. 2010 para construir un telescopio infrarrojo en la cima de Cerro Chajnantor (altitud 5640 m en el desierto de Atacama en el Norte de Chile. Para la evaluación de las características del sitio, primero se realizó el monitoreo del tiempo atmosférico, la emisividad de nubes y el seeing durante 2006. 2007. La fracción despejada fue alta (>80% y la mediana del seeing en la banda V fue de tan solo 0."69. Un telescopio explorador de 1 m llamado miniTAO fue instalado y comenzó a observar en 2009. Con éste se han obtenido imágenes satisfactorias de Paα de hidrógeno 1.875 μm como también imágenes de 30.40 μm por primera vez desde un telescopio en tierra. Estos resultados demuestran que la cima de Cerro Chajnantor es uno de los mejores sitios para la astronomía infrarroja en la Tierra.

  13. Analysis of heavy oils: Method development and application to Cerro Negro heavy petroleum

    Energy Technology Data Exchange (ETDEWEB)

    Carbognani, L.; Hazos, M.; Sanchez, V. (INTEVEP, Filial de Petroleos de Venezuela, SA, Caracas (Venezuela)); Green, J.A.; Green, J.B.; Grigsby, R.D.; Pearson, C.D.; Reynolds, J.W.; Shay, J.Y.; Sturm, G.P. Jr.; Thomson, J.S.; Vogh, J.W.; Vrana, R.P.; Yu, S.K.T.; Diehl, B.H.; Grizzle, P.L.; Hirsch, D.E; Hornung, K.W.; Tang, S.Y.

    1989-12-01

    On March 6, 1980, the US Department of Energy (DOE) and the Ministry of Energy and Mines of Venezuela (MEMV) entered into a joint agreement which included analysis of heavy crude oils from the Venezuelan Orinoco oil belt.The purpose of this report is to present compositional data and describe new analytical methods obtained from work on the Cerro Negro Orinoco belt crude oil since 1980. Most of the chapters focus on the methods rather than the resulting data on Cerro Negro oil, and results from other oils obtained during the verification of the method are included. In addition, published work on analysis of heavy oils, tar sand bitumens, and like materials is reviewed, and the overall state of the art in analytical methodology for heavy fossil liquids is assessed. The various phases of the work included: distillation and determination of routine'' physical/chemical properties (Chapter 1); preliminary separation of >200{degree}C distillates and the residue into acid, base, neutral, saturated hydrocarbon and neutral-aromatic concentrates (Chapter 2); further separation of acid, base, and neutral concentrates into subtypes (Chapters 3-5); and determination of the distribution of metal-containing compounds in all fractions (Chapter 6).

  14. Photosynthesis within Mars' volcanic craters?: Insights from Cerro Negro Volcano, Nicaragua

    Science.gov (United States)

    Rogers, K. L.; Hynek, B. M.; McCollom, T. M.

    2011-12-01

    Discrete locales of sulfate-rich bedrocks exist on Mars and in many cases represent the products of acid-sulfate alteration of martian basalt. In some places, the products have been attributed to hydrothermal processes from local volcanism. In order to evaluate the habitability of such an environment, we are investigating the geochemical and biological composition of active fumaroles at Cerro Negro Volcano, Nicaragua, where fresh basaltic cinders similar in composition to martian basalts are altered by acidic, sulfur-bearing gases. Temperatures at active fumaroles can reach as high as 400°C and the pH of the steam ranges from red algae that inhabit acidic, geothermal environments. Many of sequences related to Ktedonobacteria and Actinobacteria have also been found in acid mine drainage environments. The Archaeal community was far less diverse, with sequences matching those of unclassified Desulfurococcales and unclassified Thermoprotei. These sequences were more distant from isolated species than the bacterial sequences. Similar bacterial and archaeal communities have been found in hot spring environments in Yellowstone National Park, Greenland, Iceland, New Zealand and Costa Rica. Some of Mars' volcanoes were active for billions of years and by analogy to Cerro Negro, may have hosted photosynthetic organisms that could have been preserved in alteration mineral assemblages. Even on a generally cold and dry Mars, volcanic craters likely provided long-lived warm and wet conditions and should be a key target for future exploration assessing habitability.

  15. Elemental analysis of pottery from Cerro de las Ventanas, Zacatecas, by INAA

    International Nuclear Information System (INIS)

    Fifteen ceramic fragments samples from Cerro de las Ventanas site, Zacatecas, were analyzed by instrumental neutron activation analysis. Thirty-two elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Cluster analysis and principal component analysis were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Meso american ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Mal paso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de las Ventanas represent a new and unique chemical fingerprint in the region. (Author)

  16. Elemental analysis of pottery from Cerro de las Ventanas, Zacatecas, by INAA

    Energy Technology Data Exchange (ETDEWEB)

    Lopez del Rio, H.; Mireles G, F. [Universidad Autonoma de Zacatecas, Unidad Academica de Estudios Nucleares, Calle Cipres No. 10, Fracc. La Penuela, 98068 Zacatecas (Mexico); Mendez C, R. Y. [Universidad Autonoma de Zacatecas, Unidad Academica de Antropologia, Apdo. Postal 555 Suc. C, Zacatecas (Mexico); Nicolas C, M. [Universidad Autonoma de San Luis Potosi, Coordinacion de Ciencias Sociales y Humanidades, Av. Industrias 101-A, Fracc. Talleres, 78494 San Luis Potosi (Mexico); Speakman, R. J. [Museum Conservation Institute, Smithsonian Institution, Suitland, 20746 Maryland (United States); Glascock, M. D. [Reactor Center, University of Missouri, Columbia, 65211 Missouri (United States)

    2009-10-15

    Fifteen ceramic fragments samples from Cerro de las Ventanas site, Zacatecas, were analyzed by instrumental neutron activation analysis. Thirty-two elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Cluster analysis and principal component analysis were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Meso american ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Mal paso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de las Ventanas represent a new and unique chemical fingerprint in the region. (Author)

  17. ‘Diffuse faulting’ in the Machu Picchu granitoid pluton, Eastern Cordillera, Peru

    Science.gov (United States)

    Mazzoli, Stefano; Vitale, Stefano; Delmonaco, Giuseppe; Guerriero, Vincenzo; Margottini, Claudio; Spizzichino, Daniele

    2009-11-01

    A series of batholiths, forming part of the 'roots' of a Permo-Liassic rift system, are exposed in the high Eastern Cordillera of central Peru as a result of tectonic inversion. Shortening of the Machu Picchu granitoid pluton was accommodated by widespread shear reactivation of primary joints, by a process termed here 'diffuse faulting'. Fault-like reactivation of precursor joint surfaces, marked by chlorite, epidote and quartz shear fibres, is locally evidenced by few centimetres offsets within apparently undeformed granite. Analysis of fault slip data indicates that shear reactivation of different joint sets was kinematically consistent with ENE oriented shortening. Less frequent mylonitic shear zones appear to have evolved from the common brittle precursors. Apart from rare phyllonitic shear zones, fluid-rock interaction along the brittle precursors was generally limited, and pluton deformation appears to be mainly controlled by the geometry and distribution of primary joints. Three main sets of reactivated joints can be recognized, characterized by oblique-slip kinematics with variable reverse and strike-slip components of motion. Theoretical modelling based on quantitative fracture analysis (scan-line data) and different displacement-length relationships applied to the main reactivated joint sets yield first-order estimates of pluton finite strain. The results suggest that bulk finite strain is oblate and essentially coaxial, and is characterized by horizontal shortening not exceeding 10%. Relatively small finite strains, integrated over the size of the pluton, still result in a few kilometres of crustal shortening.

  18. Geochronology and geochemistry of granite plutons from east Khasi hills, Meghalaya

    International Nuclear Information System (INIS)

    Discordant granite plutons at Kyrdem, Nongpoh and South Khasi intrude the basement gneisses and the overlying Shillong Group of metasediments in the Meghalaya Plateau. Porphyritic granitoids ranging in composition from quartz monazonite to granite represent the dominant component in all the three plutons. Common characteristics of these granitoids are spatial association with homblende dioritic rocks, dominantly potassic and metaluminous nature. A positive correlation of SiO2, Na2O+K2O, Rb, Rb/Sr and negative correlation of CaO, MgO, FeO(T), Sr, TiO2 with Differentiation Index in the Kyrdem pluton point to fractional crystallisation processes. Rb-Sr whole rock isochron data of the plutons yield ages in the range 480-690 Ma with initial 87Sr/86Sr ratios ranging from 0.70948-0.71482. Absence of post emplacement tectonothermal event is suggested by near concordant K-Ar biotite ages. A protracted thermal event during late proterozoic-early paleozoic (500-700 Ma), possibly related to mantle upwelling, possibly triggered the generation of these granitoids. (author). 14 refs., 9 figs. , 6 tabs

  19. The geochemistry, age, and origin of groundwater in a mafic pluton, East Bull Lake, Ontario, Canada

    International Nuclear Information System (INIS)

    Atomic Energy of Canada Ltd. (AECL) is conducting geoscience investigations of several plutons in Canada's Precambrian Shield as part of the Canadian Nuclear Fuel Waste Management Program, to determine whether such rock masses are suitable for the safe disposal of nuclear fuel waste. The East Bull Lake (EBL) gabbro-anorthosite layered complex is unique in this program as it is the only mafic pluton in which hydrogeological and hydrogeochemical studies have been conducted. These results can be compared with those of similar studies of granitic rocks which have been investigated more extensively. During the period, 1983-85, hydrogeological testing and hydrochemical sampling were conducted by the National Hydrology Research Institute of Environment Canada and AECL in boreholes drilled to depths of up to 850 m into the EBL pluton (Raven et al., 1987). This paper discusses the hydrogeochemistry of the pluton and identifies the major rock-water interactions controlling the chemistry. The spatial variability in chemistry will be shown to be related to the nature of the groundwater flow systems present at this site. The ages and origins of the groundwaters and their solutes are inferred from isotopic analyses

  20. Rock-Forming feldspars of the Khibiny alkaline pluton, Kola Peninsula, Russia

    Science.gov (United States)

    Ivanyuk, G. Yu.; Pakhomovsky, Ya. A.; Konopleva, N. G.; Kalashnikov, A. O.; Korchak, Yu. A.; Selivanova, E. A.; Yakovenchuk, V. N.

    2010-12-01

    This paper describes the structural-compositional zoning of the well-known Khibiny pluton in regard to rock-forming feldspars. The content of K-Na-feldspars increases inward and outward from the Main foidolite ring. The degree of coorientation of tabular K-Na-feldspar crystals sharply increases in the Main ring zone, and microcline-dominant foyaite turns into orthoclase-dominant foyaite. The composition of K-Na-feldspars in the center of the pluton and the Main ring zone is characterized by an enrichment in Al. This shift is compensated by a substitution of some K and Na with Ba (the Main ring zone) or by an addition of K and Na cations to the initially cation-deficient microcline (the central part of the pluton). Feldspars of volcanosedimentary rocks occurring as xenoliths in foyaite primarily corresponded to plagioclase An15-40, but high-temperature fenitization and formation of hornfels in the Main ring zone gave rise to the crystallization of anorthoclase subsequently transformed into orthoclase and albite due to cooling and further fenitization. Such a zoning is the result of filling the Main ring fault zone within the homogeneous foyaite pluton with a foidolite melt, which provided the heating and potassium metasomatism of foyaite and xenoliths of volcanosedimentary rocks therein. The process eventually led to the transformation of foyaite into rischorrite-lyavochorrite, while xenoliths were transformed into aluminum hornfels with anorthoclase, annite, andalusite, topaz, and sekaninaite.

  1. Corundum-group minerals in rocks of the Khibiny alkaline pluton, Kola Peninsula

    Science.gov (United States)

    Mikhailova, Yu. A.; Konopleva, N. G.; Yakovenchuk, V. N.; Ivanyuk, G. Yu.; Men'shikov, Yu. P.; Pakhomovsky, Ya. A.

    2007-12-01

    Five minerals of the corundum group have been identified in the Khibiny pluton with certainty. Corundum proper and karelianite occur only in hornfels after volcanic and sedimentary rocks. Xenoliths of hornfels mark the ring faults that bound foidalite within the field of foyaite. Hematite occurs in hydrothermally altered nepheline syenite and crosscutting hydrothermal veins related to the ring faults. Minerals of the ilmenite-pyrophanite series are present in all rocks of the pluton, including veins. Accessory ilmenite in foyaite varies from the manganese variety and pyrophanite in the inner and outer parts of the pluton to manganese-free ilmenite in zone of the Main Ring Fault. In xenoliths of volcanic rocks and alkaline ultramafic rocks, ilmenite is enriched in magnesium. The zoning in distribution of the above-mentioned minerals and the character of variation in their compositions from margins of the pluton to its center are consistent with the petrochemical zoning formed as a result of foyaite alteration of near ring faults.

  2. Field Guide to Plutonic and Metamorphic Rocks. Earth Science Curriculum Project Pamphlet Series PS-5.

    Science.gov (United States)

    Romey, William D.

    Suggested are methods for the collection of field evidence about processes that form plutonic and metamorphic rock. Description and discussion of these types of rocks are provided. The planning and execution of a successful field trip is discussed. Advanced field projects are also discussed. Included are five appendices, references, and a…

  3. The Fontaine Pluton : an early Ross Orogeny calc-alkaline gabbro from southern Victoria Land, Antarctica

    International Nuclear Information System (INIS)

    The Fontaine Pluton is a previously undescribed mafic intrusion outcropping at Fontaine Bluff on the south side of the Carlyon Glacier in southern Victoria Land, Antarctica. It is the southern-most member of a laterally extensive mafic suite emplaced at mid-crustal depths during the initial stages of the Ross Orogeny. The pluton comprises recrystallised hornblende-biotite gabbro, which in places shows well-defined centimetre to metre scale primary igneous layering. Recrystallised ultramafic enclaves composed of amphibole-chlorite-talc are inferred to be remnants of a chemically and mineralogically distinct cumulate fraction. The intrusion has a 87Sr/86Sr(i) ratio of 0.70679 and a 143Nd/144Nd(i) ratio of 0.51187 (εNd(i) = -1.2). This, coupled with other geochemical data, implies that the Fontaine Pluton was formed by c. 15% partial melting of a depleted mantle source that was subsequently contaminated by continental crust. Preliminary U-Pb geochronology on zircon suggests an emplacement age for the pluton of 546 ± 10 Ma. These new data indicate that Ross Orogeny magmatism in this area of southern Victoria Land was initiated in the late Neoproterozoic along a subducting plate margin. (author). 55 refs., 10 figs., 3 tabs

  4. Using micro-scale evidence to understand regional-scale hydrothermal alteration of plutonic rocks

    NARCIS (Netherlands)

    Plümper, O.; King, H. E.; Putnis, A.

    2009-01-01

    Subsolidus re-equilibration of plutonic feldspars induced by hydrothermal fluids provides a valuable record of fluid-rock interactions that affect large volumes of the Earth's continental crust (Taylor, 1977). The effect of hydrothermal fluids has important implications for the interpretation of the

  5. Insights Into the Formation of Rhyolite From the Searchlight Pluton: Evidence from Oriented Quartz Clusters

    Science.gov (United States)

    Froemming, N.; Deering, C. D.; Beane, R. J.; Bachmann, O.

    2012-12-01

    The Miocene Searchlight pluton (SLP) in the Colorado River extensional corridor of southern Nevada, is well-exposed and tilted near-vertical for exceptional cross-sectional study of magma reservoir dynamics and crystal fractionation of a mid- to upper-crustal pluton (3 to 13 km depth). The upper quartz monzonite section is dominated by minerals in apparent random orientation with a medium- to fine-grained texture due to direct contact with the cold host rock. The middle granitic section is dominated by coarse-grained quartz and feldspar, and interpreted to be a zone of extracted liquid from an intermediate magma. The lower monzonite section is composed of coarse-grained plagioclase and potassium feldspar. We used the crystallographic orientations of quartz clusters, as determined by Electron Backscatter Diffraction (EBSD), to test for crystal accumulation in the SLP. Clusters of quartz crystals with matched dipyramidal faces (parallel or Esterel twin orientation) may indicate a period of crystal accumulation. By analyzing representative samples from each section of the pluton, we found that the lower section (intermediate cumulate) and upper section (crystallization front) do not have quartz clusters with matched dipyramidal faces. Although plagioclase grains are aligned in the lower section, the late crystallization of quartz appears to have prevented aligned or preferred growth orientations. In contrast, the middle section has a high percentage of quartz clusters with matched dipyramidal faces - similar to that found in granite porphyry of the Vinalhaven pluton, Maine. The aligned grains may have formed by fractional crystallization, compaction and synneusis of the early forming quartz in this granitic section. We interpret the middle section of the Searchlight pluton as being similar to shallow, upper crustal plutons (3-8 km depth) such as Vinalhaven pluton. The deep vertical exposure of the SLP, shows that the middle section was formed from periodic episodes of

  6. Magnetic fabrics and their relationship with the emplacement of the Piracaia pluton, SE Brazil

    Science.gov (United States)

    Raposo, M. Irene B.; Pressi, Leonardo Frederico; de Assis Janasi, Valdecir

    2012-04-01

    Magnetic fabric and rock-magnetism studies were performed on the four units of the 578 ± 3-Ma-old Piracaia pluton (NW of São Paulo State, southern Brazil). This intrusion is roughly elliptical (~32 km2), composed of (i) coarse-grained monzodiorite (MZD-c), (ii) fine-grained monzodiorite (MZD-f), which is predominant in the pluton, (iii) monzonite heterogeneous (MZN-het), and (iv) quartz syenite (Qz-Sy). Magnetic fabrics were determined by applying both anisotropy of low-field magnetic susceptibility (AMS) and anisotropy of anhysteretic remanent magnetization (AARM). The two fabrics are coaxial. The parallelism between AMS and AARM tensors excludes the presence of a single domain (SD) effect on the AMS fabric of the units. Several rock-magnetism experiments performed in one specimen from each sampled units show that for all of them, the magnetic susceptibility and magnetic fabrics are carried by magnetite grains, which was also observed in the thin sections. Foliations and lineations in the units were successfully determined by applying magnetic methods. Most of the magnetic foliations are steeply dipping or vertical in all units and are roughly parallel to the foliation measured in the field and in the country rocks. In contrast, the magnetic lineations present mostly low plunges for the whole pluton. However, for eight sites, they are steep up to vertical. Thin-section analyses show that rocks from the Piracaia pluton were affected by the regional strain during and after emplacement since magmatic foliation evolves to solid-state fabric in the north of the pluton, indicating that magnetic fabrics in this area of the pluton are related to this strain. Otherwise, the lack of solid-state deformation at outcrop scale and in thin sections precludes deformation in the SW of the pluton. This evidence allows us to interpret the observed magnetic fabrics as primary in origin (magmatic) acquired when the rocks were solidified as a result of magma flow, in which steeply

  7. Presence of cross flow in the Cerro Prieto geothermal field, BC; Presencia de flujo cruzado en el campo geotermico de Cerro Prieto, BC

    Energy Technology Data Exchange (ETDEWEB)

    Rodriguez Rodriguez, Marco Helio [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia General de Cerro Prieto, Mexicali, Baja California (Mexico)]. E-mail: marco.rodriguez01@cfe.gob.mx

    2011-01-15

    During the development of Cerro Prieto geothermal field, BC, exploitation has increased gradually, causing a continuous drop in pressure to almost 100 bars in the central and eastern parts of the field. This has occurred despite the high natural recharge induced by the reservoir exploitation and helped by the high permeability of the reservoir and the wide availability of natural recharge of low-temperature water in the vicinity. The strata above the production zones have significantly lower temperatures than these zones, but due to the particular characteristics of the reservoir, do not have pressure drops. As the pressure of producing strata declines, the hydraulic pressure differential between them and the overlying strata increases. Thus in recent years the phenomenon of cross flow occurs with greater frequency and severity. In this paper, this phenomenon is analyzed, detailing the specific mechanisms favoring it and identifying the stage (drilling or workover) in which it commonly occurs. Rigorous supervision during these stages is crucial to identifying cross flow and to taking necessary measures to save the well. Cross flow cases are presented at different stages in the history of a well: during drilling, repair, before and during the stimulation, and during production. [Spanish] Durante el desarrollo del campo geotermico de Cerro Prieto, BC, la explotacion se ha incrementado en forma gradual provocando una continua caida de presion, que en las porciones central y oriente ha sido de casi 100 bars. Esto ha ocurrido a pesar de la enorme recarga natural inducida por la explotacion, favorecida por la alta permeabilidad del yacimiento y la gran disponibilidad de recarga natural de agua de baja temperatura en los alrededores del mismo. Los estratos ubicados encima de las zonas productoras presentan temperaturas significativamente menores que estos, pero debido a las caracteristicas particulares del yacimiento, no han presentado abatimiento en su presion. En la

  8. Un Modelo de Vectores Autorregresivos para el Mercado Financiero Chileno Un Modelo de Vectores Autorregresivos para el Mercado Financiero Chileno

    OpenAIRE

    Christian Johnson

    1992-01-01

    Un Modelo de Vectores Autorregresivos para el Mercado Financiero Chileno Using various econometric techniques, the paper estimates the impact that interest-rare-based stabilization policy has on asset prices. To this end, vector autoregresive (VAR), as well as cointegration, error correction, and bayesian models (BVAR) were used. The results show that the disequilibria in these markets resulting from diferent shock, disappear only one year after they occur. These findings suggest that there m...

  9. Minimal thermodynamic conditions in the reservoir to produce steam at the Cerro Prieto geothermal field, BC; Condiciones termodinamicas minimas del yacimiento para producir vapor en el campo geotermico de Cerro Prieto, B.C.

    Energy Technology Data Exchange (ETDEWEB)

    Rodriguez Rodriguez; Marco Helio [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia General de Cerro Prieto, Mexicali, Baja California (Mexico)]. E-mail: marco.rodriguez01@cfe.gob.mx

    2009-01-15

    Minimal thermodynamic conditions in the Cerro Prieto geothermal reservoir for steam production are defined, taking into account the minimal acceptable steam production at the surface, considering a rank of mixed-enthalpies for different well-depths, and allowing proper assessments for the impacts of the changes in fluid reservoir pressure and enthalpy. Factors able to influence steam production are discussed. They have to be considered when deciding whether or not to drill or repair a well in a particular area of the reservoir. These evaluations become much more relevant by considering the huge thermodynamic changes that have occurred at the Cerro Prieto geothermal reservoir from its development, starting in 1973, which has lead to abandoning some steam producing areas in the field. [Spanish] Las condiciones termodinamicas minimas del yacimiento geotermico de Cerro Prieto, BC, para producir vapor se determinan tomando en cuenta la minima produccion de vapor aceptable en superficie, considerando un rango de entalpias de la mezcla y para diferentes profundidades de pozos, lo que permite valorar adecuadamente el impacto de la evolucion de la presion y entalpia del fluido en el yacimiento. Se discuten los factores que pueden afectar la produccion de vapor, los cuales se deben tomar en cuenta para determinar la conveniencia o no de perforar o reparar un pozo en determinada zona del yacimiento. Estas evaluaciones adquieren gran relevancia al considerar los enormes cambios termodinamicos que ha presentado el yacimiento geotermico de Cerro Prieto, como resultado de su explotacion iniciada en 1973, lo que ha llevado a abandonar algunas zonas del campo para la produccion de vapor. Palabras Clave: Cerro Prieto, entalpia, evaluacion de yacimientos, politicas de explotacion, presion, produccion de vapor.

  10. Extension of the Cerro Prieto field and zones in the Mexicali Valley with geothermal possibilities in the future

    Energy Technology Data Exchange (ETDEWEB)

    Fonseca L, H.L.; de la Pena L, A.; Puente C, I.; Diaz C, E.

    1981-01-01

    This study concerns the possible extension of the Cerro Prieto field and identification of other zones in the Mexicali Valley with geothermal development potential by assessing the structural geologic conditions in relation to the regional tectonic framework and the integration of geologic and geophysical surveys carried out at Cerro Prieto. This study is based on data obtained from the wells drilled to date and the available geological and geophysical information. With this information, a geologic model of the field is developed as a general description of the geometry of what might be the geothermal reservoir of the Cerro Prieto field. In areas with geothermal potential within the Mexicali Valley, the location of irrigation wells with anomalous temperatures was taken as a point of departure for subsequent studies. Based on this initial information, gravity and magnetic surveys were made, followed by seismic reflection and refraction surveys and the drilling of 1200-m-deep multiple-use wells. Based on the results of the final integration of these studies with the geology of the region, it is suggested that the following areas should be explored further: east of Cerro Prieto, Tulecheck, Riito, Aeropuerto-Algodones, and San Luis Rio Colorado, Sonora.

  11. DIREITO DE PROPRIEDADE NO MEIO AMBIENTE E AS FALHAS DE MERCADO

    OpenAIRE

    Cardoso Caldas, Ingrid

    2013-01-01

    Este artigo faz uma abordagem sobre o direito de propriedade no meio ambiente e as falhas de mercado. O assunto é abordado com base em revisões bibliográficas pertinente ao tema, segundo o qual se estabelece o conceito de falhas de mercado, economia do meio ambiente e direito de propriedade. Verifica-se a relação existente entre as falhas de mercado no meio ambiente provenientes da ausência de direitos de propriedades.

  12. Evolution of tuff ring-dome complex: the case study of Cerro Pinto, eastern Trans-Mexican Volcanic Belt

    Science.gov (United States)

    Zimmer, Brian W.; Riggs, Nancy R.; Carrasco-Núñez, Gerardo

    2010-12-01

    Cerro Pinto is a Pleistocene rhyolite tuff ring-dome complex located in the eastern Trans-Mexican Volcanic Belt. The complex is composed of four tuff rings and four domes that were emplaced in three eruptive stages marked by changes in vent location and eruptive character. During Stage I, vent clearing produced a 1.5-km-diameter tuff ring that was then followed by emplacement of two domes of approximately 0.2 km3 each. With no apparent hiatus in activity, Stage II began with the explosive formation of a tuff ring ~2 km in diameter adjacent to and north of the earlier ring. Subsequent Stage II eruptions produced two smaller tuff rings within the northern tuff ring as well as a small dome that was mostly destroyed by explosions during its growth. Stage III involved the emplacement of a 0.04 km3 dome within the southern tuff ring. Cerro Pinto's eruptive history includes sequences that follow simple rhyolite-dome models, in which a pyroclastic phase is followed immediately by effusive dome emplacement. Some aspects of the eruption, however, such as the explosive reactivation of the system and explosive dome destruction, are more complex. These events are commonly associated with polygenetic structures, such as stratovolcanoes or calderas, in which multiple pulses of magma initiate reactivation. A comparison of major and trace element geochemistry with nearby Pleistocene silicic centers does not show indication of any co-genetic relationship, suggesting that Cerro Pinto was produced by a small, isolated magma chamber. The compositional variation of the erupted material at Cerro Pinto is minimal, suggesting that there were not multiple pulses of magma responsible for the complex behavior of the volcano and that the volcanic system was formed in a short time period. The variety of eruptive style observed at Cerro Pinto reflects the influence of quickly exhaustible water sources on a short-lived eruption. The rising magma encountered small amounts of groundwater that

  13. Geología de la región del Cerro Guanaquero, Río Diamante, Mendoza Geology of Cerro Guanaquero region, Diamante River, Mendoza

    Directory of Open Access Journals (Sweden)

    Federico Fuentes

    2008-03-01

    Full Text Available El estudio realizado presenta nuevos datos sobre un sector poco conocido de la Cordillera Principal de Mendoza, en la alta cuenca del río Diamante en las adyacencias del cerro Guanaquero, y los primeros datos geocronológicos de sus rocas volcánicas. Las unidades geológicas presentes en el área se dividen en cuatro grupos principales: secuencias sedimentarias mesozoicas marinas y continentales intensamente plegadas y falladas; intrusivos y volcanitas intermedias de edad neógena; rocas volcánicas pliocenas a recientes de composición intermedia a básica, y depósitos cuaternarios inconsolidados. El cerro Guanaquero, un estratovolcán pliocuaternario intensamente erosionado por glaciares pleistocenos, con sus 4.841 metros es el rasgo orográfico más prominente. Está constituido esencialmente por andesitas grises porfíricas, piroxénicas a biotíticas. Intercaladas con las coladas andesíticas se presentan depósitos piroclásticos, aglomerados volcánicos, ignimbritas y basaltos. La datación de una andesita por el método K-Ar en roca total arrojó una edad de 1,4 ± 0,1 Ma. La deformación ándica comenzó en forma de una faja plegada y corrida de piel fina, con pliegues por despegue en el sector occidental y por propagación de falla en el oriental. La compresión al oeste de los 69º47´O terminó por invertir la fallas normales del rift mesozoico. A lo largo de este meridiano se encuentra la falla más importante de la región, la que se ha correlacionado con la falla Malargüe, bien desarrollada en latitudes más australes. Esta falla limita la faja plegada y corrida del Aconcagua, de naturaleza epidérmica, y la faja plegada y corrida de Malargüe, controlada por la inversión tectónica del basamento. El volcanismo fue muy intenso en el Plioceno y el Cuaternario, correspondiendo a un período de empinamiento de la placa oceánica subducida, en el que la región ha sido levantada pasivamente. La alta resistencia a la erosión de

  14. Simulador multi-agente para o mercado eléctrico

    OpenAIRE

    Marques, Paulo Alexandre Soares

    2008-01-01

    Esta dissertação, apresenta um simulador multi-agente para o mercado eléctrico. Neste simulador agentes heterogéneos, racionalmente limitados e com capacidade de aprendizagem, co-evoluem dinamicamente. O modelo de mercado apresentado é inspirado no mercado diário do MIBEL. É um modelo Pool, gerido por uma entidade operadora de mercado, onde compradores e vendedores podem licitar energia. No lado vendedor, empresas produtoras licitam a energia das suas unidades produtoras em pares ...

  15. Análisis del mercado interior de la electricidad: situación y perspectivas

    OpenAIRE

    Monreal Becerra, David

    2014-01-01

    El objetivo fundamental de este proyecto es el análisis de la integración de los mercados eléctrico europeos tal y como se plantea en el proyecto del Mercado Interior de la Electricidad. Se examinan igualmente las diferencias específicas que supone respecto al funcionamiento del mercado eléctrico español actual. Esta primera parte, más conceptual, se acompaña de una simulación del algoritmo que se encargará de sincronizar la ejecución de los mercados diarios de la electricidad ...

  16. Natural radiation at the Cerro Solo U-Mo deposit (Argentina)

    International Nuclear Information System (INIS)

    This paper presents results of work done to establish baseline levels of natural radiation in the vicinity of the Cerro Solo U-Mo deposit, prior to proposed uranium mining activities. This was accomplished through a number of Comision Nacional de Energia Atomica (CNEA) and International Atomic Energy Agency (IAEA) supported activities, including reprocessing and back-calibration of 1978-79 airborne gamma ray spectrometry data and acquisition of new ground gamma ray spectrometry data. The Cerro Solo U-Mo deposit is located in Chubut province in the southern Patagonia region of Argentina at 43 deg 20' south latitude and 68 deg 45' west longitude, at 630 metres above sea level. The deposit occurs as conformable layers and lenses within Cretaceous sandstone and conglomerate of Los Adobes Formation (Chubut Group). These units represent a high-energy fluvial system. The mineralized horizons occur between 60 and 120 metres below surface. Cretaceous tuffs of Cerro Barcino Formation (Chubut Group) and Jurassic andesitic rocks of the Lonco Trapial formation complement the main local geology. Regionally, a thin soil horizon is developed from the underlying bedrock. In 1978-79 the CNEA collected, under contract, approximately 100,000 line kilometres of multiparameter (gamma ray spectrometry and total field magnetic) airborne geophysical data (1) between 42 deg. - 47 deg. S and 67 deg. 30' - 70 deg. W. The survey was flown at a line spacing of 1 kilometre with a gamma ray detector volume of 48 litres. Stacked profiles and contour line maps were produced from the corrected counts for potassium, uranium and thorium. In cooperation with the IAEA and the Geological Survey of Canada (GSC) the original archive data from this survey was reprocessed and back-calibrated (2) to produce a corrected digital archive to be used for ongoing and future geological mapping, mineral exploration and environmental radiation monitoring. To support regional interpretation of the airborne geophysical

  17. Apatite trace element and halogen compositions as petrogenetic-metallogenic indicators: Examples from four granite plutons in the Sanjiang region, SW China

    Science.gov (United States)

    Pan, Li-Chuan; Hu, Rui-Zhong; Wang, Xin-Song; Bi, Xian-Wu; Zhu, Jing-Jing; Li, Chusi

    2016-06-01

    The abundances of trace elements including Sr, Ga and rare earth elements (REE) and halogens in apatite crystals from four intermediate-felsic plutons in the Zhongdian terrane in the Sanjiang region have been determined using electron microprobe and laser ablation inductively coupled plasma mass spectrometry to evaluate the potential of apatite as a petrogenic-metallogenic indicator. The selected plutons include one that is not mineralized (the Triassic Xiuwacu pluton, or the TXWC pluton), one that hosts a porphyry-type Cu deposit (the Pulang pluton, or the PL pluton), one that hosts a porphyry-type Mo deposit (the Tongchanggou pluton, or the TCG pluton), and one that hosts a vein-type Mo deposit (the Cretaceous Xiuwacu pluton, or the CXWC pluton). Except for the CXWC pluton, the other three plutons have adakite-like trace element signatures in whole rocks. The results from this study show that REE, Sr and halogens in apatite can be used to track magma compositions, oxidation states and crystallization history. Apatite crystals from the adakite-like plutons are characterized by much higher Sr/Y and δEu than the non-adakite-type pluton. This means that apatite, which is not susceptible to alteration, is a useful tool for identifying the adakite-like plutons that no longer preserve the initial Sr/Y ratios in whole rocks due to weathering and hydrothermal alteration. Based on apatite Ga contents and δEu values, it is inferred that the parental magmas for the two adakite-like plutons containing porphyry-type Cu and Mo mineralization are more oxidized than that for the non-adakite-type pluton containing vein-type Mo mineralization. Apatite crystals from the vein-type Mo deposit have much lower Cl/F ratios than those from the porphyry-type Cu and Mo deposits. Apatite crystals from the adakite-like pluton without Cu or Mo mineralization is characterized by much lower Cl/F ratios than those from the adakite-like plutons that host the porphyry-type Cu and Mo deposits. The

  18. The rapakivi granite plutons of Bodom and Obbnäs, southern Finland: petrography and geochemistry

    Directory of Open Access Journals (Sweden)

    Kosunen, P.

    1999-12-01

    Full Text Available The Obbnäs and Bodom granite plutons of southernmost Finland show the typical petrographic and geochemical features of the Proterozoic rapakivi granites in Finland and elsewhere: they cut sharply across the 1900 Ma Svecofennian metamorphic bedrock and have the geochemical characteristics of subalkaline A-type granites. The Bodom pluton is composed of porphyritic granites (hornblende-, hornblende-biotite-, and biotite-bearing varieties and an even-grained granite that probably represent two separate intrusive phases. This lithologic variation does not occur in the Obbnäs pluton, which is almost entirely composed of porphyritic hornblende-biotite granite that gradually becomes more mafic to the southwest. Three types of hybrid granitoids resulting from magma mingling and mixing occur on the southwestern tip of the Obbnäs peninsula. The Bodom granites are syenogranites, whereas the composition of the Obbnäs granite varies from syeno- to monzogranite. The main silicates of both the Bodom and Obbnäs granites are quartz, microcline, plagioclase (An1541, biotite (siderophyllite, and generally also amphibole (ferropargasite or hastingsite. Plagioclase-mantled alkali feldspar megacrysts are absent or rare. The accessory minerals are fluorite, allanite, zircon, apatite, and iron-titanium oxides; the Obbnäs granite also contains titanite. The Bodom and Obbnäs granites are metaluminous to weakly peraluminous, with average A/CNK of 1.00 and 1.05, respectively, have high Fe/Mg (average FeOtot/[FeOtot+MgO] is 0.94 for the Bodom and 0.87 for the Obbnäs granites, and high Ga/Al (3.78 to 5.22 in Bodom and 2.46 to 4.18 in Obbnäs. The REE contents are high with LREE-enriched chondrite-normalized patterns and moderate (Obbnäs to relatively strong (Bodom negative Eu-anomalies. The Obbnäs granite is enriched in CaO, TiO2, MgO, and FeO, and depleted in SiO2 and K2O compared to the Bodom granites. Also, there are differences in the Ba, Rb, and Sr contents of

  19. Mercados derivados de los derechos de emisión del protocolo de Kioto : ¿un nuevo mercado de futuros?

    OpenAIRE

    Domínguez Conde, María José; García Machado, Juan José

    2006-01-01

    Este trabajo analiza pormenorizadamente el mercado derivado de los derechos de emisión de gases de efecto invernadero (GEI) creado con la finalidad de cumplir con el Protocolo de Kioto, así como su evolución. Se trata de un mercado que, pese a su carácter incipiente, se está desarrollando con grandes volúmenes monetarios y avances de gestión importantes, aunque se le califica aún de inmaduro y de escasa liquidez. Se estudian los mecanismos de flexibilidad de dicho mercado, c...

  20. O ENSINO SUPERIOR EM TURISMO: HUMANO OU MERCADO?

    Directory of Open Access Journals (Sweden)

    Waléria Thabata Roldão Niquini

    2013-06-01

    Full Text Available Desde La creación de la educación superior en el Turismo en Brasil, en La década de 1970, se han producido algunas discusiones en relación a la formación del estudiante y su desempeño en el mercado laboral. Sin embargo hay varios puntos educativos significantes incluso antes de la aparición de la inserción profesional. La preparación de los estudiantes, las acciones de los maestros en la esfera de investigación y extensión y la necesidad del pensamiento crítico son supuestos que poden justificar tal curso mientras que la práctica educativa libertadora. Estas son las cuestiones discutidas en esta investigación destinada a comprender las perspectivas docente y dicente, en la licenciatura en Turismo, sobre la relación entre la enseñanza y el aprendizaje y sus aspectos esenciales, en una más amplia visión y menos fragmentada, entre la destacada dicotomía y el mercado de laboro y el pensamiento crítico científico. Se concluye que el debate académico sobre la educación en el Turismo todavía se disocia sólo entre los intereses del mercado y las discusiones humanas, sin una integración profunda en la relación enseñanza-aprendizaje.

  1. Dynamics of a geothermal field traced by noble gases: Cerro Prieto, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Mazor, E. (Weizmann Inst. of Science, Rehovot, Israel); Truesdell, A.H.

    1981-01-01

    Noble gases have been measured mass spectrometrically in samples collected during 1977 from producing wells at Cerro Prieto. Positive correlations between concentrations of radiogenic (He, /sup 40/Ar) and atmospheric noble gases (Ne, Ar, and Kr) suggest the following dynamic model: the geothermal fluids originated from meteoric water penetrated to more than 2500 m depth (below the level of first boiling) and mixed with radiogenic helium and argon-40 formed in the aquifer rocks. Subsequently, small amounts of steam were lost by a Raleigh process (0 to 3%) and mixing with shallow cold water occurred (0 to 30%). Noble gases are sensitive tracers of boiling in the initial stages of 0 to 3% steam separation and complement other tracers, such as Cl or temperature, which are effective only beyond this range.

  2. Stratigraphic and tectonic revision of Cerro Olivo Complex located of Southeastern of Uruguay

    International Nuclear Information System (INIS)

    This paper presents a stratigraphic and tectonic revision of Cerro Olivo Complex, located in the Southeastern part of the Uruguayan Predevonian Shield. This informal lithostratigraphic unit constitutes the country rock for the emplacement of late-orogenic granitoids, during Neoproterozoic to Cambrian times. This unit groups all the lithodemes affected by deformation and metamorphism. Recent studies indicate the presence of straight gneisses of quartzo-feldspathic composition in the coast of Maldonado Department. These rocks were interpreted as the result of intense deformation in high temperature. These tectonites base a new stratigraphic insight for the complex. They allow their lithotypes to be organized by petrotectonic features, being a function of PT conditions for every last strain process

  3. Did stresses from the Cerro Prieto Geothermal Field influence the El Mayor-Cucapah rupture sequence?

    Science.gov (United States)

    Trugman, Daniel T.; Borsa, Adrian A.; Sandwell, David T.

    2014-12-01

    The Mw 7.2 El Mayor-Cucapah (EMC) earthquake ruptured a complex fault system in northern Baja California that was previously considered inactive. The Cerro Prieto Geothermal Field (CPGF), site of the world's second largest geothermal power plant, is located approximately 15 km to the northeast of the EMC hypocenter. We investigate whether anthropogenic fluid extraction at the CPGF caused a significant perturbation to the stress field in the EMC rupture zone. We use Advanced Land Observing Satellite interferometric synthetic aperture radar data to develop a laterally heterogeneous model of fluid extraction at the CPGF and estimate that this extraction generates positive Coulomb stressing rates of order 15 kPa/yr near the EMC hypocenter, a value which exceeds the local tectonic stressing rate. Although we cannot definitively conclude that production at the CPGF triggered the EMC earthquake, its influence on the local stress field is substantial and should not be neglected in local seismic hazard assessments.

  4. Bottom Topography, Recent Sedimentation and Water Volume of the Cerro Prieto Dam, NE Mexico

    Science.gov (United States)

    Yutsis, V. V.

    2012-12-01

    Cerro Prieto dam, relatively small water reservoir in the NE of Mexico, is characterized by a very high velocity of recent sedimentation, irregular bottom topography and sub-bottom seepage. Very high resolution seismic study using non-linear parametric echo sounder SES-2000 was carried out in this water reservoir, which is one of the main resources of potable water for the Monterrey, the city with a population of about four million inhabitants. A strong difference between water depth and hence the volume capacity calculated by National Commission of Water (Comision Nacional del Agua, CNA), Digital Elevation Model (DEM), and acoustic data was discovered. Very high rate of recent sedimentation due to damming is discussed. SES data interpretation shows that the thickness of recent sediments due to siltation of the reservoir reaches 3.5-4.0 m. Differences between the CNA and SES data indicate storage losses from 8-10 up to 30 million cubic meters due to sedimentation.

  5. Comments on some of the drilling and completion problems in Cerro Prieto geothermal wells

    Energy Technology Data Exchange (ETDEWEB)

    Dominguez A, B.; Sanchez G, G.

    1981-01-01

    From 1960 to the present, 85 wells with a total drilling length exceeding 160,000 m have been constructed at Cerro Prieto, a modest figure compared to an oil field. This activity took place in five stages, each characterized by changes and modifications required by various drilling and well-completion problems. Initially, the technical procedures followed were similar to those used in the oil industry. However, several problems emerged as a result of the relatively high temperatures found in the geothermal reservoir. The various problems that have been encountered can be considered to be related to drilling fluids, cements and cementing operations, lithology, geothermal fluid characteristics, and casings and their accessories. As the importance of high temperatures and the characteristics of the geothermal reservoir fluids were better understood, the criteria were modified to optimize well-completion operations, and satisfactory results have been achieved to date.

  6. Hydrothermal alteration of sediments associated with surface emissions from the Cerro Prieto geothermal field

    Energy Technology Data Exchange (ETDEWEB)

    Valette-Silver, J.N.; Esquer P., I.; Elders, W.A.; Collier, P.C.; Hoagland, J.R.

    1981-01-01

    A study of the mineralogical changes associated with these hydrothermal vents was initiated with the aim of developing possible exploration tools for geothermal resources. The Cerro Prieto reservoir has already been explored by extensive deep drilling so that relationships between surface manifestations and deeper hydrothermal processes could be established directly. Approximately 120 samples of surface sediments were collected both inside and outside of the vents. The mineralogy of the altered sediments studied appears to be controlled by the type of emission. A comparison between the changes in mineralogy due to low temperature hydrothermal activity in the reservoir, seen in samples from boreholes, and mineralogical changes in the surface emission samples shows similar general trends below 180 C: increase of quartz, feldspar and illite, with subsequent disappearance of kaolinite, montmorillonite, calcite and dolomite. These mineral assemblages seem to be characteristic products of the discharge from high intensity geothermal fields.

  7. Study of the atmospheric conditions at Cerro Armazones using astronomical data

    CERN Document Server

    Lakicevic, Masha; Noll, Stefan; Kausch, Wolfgang; Unterguggenberger, Stefanie; Kerber, Florian

    2016-01-01

    Aims: We studied the precipitable water vapour (PWV) content near Cerro Armazones and discuss the potential use of our technique of modelling the telluric absorbtion lines for the investigation of other molecular layers. The site is designated for the European Extremely Large Telescope (E-ELT) and the nearby planned site for the Cherenkov Telescope Array (CTA). Methods: Spectroscopic data from the Bochum Echelle Spectroscopic Observer (BESO) instrument were investigated by using line-by-line radiative transfer model (LBLRTM) radiative transfer models for the Earths atmosphere with the telluric absorption correction tool molecfit. All observations from the archive in the period from December 2008 to the end of 2014 were investigated. The dataset completely covers the El Nino event registered in the period 2009-2010. Models of the 3D Global Data Assimilation System (GDAS) were used for further comparison. Moreover, for those days with coincidence of data from a similar study with VLT/X-shooter and microwave rad...

  8. Ordenación de espacios naturales: Los Cerros de Escazú (Costa Rica)

    OpenAIRE

    Zúñiga Venegas, William

    2004-01-01

    La presente tesis doctoral se realizó en Costa Rica, país del Istmo Centroamericano que ocupa el tercer lugar en extensión entre los siete países que lo integran, con un territorio de 51.100km2 y una población de 3.824.593 habitantes. De su extensión terrestre, por lo menos el 26% (13 286km2), cuenta con algún tipo de figura legal de protección ya sea ambiental o de los recursos naturales. El área específica de la investigación se localiza en la Zona Protectora de los Cerros de Escazú; que c...

  9. Using of gamma spectrometric data for geological mapping of the Berra Bonita Cerro Azul - PR - Brazil

    International Nuclear Information System (INIS)

    The present paper discuss a geological-geophysical study at Cerro Azul district, state of Parana, Brazil, in an area of 42 Km2. The district is part of the proterozoic Ribeira belt, and it contains metamorphic rocks, two syn collisional granitic intrusions (Tres Corregos and Morro Grande) as well as Mesozoic mafic dikes. Comparing geological map and gamma spectro metrical data (K, U, Th) aerial and terrestrial, it was observed that: the thorium values and profiles seem to reflect the distinct lithologies of the area; potassium maps and profiles show the contacts between granites and host rocks, as well as, the different facies at the Tres Corregos granite; comparing the U, K and Th values of the two granite bodies, Morro Grande is more radioactive. (author)

  10. MOVIMIENTOS DE LADERA Y PLANEAMIENTO URBANÍSTICO: EL CONFLICTO DEL CERRO DEL OPE, ARCHENA (MURCIA

    Directory of Open Access Journals (Sweden)

    María Dolores Gómez Moreno

    2009-01-01

    Full Text Available Los desprendimientos son un proceso natural que afecta, de forma generalizada en el Valle de Ricote, a las laderas del tipo cantil-talud. Su peligrosidad radica en que los bloques desprendidos del escarpe ruedan con facilidad, talud abajo, cuando son descalzados por efecto de la escorrentía superfi cial o desestabilizados por movimientos sísmicos. El planeamiento urbanístico se convierte en factor inductor del riesgo al clasifi car como urbanizables y urbanos suelos que, por su ubicación en pie de ladera, deberían excluirse de cualquier proceso urbanizador. Este es el caso de Archena en el entorno inmediato del cerro del Ope.

  11. Mid amphibolite facies metamorphism of harzburgites in the Neoproterozoic Cerro Mantiqueiras Ophiolite, southernmost Brazil

    Directory of Open Access Journals (Sweden)

    HARTMANN LÉO A.

    2003-01-01

    Full Text Available Valuable information is retrieved from the integrated investigation of the field relationships, microstructure and mineral compositions of harzburgites from the Neoproterozoic Cerro Mantiqueiras Ophiolite. This important tectonic marker of the geological evolution of southernmost Brazilian Shield was thoroughly serpentinized during progressive metamorphism, because the oldest mineral assemblage is: olivine + orthopyroxene + tremolite + chlorite + chromite. This M1 was stabilized in mid amphibolite facies - 550-600ºC as calculated from mineral equilibria. No microstructural (e.g. ductile deformation of olivine or chromite or compositional (e.g. mantle spinel remnant of mantle history was identified. A metamorphic event M2 occurred in the low amphibolite facies along 100 m-wide shear zones, followed by intense serpentinization (M3 and narrow 1-3 m-wide shear zones (M4 containing asbestos.

  12. Condiciones de las tensiones en los mercados financieros internacionales

    OpenAIRE

    Bobillo Álvarez, Cristian

    2015-01-01

    Toda crisis monetaria o financiera que estalla en las distintas economias o mercados internacionales requiere un tratamiento que explique como se ha llegado a esa situación de inestabilidad, y habitualmente, es un análisis que se realiza aposteriori por parte de la ciencia económica. Con todo esto, surgen diferentes modelos que tratan de explicar algunas crisis que se han dado en las economías mundiales en las últimas decadas y analizar las causas y consecuencias de cada una de ellas. A raiz ...

  13. Ensayos sobre la sonrisa de volatilidad en mercados de opciones

    OpenAIRE

    Serna Calvo, Gregorio

    2000-01-01

    La tesis comienza analizando los determinantes de la "sonrisa de volatilidad" en el mercado de opciones sobre el indice IBEX-35,obteniendose evidencia de causalidad lineal en el sentido de Granger de los costes de transacción, representados por el diferencial "bid-ask" relativo, ala forma de la sonrisa. A continuación, se propone un modelo de Black-Scholes ampliando donde la volatilidad depende del precio de ejercicio y del diferencial "bid-ask" relativo, obteniendose que dicho modelo no mejo...

  14. Estudio sobre el mercado de arrendamiento de vivienda en Colombia

    OpenAIRE

    Jorge Enrique Torres Ramírez

    2012-01-01

    Históricamente la producción formal de vivienda en Colombia ha presentado limitaciones en su dimensión y composición por la localización, el precio, el tipo de vivienda, etc. Esta oferta ha atendido las demandas de servicios habitacionales de los grupos de ingresos medios altos y altos. Los hogares de ingresos bajos y medios bajos han compensado esta condición del mercado principalmente mediante la producción informal y el arrendamiento. Sin embargo, la producción informal de vivienda acoge, ...

  15. World markets and dependence Mercado mundial y dependencia

    Directory of Open Access Journals (Sweden)

    Betz Karl

    1994-06-01

    Full Text Available This work is one of monetary Keynesianism, known as the Berlin School. The school proposes a monetary theory of production which links the real sector to the monetary sector and on this bases offers an explanation of underdevelopment and dependence. Capitalist relationships are seen as the quest for monetary surpluses over money investments; and money not only rules the decisions of economic agents but also govern contractual relations. Each currency is a system of relationships, a "monetary space". Therefore, the theory of international re1ations should include a market which
    does not exist in models of closed economies the currency market and the specific function of money in this context, i.e. the "external function". World markets have establish a hierarchy of currencies, some strong, others weak. The former enable their national interests to be imposed to the countries with weak currencies and these are relegated to a situation of indebtedness to the strong currencies, dependence and underdevelopment from which very few can
    escape.
    Este trabajo se inscribe en el keynesianismo monetario, conocido como "escuela de Berlín". Está escuela propone una teoría monetaria de la producción que vincula la esfera real con la monetaria y con base en ella explica el subdesarrollo y la independencia. Las relaciones capitalistas se caractesizan por la búsqueda de un excedente monetario sobre la inversión en dinero; el dinero no sólo determina los cálculos de los agentes económicos sino que también expresa las relaciones contractuales. Cada moneda expresa un sistema de relaciones, un espacio monetario. Por tanto, la teoría de las relaciones internacionales debe incluir un mercado que no existe en los mercados de economía cerrada, el mercado de divisas, así como la función específica del dinero en este contexto, es decir, la llamada "función externa". El mercado mundial establece una jerarquía monetaria que da lugar a las

  16. Bio-sociodiversidade: preservação e mercado

    Directory of Open Access Journals (Sweden)

    Mauro Leonel

    2000-04-01

    Full Text Available VÁRIOS estudos vêm revelando possibilidades de aproveitamento de conhecimentos indígenas e de outras culturas tradicionais, entre eles, medicamentos, cosméticos, novos materiais, alimentos, sementes e conservantes como produtos de mercado. A prática do mercado vem sendo a de apropriar-se desses bens culturais, registrá-los após adaptações e devolvê-los como mercadorias protegidas por patentes, inclusive aos países onde tais conhecimentos foram desenvolvidos, geralmente ao sul do Equador. Frente à escala da degradação social e ambiental, como na Amazônia, surgiu um novo otimismo, o de que resultados financeiros de tais produtos pudessem reverter às populações, modificando-se a legislação internacional e associando-se cooperativas de produtores com a biotecnologia e as transnacionais. O mercado, o principal adversário da preservação da bio e da sociodiversidade, seria assim convidado - empresas e consumidores - a tornar-se aliado da manutenção da floresta em pé e da diferença cultural, por exemplo, mediante certificados de origem. No entanto, são numerosos os entraves para que essas populações possam abrir brechas no mercado, ou nos sistemas internacionais de registro de patentes, frente à lógica da concentração de capital e tecnologia.SEVERAL studies have been revealing prospects of capitalizing on native knowledge and traditional cultures in order to launch new market products, such as drugs, cosmetics, new materials, foods, seeds and preservers. The market has adopted the practice of appropriating such cultural goods, which after slight adaptation are registered and turned out as patent-protected products and sold even to the countries where that knowledge was first developed, south of the equator as a rule. Vis-à-vis the social and evironmental degradation scale, as is the case of the Amazon area, a new optimism has risen: the hope that financial results from such products could benefit the native peoples

  17. Geometría en una plaza de mercado

    OpenAIRE

    Zambrano, Jennyfer Alejandra; Gónzalez, Jenny

    2011-01-01

    Se presenta parte de un proceso de investigación etnográfica que corresponde a las diferentes prácticas matemáticas que realiza un grupo de trabajadores del mercado Corabastos, vistas desde la etnomatemática enfocada en un contexto urbano y desde las actividades universales presentadas por Bishop (1999). Sin embargo, en esta ponencia centraremos la mirada en la actividad matemática que corresponde a diseñar en un contexto laboral, específicamente se trata de la aplicación de conceptos geométr...

  18. Estudio de viabilidad de un mercado en Cunit

    OpenAIRE

    Sayavera Giménez, Alberto; Vicente Barbero, Alexandra

    2010-01-01

    El trabajo que a continuación se expone tiene como objetivo desarrollar el estudio de las variables que determinan la viabilidad de la construcción y explotación de un mercado de producto fresco y ecológico, ubicado en la población de Cunit (Tarragona). La idea de este estudio surge de la carencia que presenta el municipio de Cunit, en cuanto a equipamientos se refiere, debido al inesperado aumento de la población que se produjo entre los años 1.990 y 2.000. Asimismo, el com...

  19. La competitividad del aguacate mexicano en el mercado estadounidense

    OpenAIRE

    Torres Preciado, Víctor Hugo

    2009-01-01

    Resumen El objetivo de esta investigación consiste en analizar la competitividad de las exportaciones del aguacate mexicano hacia Estados Unidos. Para tal fin, se aplica el Índice de Ventaja Relativa de Exportación (VRE) y el método de Participación Constante de Mercado (CMS). Los resultados sugieren que México es altamente competitivo en las exportaciones de aguacate y que esta tendencia parece sostenerse en los próximos años. Abstract This research aims to analyze the competitiveness of the...

  20. Distinctly different parental magmas for calc-alkaline plutons and tholeiitic lavas in the central and eastern Aleutian arc

    Science.gov (United States)

    Cai, Yue; Rioux, Matthew; Kelemen, Peter B.; Goldstein, Steven L.; Bolge, Louise; Kylander-Clark, Andrew R. C.

    2015-12-01

    Cenozoic calc-alkaline plutons that comprise the middle crust of the central and eastern Aleutians have distinct isotopic and elemental compositions compared to Holocene tholeiitic lavas in the same region, including those from the same islands. Therefore the Holocene lavas are not representative of the net magmatic transfer from the mantle into the arc crust. Compared to the lavas, the Eocene to Miocene (9-39 Ma) intermediate to felsic plutonic rocks show higher SiO2 at a given Fe/Mg ratio, and have higher εNd-εHf values and lower Pb-Sr isotope ratios. However, the plutonic rocks strongly resemble calc-alkaline Holocene volcanics with more "depleted" isotope ratios in the western Aleutians, whose composition has been attributed to significant contributions from partial melting of subducted basaltic oceanic crust. These data could reflect a temporal variation of central and eastern Aleutian magma source compositions, from predominantly calc-alkaline compositions with more "depleted" isotope ratios in the Paleogene, to tholeiitic compositions with more "enriched" isotopes more recently. Alternatively, the differences between central Aleutian plutonic and volcanic rocks may reflect different transport and emplacement processes for the magmas that form plutons versus lavas. Calc-alkaline parental magmas, with higher SiO2 and high viscosity, are likely to form plutons after extensive mid-crustal degassing of initially high water contents. This conclusion has overarching importance because the plutonic rocks are chemically similar to bulk continental crust. Formation of similar plutonic rocks worldwide may play a key role in the genesis and evolution of continental crust.

  1. Geochemistry and geochronology of the volcano-plutonic rocks associated with the Glojeh epithermal gold mineralization, NW Iran

    OpenAIRE

    Siani Majid Ghasemi; Mehrabi Behzad; Azizi Hossein; Wilkinson Camilla Maya; Ganerød Morgan

    2015-01-01

    Eocene to Oligocene volcano-plutonic rocks are widespread throughout NW Iran. The Tarom-Hashtjin metallogenic province is one of the most promising epithermal-porphyry ore mineralized districts in NW Iran. The Glojeh gold deposit, located in the center of this province, is a typical high to intermediate sulfidation epithermal system, spatially and temporally associated with a granite intrusion and associated high-K calc-alkaline to shoshonitic volcano-plutonic rocks. T...

  2. Petrology and U-Pb geochronology of buried Avalonian plutonic rocks on southeastern Cape Cod

    Science.gov (United States)

    Leo, G.W.; Mortensen, J.K.; Barreiro, B.; Phillips, J.D.

    1993-01-01

    Plutonic rocks have been intersected by two separate drill holes on souteastern Cape Cod. Hole CC2 is located about 7 km south of the Nauset anomaly, an east-northeast-trending magnetic lineament that was considered to separate the distinct plutonic zones of Avalon terrane. This drill hole intersected weakly foliated, fairly homogeneous biotite granite. Zircons from this granite give a U-Pb age of 584+9/-8 Ma. Hole CC1 is located about 12 km north of the Nauset anomaly. The drill core intersected foliated, sheared, biotite granodiorite and biotite-hornblende-clinopyroxene-quartz gabbro, metamorphosed to greenschist facies. The deformed and altered state of these rocks, as well as their geochemistry, suggest that their origin and possibly their ages are distinct from the granite in hole CC2. No datable zircons were obtained from rocks in CC1. -from Authors

  3. Isotopic studies of the late Archean plutonic rocks of the Wind River Range, Wyoming.

    Science.gov (United States)

    Stuckless, J.S.; Hedge, C.E.; Worl, R.G.; Simmons, K.R.; Nkomo, I.T.; Wenner, D.B.

    1985-01-01

    Two late Archaean intrusive events were documented in the Wind River Range by isotopic studies of the Rb-Sr and U-Th-Pb systems in whole-rock samples and the U-Pb systematics for zircon. An age of approx 2630(20) m.y. for the Louis Lake batholith and apparent ages of 2504(40) to 2575(50) m.y. for the Bear Ears pluton were obtained. Post-magmatic hydrothermal events approximately Tertiary in age, lowered delta 18O values and disturbed parent-daughter relationships in most of the isotopic systems investigated. The two intrusive units apparently were derived from different protoliths. Initial isotopic ratios and petrochemistry for the Louis Lake batholith are consistent with an early Archaean trondhjemitic to tonalitic source. The protolith for the Bear Ears pluton must have been subjected to high-grade metamorphism that caused loss of Rb and U prior to magma generation. -L.C.H.

  4. Contributions to pegmatite exploration within granitic plutons in Central and Northern Portugal

    OpenAIRE

    Pereira, B; Azevedo, J.; de Oliveira, J.; Dias, P. A.; Gomes, C. Leal; Carvalho, José

    2013-01-01

    Exploration programs for granitic pegmatites face the lack of detectable contrasts, either geophysical or geochemical, between pegmatites and their granitic host-rocks. The known productive sectors bearing pegmatites located inside granitic plutons, with economic interest for quartz and feldspar provide adequate field testing for alternative research, dealing with the peculiarities of lithological diversity and the arrangement of structural elements, around pegmatite swarms at suitable granit...

  5. Potassium-argon and lead-alpha ages of plutonic rocks, Bokan Mountain area, Alaska

    Science.gov (United States)

    Lanphere, M.A.; MacKevett, E.M., Jr.; Stern, T.W.

    1964-01-01

    Most of the granitic rocks in the Bokan Mountain area, southeastern Alaska, are early Paleozoic (probably Ordovician) judged by potassium-argon and lead-alpha age measurements. The Bokan Mountain Granite, the youngest intrusive unit in the area, belongs to a Mesozoic plutonic episode. These age measurements are the first direct evidence for the emplacement of early Paleozoic granitic intrusive rocks close to the Pacific margin of North America.

  6. Potassium-Argon and Lead-Alpha Ages of Plutonic Rocks, Bokan Mountain Area, Alaska.

    Science.gov (United States)

    Lanphere, M A; Mackevett, E M; Stern, T W

    1964-08-14

    Most of the granitic rocks in the Bokan Mountain area, southeastern Alaska, are early Paleozoic (probably Ordovician) judged by potassium-argon and lead-alpha age measurements. The Bokan Mountain Granite, the youngest intrusive unit in the area, belongs to a Mesozoic plutonic episode. These age measurements are the first direct evidence for the emplacement of early Paleozoic granitic intrusive rocks close to the Pacific margin of North America. PMID:17754670

  7. Tertiary plutonic rocks of southern Serbia Vardar Zone as dimension stone

    OpenAIRE

    Kurešević Lidja; Simić Vladimir

    2014-01-01

    Three granitoid plutons of south-Serbian part of the Vardar Zone, of Tertiary age were studied in order to establish their potential for utilization as dimension stone. These rocks vary in composition from quartzmonconite to quartzdiorite. Field study aimed at establishing the geological factors - presence of fractures, harmful minerals, alterations, jointing type and fabric homogeneity in order to determine the possibility of obtaining large size blocks of...

  8. Volcanic-plutonic connections in a tilted nested caldera complex in Hong Kong

    OpenAIRE

    Sewell, Roderick J.; Tang, Denise L.K.; Campbell, S. Diarmad G.

    2012-01-01

    Exceptional exposures of four, precisely-dated, Middle Jurassic to Early Cretaceous,silicic volcanic centers and their plutonic equivalents in Hong Kong have provided an excellent opportunity to examine close connections in time and space between magma chambers and their overlying calderas. Here, we describe a ~14 km crustal section through a collapsed caldera in southeastern Hong Kong where the intracaldera fill suggests that the magmatic discharge was of supereruption scale. The main subvol...

  9. Zircon LA-ICPMS study and petrogenesis simulation of Dahuabei pluton in the Wulashan area,Inner Mongolia

    Institute of Scientific and Technical Information of China (English)

    Dapeng Li; Yuelong Chen; Liemeng Chen; Zhong Wang; Jinbao Liu

    2009-01-01

    Dahuabei pluton in the Wulashan area,Inner Mongolia,is an alkaline and peraluminous granitic pluton.LA-ICPMS U-Pb dating of zircons indicates that this pluton crystallized at 330±10 Myr.The pluton did not experience apparent zircon fractionation.The consistent temperatures between Zr saturation (765℃) and the average zircon-rutile Ti equilibrium (780℃),together with zircon ages and their CL images,indicated that there were no inherited zircons in this pluton.Through the simulation of the dry-system crystallization process of magma cooling at 200 MPa and 1100-709℃,the phase diagram and composition evolution tendency of different phases were obtained.The magma reached its liquidus at 1069℃.Sanidine was the first crystallized phase;at 709℃ the residual magma was less than 4%,and the range of 1069-719℃ should be the most suitable approach to the real condition.It is shown that at least some part of the pluton underwent such isobaric equilibrium crystallization processes during its crystallization.

  10. Geochemical evaluation of felsic plutonic rocks in the eastern and southeastern Arabian Shield, Kingdom of Saudi Arabia

    Science.gov (United States)

    Du Bray, E.A.; Elliott, James E.; Stoeser, D.B.

    1983-01-01

    In a geochemical evaluation of the eastern and southeastern Arabian Shield, which included collection of 696 rock samples and 694 pan concentrate samples, a province of tin-anomalous granitoid plutons was defined. Pan concentrates collected in and around these plutons were enriched in tin and tungsten relative to the concentrate population. Rock samples of these leucocratic, muscovite-bearing, peraluminous granites contained anomalously high concentrations of lithium, fluorine, beryllium, lead, rubidium, niobium, yttrium, tin, bismuth, silver, and tungsten. Ten tin-anomalous plutons were located in the study area. The plutons are typically small, less than 10 km2 in areal extent, and circular to elliptical in plan view. The resource potential of these latest Proterozoic plutons has not been established; economically exploitable concentrations of tin, tungsten, molybdenum, or zinc may be present, and followup studies are warranted. Further, two of the plutons are characterized by higher than normal total-count radioactivity and have potential for uranium, thorium, or rare-earth element deposits.

  11. Un Modelo de Vectores Autorregresivos para el Mercado Financiero Chileno Un Modelo de Vectores Autorregresivos para el Mercado Financiero Chileno

    Directory of Open Access Journals (Sweden)

    Christian Johnson

    1992-03-01

    Full Text Available Un Modelo de Vectores Autorregresivos para el Mercado Financiero Chileno Using various econometric techniques, the paper estimates the impact that interest-rare-based stabilization policy has on asset prices. To this end, vector autoregresive (VAR, as well as cointegration, error correction, and bayesian models (BVAR were used. The results show that the disequilibria in these markets resulting from diferent shock, disappear only one year after they occur. These findings suggest that there may be some benefits associated to a monetary policy aimed at short run financial market stabilization. This might avoid strong and persistent disequilibria in equity and exchange market.

  12. Synthesis of the works of geophysical (electrical soundings) carried out in the region of the anomalies of Yerba Sola (Cerro Largo) Uruguay

    International Nuclear Information System (INIS)

    In this report has been studied geographical localization, geology, geophysics prospection, equipment and methods used and their results in Yerba Sola anomalies Province Cerro Largo and Fraile Muerto formation

  13. Two stages of isotopic exchanges experienced by the Ertaibei granite pluton, northern Xinjiang, China

    Institute of Scientific and Technical Information of China (English)

    刘伟

    2000-01-01

    18O/16O and D/H of coexisting feldspar, quartz, and biotite separates of twenty samples collected from the Ertaibei granite pluton, northern Xinjiang, China are determined. It is shown that the Ertaibei pluton experienced two stages of isotopic exchanges. The second stage of 18O/16O and D/H exchanges with meteoric water brought about a marked decrease in the δ18O values of feldspar and biotite from the second group of samples. The D/H of biotite exhibits a higher sensitivity to the meteoric water alteration than its 18O/16O. However, the first stage of 18O/16O exchange with the 18O-rich aqueous fluid derived from the dehydration within the deep crust caused the Δ18OQuariz-Feidspar reversal. It is inferred that the dehydration-melting may have been an important mechanism for anatexis. It is shown that the deep fluid encircled the Ertaibei pluton like an envelope which serves as an effective screen to the surface waters.

  14. Two stages of isotopic exchanges experienced by the Ertaibei granite pluton, northern Xinjiang, China

    Institute of Scientific and Technical Information of China (English)

    2000-01-01

    18O/16O and D/H of coexisting feldspar, quartz, and biotite separates of twenty samples collected from the Ertaibei granite pluton, northern Xinjiang, China are determined. It is shown that the Ertaibei pluton experienced two stages of isotopic exchanges. The second stage of 18O/16O and D/H exchanges with meteoric water brought about a marked decrease in the δ18O values of feldspar and biotite from the second group of samples. The D/H of biotite exhibits a higher sensitivity to the meteoric water alteration than its 18O/16O. However, the first stage of 18O/16O exchange with the 18O-rich aqueous fluid derived from the dehydration within the deep crust caused the δ18OQuartz-Feldspar reversal. It is inferred that the dehydration-melting may have been an important mechanism for anatexis. It is shown that the deep fluid encircled the Ertaibei pluton like an envelope which serves as an effective screen to the surface waters.

  15. Spinel-group minerals in rocks of the Khibiny alkaline pluton, Kola Peninsula

    Science.gov (United States)

    Ivanyuk, G. Yu.; Pakhomovsky, Ya. A.; Konopleva, N. G.; Yakovenchuk, V. N.; Men'shikov, Yu. P.; Mikhailova, Yu. A.

    2007-12-01

    Seven spinel-group minerals in various geological settings have been revealed in the rocks of the Khibiny pluton. Hercynite, gahnite, and vuorelainenite occur only in xenoliths of hornfels after volcanic and sedimentary rocks, whereas spinel and magnesiochromite occur in alkaline ultramafic rocks of dike series. Franklinite has been discovered in a low-temperature hydrothermal vein. Ubiquitous magnetite is abundant in foyaite, foidolites, alkaline ultrabasic rocks, and pegmatite and hydrothermal veins and may even be the main mineral in some foidolite varieties. The spinel-group minerals are characterized by various chemical compositions due to the fractionation of nepheline syenites resulting in formation of the Main ring of foidolites and apatite-nepheline ore. Like most other minerals found throughout the pluton, magnetite is characterized by variation in the chemical composition along the radial line from the contact with country Proterozoic volcanic rocks to the geometric center of the pluton. Toward the center, the total Ti and Mn contents in magnetite increase from 5 15 up to 40 at %.

  16. Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A.

    Science.gov (United States)

    Brew, David A.; Morrell, Robert P.

    1983-01-01

    About 30 percent of the 175,000-km2 area of southeastern Alaska is underlain by intrusive igneous rocks. Compilation of available information on the distribution, composition, and ages of these rocks indicates the presence of six major and six minor plutonic belts. From west to east, the major belts are: the Fairweather-Baranof belt of early to mid-Tertiary granodiorite; the Muir-Chichagof belt of mid-Cretaceous tonalite and granodiorite; the Admiralty-Revillagigedo belt of porphyritic granodiorite, quartz diorite, and diorite of probable Cretaceous age; the Klukwan-Duke belt of concentrically zoned or Alaskan-type ultramafic-mafic plutons of mid-Cretaceous age within the Admiralty-Revillagigedo belt; the Coast Plutonic Complex sill belt of tonalite of unknown, but perhaps mid-Cretaceous, age; and the Coast Plutonic Complex belt I of early to mid-Tertiary granodiorite and quartz monzonite. The minor belts are distributed as follows: the Glacier Bay belt of Cretaceous and(or) Tertiary granodiorite, tonalite, and quartz diorite lies within the Fair-weather-Baranof belt; layered gabbro complexes of inferred mid-Tertiary age lie within and are probably related to the Fairweather-Baranof belt; the Chilkat-Chichagof belt of Jurassic granodiorite and tonalite lies within the Muir-Chichagof belt; the Sitkoh Bay alkaline, the Kendrick Bay pyroxenite to quartz monzonite, and the Annette and Cape Fox trondhjemite plutons, all interpreted to be of Ordovician(?) age, together form the crude southern southeastern Alaska belt within the Muir-Chichagof belt; the Kuiu-Etolin mid-Tertiary belt of volcanic and plutonic rocks extends from the Muir-Chichagof belt eastward into the Admiralty-Revillagigedo belt; and the Behm Canal belt of mid- to late Tertiary granite lies within and next to Coast Plutonic Complex belt II. In addition, scattered mafic-ultramafic bodies occur within the Fairweather-Baranof, Muir-Chichagof, and Coast Plutonic Complex belts I and II. Palinspastic

  17. Despertando o mercado de trabalho para o idoso

    Directory of Open Access Journals (Sweden)

    Ana Maya Goto Uyehara

    2007-12-01

    Full Text Available O expressivo aumento do número de idosos que ocorreu no fim do século XX tem suscitado debates cada vez mais intensos sobre a qualidade de vida do homem no processo de envelhecimento. Este artigo pretende demonstrar que o trabalho pode articular outros projetos de vida para os idosos e evitar patologias psíquicas que decorrem da perda de identidade pessoal, da falta de envolvimento em atividades motivadoras, ou da adoção de formas de consumo e estilos de vida inadequados. Para tanto, opta-se por uma linha de explicação de caráter preventivo, sob duas vertentes: a primeira refere-se ao fato de que, se o trabalho enobrece o homem, cabe a ele adquirir ou melhorar suas competências individuais, adequando-as às novas exigências do mercado para continuar empregado, ou mesmo reativar sua vida profissional segundo novos projetos de vida. A segunda segue o rumo do descobrimento das potencialidades dos idosos pelas empresas, que podem adequar as qualidades e limitações deste segmento ao perfil das muitas funções existentes nas próprias organizações. A contratação/ manutenção de pessoas idosas no quadro de pessoal pode representar diferencial competitivo para as empresas atentas à sua imagem no mercado, distinguindo-a de seus concorrentes.

  18. MERCADO FUTURO DE CAFÉ : UM ESTUDO DE CASO.

    Directory of Open Access Journals (Sweden)

    TÁCITO AUGUSTO FARIAS

    2014-08-01

    Full Text Available Resumo: O café é a commodity agrícola brasileira que possui o mercado mais desenvolvido, dentre os contratos negociados na Bolsa de Mercadorias e Futuros (BM&F é o que apresenta negociações em maior volume, além de apresentar maiores volatilidades, tornando as operações de hedge uma importante ferramenta para diminuição de riscos para quem participa desse mercado. Realizando o hedge, o produtor acaba eliminando totalmente o risco de variação do preço só que passa a lidar o risco de variação de base. Deste modo, objetivou-se identificar o modelo mais adequado à análise do risco de base do café por meio dos índices Esalq e BM&F Os resultados empíricos sugerem a necessidade de modelagem da série pelo modelo ARIMA (Autorregressivo – Integrado – Média Móvel. Também foram utilizados os resultados da estatística U-Theil, que apresentam bons indicadores para fins de previsão.

  19. ¿Qué tan verde es tu mercado?

    Directory of Open Access Journals (Sweden)

    Wilmar R. Olaya-González

    2011-01-01

    Full Text Available El mercado de lo verde y lo ecológico es una tendencia indiscutible en nuestro mundo globalizado, que busca de alguna manera resarcir el daño infringido sobre el medio ambiente. Más allá de simple altruismo, la ecología se ha convertido en una moda, de la cual unos y otros toman ventaja a su mejor acomodo, haciendo del mercado de productos y servicios su tribuna; eco-diseño, planes de responsabilidad social y ambiental, campañas por el reciclaje y consumo de productos "más amigables" con el medio ambiente hacen parte del panorama que se intenta describir en esta reseña. Por medio de un estudio de caso, se hará énfasis en cómo la comunicación asume un papel crucial en la verdadera apropiación del concepto de "consumidor verde" y "consumidor responsable", de manera que la propuesta transversal de las tic se convierta en una herramienta no solo tecnológica, sino también de empoderamiento del papel que la sociedad puede representar en el cuidado de los recursos naturales.

  20. Análise do mercado de remessas: Portugal/Brasil

    OpenAIRE

    João Peixoto; António Vasco Marques

    2010-01-01

    Estudo para o conhecimento do mercado de remessas de imigrantes de Portugal para o Brasil. O estudo inclui as tendências e características actuais da imigração brasileira em Portugal e o contexto regulador do mercado.

  1. La economía colombiana en la década de los noventa: dilema entre el mercado interno y el mercado internacional.

    OpenAIRE

    Restrepo Uribe , Ramiro

    2011-01-01

    El proceso de "Apertura y Modernización" de la economía colombiana forzó a algunos sectores económicos al reto de la competencia internacional. En la década de los noventa el proceso produjo la caída de la participación relativa de la agricultura y la industria manufacturera en PIB y el sacrificio del mercado interno sin el correspondiente éxito en el mercado internacional.

  2. Reflexiones en torno a la vulnerabilidad social y residencial de los asentamiento informales de los cerros de Valparaíso, Chile

    OpenAIRE

    Bailey, Christine; Zenteno, Elizabeth

    2015-01-01

    El incendio del pasado abril del 2014 ha abierto una serie de reflexiones respecto a las condiciones y riesgos que viven miles de familias de asentamientos informales de los cerros de Valparaíso. Aplicando una serie de entrevistas en profundidad a mujeres residentes en los cerros y quebradas, el estudio apunta a comprender las condiciones que las llevaron a habitar en aquellas zonas, visualizando el lento e infinito proceso de construcción de sus viviendas y asentamiento ...

  3. A synthesis of palynological data from the Lower Permian Cerro Pelado Formation (Parana Basin, Uruguay): A record of warmer climate stages during Gondwana glaciations

    OpenAIRE

    Beri, A.; Martínez-Blanco, X.; Mourelle, D.

    2010-01-01

    This paper presents a synthesis of the palynological record in the Cerro Pelado Formation deposits (Lower Permian, Paraná basin, Cerro Largo Department, north-eastern Uruguay) based on pre-existing data and new findings. The successions studied in this formation consist mainly of non-marine to glacial-marine mudstones and sandy mudstones. The palynological assemblages yielded by 32 samples collected from two outcrops and thirty borehole samples demonstrate that not significant floral changes ...

  4. Report of the seismic activity at the Cerro Prieto B.C., Mexico, geothermal field during 1996; Reporte de la actividad sismica registrada en el campo geotermico de Cerro Prieto, B.C., Mexico, durante 1996

    Energy Technology Data Exchange (ETDEWEB)

    Escamilla Hernandez, Abelardo [Gerencia de Proyectos Geotermoelectricos de la Comision Federal de Electricidad, Morelia (Mexico)

    1997-05-01

    In February 1996 started the operation of the Seismic Network of Cerro Prieto Geothermal Field (RESICP). It is constituted by five digital stations with velocity sensors of three components and a natural period of one second. The network worked continuously until December 2, 1996. During this period, we located 270 events in the field area and its neighborhood, with coda-length magnitude 1Cerro Prieto Dos and Cerro Prieto Tres. The recorded activity is less than in Zone A, focal depths are between five and seven km, and the coda- length magnitude is 1Cerro Prieto volcano and to the NW of it. The activity was of swarm type mainly, and inside this zone was recorded the greater event for the region (M{sub c}=4.21, 30 August at 06:245 Universal Time), coda-length magnitude 1 Cerro Prieto (RESICP); consta de cinco estaciones de tipo digital, sensores de velocidad de tres componentes, y periodo natural de un segundo. Trabajo en forma ininterrumpida hasta el 2 de diciembre de 1996. Durante ese periodo se localizaron

  5. Corrosion in pipelines and well casings at the Cerro Prieto geothermal field, BC; Corrosion en tuberias de linea y de revestimiento de pozos del campo geotermico de Cerro Prieto, BC

    Energy Technology Data Exchange (ETDEWEB)

    Miranda Herrera, Carlos A.; Canchola Felix, Ismael; Raygoza Flores, Joaquin; Mora Perez, Othon [Comision Federal de Electricidad, Residencia General de Cerro Prieto, Mexicali, Baja California (Mexico)]. E-mail: carlos.miranda02@cfe.gob.mx

    2009-07-15

    In the area called Poligono Hidalgo, inside the Cerro Prieto IV zone in the Cerro Prieto geothermal field, BC, corrosion has occurred in the last few years on well casings and pipelines used for geothermal fluids. Corrosion test results are presented here for pipes, type API L-80 and ASTM A-53 grade B, which were subjected to condensate from wells 403 and 424. These wells have thrown corroded material from their respective casings. With these data we pinpoint corrosive conditions in this field area and determine which pipes are adequate to case wells in similar chemical, production conditions to minimize adverse effects and extend the life of the well, allowing more efficient exploitation of the deepest production zones in the reservoir. [Spanish] En el campo geotermico de Cerro Prieto, BC, dentro del area del Poligono Hidalgo en el sector conocido como Cerro Prieto IV, algunos pozos han presentado en los ultimos anos desgastes en sus tuberias de revestimiento y en las tuberias de linea para el transporte del fluido geotermico. Se presentan resultados de pruebas de corrosion con tuberias tipo API L-80 y ASTM A-53 grado B al ser sometidas al condensado de los pozos 403 y 424, los cuales han estado arrojando material de sus respectivas tuberias de revestimiento. Con estos datos se pretende conocer las condiciones corrosivas de esa zona del campo y determinar cual seria la tuberia ideal a utilizar en pozos con condiciones quimicas de produccion semejantes a fin de minimizar este efecto adverso y prolongar la vida de los pozos, a la vez que se permita la explotacion eficiente de las zonas productoras mas profundas del yacimiento.

  6. Natural radioactivity and radiation index of the major plutonic bodies in Greece

    International Nuclear Information System (INIS)

    The natural radioactivity of the major plutonic bodies in Greece, as well as the assessment of any potential health hazard due to their usage as decorative building materials is studied. One hundred and twenty one samples from every major plutonic body in Greece, including various rock-types from gabbro to granite, have been measured for their natural radioactivity using γ-spectrometry methodology. According to the experimental results, the natural radioactivity levels were ranged up to 315 Bq kg−1 for 226Ra, up to 376 Bq kg−1 for 232Th and up to 1632 Bq kg−1 for 40K, with arithmetic mean values and standard deviations of 74 (±51), 85 (±54) and 881 (±331) Bq kg−1 respectively, which are below the international representative mean values for granite stones. The excess on the effective dose received annually indoors due to granite tiles usage is estimated considering a standard room model where granite tiles with 1.5 cm in thickness cover only the floor of the room. The increment on the external γ-radiation effective dose rate shows a Gaussian distribution well dispersed below 0.3 mSv y−1, presenting a mean value of 0.14 (±0.06) mSv y−1. In case of the internal α-radiation a log-normal distribution is appeared scattering below 0.5 mSv y−1 with a mean value 0.19 (±0.13) mSv y−1, for a well-ventilated living environment. In case of a poor-ventilated room the increment on internal effective dose rate is estimated with a mean value 0.27 (±0.19) mSv y−1 scattering below 0.8 mSv y−1. The majority of the samples increase the external as well as the internal dose less than 30% of the maximum permitted limit of the effective dose rate. Therefore, at least from radiological point of view, the plutonic rocks of Greece could be safely used as decorative building materials. -- Highlights: • Data upon natural radioactivity of all the major plutons of Greece are presented. • The samples from Pelagonian zone present the lower excess of the total

  7. From Migmatites to Plutons: Power Law Relationships in the Evolution of Magmatic Bodies

    Science.gov (United States)

    Soesoo, Alvar; Bons, Paul D.

    2015-07-01

    Magma is generated by partial melting from micrometre-scale droplets at the source and may accumulate to form >100 km-scale plutons. Magma accumulation thus spans well over ten orders of magnitude in scale. Here we provide measurements of migmatitic leucosomes and granitic veins in drill cores from the Estonian Proterozoic basement and outcrops at Masku in SW Finland and Montemor-o-Novo, central Portugal. Despite the differences in size and number of measured leucosomes and magmatic veins, differences in host rock types and metamorphic grades, the cumulative width distribution of the studied magmatic leucosomes/veins follows a power law with exponents usually between 0.7 and 1.8. Published maps of the SE Australian Lachlan Fold Belt were used to investigate the distribution of granitoid pluton sizes. The granites occupy ca. 22 % of the 2.6 × 105 km2 area. The cumulative pluton area distributions show good power law distributions with exponents between 0.6 and 0.8 depending on pluton area group. Using the self-affine nature of pluton shapes, it is possible to estimate the total volume of magma that was expelled from the source in the 2.6 × 105 km2 map area, giving an estimated 0.8 km3 of magma per km2. It has been suggested in the literature that magma batches in the source merge to form ever-bigger batches in a self-organized way. This leads to a power law for the cumulative distribution of magma volumes, with an exponent m V between 1 for inefficient melt extraction, and 2/3 for maximum accumulation efficiency as most of the volume resides in the largest batches that can escape from the source. If m V ≥ 1, the mass of the magma is dominated by small batches; in case m = 2/3, about 50 % of all magma in the system is placed in a single largest batch. Our observations support the model that the crust develops a self-organized critical state during magma generation. In this state, magma batches accumulate in a non-continuous, step-wise manner to form ever

  8. Development of modal layering in granites: a case study from the Carna Pluton, Connemara, Ireland

    Science.gov (United States)

    McKenzie, Kirsty; McCarthy, William; Hunt, Emma

    2016-04-01

    Modal layering in igneous rocks uniquely record dynamic processes operating in magma chambers and also host a large proportion of Earth's strategic mineral deposits. This research investigates the origin of biotite modal layering and primary pseudo-sedimentary structures in felsic magmas, by using a combination of Crystal Size Distribution (CSD) analysis and Electron Probe Microanalysis (EPMA) to determine the mechanisms responsible for the development of these structures in the Carna Pluton, Connemara, Ireland. The Carna Pluton is a composite granodiorite intrusion and is one of five plutons comprising the Galway Granite Complex (425 - 380 Ma). Prominent 30 cm thick modal layers are defined by sharp basal contacts to a biotite-rich (20%) granite, which grades upward over 10 cm into biotite-poor, alkali-feldspar megacrystic granite. The layering strikes parallel to, and dips 30-60° N toward the external pluton contact. Pseudo-sedimentary structures (cross-bedding, flame structures, slumping and crystal graded bedding) are observed within these layers. Petrographic observations indicate the layers contain euhedral biotite and fresh undeformed quartz and feldspar. Throughout the pluton, alkali-feldspar phenocrysts define a foliation that is sub-parallel to the strike of biotite modal layers. Together these observations indicate that the intrusion's concentric foliation, biotite layers and associated structures formed in the magmatic state and due to a complex interaction between magma flow and crystallisation processes. Biotite CSDs (>250 crystals per sample) were determined for nine samples across three biotite-rich layers in a single unit. Preliminary CSD results suggest biotite within basal contacts accumulated via fractional crystallisation within an upward-growing crystal pile, likely reflecting the yield strength of the magma as a limiting factor to gravitational settling of biotite. This is supported by the abrupt decrease in mean biotite crystal size across

  9. Description of a New Galapagos Giant Tortoise Species (Chelonoidis; Testudines: Testudinidae from Cerro Fatal on Santa Cruz Island.

    Directory of Open Access Journals (Sweden)

    Nikos Poulakakis

    Full Text Available The taxonomy of giant Galapagos tortoises (Chelonoidis spp. is currently based primarily on morphological characters and island of origin. Over the last decade, compelling genetic evidence has accumulated for multiple independent evolutionary lineages, spurring the need for taxonomic revision. On the island of Santa Cruz there is currently a single named species, C. porteri. Recent genetic and morphological studies have shown that, within this taxon, there are two evolutionarily and spatially distinct lineages on the western and eastern sectors of the island, known as the Reserva and Cerro Fatal populations, respectively. Analyses of DNA from natural populations and museum specimens, including the type specimen for C. porteri, confirm the genetic distinctiveness of these two lineages and support elevation of the Cerro Fatal tortoises to the rank of species. In this paper, we identify DNA characters that define this new species, and infer evolutionary relationships relative to other species of Galapagos tortoises.

  10. Oxygen isotope exchange in rocks and minerals from the Cerro Prieto geothermal system: indicators of temperature distribution and fluid flow

    Energy Technology Data Exchange (ETDEWEB)

    Williams, A.E.; Elders, W.A.

    1981-01-01

    Oxygen isotopic compositions have been measured in drill cuttings and core samples from more than 40 wells ranging in depth to more than 3.5 km in the Cerro Prieto geothermal field. Oxygen isotopic profiles of pore-filling calcites in sandstones appear to be a reliable measure of the recent equilibrium temperature distribution in the field before production began. From these data, a detailed, three-dimensional map has been developed, showing the equilibrium temperatures in the geothermal field. A mass balance calculation has been performed using measured /sup 18/O enrichment of the geothermal brine. This calculation implies an overall water; rock volume ratio of approximately 3:1 during the history of the Cerro Prieto system. Paleotemperatures different from the present thermal regime have been studied by examining coexisting mineral systems which exchanged their oxygen with the geothermal brines at different rates.

  11. Nueva edad de la base del grupo Chubut en la mena uranífera Cerro Solo, provincia del Chubut

    Directory of Open Access Journals (Sweden)

    Nilda Marveggio

    2013-09-01

    Full Text Available En este trabajo se analizan las características litológicas de la roca hospedante de la mineralización de uranio del yacimiento Cerro Solo, que corresponde al miembro inferior de la Formación Los Adobes, unidad basal del Grupo Chubut en su sector norte. Se analiza la asociación de polen angiospérmico de allí recuperada, y en base a ese análisis, se establece una edad albiana temprana para la asociación polínica, que determina una edad más joven que la considerada hasta el momento para el inicio de la depositación de las sedimentitas del Grupo Chubut en el depocentro del yacimiento Cerro Solo.

  12. Oxygen isotope exchange in rocks and minerals from the Cerro Prieto geothermal system: Indicators of temperature distribution and fluid flow

    Energy Technology Data Exchange (ETDEWEB)

    Williams, A.E.; Elders, W.A.

    1981-01-01

    Oxygen isotopic compositions have been measured in drill cuttings and core samples from more than 40 wells ranging in depth to more than 3.5 km in the Cerro Prieto geothermal field. Profiles of isotopic ratios versus sampling depths provide information on the three-dimensional distribution of temperature and fluid flow. These parameters also indicate variations in the history of hydrothermal processes in different areas of the geothermal field.

  13. Los marsupiales (Mammalia) del Mioceno Superior de la Formación Cerro Azul (Provincia de La Pampa, Argentina)

    OpenAIRE

    Visconti, G; Montalvo, C. I.; Goin, F J

    2000-01-01

    We describe the most complete South American marsupial association of Huayquerian Age (late Miocene). Specimens were recovered from several new localities of central and northern La Pampa province (central Argentina), at levels assignable to Cerro Azul Fm.: Bajo Giuliani, Quehué, Telén, El Guanaco, and Laguna Chillhué. Loessoid sediments studied from this formation are indicative of lacustrine deposits overlaid by eolian levels bearing evidences of pedogenesis. A study of these...

  14. ‘Looking at risk with both eyes’: health and safety in the Cerro Rico of Potosí (Bolivia)

    OpenAIRE

    Lopez-Trueba, Mei

    2014-01-01

    This thesis is concerned with core assumptions and practices in dominant approaches to Occupational Health and Safety (hereafter, OHS). I critically evaluate these through an anthropological exploration of the everyday perceptions, experiences and practices related to OHS risks amongst the cooperative miners employed in the Cerro Rico of Potosi (Bolivian Highlands). Drawing on 17 months of ethnographic fieldwork conducted between 2009 and 2011, the thesis examines the lives and livelihood...

  15. Definition of magmatic suites in ediacaran bodies of the NE Province Borborema (State of Rio Grande do Norte: Pitombeira, Taipu and Gameleira Plutons

    Directory of Open Access Journals (Sweden)

    Maria Tatiany Duarte de Oliveira

    2014-12-01

    Full Text Available The Pitombeira, Taipu and Gameleira plutons, located in the northeasternmost portion of the São José do Campestre Domain within the Borborema Province (NE, Brazil, are subjects of lithogeochemical studies in the present work. The Pitombeira Pluton comprises a monzo- to syenogranitic facies defined by K-feldspar phenocrysts, and a quartz-dioritic to tonalitic facies, mainly as enclaves, with laths of plagioclase showing compositional zoning and chilled rims. The Taipu Pluton is made of equigranular, locally porphyritic, monzo- to syenogranites, whereas the Gamaleira Pluton encompasses tonalitic and grano- dioritic rocks with porphyritic textures and compositionally zoned plagioclase crystals. Geochemical discriminant diagrams reveal that the rocks forming the Gameleira Pluton are metaluminous, with a calc-alkaline signature and magnesian character, contrasting with the subalkaline (high-K calc-alkaline signature and ferroan character of the Taipu and Pitombeira Plutons, where the former is highly peraluminous and the latter is metaluminous to slightly peraluminous. Rare Earth Elements patterns are similar to all plutons and register negative Eu anomalies and a relative enrichment of LREE over HREE, with LaN/YbN ratios between 9.38 to 16.20 (Gamaleira Pluton, 17.99 to 31.39 (granitic facies of the Pitombeira Pluton, 14.15 to 21.81 (dioritic facies of the Pitombeira Pluton and 15.17 to 175.41 (Taipu Pluton. Based on the combined investigation of structural, textural and geochemical data, a late- to post-collisional tectonic environment is suggested for the plutons here studied.

  16. Reconstructing the Late Paleozoic : Early Mesozoic plutonic and sedimentary record of south-east Peru : Orphaned back-arcs along the western margin of Gondwana

    OpenAIRE

    Reitsma, Martje Jel

    2012-01-01

    This thesis investigates the sedimentary, plutonic and tectonic evolution of the Eastern Cordillera region of south-east Peru during assembly of the Pangea supercontinent and subsequent early pulses of break-up. We present a chronostratigraphic framework for the Carboniferous to Triassic sedimentary and plutonic record using geochronological, geochemical and isotopic methods, integrated with field observations. The first chapter investigates the plutonic record and its relation to growth of t...

  17. Multi-stage emplacement of the Götemar Pluton, SE Sweden: new evidence inferred from field observations and microfabric analysis, including cathodoluminescence microscopy

    OpenAIRE

    Friese, Nadine; Vollbrecht, Axel; Tanner, David; Fahlbusch, Wiebke; Weidemann, Miriam

    2011-01-01

    The emplacement of the Mesoproterozoic Götemar Pluton into Paleoproterozoic granitoid host rocks of the Transscandinavian Igneous Belt is re-examined by microfabric analysis, including cathodoluminescence microscopy. Field data on the pluton-host rock system are used to strengthen the model. The Götemar Pluton, situated on the Baltic Shield of SE Sweden, is a horizontally zoned tabular structure that was constructed by the intrusion of successive pulses of magma with different crystal/melt ra...

  18. Consistent magmatic and magnetic anisotropy data in La Gloria Pluton, central Chile: Implications for the magma flow record in a shallow pluton

    Science.gov (United States)

    Payacan, I.; Gutierrez, F. J.; Bachmann, O.; Parada, M.

    2012-12-01

    The magmatic origin of the anisotropy of magnetic susceptibility (AMS) is examined in comparison with magmatic anisotropy data in a small, shallow, silicic magma reservoir in the upper crust. La Gloria Pluton (LGP) is a 10 Ma granodiorite/quartz monzonite of about 250 km3 located in the southern Andes, central Chile. LGP represents a particularly simple case of a silicic intrusion which was assembled in a few pulses and cooled over a short time interval. Hornblende, biotite and minor magnetite are ubiquitous mafic phases. The AMS tensor indicates that magnetic fabric has an oblate shape (i.e. magnetic foliation is higher than magnetic lineation). Lineations are weak (values up to 1.05), have a N-NW trend with a nearly horizontal dip and represent axisymmetric convection parallel to the main pluton elongation. Foliations are more pronounced (values up to 1.14), having NW trends and dips that vary gradually from vertical at the walls, to horizontal at the center and near the roof of the chamber. We interpret this to represent shear localization near the magma locking point along solidification fronts. Magmatic anisotropy data were obtained by measuring mineral length, width and orientation in the three main planes of the AMS tensor. We define the planes Pmax, Pint, and Pmin as orthogonal to the maximum, intermediate, and minimum axes of the AMS tensor, respectively. Mineral data were collected for plagioclase and amphibole + bitotite independently. For each site, the Bingham distribution with 95% of confidence is used to determine the mean mineral orientation and their angle difference with the AMS axes. Preliminary results indicate that mean crystal orientations are well defined for Pmax and Pint for all analyzed minerals, but Pmin is only well constrained for amphibole + bitotite and poorly constrained for plagioclase. Angle differences generally decrease with magnetic anisotropy but are independent of the size and aspect ratio of the crystals. Mean values of

  19. Estrutura de mercado e tendências da atividade comercial

    Directory of Open Access Journals (Sweden)

    Jefferson Mariano

    2007-11-01

    Full Text Available O presente artigo busca realizar uma caracterização do setor comercial, com ênfase na RMSP, destacando o processo de concentração, evidenciado principalmente no segmento de hiper e supermercados. Na primeira seção, busca-se ilustrar o processo de concentração em alguns segmentos do comércio varejista, à luz das teorias de estrutura de mercado. Na segunda, apresenta se um painel com o perfil dessa atividade econômica, com informações agregadas para Brasil, Estado de São Paulo e Região Metropolitana de São Paulo. Na terceira, são apontadas as tendências e perspectivas do setor.

  20. Modelos de equilibrio e eficiencia no mercado de capitais

    OpenAIRE

    López Penabad, Celia

    2013-01-01

    Esta unidade didáctica enmárcase na materia de Investimentos Financeiros correspondente ao 4º curso do Grao en Administración e Dirección de Empresas, é unha materia optativa de Finanzas. Céntrase no estudo da Teoría da Eficiencia do mercado e nas súas implicacións para a xestión de carteiras e nos dous modelos mais coñecidos e empregados en valoración de activos financeiros, o CAPM e o APT. O contido desta unidade é moi importante para calquera suxeito que se enfronte á xestión dunha ...

  1. commodity: el caso del mercado internacional del azúcar

    Directory of Open Access Journals (Sweden)

    Julio César Alonso

    2013-01-01

    Full Text Available Este trabajo estudia el comportamiento estacional de los precios internacionales del azúcar transados en Nueva York y Londres. Para este caso, empleando pruebas de raíces estacionales y una muestra mensual desde enero de 1989 hasta diciembre de 2010, se encuentra la existencia de un comportamiento estacional estocástico no estacionario. Dicha conducta implica que un “verano” se puede convertir en un “invierno”, resultado que no había sido documentado previamente en estos mercados. Por otro lado, empleando dicho hallazgo, los resultados muestran que es posible construir un modelo autorregresivo de media móvil que se comporta relativamente mejor al pronosticar el precio frente a un modelo que no tiene en cuenta dicho tipo de estacionalidad.

  2. Convergencia entre educación superior y mercado laboral

    OpenAIRE

    Pacenza, María Inés; Lanari, María Estela

    2001-01-01

    El propósito de esta comunicación es dar cuenta de la participación que posee la oferta laboral con el más alto nivel de instrucción formal, en el mercado de trabajo del aglomerado Mar del Plata-Batán. Se incluye en el análisis a la educación superior como una variable interviniente de la calidad de la fuerza de trabajo con relación al mayor grado de instrucción formal alcanzado: nivel universitario y no universitario, completo o incompleto, y según la condición de asistencia -estudiantes, eg...

  3. O ENSINO SUPERIOR EM TURISMO: HUMANO OU MERCADO?

    OpenAIRE

    Waléria Thabata Roldão Niquini; Leandro Benedini Brusadin

    2013-01-01

    Desde La creación de la educación superior en el Turismo en Brasil, en La década de 1970, se han producido algunas discusiones en relación a la formación del estudiante y su desempeño en el mercado laboral. Sin embargo hay varios puntos educativos significantes incluso antes de la aparición de la inserción profesional. La preparación de los estudiantes, las acciones de los maestros en la esfera de investigación y extensión y la necesidad del pensamiento crítico son supuestos que poden justif...

  4. Fabric and microstructural analysis of the Loch Borralan pluton, Northwest Highlands, Scotland

    Science.gov (United States)

    Calhoun, Justin

    The Loch Borralan pluton was emplaced within the Assynt Region of the Moine Thrust zone during the Scandian event (ca. 435-425 Ma) of the Caledonian Orogeny (478-425 Ma). It consists of two major magma suites, the syenitic early suite (431.1 +/- 1.2 Ma), and the quartz syenitic later suite (429.2 +/- 0.5 Ma). The region is characterized by a series of in-sequence thrust faults that strike NE-SW and dip approximately 20° to the SE, including (from lower to upper): the Sole Thrust, the Borralan Thrust (hypothesized, but not exposed), the Ben More Thrust, and the Moine Thrust. A series of imbricate thrusts between the Sole and Borralan Thrusts juxtapose repeated Cambrian and Ordovician strata. The Loch Borralan pluton intruded between the Sole and Ben More thrust faults, and may be bounded below by a hypothesized Borralan Thrust fault. Based on the overlap in pluton crystallization age and orogenic activity, the combination of macroscopic field lineation and foliation measurements, anisotropy of magnetic susceptibility (AMS) lineation and foliations measurements, mineral shape preferred orientation (SPO) analysis, and petrographic deformation microstructure analysis will be used to determine if the pluton expresses deformation features and fabrics corresponding to thrust fault tectonics. The dominant magnetic mineralogy as determined by thermomagnetic data and hysteresis plots was determined to be magnetite and titanomagnetite. Some paramagnetic components were seen in the early suite, and can be attributed to biotite. Both minerals contributed to the AMS signal that was used to interpret pluton fabrics. The pluton contains S>L (foliation stronger than lineation) fabrics throughout, defined by alignment of alkali feldspar grains. The foliation strike of both the early and late suites are subparallel to the thrust faults, providing evidence that the fabrics are related to deformation. The early suite is only well exposed in the southeast at the top of the Borralan

  5. El mercado hipotecario y el financiamiento de la vivienda

    Directory of Open Access Journals (Sweden)

    Gustavo A. Salas Rada

    2015-12-01

    Full Text Available El financiamiento a la vivienda en Colombia ha alcanzado en los últimosaños un significativo desarrollo. Para ello ha sido fundamental la configuración de tres elementos complementarios: 1 la eliminación del efecto de la inflación sobre el valor de las deudas de largo plazo, primero por la vía de desarrollar una unidad de cuenta indexada a la inflación, que sea creíble y transparente (la UVR y, posteriormente, con el abatimiento de la inflación como fenómeno macroeconómico; 2 la reforma al régimen de financiación con la expedición de la Ley 546/99, que fue clave para el nacimiento y progreso de un mercado de títulos hipotecarios, y 3 la política social de vivienda, según la cual el Estado se ha ido moviendo progresivamente, aunque tal vez con lentitud, hacia el subsidio de la demanda de vivienda de los grupos con más dificultades de acceso a los mercados privados de financiamiento. Los cambios en el entorno macroeconómico, en la legislación de la construcción y la categórica definición de un derecho a la vivienda digna comprometen al Estado colombiano a diseñar estrategias para responder al mandato constitucional, pues los esfuerzos no han sido de impactos significativos, y la política de financiamiento ha presentado fluctuaciones que han afectado su efectividad.

  6. Mercado regional en el Golfo de California (1848-1910

    Directory of Open Access Journals (Sweden)

    Alfonso Guillén Vicente

    2001-01-01

    Full Text Available El comercio marítimo que apareció en el Golfo de California a finales del siglo X V I I I, se afianzó en las primeras décadas del siglo XIX merced a la navegación de altura que tuvo como eje el puerto de San Blas, Nayarit, y al intercambio efectuado por las naves que cubrían los diversos destinos de la región con productos agrícolas y pecuarios. Su despegue definitivo, sin embargo, ocurrió con motivo de la fiebre del oro en California, que permitió el establecimiento de rutas regulares que tocaban los puertos de Guaymas, Mazatlán y La Paz . El propio desarrollo urbano de estas localidades constituyó un mercado interesante para los buques de vapor que se movían a lo largo del Pacífico. Los comerciantes locales se hicieron así de un respetable capital que invirtieron en otros sectores productivos de la región, además de fortalecer los lazos establecidos entre ellos. La entrada del ferrocarril a Sonora en la década de los ochenta del siglo XIX no eclipsó por completo a Guaymas, que por todo el resto de la centuria conservó un papel relevante como centro comercial regional. En la medida que el caballo de hierro abatió sus costos y se acreditó entre los sectores minero e industrial sonorenses y, sobretodo, cuando el Sudpacífico continuó su marcha hacia el Sur, al entrar en Sinaloa, el importante mercado regional del Golfo de California cayó de manera significativa.

  7. La Red: el nuevo mercado de la vida privada

    Directory of Open Access Journals (Sweden)

    Lic. María Teresa Sandoval Martín

    2001-01-01

    Full Text Available Mientras el mercado publicitario en Internet demanda cada vez más información de los ciberusuarios, diferentes organizaciones y determinados gobiernos defienden el respeto a la intimidad y a la privacidad en el nuevo entorno tecnológico. Algunos de estos países proponen leyes y otros prefieren la autorregulación, pero, a la vez, también se van incrementando las medidas y los sistemas de vigilancia con el supuesto fin de proteger a la sociedad. Además de la regulación, las normas o el desarrollo de códigos por las empresas, el mercado e incluso la propia tecnología pueden limitar la información que se toma de los navegantes de la red de redes. La mayoría de los especialistas consideran que en un futuro próximo los internautas deseos de discreción pagarán un precio por la seguridad de sus datos, mientras que los otros verán su intimidad ofrecida como mercancía.ABSTRACTWhile market in Internet demands more and more information about users, different organizations and certain governments defend the respect to the intimacy and the privacy in the new technological environment. Some of these countries propose laws and others lean for a self-regulation. At the same time, they also leave increasing the measures and systems of surveillance with the supposed end of protecting to society. Besides the regulation, the rules or the development of codes for the companies, the market and the own technology can even limit the information of users in the net. Most of the specialists consider that in a next future, some of the users will pay a price for the security of their data, while the other ones will see their intimacy offered as a merchandise.

  8. An integrated geological, geochemical, and geophysical investigation of uranium metallogenesis in selected granitic plutons of the Miramichi Anticlinorium, New Brunswick

    International Nuclear Information System (INIS)

    Integrated geological, geochemical, and geophysical data for the post-tectonic granitic rocks of the North Pole, Burnthill, Dungarvon, Trout Brook, and Rocky Brook plutons and surrounding areas were examined to assess their potential for uranium mineralization. Geological, geochemical, and geophysical criteria that are thought to be useful guides for uranium exploration were also established for the host granites. The granitic plutons were emplaced discordantly, late in the tectonomagmatic sequence and at shallow depths within the metasedimentary rocks of the Miramichi Anticlinorium. Geochemically, the host granites are highly evolved (Si02 > 75 wt. %), peraluminous and have strong similarities with ilmenite-series 'S-type' and 'A-type' granitoids. Uranium occurrences are spatially and perhaps temporally associated with late-phase differentiates of the plutons where elevated levels of other lithophile elements such as Sn, W, Mo, and F were also detected. Geophysically, the granitic plutons are associated with distinctively high aeroradiometric eU, eTh, and K anomalies that coincide with strong negative Bouguer anomalies and low magnetic values. Conceptual models involving magmatic and hydrothermal processes have been adopted to explain the concentration of uranium and associated metals in the granitic plutons

  9. Geochemistry of Mesozoic plutons, southern Death Valley region, California: Insights into the origin of Cordilleran interior magmatism

    Science.gov (United States)

    Ramo, O.T.; Calzia, J.P.; Kosunen, P.J.

    2002-01-01

    Mesozoic granitoid plutons in the southern Death Valley region of southeastern California reveal substantial compositional and isotopic diversity for Mesozoic magmatism in the southwestern US Cordillera. Jurassic plutons of the region are mainly calc-alkaline mafic granodiorites with ??Ndi of -5 to -16, 87Sr/86Sri of 0.707-0.726, and 206Pb/204Pbi of 17.5-20.0. Cretaceous granitoids of the region are mainly monzogranites with ??Ndi of -6 to -19, 87Sr/86Sri of 0.707-0.723, and 206Pb/204Pbi of 17.4-18.6. The granitoids were generated by mixing of mantle-derived mafic melts and pre-existing crust - some of the Cretaceous plutons represent melting of Paleoproterozoic crust that, in the southern Death Valley region, is exceptionally heterogeneous. A Cretaceous gabbro on the southern flank of the region has an unuasually juvenile composition (??Ndi -3.2, 87Sr/86Sri 0.7060). Geographic position of the Mesozoic plutons and comparison with Cordillera plutonism in the Mojave Desert show that the Precambrian lithosphere (craton margin) in the eastern Mojave Desert region may consists of two crustal blocks separated by a more juvenile terrane.

  10. Asymmetric textural and structural patterns of a granitic body emplaced at shallow levels: The La Chinchilla pluton, northwestern Argentina

    Science.gov (United States)

    Macchioli Grande, M.; Alasino, P. H.; Rocher, S.; Larrovere, M. A.; Dahlquist, J. A.

    2015-12-01

    New mapping and a detailed structural study of the La Chinchilla stock, Sierra de Velasco, NW Argentina, suggest an asymmetrical shape of the pluton and provide strong evidence for its shallow emplacement depth. The pluton is a Lower Carboniferous monzogranite composed of K-feldspar, quartz, plagioclase and biotite. It exhibits an internal asymmetric textural zoning, defined by porphyritic granite in the southeastern region to equigranular granite in the northwestern region. The presence of subhorizontal dikes in the northwestern area, where the contacts dip shallowly, and subvertical dikes intruding the host rock nearby steep-dipping intrusive contacts in the southeastern region are compatible with an overall asymmetrical shape and internal structure of this pluton. Considering published crystallization ages, a dominant strain field occurring at around 12 Ma is inferred based on magmatic fabrics in the pluton and its host rock (the Huaco pluton), with a principal shortening direction oriented SW-NE, consistent with the general NW-SE strike of the body. Field evidence supports brittle fracturing and block displacement as the dominant emplacement mechanism, suggesting that magmatic stoping dominated during the late stage of the evolution of the magma chamber.

  11. The Final Days of Paracas in Cerro del Gentil, Chincha Valley, Peru

    Science.gov (United States)

    2016-01-01

    This article describes and analyzes a highly significant archaeological context discovered in a late Paracas (400–200 BCE) sunken patio in the monumental platform mound of Cerro Gentil, located in the Chincha Valley, Peru. This patio area was used for several centuries for ritual activities, including large-scale feasting and other public gatherings. At one point late in this historical sequence people deposited a great deal of objects in what is demonstrably a single historical event. This was quickly followed by a series of minor events stratigraphically immediately above this larger event. This entire ritual process included the consumption of liquids and food, and involved the offering of whole pottery, pottery fragments, botanical remains, bone, lithics, baskets, pyro-engraved gourds, mummies, and other objects. We interpret these events as an “abandonment ceremony” or “termination ritual” during the late Paracas period, one that may have lasted for weeks or even months. The subsequent Topará occupation at the site (ca. 200 BCE- AD 100) involved the architectural enhancement of the mound area, but the pattern of use of the patio itself ended. Such a termination ritual signals a reorganization in the regional political structure of Paracas society. PMID:27144824

  12. Soil mercury levels in the area surrounding the Cerro Prieto geothermal complex, MEXICO.

    Science.gov (United States)

    Pastrana-Corral, M A; Wakida, F T; García-Flores, E; Rodriguez-Mendivil, D D; Quiñonez-Plaza, A; Piñon-Colin, T D J

    2016-08-01

    Even though geothermal energy is a renewable energy source that is seen as cost-effective and environmentally friendly, emissions from geothermal plants can impact air, soil, and water in the vicinity of geothermal power plants. The Cerro Prieto geothermal complex is located 30 km southeast of the city of Mexicali in the Mexican state of Baja California. Its installed electricity generation capacity is 720 MW, being the largest geothermal complex in Mexico. The objective of this study was to evaluate whether the emissions generated by the geothermal complex have increased the soil mercury concentration in the surrounding areas. Fifty-four surface soil samples were collected from the perimeter up to an approximate distance of 7660 m from the complex. Additionally, four soil depth profiles were performed in the vicinity of the complex. Mercury concentration in 69 % of the samples was higher than the mercury concentration found at the baseline sites. The mercury concentration ranged from 0.01 to 0.26 mg/kg. Our results show that the activities of the geothermal complex have led to an accumulation of mercury in the soil of the surrounding area. More studies are needed to determine the risk to human health and the ecosystems in the study area. PMID:27418073

  13. New mammalian records in the Parque Nacional Cerros de Amotape, northwestern Peru

    Directory of Open Access Journals (Sweden)

    Cindy M. Hurtado

    2015-04-01

    Full Text Available The Pacific Tropical Rainforest and Equatorial Dry Forest are found only in southern Ecuador and northern Peru, and are among the most poorly known ecosystems of South America. Even though these forests are protected in Parque Nacional Cerros de Amotape (PNCA, they are threatened by fragmentation because of farming and agriculture. The aim of this study was to determine the medium and large mammalian species richness, using transect census, camera trapping, and specimen bone collection. Nine transects were established and 21 camera trap stations were placed along 16 km2 in three localities of PNCA, from August 2012 to April 2013. Total sampling effort was 215 km of transects and 4077 camera-days. We documented 22 species; including 17 with camera trapping, 11 with transect census, and 10 with specimen collection.  Camera traps were the most effective method, and four species (Dasyprocta punctata, Cuniculus paca, Leopardus wiedii and Puma concolor were documented only with this method. This comprised the first Peruvian record for Dasyprocta punctata, and the first record for the western slope of the Peruvian Andes for Cuniculus paca. Also, both specimen collections and sightings confirm the presence of Potos flavus, first record in the western slope of the Peruvian Andes. Panthera onca, Tremarctos ornatus and Saimiri sciureus are considered locally extinct, while several species are in need of further research. We highlight the importance of the high diversity of this rainforests and encourage local authorities to give the area the highest priority in conservation.

  14. Monitoring the atmospheric throughput at Cerro Tololo Inter-American Observatory with aTmCam

    CERN Document Server

    Li, Ting; Marshall, J L; Nagasawa, D Q; Carona, D W; Boada, S

    2014-01-01

    We have built an Atmospheric Transmission Monitoring Camera (aTmCam), which consists of four telescopes and detectors each with a narrow-band filter that monitors the brightness of suitable standard stars. Each narrowband filter is selected to monitor a different wavelength region of the atmospheric transmission, including regions dominated by the precipitable water vapor and aerosol optical depth. The colors of the stars are measured by this multi narrow-band imager system simultaneously. The measured colors, a model of the observed star, and the measured throughput of the system can be used to derive the atmospheric transmission of a site on sub-minute time scales. We deployed such a system to the Cerro Tololo Inter-American Observatory (CTIO) and executed two one-month-long observing campaigns in Oct-Nov 2012 and Sept-Oct 2013. We have determined the time and angular scales of variations in the atmospheric transmission above CTIO during these observing runs. We also compared our results with those from a G...

  15. Forecast of surface layer meteorological parameters at Cerro Paranal with a mesoscale atmospherical model

    CERN Document Server

    Lascaux, Franck; Fini, Luca

    2015-01-01

    This article aims at proving the feasibility of the forecast of all the most relevant classical atmospherical parameters for astronomical applications (wind speed and direction, temperature) above the ESO ground-base site of Cerro Paranal with a mesoscale atmospherical model called Meso-Nh. In a precedent paper we have preliminarily treated the model performances obtained in reconstructing some key atmospherical parameters in the surface layer 0-30~m studying the bias and the RMSE on a statistical sample of 20 nights. Results were very encouraging and it appeared therefore mandatory to confirm such a good result on a much richer statistical sample. In this paper, the study was extended to a total sample of 129 nights between 2007 and 2011 distributed in different parts of the solar year. This large sample made our analysis more robust and definitive in terms of the model performances and permitted us to confirm the excellent performances of the model. Besides, we present an independent analysis of the model p...

  16. Characterization of the sodium layer at Cerro Pachon, and impact on laser guide star performance

    CERN Document Server

    Neichel, Benoit; Callingham, Joseph; Rigaut, Francois; Winge, Claudia; Trancho, Gelys; 10.1093/mnras/sts631

    2013-01-01

    Detailed knowledge of the mesopheric sodium layer characteristics is crucial to estimate and optimize the performance of Laser Guide Star (LGS) assisted Adaptive Optics (AO) systems. In this paper, we present an analysis of two sets of data on the mesospheric sodium layer. The first set comes from a laser experiment that was carried out at Cerro Tololo to monitor the abundance and altitude of the mesospheric sodium in 2001, during six runs covering a period of one year. This data is used to derive the mesospheric sodium column density, the sodium layer thickness and the temporal behavior of the sodium layer mean altitude. The second set of data was gathered during the first year of the Gemini MCAO System (GeMS) commissioning and operations. GeMS uses five LGS to measure and compensate for atmospheric distortions. Analysis of the LGS wavefront sensor data provides information about the sodium photon return and the spot elongation seen by the WFS. All these parameters show large variations on a yearly, nightly ...

  17. Research Experiences for Undergraduates at Cerro Tololo Inter-American Observatory

    Science.gov (United States)

    Hoard, D. W.; Smith, R. C.

    1999-12-01

    Each year, Cerro Tololo Inter-American Observatory (CTIO) hosts a Research Experiences for Undergraduates (REU) program funded by the National Science Foundation. In general, REU programs bring a group of undergraduate students to the host institute for 10 weeks, where they are teamed-up with staff members to perform research projects. Unlike REU programs at other U.S. institutions, the CTIO program takes place outside the United States and during the southern summer/northern winter months. This offers students not only a chance to perform research and participate in the day-to-day life at a major astronomical observatory, but also provides a unique exposure to a foreign culture and an option for students who can take advantage of a non-traditional work experience during the academic year. CTIO REU students also benefit from interaction with their Chilean counterparts participating in the Prácticas de Investigación en Astronomía, an REU-like program operated by CTIO for Chilean undergraduates. Since 1995, CTIO has hosted 16 REU students (with 4 more coming in 2000). Thirteen (and counting) publications have resulted from CTIO REU projects; all 4 REU students in the 1999 program attended the 194th AAS meeting to present posters based on their projects. We present here an overview of the REU program at CTIO.

  18. Research Experiences for Undergraduates at Cerro Tololo Inter-American Observatory

    Science.gov (United States)

    Hoard, D. W.; Smith, R. C.

    2000-12-01

    Each year, Cerro Tololo Inter-American Observatory (CTIO), located in La Serena, Chile, hosts a Research Experiences for Undergraduates (REU) Program funded by the National Science Foundation. In general, REU programs bring a group of undergraduate students to the host institute for 10 weeks, where they are teamed-up with staff members to perform research projects. Unlike REU programs at other U.S. institutions, the CTIO program takes place outside the United States and during the southern summer/northern winter months of January--March. This offers students not only a chance to perform research and participate in the day-to-day life at a major astronomical observatory, but also provides a unique exposure to a foreign culture and an option for students who can take advantage of a non-traditional work experience during the academic year. CTIO REU students also benefit from interaction with their Chilean counterparts participating in the Prácticas de Investigación en Astronomía, an REU-like program operated by CTIO for Chilean undergraduates. Since 1995, CTIO has hosted 20 REU students (with 4 more coming in 2001). Twenty (and counting) publications have resulted from CTIO REU projects. In addition, since 1999, 100% of the CTIO REU students have presented the results of their research projects at meetings of the American Astronomical Society. We present here an overview of the REU program at CTIO.

  19. The Final Days of Paracas in Cerro del Gentil, Chincha Valley, Peru.

    Science.gov (United States)

    Tantaleán, Henry; Stanish, Charles; Rodríguez, Alexis; Pérez, Kelita

    2016-01-01

    This article describes and analyzes a highly significant archaeological context discovered in a late Paracas (400-200 BCE) sunken patio in the monumental platform mound of Cerro Gentil, located in the Chincha Valley, Peru. This patio area was used for several centuries for ritual activities, including large-scale feasting and other public gatherings. At one point late in this historical sequence people deposited a great deal of objects in what is demonstrably a single historical event. This was quickly followed by a series of minor events stratigraphically immediately above this larger event. This entire ritual process included the consumption of liquids and food, and involved the offering of whole pottery, pottery fragments, botanical remains, bone, lithics, baskets, pyro-engraved gourds, mummies, and other objects. We interpret these events as an "abandonment ceremony" or "termination ritual" during the late Paracas period, one that may have lasted for weeks or even months. The subsequent Topará occupation at the site (ca. 200 BCE- AD 100) involved the architectural enhancement of the mound area, but the pattern of use of the patio itself ended. Such a termination ritual signals a reorganization in the regional political structure of Paracas society. PMID:27144824

  20. Optical and infrared observations of SN 1987A from Cerro Tololo Inter-American Observatory

    International Nuclear Information System (INIS)

    Results from optical and infrared observations of SN 1987A obtained at Cerro Tololo Inter-American Observatory over the first seven months since core collapse are reviewed. Around 130 days after outburst, the bolometric light curve began to smoothly decline at a rate of ∼ 0.01 mag day-1, providing dramatic confirmation of the prediction that radioactivity had powered the optical display after the first month./ the peculiar color changes are kinks observed beginning on the 25th day probably signaled the initial release of trapped energy from mass 56 material. The bolometric luminosity of SN 1987A was unusually low at first, but reached a value more typical of other type II supernovae by the time that the final exponential decline had begun. Over much of the period covered by these observations, the optical and infrared spectra were characterized by strong absorption lines of Ba II and Sr II. Comparison with the spectra of other type II supernovae at similar stages of evolution supports the suggestion that s-processed elements were enriched in the hydrogen envelope of the progenitor, Sanduleak - 69 degrees 202

  1. El mercado y la exclusión del consumo por el sistema de precios

    OpenAIRE

    Anchorena, Sergio Oscar; Gaviola, Saúl Ricardo

    2014-01-01

    En la enseñanza de materias introductorias al estudio de la microeconomía, el concepto de equilibrio como una situación estable y deseable juega un rol demasiado central. Desde la perspectiva dominante aprender microeconomía es aprender a encontrar equilibrios de mercado en modelos simplificados. Esta búsqueda del equilibrio parcial de mercado oculta una de sus características, que es que, dados diferentes niveles de ingreso por parte de las unidades de consumo, el equilibrio de mercado impli...

  2. Estudio sobre el mercado laboral yerbatero, sus protagonistas, y sus luchas

    Directory of Open Access Journals (Sweden)

    María Angélica Jordán

    2013-12-01

    Full Text Available Reseña bibliográfica acerca del libro “Cosechando yerba mate. Estructuras sociales de un mercado agrario en el Nordeste argentino” (2012 de Victor Rau. Dicho estudio analiza el mercado laboral agrario yerbatero, recuperando su historicidad en la región, atendiendo a las estructuras sociales que han condicionando su funcionamiento, como las variables que permitieron la reconfiguración de la estructura del mercado actual, sobretodo a partir de los años ’90. Para ello, se enfoca en los asalariados agrícolas, sus condiciones de venta de fuerza de trabajo, y sus acciones colectiva de protesta.

  3. MERCADO DE LUXO: ESTRATÉGIAS PARA INTERNACIONALIZAÇÃO DE EMPRESAS JOALHEIRAS DO BRASIL

    OpenAIRE

    Chaline Gasperin; Valesca Persch Reichelt

    2009-01-01

    Neste artigo pretende-se fazer uma análise do mercado de luxo e das empresas de jóias brasileiras. O objetivo geral é analisar a atratividade do mercado externo para a internacionalização de marcas de luxo, dando ênfase para as empresas joalheiras do Brasil. Primeiramente apresenta-se o panorama nacional do mercado de luxo e de jóias brasileiras. Em seguida, abordam-se os possíveis objetivos, riscos e oportunidades que as empresas joalheiras internacionalizadas enfrentam no processo de expans...

  4. Seguimiento a las restricciones del mercado eléctrico colombiano

    OpenAIRE

    Cadavid Mazo, Edgar

    2008-01-01

    Se presenta la importancia de la red de transmisión en la operación de los mercados competitivos de electricidad, describiendo cómo son consideradas las limitaciones de la red en la operación del mercado e introduciendo el concepto de las restricciones eléctricas. El concepto de restricción es tratado a partir de cómo es considerado en el Mercado de Electricidad Colombiano y cómo se liquida, por tanto se introducen los conceptos de Reconciliación Positiva y Negativa utilizados en el cálculo d...

  5. Las características del mercado de derechos de agua en España

    OpenAIRE

    Antonio Embid Irujo

    2013-01-01

    Por diversas circunstancias el derecho español conoce desde 1999 de una regulación jurídica de los mercados de derechos de uso de aguas. De ellos se ha hecho bastante utilización durante la última gran sequía (2005-2009) y la experiencia ha sido favorable. La regulación de los mercados intenta evitar la especulación y el acaparamiento de derechos. Sin que sea gran cantidad de agua la que se mueve por razón de los mercados, sí que es suficiente para evitar graves inconvenientes y, con el adecu...

  6. Comentarios sobre el comercio y mercados del agua subterránea en Canarias

    OpenAIRE

    Custodio Gimena, Emilio

    2011-01-01

    Los mercados del agua subterránea son una interesante posibilidad para la gestión del agua subterránea. Estos mercados han existido desde hace muchas décadas en las islas principales del Archipiélago Canario y han contribuido en parte al importante proceso de desarrollo del último medio siglo. Con variantes de isla a isla y de un lugar a otro, los mercados de agua subterránea son la superposición de tres elementos, el de propiedad del agua a modo de participaciones y acciones que se compran y...

  7. Anuncios macroeconómicos y mercados Accionarios: El caso Latinoamericano

    OpenAIRE

    Agudelo, Diego A.; Gutiérrez, Ángelo

    2011-01-01

    ¿Reflejan los mercados accionarios los fundamentales macroeconómicos de un país? La hipótesis de eficiencia semifuerte (Fama, 1970) implica que los mercados accionarios deben reaccionar inmediatamente, y sin sobre ni subreacción predecible, a las sorpresas en los anuncios macroeconómicos relevantes. Ponemos a prueba esta implicación en los seis principales mercados accionarios de Latinoamérica: Argentina, Brasil, Chile, Colombia, México y Perú ante los anuncios de inflación, tasa de interés d...

  8. ALCANCES, LIMITACIONES E IMPACTO DE LA REFORMA A LA LEY REGULADORA DEL MERCADO DE VALORES

    OpenAIRE

    Julio César Espinosa Rodríguez

    2011-01-01

    La nueva ley de valores establece una serie de parámetros requeridos para el desarrollo del mercado de valores, enmarcado dentro de una mejor regulación y mayor seguridad para los inversionistas. En general establece las bases para pasar a una nueva etapa de desarrollo del sistema financiero, donde el énfasis será el mercado de largo plazo. Asimismo, la propuesta de la Bolsa Nacional de Valores para desarrollar el mercado accionario se ha transformado en un mecanismo complementario a ese come...

  9. Análise de Concorrência no Mercado Mundial de Café Verde

    OpenAIRE

    Marislei Nishijima; Maria Sylvia Macchione Saes; Fernando Antonio Slaibe Postali

    2012-01-01

    A literatura argumenta que o Brasil, embora ainda seja o maior exportador mundial de café verde, tem perdido poder neste mercado, pois a concorrência (rivalidade e probabilidade de entrada) imposta por países como a Colômbia e o Vietnã é forte o suficiente para tornar este mercado bastante competitivo. Assim, este artigo avalia o padrão recente de concorrência do mercado mundial de café verde utilizando uma metodologia econométrica mais usualmente empregada em análise antitruste. Para avaliar...

  10. O Perfil das Empresas Portuguesas com Relações Comerciais no Mercado Angolano

    OpenAIRE

    Carvalho, Teresa

    2014-01-01

    O presente Relatório de Estagio visa traçar o perfil das empresas portuguesas que tem relações comerciais com o mercado angolano. Neste contexto, tendo como alicerce o referencial teórico sobre internacionalização, foram observadas, através de inquérito por questionário, empresas portuguesas que estão presentes no mercado angolano, com o propósito de as caracterizar, identificar as motivações da escolha do mercado angolano, os obstáculos que mais se destacaram no decurso do processo de intern...

  11. Características y factores diferenciales del mercado de trabajo español

    OpenAIRE

    Peña Sanz, Marta

    2014-01-01

    El objetivo de mi trabajo ha sido realizar un estudio del actual mercado de trabajo español y como éste se ha visto afectado por la crisis económica que España sufre desde el año 2008. Indicaré las características del mercado de trabajo español y los problemas de los que adolece y las posibles soluciones de los problemas del mercado de trabajo español.

  12. La agricultura comercial peruana: incentivos de mercado para la inversión

    OpenAIRE

    Rosario Gómez

    2007-01-01

    "Esta investigación analiza los factores que favorecen la inversión en el sector agroexportador, así como los principales resultados de dicha inversión, principalmente en términos de productividad y acceso a mercados. Asimismo, busca mostrar que el crecimiento del mercado internacional por productos hortofrutícolas, las exigencias de calidad del mercado, la estabilidad macroeconómica y la seguridad interna han favorecido la inversión en este sector."

  13. Análisis de la competitividad del mercado de leche en la Argentina

    OpenAIRE

    Loza, Andrés

    2001-01-01

    El mercado mayorista de leche en Argentina muestra una estructura apropiada para que las empresas tengan poder de mercado y se apropien de parte de la renta que correspondería a los productores rurales en un entorno competitivo. La presente investigación utiliza las modernas técnicas de la Nueva Organización Industrial Empírica, para resolver si las empresas mayoristas elaboradoras de leche ejercen su poder de mercado sobre el productor o tambero. Tanto las pruebas paramétricas y no paramétri...

  14. Análisis de la competitividad del mercado primario de leche en Argentina.

    OpenAIRE

    Andrés Loza

    2001-01-01

    El mercado mayorista de leche en Argentina muestra una estructura apropiada para que las empresas tengan poder de mercado y se apropien de parte de la renta que correspondería a los productores rurales en un entorno competitivo. La presente investigación utiliza las modernas técnicas de la Nueva Organización Industrial Empírica, para resolver si las empresas mayoristas elaboradoras de leche ejercen su poder de mercado sobre el productor o tambero. Tanto las pruebas paramétricas y no paramétri...

  15. El estado del arte de la orientación al mercado en las organizaciones culturales

    OpenAIRE

    José Ignacio Azuela Flores; Nadia H. Jiménez Torres

    2014-01-01

    Desde hace tiempo se han desarrollado diversas investigacio - nes centradas en determinar la contribución de la orientación al mercado en los resultados empresariales. Sin embargo, el estudio del efecto de la orientación al mercado en el desem - peño de las organizaciones culturales representa un área de investigación incipiente. Atendiendo a esta situación, nuestro trabajo tiene como principal objetivo realizar una revisión de los aspectos esenciales de la orientación al mercado en las or - ...

  16. Análisis de la competitividad del mercado primario de leche en Argentina

    OpenAIRE

    Loza, Andrés

    2001-01-01

    El mercado mayorista de leche en Argentina muestra una estructura apropiada para que las empresas tengan poder de mercado y se apropien de parte de la renta que correspondería a los productores rurales en un entorno competitivo. La presente investigación utiliza las modernas técnicas de la Nueva Organización Industrial Empírica, para resolver si las empresas mayoristas elaboradoras de leche ejercen su poder de mercado sobre el productor o tambero. Tanto las pruebas paramétricas y no paramétri...

  17. CORTE TRANSVERSAL DE LOS RETORNOS ESPERADOS EN EL MERCADO ACCIONARIO CHILENO

    OpenAIRE

    Fernando Rubio

    2004-01-01

    La presente investigación intenta replicar el trabajo de Fama y French (1992) para el mercado chileno, dentro de cierto marco de limitaciones generales. Específicamente, el objetivo de la investigación es evaluar el rol conjunto del beta de mercado, el tamaño, la razón utilidad a precio, el leverage y la razón bolsa a libro en la explicación de corte transversal de los retornos promedios de las acciones en el mercado bursátil chileno. El estudio consta de tres partes: La primera presenta la e...

  18. La orientación al mercado como estrategia competitiva de la organización

    OpenAIRE

    Rivera Camino, Jaime

    1999-01-01

    Considerando que la literatura sobre marketing y estrategia aún mantienen discrepancias sobre la definición de la orientación al mercado, el presente artículo expone un marco teórico para definir la orientación al mercado como una estrategia organizacional. El estudio se ha realizado en muestras representativas de dos países para analizar la identidad de la orientación al mercado en un contexto no estadounidense, En esta investigación también se ha validado la relación positiva en...

  19. La orientación al mercado y sus efectos en los resultados de la empresa

    OpenAIRE

    Llonch i Andreu, Joan

    1993-01-01

    La presente tesis doctoral pretende demostrar la existencia de una relación positiva entre el grado de orientación al mercado y los resultados de la empresa. A estos efectos se construye un modelo sobre la orientación de la empresa al mercado. Para probar las hipótesis que se formulan se realiza una investigación entre 144 empresas industriales con los resultados siguientes: 1) el grado de orientación al mercado puede medirse a través de un modelo unidimensional con tres componentes (orientac...

  20. Subsurface Connections and Magma Mixing as revealed by Olivine- and Pyroxene-Hosted Melt Inclusions from Cerro Negro Volcano and the Las Pilas-El Hoyo Complex, Nicaragua.

    Science.gov (United States)

    Venugopal, S.; Moune, S.; Williams-Jones, G.

    2015-12-01

    Cerro Negro, the youngest volcano in the Central American Volcanic Belt, is a polygenetic cinder cone with relatively frequent explosive basaltic eruptions. Las Pilas, on the other hand, is a much larger and older complex with milder and less frequent eruptions. Based on historical data, these two closely spaced volcanoes have shown concurrent eruptive behavior, suggesting a subsurface connection. To further investigate this link, melt inclusions, which are blebs of melt trapped in growing crystals, were the obvious choice for optimal comparison of sources and determination of pre-eruptive volatile contents and magmatic conditions. Olivine-hosted inclusions were chosen for both volcanoes and pyroxene-hosted inclusions were also sampled from Las Pilas to represent the evolved melt. Major, volatile and trace elements reveal a distinct geochemical continuum with Cerro Negro defining the primitive end member and Las Pilas representing the evolved end member. Volatile contents are high for Cerro Negro (up to 1260 ppm CO2, 4.27 wt% H2O and 1700 ppm S) suggesting that volatile exsolution is likely the trigger for Cerro Negro's explosive eruptions. Las Pilas volatile contents are lower but consistent with degassing and evolutionary trends shown by major oxides. Trace element contents are rather unique and suggest Cerro Negro magmas fractionally crystallize while Las Pilas magmas are the products of mixing. Magmatic conditions were estimated with major and volatile contents: at least 2.4 kbar and 1170 °C for Cerro Negro melts and 1.3 kbar and 1130 °C for Las Pilas melts with an overall oxygen fugacity at the NNO buffer. In combination with available literature data, this study suggests an interconnected subsurface plumbing system and thus Cerro Negro should be considered as the newest vent within the Las Pilas-El Hoyo Complex.

  1. Mineralogy, geochemistry, and evolution of the Mivehrood skarn and the associated pluton, northwest Iran

    Science.gov (United States)

    Alirezaei, Saeed; Einali, Morteza; Jones, Peter; Hassanpour, Shohreh; Arjmandzadeh, Reza

    2016-04-01

    An Upper Miocene (9.12 ± 0.19 Ma; biotite 40Ar/39Ar) shallow pluton and numerous dykes and sills of felsic-intermediate compositions intruded the Upper Cretaceous, flysch-type sediments in the Mivehrood area, northwest Iran. The intrusions caused extensive thermal metamorphism and metasomatism, leading to the formation of hornfels and skarn. A massive skarn, 1-10 m thick, immediate to the intrusive contact, is bordered by a banded skarn, 100-400 m thick, that grades outward into hornfels and original sediments. The Mivehrood pluton is characterized by steep REE pattern, high Al2O3 (14.64-16.4 wt%) and Sr (380-786 ppm), and low MgO (1.3-3.4 wt%), Y (4.8-10.7 ppm), and Yb (0.35-0.95 ppm), characteristics typical of high-silica adakites. Skarn formation started with thermal metamorphism, followed by anhydrous prograde and hydrous retrograde stages. Prograde and retrograde mineral assemblages are developed in both skarns, represented by garnet-clinopyroxene-wollastonite and epidote-actinolite-scapolite-chlorite, respectively. Granditic F-bearing garnet dominates clinopyroxene in both skarns. The banded skarn contains minor scapolite of marialite composition. The calc-silicate mineral assemblages and the mineral chemistry allow the Mivehrood skarn to be classified as a calcic, oxidized skarn. Mass balance assessments suggest that Fe, Si, and S were significantly enriched, and Na, LILEs, and LREEs were strongly depleted, in the massive skarn. In the banded skarn, Na, K, Si, and S were enriched. Significant dehydration and carbon degassing occurred in both skarns. Stockworks, veins, and replacement bodies of pyrite ± chalcopyrite locally occur in the pluton and the dykes and in the skarns. The δ34SCDT values for the sulfides fall in a narrow range around 0.0 ‰, suggesting a magmatic source for sulfur and possibly the hydrothermal water and solutes involved in the skarn formation.

  2. Ductile strain rate recorded in the Symvolon syn-extensional plutonic body (Rhodope core complex, Greece)

    Science.gov (United States)

    Cirrincione, Rosolino; Fazio, Eugenio; Ortolano, Gaetano; Fiannacca, Patrizia; Kern, Hartmut; Mengel, Kurt; Pezzino, Antonino; Punturo, Rosalda

    2016-04-01

    The present contribution deals with quantitative microstructural analysis, which was performed on granodiorites of the syn-tectonic Symvolon pluton (Punturo et al., 2014) at the south-western boundary of the Rhodope Core Complex (Greece). Our purpose is the quantification of ductile strain rate achieved across the pluton, by considering its cooling gradient from the centre to the periphery, using the combination of a paleopiezometer (Shimizu, 2008) and a quartz flow law (Hirth et al., 2001). Obtained results, associated with a detailed cooling history (Dinter et al., 1995), allowed us to reconstruct the joined cooling and strain gradient evolution of the pluton from its emplacement during early Miocene (ca. 700°C at 22 Ma) to its following cooling stage (ca. 500-300°C at 15 Ma). Shearing temperature values were constrained by means of a thermodynamic approach based on the recognition of syn-shear assemblages at incremental strain; to this aim, statistical handling of mineral chemistry X-Ray maps was carried out on microdomains detected at the tails of porphyroclasts. Results indicate that the strain/cooling gradients evolve "arm in arm" across the pluton, as also testified by the progressive development of mylonitic fabric over the magmatic microstructures approaching the host rock. References • Dinter, D. A., Macfarlane, A., Hames, W., Isachsen, C., Bowring, S., and Royden, L. (1995). U-Pb and 40Ar/39Ar geochronology of the Symvolon granodiorite: Implications for the thermal and structural evolution of the Rhodope metamorphic core complex, northeastern Greece. Tectonics, 14 (4), 886-908. • Shimizu, I. (2008). Theories and applicability of grain size piezometers: The role of dynamic recrystallization mechanisms. Journal of Structural Geology, 30 (7), 899-917. • Hirth, G., Teyssier, C., and Dunlap, J. W. (2001). An evaluation of quartzite flow laws based on comparisons between experimentally and naturally deformed rocks. International Journal of Earth

  3. Occurrence of parsonite, a secondary uranium mineral, in alaskite of the Wheeler Creek pluton, Alaska

    International Nuclear Information System (INIS)

    Reconnaissance investigations in the Purcell Mountains of westcentral Alaska in 1977 revealed the presence of parsonite, a hydrous phosphate of lead and uranium with the formula Pb2UO2(PO4)22H2O. This is the first reported occurrence of parsonite in Alaska. The parsonite occurs as a soft, yellow to chocolate brown coating closely associated with green muscovite on fracture surfaces in a shear zone in alaskite of the Wheeler Creek pluton. Thin magnetite veinlets are also present. The identification of parsonite was confirmed by x-ray diffraction. Delayed neutron analysis were run on samples of the Alaskite

  4. Redox potential of the Khibiny magmatic system and genesis of abiogenic hydrocarbons in alkaline plutons

    Science.gov (United States)

    Ryabchikov, I. D.; Kogarko, L. N.

    2009-12-01

    The temperature and redox conditions of the crystallization of rocks from the Khibiny alkaline pluton have been estimated based on an analysis of coexisting magnetite, ilmenite, titanite, and pyroxene. Under redox conditions characteristic of the Khibiny Complex, CO2 is contained in fluid and carbonate anions are contained in melt at high temperature; then graphite is released and an appreciable amount of hydrocarbons appear at a lower temperature as products of reaction of graphite with fluid. Abiogenic hydrocarbons can arise in igneous complexes owing to a processes distinct from Fischer-Tropsch synthesis.

  5. Sm-Nd whole-rock isotope system of the Eye-Dashwa Lakes pluton

    International Nuclear Information System (INIS)

    An unaltered drill-core sample of the Eye-Dashwa Lakes pluton (sample ATK-1 (990.97-996.78)) is light rare earth enriched, with a 147Sm/144Nd ratio of 0.08699 and a 143Nd/144Nd ratio of 0.510815. The depleted mantle model age of 2.68 Ga agrees with emplacement ages, indicating that parental magma or its protolith was derived directly from a depleted mantle and that the crustal residence time was short

  6. Pluton accommodation at high strain rates in the upper continental crust. The example of the Central Extremadura batholith, Spain

    Science.gov (United States)

    Fernández, Carlos; Castro, Antonio

    1999-08-01

    Emplacement in the tensional bridge of a stepped dextral shear zone system is proposed for the Central Extremadura batholith (Spain). The country rocks show a pervasive anisotropy that conditioned the style of the structures developed as a consequence of the transference of displacement from the stepped shear zones to the releasing area. The kinematic evolution of the resulting megakink fold provided the volume increase necessary for the granite emplacement. Thermal and kinematic models suggest that the growth of individual plutons took place in periods of no more than several hundred to a few thousand years. Fast strain rates (10 -10-10 -11 s -1) must concentrate in local structures (e.g. initiation of kink folds) even in zones deforming as a whole under typical strain rates (10 -14±1 s -1). Granite plutons might be used as strain-rate gauges for syn-plutonic structures.

  7. Simulação interactiva do mercado de energia eléctrica

    OpenAIRE

    Adão, Bruno Miguel Ferreira

    2011-01-01

    A área de comercialização de energia eléctrica conheceu uma profunda mudança após a liberalização do sector eléctrico, que levou à criação de algumas entidades, as quais gerem os mercados de electricidade europeus. Relativamente a Portugal e Espanha, durante esse processo de liberalização, deu-se também um acordo que os levou à criação de um mercado conjunto, um mercado Ibérico (MIBEL). Dentro deste mercado estão contemplados dois operadores, sendo que um deles representa o pólo Português (OM...

  8. Mercado de datos: conceptos y metodologías de desarrollo

    Directory of Open Access Journals (Sweden)

    Ricardo Chinchilla Arley

    2011-10-01

    Full Text Available En este artículo se ofrece una descripción sobre la importancia del depósito y del mercado de datos. Además, identifican y formulan las principales definiciones, esquemas y términos básicos relacionados con el mercado de datos. Igualmente, se establecen y desarrollan los modelos de implementación y las metodologías para el desarrollo de un mercado de datos. Por último, se consideran las formas tecnológicas de procesamiento analítico en línea (OLAP y su utilidad en el análisis del mercado de datos.

  9. Investigation of the mineral potential of the Clipper Gap, Lone Mountain-Weepah, and Pipe Spring plutons, Nevada

    International Nuclear Information System (INIS)

    The Clipper Gap pluton, composed mostly of quartz monzonite with minor granite, granodiorite, and crosscutting alaskite dikes, intrudes Paleozoic western facies strata. A narrow zone of contact metamorphism is present at the intrusive-sediment contact. No mineral production has been recorded from Clipper Gap, but quartz veins containing gold-silver-copper mineral occurrences have been prospected there from the late 1800's to the present. Areas of the Lone Mountain-Weepah plutons that were studied are located in Esmeralda County about 14 km west of Tonopah, Nevada. At Lone Mountain, a Cretaceous intrusive cuts folded Precambrian and Cambrian sediments. Lead-zinc ores have been mined from small replacement ore bodies in the Alpine district, west of Lone Mountain. Copper and molybdenum occurrences have been found along the east flank of Lone Mountain, and altered areas were noted in intrusive outcrops around the south end of Lone Mountain. Mineral occurrences are widespread and varied with mining activity dating back to the 1860's. The Pipe Spring pluton study area is flanked by two important mining districts, Manhattan to the north and Belmont to the northeast. Mining activity at Belmont dates from 1865. Activity at Manhattan was mainly between 1907 and 1947, but the district is active at the present time (1979). Four smaller mining areas, Monarch, Spanish Springs, Baxter Spring, and Willow Springs, are within the general boundary of the area. The Pipe Spring pluton study area contains numerous prospects along the northern contact zone of the pluton. Tungsten-bearing veins occur within the pluton near Spanish Springs, with potential for gold-tungsten placer in the Ralston Valley. Nickel and associated metals occur at Willow Spring and Monarch Ranch, where prospects may be associated with the margin of the Big Ten Peak Caldera

  10. Say, Sismondi e o debate continental sobre os mercados

    Directory of Open Access Journals (Sweden)

    Rogério Arthmar

    2009-06-01

    Full Text Available O artigo versa sobre o debate travado entre Say e Sismondi a respeito da possibilidade de saturação geral dos mercados. Na primeira seção, descreve-se o contexto histórico da Europa continental nas primeiras décadas do século 19, destacando-se as particularidades da experiência francesa de industrialização ante a liderança britânica nesse campo. A seguir, traça-se breve perfil da formação intelectual de Say a fim de apresentar sua visão sobre o funcionamento dos mercados. Na continuação, examina-se a perspectiva histórica de Sismondi em sua crítica da ortodoxia clássica, bem como sua versão para a tendência do sistema capitalista à superprodução. Nas duas últimas partes, recuperam-se os comentários recíprocos de Say e Sismondi a respeito de suas divergências teóricas sobre os limites da acumulação de capital.This paper deals with the debate happened between Say and Sismondi regarding the possibility of a general glut. The first section describes the historical context of the first decades of nineteenth century continental Europe, focusing on the French industrialization experience vis-à-vis the British leadership in this field. Next, a brief intellectual profile of the evolution of Say's thought is made in order to present his vision about the proper working of markets. After that, the historical approach used by Sismondi in his criticism of classical orthodoxy is examined, as well as his own version to the capitalistic system inner tendency towards overproduction. The last two sections retrieve the exchange between Say and Sismondi over their theoretical disagreements on the limits to capital accumulation.

  11. Cambios en la posici??n de mercado de las empresas colombianas

    OpenAIRE

    Ram??rez Hassan, Andr??s; Garc??a Pel??ez, Santiago; Garc??s Ceballos, Jos?? David.

    2011-01-01

    En la posici??n de mercado de las empresas colombianas, seg??n la matriz crecimiento-participaci??ndesarrollada por la firma Boston Consulting Group. Para ello se utilizan datos de laSuperintendencia de Sociedades de Colombia y se aplican modelos logit multinomiales. Losresultados indican que en t??rminos generales, las variables financieras afectan de manerasimilar la posici??n de mercado de todas las empresas, mientras que variables de organizaci??nindustrial tienen efectos distintos que de...

  12. Elementos institucionales en la oligopolización de los mercados

    OpenAIRE

    Buesa Blanco, Mikel

    1987-01-01

    Este texto pone de relieve la importancia que la configuración institucional de los mercados tiene para la existencia en ellos de condiciones estructurales que constriñen el clima competitivo. Para ello, el autor analiza, en una perspectiva teórica, las vinculaciones interempresariales, el control del capital y las principales políticas económicas que influyen, favoreciéndola o desestimulándola, sobre la competencia en los mercados.

  13. EFICIENCIA DE MERCADO, ADMINISTRACION DE CARTERAS DE FONDOS Y BEHAVIOURAL FINANCE

    OpenAIRE

    Fernando Rubio

    2005-01-01

    El presente documento de trabajo, muestra un analisis y la evolucion historica reportada de la eficiencia de mercado, la administracion de carteras de fondos y sobre behavioural finance, principalmente en el mercado de USA, por lejos el mas importante del mundo. Tambien, se muestra investigacion en España. Primero, se discute brevemente la teoria al respecto, para luego concentrarse en la evidencia empirica reportada. Nota: se indica mas informacion bibliografica que la reportada.

  14. Regional geochemical study of the felsic plutonic rocks in the Nuqrah Quadrangle, sheet 25E, Kingdom of Saudi Arabia

    Science.gov (United States)

    Hall, W.E.; Dellinger, David; Selner, G.I.

    1985-01-01

    A regional geochemical investigation of the felsic plutonic rocks of the Nuqrah quadrangle, sheet 25 E, Kingdom of Saudi Arabia, in which pan concentrates of 384 wadi samples, and 145 rock samples, were collected, defined two separate and distinct anomalous areas. One area contains Jabal Tuwalah and Jabal Awja, and the other is at the north end of Jabal Safad. Both pan concentrates and the rock samples in the Jabal Tuwalah and Jabal Awja areas contain high concentrations of Be, F, La, Mo, Nb, Pb, Th, U, Sn, Y, and Zr, and the plutons underlying those areas are characterized by high total-count radioactivity.

  15. Santa Eulália Plutonic Complex (Southern Portugal): petrology, geochemistry and structural control of a late variscan structure

    OpenAIRE

    Lopes, Luis; Lopes, José Carrilho; Sant'Ovaia, Helena; Nogueira, Pedro; Ribeiro, Maria dos Anjos

    2013-01-01

    The Santa Eulália Plutonic Complex (SEPC) is a 400 km2 late variscan granitic pluton in the SW sector of the Iberian Variscides which cross-cuts the regional NW-SE Upper Proterozoic to Lower Palaeozoic lithological units. From the rim to the core, SEPC shows a medium- to coarse-grained pink granite (G0 group) involving large elongated masses of mafic to intermediate rocks (M group) and a central grey monzonitic granite (G1 group) mainly represented by medium-grained textures. Elemental geo...

  16. The gabbro (shoshonitic)-monzonite-granodiorite association of Khankandi pluton, Alborz Mountains, NW Iran

    Science.gov (United States)

    Aghazadeh, Mehraj; Castro, Antonio; Omran, Nematallah Rashidnejad; Emami, Mohamad Hashem; Moinvaziri, Hossien; Badrzadeh, Zahra

    2010-05-01

    The Khankandi pluton forms part of a group of gabbro-granodiorite intrusions in the Alborz Mountains of NW Iran. A petrographical and geochemical study of this plutonic association reveals the existence of several magmatic cycles with different origins and slight differences in age. The oldest cycle (C1) is represented by granodiorites. A second cycle (C2) is formed by a gabbro-monzonite association, with a clear shoshonitic affinity, that dominates most of the intrusive volume. Gabbros and monzonites form a co-magmatic association. Zircons from the monzonites were analyzed by LA-ICP-MS for U-Pb dating. An average age of 28.9 Ma, ranging from 23.7 to 33.6 Ma was obtained. Gabbros, monzonites and granodiorites share a nearly common isotopic ratio for Sr and Nd. Both initial Sr and Nd ratios are clustered within a narrow range from 0.7045 to 0.7047 for the 87Sr/ 86Sr ratio and ɛNd from 1.46 to 1.89. Comparison with experimental studies, together with mantle-like isotopic ratios and comparisons of REE patterns, points to an origin by variable melting rates from a common metasomatised mantle source for gabbros and monzonites. Melting of a subducted mélange is suggested for the granodiorite magmas predating the gabbro-monzonite intrusion. The two sources, a metasomatised mantle and ascending silicic plumes, are direct consequence of subduction.

  17. Model of formation of the Khibiny-Lovozero ore-bearing volcanic-plutonic complex

    Science.gov (United States)

    Arzamastsev, A. A.; Arzamastseva, L. V.; Zhirova, A. M.; Glaznev, V. N.

    2013-09-01

    The paper presents the results of a study of the large Paleozoic ore-magmatic system in the northeastern Fennoscandian Shield comprising the Khibiny and Lovozero plutons, the Kurga intrusion, volcanic rocks, and numerous alkaline dike swarms. As follows from the results of deep drilling and 3D geophysical simulation, large bodies of rocks pertaining to the ultramafic alkaline complex occur at the lower level of the ore-magmatic system. Peridotite, pyroxenite, melilitolite, melteigite, and ijolite occupy more than 50 vol % of the volcanic-plutonic complex within the upper 15 km accessible to gravity exploration. The proposed model represents the ore-magmatic system as a conjugate network of mantle magmatic sources localized at different depth levels and periodically supplying the melts belonging to the two autonomous groups: (1) ultramafic alkaline rocks with carbonatites and (2) alkali syenites-peralkaline syenites, which were formed synchronously having a common system of outlet conduits. With allowance for the available isotopic datings and new geochronological evidence, the duration of complex formation beginning from supply of the first batches of melt into calderas and up to postmagmatic events, expressed in formation of late pegmatoids, was no less than 25 Ma.

  18. The Precambrian/Lower Cambrian pluton from Vila Nova (Central Portugal)

    Energy Technology Data Exchange (ETDEWEB)

    Reis, A. I. M.; Silva, M. M. V. G.; Antunes, I. M. H. R.

    2010-07-01

    The Vila Nova pluton is a small, Pre-Variscan granitic body that intruded rocks of the Central Iberian Zone near the contact with the Ossa Morena Zone and is affected by several shear zones and faults. Its contact metamorphic aureole is constituted by micaschist with porphyroblasts in the outer zone and hornfels in the inner zone. Small mainstreamed xenoliths are dispersed all over the body. The pluton has a great mineralogical heterogeneity with pronounced variations in muscovite/biotite and plagioclase/ microcline contents and is classified as granite, granodiorite or tonalite. It is a leuco granite, highly peraluminous (A/CN K = 1.31 - 1.64), magnesian and calc-alkaline to alkaline-calcic. The variation diagrams show curvilinear trends with silica. Eu/Eu* = 0.47 - 0.77 and there is a slight enrichment in LREE relative to HREE. The normalized diagrams indicated dominantly crustal granite, related to subduction. U-Pb isotopic data of zircon and monazite gives 540-542 Ma age. (Author) 19 refs.

  19. Plutonic rocks of Jurassic age in the Alaska-Aleutian Range batholith: chemical variation and polarity.

    Science.gov (United States)

    Reed, B.I.; Miesch, A.T.; Lanphere, M.A.

    1983-01-01

    Plutonic rocks of Jurassic age exposed on the Pacific side of this batholith form a compositionally continuous calc-alkaline suite that ranges from hornblende gabbro to quartz monzonite. Tonalite and quartz diorite are the dominant rock types. Trend-surface analysis of 102 samples indicates that the direction of slope of the trend is approximately normal to the Jurassic magmatic arc. K2O and SiO2 increase towards the E-SE and the other oxides towards the W-NW. If the chemical trends reflect the approximate geometry of a palaeo-subduction zone, the polarity of the Jurassic magmatic arc is to the NW, i.e. subduction was directed towards the SE. Thus the palaeo-subduction zone is on the opposite side of the arc from the position that has generally been assumed, indicating that the Jurassic plutonic rocks were not generated in response to classical Andean-type convergent plate margins. The magmatic arc may have been formed in an intra-ocean environment and subsequently has been rafted northwards and accreted to this part of the N Pacific rim during the late Mesozoic. Middle and Upper Jurassic clastics underlying Cook Inlet to the SE and derived from the magmatic arc are classified as back-arc deposits, rather than as an arc-trench gap sequence.-L.C.H.

  20. Reworked old crust-derived shoshonitic magma: The Guarany pluton, Northeastern Brazil

    Science.gov (United States)

    Ferreira, Valderez P.; Sial, Alcides N.; Pimentel, Marcio M.; Armstrong, Richard; Guimarães, Ignez P.; da Silva Filho, Adejardo F.; de Lima, Mariucha Maria C.; da Silva, Thyego R.

    2015-09-01

    The 572 Ma Guarany stock consists of magmatic epidote-bearing hornblende monzodiorite to biotite granite that intruded Paleoproterozoic orthogneisses about 10 km inland from the coast in northeastern Brazil. Co-magmatic diorite enclaves and dikes are abundant throughout the pluton. The monzodiorite-granite pluton and diorite enclaves are shoshonitic and display continuous trends in variation diagrams. They display chemical and isotopic characteristics of crustal melts, such as enrichment in incompatible elements, high back-calculated initial 87Sr/86Sr ratios (avg. 0.71253), negative εNd (0.57Ga) values (avg. - 14.58), as well as high and variable (+ 9.1 to + 11.1‰VSMOW) δ18O (zircon) values. Correlations between O-isotope and whole-rock silica contents, as well as initial 87Sr/86Sr ratios with 1/Sr concentrations, suggest hybridization of a lower continental crustal melt with more felsic crustal rocks, concomitant with fractional crystallization. Amphibole chemistry and whole rock Zr, TiO2 and P2O5 contents suggest magma solidification at a pressure ~ 7 kbar and near liquidus temperature ~ 900 °C. The parental magma was likely formed by partial melting of old (tDM = 2.0 Ga) amphibolitic lower continental crustal rocks, in a post-collisional setting, probably triggered by underplating of mantle-derived mafic magma during the period of relaxation after collision.

  1. Poder de mercado en mercados spot de generación eléctrica: metodología para su análisis

    OpenAIRE

    García, John J.; Bohórquez, Santiago; López, Gustavo; Marín, Fredy

    2013-01-01

    Después de analizar las experiencias internacionales relacionadas con el monitoreo y control de poder de mercado, se establece una metodología acorde a las características del pool eléctrico en Colombia, la cual permite hacer seguimiento sobre comportamientos estratégicos respecto al precio en bolsa en este mercado. Se propone un modelo exponencial para la función de oferta en el pool basado en un modelo de precios spot, explicado por los costos, las condiciones climáticas, las intervenciones...

  2. Propuestas de cambios en el mercado eléctrico español para aumentar el volumen y la competitividad en los mercados a plazo

    OpenAIRE

    Hernández Alonso, Noé

    2014-01-01

    La energía se ha convertido en la actualidad en un pilar básico que influye en todos los ámbitos de las sociedades avanzadas, desde las grandes industrias hasta las casas pasando por los servicios como hospitales o transporte. Por ello el sector energético se ha convertido en un sector clave para todos los países. Una pieza importante dentro del sector energético español es el mercado eléctrico, en el cual los agentes de mercado (generadores y consumidores) transaccionan la energía que uno...

  3. Inteligencia de mercados: comportamientos estratégicos sobre precios de oferta en el mercado spot eléctrico Colombiano

    OpenAIRE

    Bastidas Olivares, Manuela; Quintero M, O. Lucia; García, John J.

    2013-01-01

    El mercado de energía mayorista es uno de los sectores industriales más competitivos de Colombia, y representa uno de los ejes principales en la economía del país. Este mercado ha sido objeto de estudio de varias áreas de conocimiento como la ingeniería eléctrica, economía, finanzas y otros. Aquí se presenta un análisis de los posibles comportamientos estratégicos de los principales agentes de la industria, desde la perspectiva de la inteligencia artificial orientada a la inteligencia de m...

  4. Update of the basement model of the Cerro Prieto, B. C., geothermal field, Mexico; Actualizacion del modelo del basamento en el campo geotermico de Cerro Prieto, B.C., Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Gonzalez Lopez, Macario [Residencia General de Cerro Prieto, Comision Federal de Electricidad, Mexicali, Baja California (Mexico)

    1999-04-01

    With the aim to actualize the basement model of the Cerro Prieto Geothermal Field, a gravity interpretation has been held. We modeled in 2.5 D, nine profiles traced over the Bouguer anomaly map. Well data concerning lithology and density changes were used to fit the gravity models. Results of this work confirm that the geometry of the basement of Cerro Prieto, corresponds to a structural sequence. From west to east it starts as a big depression, continues with a strong uplift of the basement in the middle sector and finally deepens eastward in steps. The basement model proposed in the present work, defines a similar trend to that established by Fonseca y Razo (1980), but there are differences in basement depth in some areas. In the present model we interpret basement depths between 200 and 400 m deeper than in previous models to the south and northwest of the actual exploitation zone. [Spanish] Con el fin de actualizar el modelo del basamento en el Campo Geotermico de Cerro Prieto, se realizo una reinterpretacion gravimetrica, modelando en 2.5 D, 9 perfiles trazados sobre el mapa de anomalia de Bouguer. Utilizando la informacion litologica obtenida a traves de numerosas perforaciones profundas, se hicieron coincidir, dentro de los mofelos gravimetricos, las principales variaciones litologicas con cambios en la densidad. Los resultados de este trabajo reiteran que la geometria del basamento del Campo de Cerro Prieto, vista de W a E, corresponde con una secuencia estructural que se inicia con una gran depresion en el W, continua con un fuerte levantamiento y finalmente se extiende con una tendencia a profundizarse hacia el E de forma escalonada. El modelo de basamento derivado del presente trabajo, define una tendencia muy similar al modelo de basamento establecido (Fonseca y Razo, 1980), pero difiere en cuanto a la profundidad en algunos sectores del campo. En el actual trabajo se interpreta una profundidad entre 200 y 400 m mayor hacia el sur y noroeste de la

  5. Evolution of the CP-I sector of the Cerro Prieto geothermal reservoir, BC, and exploitation alternatives; Evolucion del sector CP-I del yacimiento geotermico de Cerro Prieto, BC, y alternativas de explotacion

    Energy Technology Data Exchange (ETDEWEB)

    Rodriguez Rodriguez, Marco Helio [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia General de Cerro Prieto, Mexicali, Baja California (Mexico)]. E-mail: marco.rodriguez01@cfe.gob.mx

    2010-01-15

    After 35 years of exploitation of the CP-I (Cerro Prieto I) sector of the Cerro Prieto geothermal field, its thermal conditions have been declined substantially; the number of production wells is reduced and exploitation has been abandoned in some zones. However with a binary cycle, it is still possible to generate electricity from the remaining reservoir energy. To do so, one needs to know a detailed reservoir history of the sector, identifying the best potential strata to be assessed. In this paper, the CP-I reservoir evolution is presented and its exploitation and main reservoir characteristics -which play important roles- are identified. The CP-I zones offering the best conditions for binary cycle exploitation are identified. Exploiting partially abandoned reservoir sections is crucial for the future of the field. If such sections can be made to produce, this will help reduce the progressive steam-production decline in the occurring since production began. The production decline had been mitigated by a large area available for drilling replacement production wells, but such an area is limited now, due to the vast number of operating wells. [Spanish] Despues de 35 anos de explotacion del yacimiento en el sector de CP-I (Cerro Prieto I) del campo geotermico de Cerro Prieto, BC, sus condiciones termicas han declinado considerablemente, por lo que el numero de pozos productores ha disminuido, dejando algunas zonas abandonadas a la explotacion. Sin embargo, aun es posible aprovechar la energia que contiene este sector del yacimiento para la generacion de electricidad mediante ciclo binario. Para ello primeramente se debe conocer en detalle cual ha sido la evolucion del yacimiento en este sector, identificando los estratos de mejor potencial para evaluarlos posteriormente. En este estudio se presenta la evolucion del yacimiento de CP-I como respuesta a su explotacion, identificando las principales caracteristicas del yacimiento que determinan su comportamiento. Asi

  6. Criteria to determine the depth of the production interval in wells of the Cerro Prieto geothermal field, Mexico; Criterios para determinar la profundidad del intervalo productor en pozos del campo geotermico de Cerro Prieto, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Leon Vivar, Jesus Saul de [Comision Federal de Electricidad, Residencia General de Cerro Prieto, Mexicali, B.C. (Mexico)]. E-mail: jesus.deleon@cfe.gob.mx

    2006-07-15

    Ways to select the depth of the production interval or to complete wells in the Cerro Prieto geothermal field have changed during the development of the field. From 1961 when drilling began to the middle of 2005, a total of 325 wells were drilled. The paper compares the approaches used in the past with those of the last ten years. The Cerro Prieto system has been classified as being of liquid-dominated and high-temperature. Today, after 33 years of commercial exploitation, it has experienced a series of thermal and geochemical fluid changes making it necessary to modify the ways to select the depth of the well production intervals, according to the observed behavior of the reservoir. The new criteria include the thermal approach, the geological approach, the geochemical approach and a comparative approach with neighboring wells. If most of these criteria are interpreted correctly, the success of a well is ensured. [Spanish] Los criterios para seleccionar la profundidad del intervalo productor o la terminacion de los pozos en el campo geotermico de Cerro Prieto han cambiado durante el desarrollo del mismo. De 1961, cuando se perforaron los primeros pozos, hasta mediados del 2005 se han perforado un total de 325 pozos. En el presente articulo se hara una breve revision de cuales han sido los criterios usados en el pasado y los que se han venido empleando en los ultimos diez anos. El yacimiento de Cerro Prieto ha sido clasificado como de liquido dominante, de alta temperatura, pero actualmente, despues de 33 anos de explotacion comercial, ha sufrido una serie de cambios termicos y geoquimicos en sus fluidos, por lo que ha sido necesario modificar los criterios para seleccionar la profundidad del intervalo productor de los pozos de acuerdo al comportamiento observado en el yacimiento. Los criterios actuales se dividen en cuatro: 1. Criterio termico, 2. Criterio geologico, 3. Criterio geoquimico y 4. Criterio comparativo de los pozos vecinos. Cuando la mayoria de estos

  7. ESTRATEGIA DE REMONTAJE APLICADA SOBRE EL REGISTRO CERÁMICO DEL SITIO LOS TRES CERROS 1 (DELTA SUPERIOR DEL RÍO PARANÁ) / Refitting applied to pottery from Los Tres Cerros 1 site (Upper Delta of Paraná River)

    OpenAIRE

    Violeta Soledad Di Prado; Canela Castro

    2014-01-01

    El sitio arqueológico Los Tres Cerros 1 se encuentra ubicado en el departamento Victoria, Entre Ríos, y consiste en una estructura monticular con una compleja historia ocupacional. La abundancia y fragmentación del registro cerámico del sitio, llevaron a aplicar la estrategia de remontajes, con el propósito de reconstruir la historia de vida de las vasijas e identificar las prácticas humanas y los agentes naturales que actuaron en la configuración del depósito. Sobre una muestra del total de ...

  8. Tracking the growth of plutons: the contribution of high-precision U-Pb zircon dating

    International Nuclear Information System (INIS)

    Full text: A growing body of high-precision U-Pb data from magmatic zircon indicates that plutons grow over timescales of 105-106 years. A complex interplay of processes - including accumulation of melt batches from lower and middle crustal levels, crystallization, remelting of solidified crystal mushes, mixing and mingling, transfer of pheno- and xenocrysts between melt portions, and many more - results in equally complicated pluton structures and rock textures. The use of (202Pb-) 205Pb-233U-235U tracer solutions in U-Pb dating of magmatic zircon can lead to a precision of 0.1 % in the 206Pb/238U age of an individual zircon analysis, and to as low as 0.02 % for a weighted mean of 6-10 coeval analyses. Such uncertainty is well within the time interval of zircon crystallization and residence in intermediate and acid magmatic liquids and allows resolution of incremental accumulation of melt batches in plutons. We demonstrate that we can achieve sub-permil precisions with MSWD values of around 1 on weighted mean dates by analyzing simultaneously precipitated zircon from H2O-enriched residual liquids within zircon-undersaturated basalt. Any age variation in granitoid rocks beyond this analytical spread is therefore considered real age dispersion, leading to an array of non-equivalent, analytically concordant points (within decay constant uncertainty). The reasons for such age dispersion may be the following: incorporation of antecrystic zircon from earlier magma batches of the same magmatic system, which have crystallized 104 to 105 years earlier; protracted zircon crystallization within a single batch of magma during its ascent and emplacement; presence of smallest xenocrystic cores in the analyzed zircons which contain a small proportion of older lead; minor degrees of unresolved lead loss that lead to slightly young ages. Though Pb-loss can largely be avoided by applying chemical abrasion prior to analysis, its effects are difficult to rule out completely

  9. Subduction and exhumation structures preserved in Cerro del Almirez HP metaserpentinites (Betic Cordillera, SE Spain)

    Science.gov (United States)

    Jabaloy-Sánchez, Antonio; López Sánchez-Vizcaíno, Vicente; Gómez-Pugnaire, María Teresa; Padrón-Navarta, José Alberto; Garrido, Carlos J.

    2014-05-01

    The Cerro del Almirez massif (Nevado-Filábride Complex, Betic Cordillera, SE Spain) is composed of antigorite serpentinite and chlorite harzburgite separated by a thin reaction front in a paleo-subduction setting. Structural analysis of ultramafic lithologies and metasedimentary host rocks provides information on the tectonic evolution of this massif during prograde metamorphism in a subduction zone and during subsequent exhumation. Here we report for the first time HP structures related to a subduction event underwent by ultramafic rocks of the Nevado-Filábride Complex. The oldest subduction-related structures are preserved in Atg-serpentinites: a penetrative S1 foliation and associated L1 stretching lineation were formed in a non-coaxial regime with a top-to-the-W sense of shearing. This planar linear fabric is crosscut by olivine ± Ti-clinohumite veins formed during the prograde breakdown of brucite and pre-metamorphic clinopyroxene at temperatures ranging from 465 to 500 ºC [1]. Veins occur as a system of decimetric long joints, some of them hybrid open and sheared veins with associated drag folds. They recorded embrittlement processes due to the release of 6% vol. H2O of the rock. S1 foliation can, however, be simultaneous with or be overgrown by olivine and/or tremolite porphyroblasts, product of the prograde reaction Di + Atg → Fo + Tr + H2O, which occurred at T > 600 ºC and P = 1.7-1.9 GPa [1]. Generation of S1/L1 fabric was followed by static annealing at ca. 680 ºC and 1.6-1.9 GPa [2]. The S1/L1 fabric in Atg-serpentinite is crosscut by the Atg-out isograd and overgrown by the Atg-serpentinite dehydration products that gave place to Chl-harzburgite. Peak metamorphic conditions of the Chl-harzburgite assemblage reached 680-710 ºC and 1.6-1.9 GPa [3]. Prograde Chl-harzburgite is crosscut by sets of conjugate zones associated to grain-size reduction of olivine grains [3]. These grain size reduction zones are interpreted as brittle structures

  10. Shallow earthquake inhibits unrest near Chiles-Cerro Negro volcanoes, Ecuador-Colombian border

    Science.gov (United States)

    Ebmeier, Susanna K.; Elliott, John R.; Nocquet, Jean-Mathieu; Biggs, Juliet; Mothes, Patricia; Jarrín, Paúl; Yépez, Marco; Aguaiza, Santiago; Lundgren, Paul; Samsonov, Sergey V.

    2016-09-01

    Magma movement or reservoir pressurisation can drive swarms of low-magnitude volcano-tectonic earthquakes, as well as occasional larger earthquakes (>M5) on local tectonic faults. Earthquakes >M5 near volcanoes are challenging to interpret in terms of evolving volcanic hazard, but are often associated with eruptions, and in some cases enhance the ascent of magma. We present geodetic observations from the first episode of unrest known to have occurred near Chiles and Cerro Negro de Mayasquer volcanoes on the Ecuador-Colombian border. A swarm of volcano-tectonic seismicity in October 2014 culminated in a Mw 5.6 earthquake south of the volcanoes. Satellite radar data spanning this earthquake detect displacements that are consistent with dextral oblique slip on a reverse fault at depths of 1.4-3.4 km within a SSW-NNE trending fault zone that last ruptured in 1886. GPS station measurements capture ∼20 days of uplift before the earthquake, probably originating from a pressure source ∼10-15 km south of Volcán Chiles, at depths exceeding 13 km. After the Mw 5.6 earthquake, uplift ceased and the rate of seismicity began to decrease. Potential mechanisms for this decline in activity include a decrease in the rate of movement of magma into the shallow crust, possibly caused by the restriction of fluid pathways. Our observations demonstrate that an earthquake triggered during volcanic unrest can inhibit magmatic processes, and have implications for the hazard interpretation of the interactions between earthquakes and volcanoes.

  11. Glacier mass balance reconstruction by sublimation induced enrichment of chemical species on Cerro Tapado (Chilean Andes

    Directory of Open Access Journals (Sweden)

    P. Ginot

    2006-01-01

    Full Text Available A 36 m long ice core down to bedrock from the Cerro Tapado glacier (5536 m a.s.l, 30°08' S, 69°55' W was analyzed to reconstruct past climatic conditions for Northern Chile. Because of the marked seasonality in the precipitation (short wet winter and extended dry summer periods in this region, major snow ablation and related post-depositional processes occur on the glacier surface during summer periods. They include predominantly sublimation and dry deposition. Assuming that, like measured during the field campaign, the enrichment of chloride was always related to sublimation, the chemical record along the ice core may be applied to reconstruct the history of such secondary processes linked to the past climatic conditions over northern Chile. For the time period 1962–1999, a mean annual net accumulation of 316 mm water equivalent (weq and 327 mm weq loss by sublimation was deduced by this method. This corresponds to an initial total annual accumulation of 539 mm weq. The annual variability of the accumulation and sublimation is related with the Southern Oscillation Index (SOI: higher net-accumulation during El-Niño years and more sublimation during La Niña years. The deepest part of the ice record shows a time discontinuity; with an ice body deposited under different climatic conditions: 290 mm higher precipitation but with reduced seasonal distribution (+470 mm in winter and –180 mm in summer and –3°C lower mean annual temperature. Unfortunately, its age is unknown. The comparison with regional proxy data however let us conclude that the glacier buildup did most likely occur after the dry mid-Holocene.

  12. Water Quality Monitoring in the Cerro Solo U District Chubut, Argentina

    International Nuclear Information System (INIS)

    Full text: This work was carried out on behalf of the European Union INCO DC project called Water Quality in Mining Areas of Latin America. The Cerro Solo U district is located in Chubut province in the southern Patagonia region of Argentina at 43o20' south latitude and 68o45' west longitude, at 630 metres above sea level and covering an area of 420 square kilometers. The main deposit occurs as conformable layers and lenses within Cretaceous sandstones and conglomerates of the Los Adobes formation (Chubut Group). These units represent a high-energy fluvial system. The mineralized horizons occur between 60 and 120 metres below the surface. The average grade is 0.4% U, and the uranium resources (RAR + EAR I) are calculated in 4 600 tonnes of recoverable uranium. Cretaceous tuffs of the Cerro Barcino formation (Chubut Group) and Jurassic andesitic rocks of the Lonco Trapial formation complement the main local geology. In this area, a water quality monitoring network was established in order to evaluate the pre-mining hydro-geochemistry baseline of the district. The sampling stations include: exploration boreholes (8), springs and wells (5), streams (2) and an artesian well (1). The boreholes belong to the Cerro Solo deposit and represent the groundwater in contact with the mineralized bodies. The spring and well stations are located close to the deposit area and provide a source of water for human and animal consumption in the surrounding farms. The stream stations are located in the Chubut River, which is the only perennial stream in the region and represents the background for surface water quality. Finally, the artesian well represents a mineralized water source in the study area. In order to evaluate the seasonal variations in the water composition, the samples were collected both in the wet and dry periods of the year. Water samples were filtered (0.4 μm), and collected in pre-cleaned, high-density polyethylene bottles. Temperature, pH, Eh, dissolved oxygen

  13. Nem Deus nem Mercado: a Campanha da Fraternidade de 2010

    Directory of Open Access Journals (Sweden)

    José Rodorval Ramalho

    2016-05-01

    Full Text Available O presente texto analisa o tema da Campanha da Fraternidade Ecumênica de 2010 “Economia e Vida: Vocês não podem servir a Deus e ao Dinheiro”, promovida, entre outras instituições cristãs, pela Conferência Nacional dos Bispos do Brasil. Partindo dos principais documentos da referida campanha, realizamos uma comparação das categorias econômicas utilizadas com aquelas expressas no corpus da Doutrina Social da Igreja Católica. Concluímos que os bispos brasileiros fazem uso seletivo dos documentos papais, enfatizando as críticas às economias de mercado e realçando a necessidade da defesa de formas coletivistas e igualitaristas das relações econômicas. A base teórica para tais exercícios interpretativos da realidade econômica, sobretudo brasileira, é um marxismo economicista e insensível às mudanças ocorridas na estrutura do capitalismo contemporâneo. Os textos do episcopado brasileiro também ignoram o fracasso das experiências socialistas, sobretudo no século XX.

  14. Mercado de trabalho e rendimento no meio rural brasileiro

    Directory of Open Access Journals (Sweden)

    Gilnei C. Santos

    2010-09-01

    Full Text Available O presente trabalho analisa a entrada de homens e mulheres no mercado de trabalho rural e gera equações de rendimento para o meio rural brasileiro em 2007 com os microdados da PNAD. O procedimento de Heckman é adotado para se evitar viés de seletividade. Os resultados mostraram gaps ou diferenciais na seleção e rendimentos por gênero e raça. Apesar das mulheres apresentarem um nível de qualificação maior que o dos homens, observa-se que o rendimento destes tende a ser mais elevado do que o feminino. Adicionalmente, mulheres contempladas com o Bolsa Família tendem a reduzir a oferta de trabalho.This paper analyzes the entrance of men and women into the rural labor market and generates earning equations for the Brazilian rural areas in 2007 with the PNAD microdata. The Heckman procedure is adopted to avoid selectivity bias. Results had also shown the Brazilian rural labor market. Besides the fact that female workers on average have a higher level of qualification than male workers, male's earnings are higher than the female's. Women that receive the governmental transfer program Bolsa Família , tend to offer less work in the rural labor market.

  15. Structural control on geothermal circulation in the Cerro Tuzgle-Tocomar geothermal volcanic area (Puna plateau, Argentina)

    Science.gov (United States)

    Giordano, Guido; Pinton, Annamaria; Cianfarra, Paola; Baez, Walter; Chiodi, Agostina; Viramonte, José; Norini, Gianluca; Groppelli, Gianluca

    2013-01-01

    The reconstruction of the stratigraphical-structural framework and the hydrogeology of geothermal areas is fundamental for understanding the relationships between cap rocks, reservoir and circulation of geothermal fluids and for planning the exploitation of the field. The Cerro Tuzgle-Tocomar geothermal volcanic area (Puna plateau, Central Andes, NW Argentina) has a high geothermal potential. It is crossed by the active NW-SE trans-Andean tectonic lineament known as the Calama-Olacapato-Toro (COT) fault system, which favours a high secondary permeability testified by the presence of numerous springs. This study presents new stratigraphic and hydrogeological data on the geothermal field, together with the analysis from remote sensed image analysis of morphostructural evidences associated with the structural framework and active tectonics. Our data suggest that the main geothermal reservoir is located within or below the Pre-Palaeozoic-Ordovician basement units, characterised by unevenly distributed secondary permeability. The reservoir is recharged by infiltration in the ridges above 4500 m a.s.l., where basement rocks are in outcrop. Below 4500 m a.s.l., the reservoir is covered by the low permeable Miocene-Quaternary units that allow a poor circulation of shallow groundwater. Geothermal fluids upwell in areas with more intense fracturing, especially where main regional structures, particularly NW-SE COT-parallel lineaments, intersect with secondary structures, such as at the Tocomar field. Away from the main tectonic features, such as at the Cerro Tuzgle field, the less developed network of faults and fractures allows only a moderate upwelling of geothermal fluids and a mixing between hot and shallow cold waters. The integration of field-based and remote-sensing analyses at the Cerro Tuzgle-Tocomar area proved to be effective in approaching the prospection of remote geothermal fields, and in defining the conceptual model for geothermal circulation.

  16. Magma flow paths and strain patterns in magma chambers growing by floor subsidence: a model based on magnetic fabric study of shallow-level plutons in the Stiavnica volcano-plutonic complex, Western Carpathians

    Czech Academy of Sciences Publication Activity Database

    Tomek, Filip; Žák, J.; Chadima, Martin

    2014-01-01

    Roč. 76, č. 11 (2014), Article 873. ISSN 0258-8900 Institutional support: RVO:67985831 Keywords : anisotropy of magnetic susceptibility (AMS) * caldera * intrusive strain * magma emplacement * pluton floor subsidence * stratovolcano Subject RIV: DB - Geology ; Mineralogy Impact factor: 2.519, year: 2014

  17. Dieta de murciélagos nectarívoros del Parque Nacional Cerros de Amotape, Tumbes

    OpenAIRE

    Edith Arias; Richard Cadenillas; Víctor Pacheco

    2011-01-01

    En el Perú se reporta la presencia de 18 especies de murciélagos nectarívoros, sin embargo se cuenta con poca información sobre la dieta de estas especies. En este estudio se reporta por primera vez la dieta de los nectarívoros Glossophaga soricina, Lonchophylla hesperia y Anoura geoffroyi en el bosque seco ecuatorial y del bosque tropical del Pacífico del Parque Nacional Cerros de Amotape, Tumbes. Analizamos 21 contenidos gastrointestinales e identificamos ocho morfotipos de polen pertenecie...

  18. Palaeoenvironment reconstruction, volcanic evolution and geochronology of the Cerro Blanco subcomplex, Nevados de Chillan volcanic complex, Central Chile

    OpenAIRE

    Mee, Katy; Gilbert, Jennie S.; McGarvie, David W.; Naranjo, Jose A.; Pringle, Malcolm S.

    2009-01-01

    Nevados de Chillán Volcanic Complex, central Chile, has been active for at least 640 ka—a period spanning a number of glacial and interglacial periods. Geologic mapping, radiometric dating and geochemical analysis have identified six new volcanic units and produced four new 40Ar/39Ar ages for Cerro Blanco, the northern subcomplex of Nevados de Chillán volcano. Compositions range from dacite to basaltic-andesite and a new geologic map is presented. Examination of lava fracture structures on bo...

  19. Los marsupiales (Mammalia) del Mioceno Superior de la formación Cerro Azul (Provincia de la Pampa, Argentina)

    OpenAIRE

    Goin, Francisco Javier; Montalvo, Claudia; Visconti, G

    2000-01-01

    Se describe la asociación de marsupiales sudamericanos fósiles de edad Huayqueriense (Mioceno tardío) más completa hasta ahora conocida. Los ejemplares fueron exhumados de varias localidades fosilíferas nuevas del centro y norte de la provincia de La Pampa (Argentina central), en sedimentos asignables a la Formación Cerro Azul: Bajo Giuliani, Quehué, Telén, El Guanaco y Laguna Chillhué. El conjunto de las sedimentitas loessoides analizadas en los diferentes afloramientos de esta formación ind...

  20. Production induced boiling and cold water entry in the Cerro Prieto geothermal reservoir indicated by chemical and physical measurements

    Energy Technology Data Exchange (ETDEWEB)

    Grant, M.A. (DSIR, Wellington, New Zealand); Truesdell, A.H.; Manon, A.

    1981-01-01

    Chemical and physical data suggest that the relatively shallow western part of the Cerro Prieto reservoir is bounded below by low permeability rocks, and above and at the sides by an interface with cooler water. There is no continuous permeability barrier around or immediately above the reservoir. Permeability within the reservoir is dominantly intergranular. Mixture with cooler water rather than boiling is the dominant cooling process in the natural state, and production causes displacement of hot water by cooler water, not by vapor. Local boiling occurs near most wells in response to pressure decreases, but no general vapor zone has formed.

  1. Importaciones áticas del siglo V a.C. del Cerro del Prado (Algeciras, Cádiz)

    OpenAIRE

    Cabrera, Paloma; Perdigones, Lorenzo

    1996-01-01

    In this paper we analyze a group of Attic imports, found in the excavations of Cerro del Prado, a settlement situated in the Bahía de Algeciras (Cádiz). The great interest of this group lies in the fact that it belongs to a particular chronological period, the last third of the 5th century B.C., as we have not found later imports, and in the almost exclusive presence of black glazed vases, which gives US an idea of a very definitive demand of the punic society of the Iberian Peninsula regardi...

  2. Vertical movement along the Cerro Prieto transform fault, Baja California, Mexico - a mechanism for geothermal energy renewal

    Energy Technology Data Exchange (ETDEWEB)

    Vonder Haar, S.; Noble, J.E.; Puente Cruz, I.

    1979-03-01

    Data from 53 geothermal wells to depths of 1 to 3 km on either side of the right-lateral Cerro Prieto fault, as well as geophysical data, indicate vertical displacements of this fault of 400 to 600 m. This episoidic vertical movement has offset deltaic sandstone reservoirs that are primarily at 1200 m and 1800 m depth and contain 250{sup 0} to 345{sup 0}C water. A major fracture system for convective fluid movement has been thus maintained, with production at 150 MW.

  3. Trace element and isotopic chemistry of the surficial hydrothermal waters in the Cerro Prieto, Geothermal Field, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Valette-Silver, J.N.; Ganje, T.J.; Bradford, G.R.; Coplen, T.

    1982-08-10

    In the Cerro Prieto Geothermal Field, five kinds of surface emissions were discovered in spring, mud pot, geysers, fumarole, and cool pool. The major element composition of the 163 fluid samples collected in 1979, was previously performed. This study was recently completed by a determination of trace element concentrations, deuterium and oxygen isotope ratios. This geochemical analysis shows, as the major elements do, that each type of surficial emission is characterized by its own unique chemistry. Each category of surface emission appears to result from different processes; trace chemistry as well as isotope composition confirm the various origins of the different surface hydrothermal fluids.

  4. TITAN2D simulations of pyroclastic flows at Cerro Machín Volcano, Colombia: Hazard implications

    Science.gov (United States)

    Murcia, H. F.; Sheridan, M. F.; Macías, J. L.; Cortés, G. P.

    2010-03-01

    Cerro Machín is a dacitic tuff ring located in the central part of the Colombian Andes. It lies at the southern end of the Cerro Bravo-Cerro Machín volcanic belt. This volcano has experienced at least six major explosive eruptions during the last 5000 years. These eruptions have generated pyroclastic flows associated with Plinian activity that have traveled up to 8 km from the crater, and pyroclastic flows associated with Vulcanian activity with shorter runouts of 5 km from the source. Today, some 21,000 people live within a 8 km radius of Cerro Machín. The volcano is active with fumaroles and has shown increasing seismic activity since 2004, and therefore represents a potentially increasing threat to the local population. To evaluate the possible effects of future eruptions that may generate pyroclastic density currents controlled by granular flow dynamics we performed flow simulations with the TITAN2D code. These simulations were run in all directions around the volcano, using the input parameters of the largest eruption reported. The results show that an eruption of 0.3 km 3 of pyroclastic flows from a collapsing Plinian column would travel up to 9 km from the vent, emplacing a deposit thicker than 60 m within the Toche River valley. Deposits >45 m thick can be expected in the valleys of San Juan, Santa Marta, and Azufral creeks, while 30 m thick deposits could accumulate within the drainages of the Tochecito, Bermellón, and Coello Rivers. A minimum area of 56 km 2 could be affected directly by this kind of eruption. In comparison, Vulcanian column-collapse pyroclastic flows of 0.1 km 3 would travel up to 6 km from the vent depositing >45 m thick debris inside the Toche River valley and more than 30 m inside the valleys of San Juan, Santa Marta, and Azufral creeks. The minimum area that could be affected directly by this kind of eruption is 33 km 2. The distribution and thickness of the deposits obtained by these simulations are consistent with the hazard

  5. Estudio de la líqueno flora encontrada en el Cerro de Quininí, Tibacuy, Cundinamarca

    OpenAIRE

    Hormaza Francisco; Vivas Oscar; Parra Alejandro

    2000-01-01

    Se realizó un muestreo de la liquen o flora del cerro de Quininí, Tibacuy, Cundinamarca para estudiar las características morfológicas externas de los géneros de líquenes encontrados en el. A su vez se hizo la revisión bibliográfica acerca de dichos géneros, datando así la riqueza de líquenes en la zona con 8 géneros en total y con respecto al papel de bioindicadores se mostró el grado de intervención para el lugar.

  6. Estructura, composición y diversidad de la selva baja caducifolia del Cerro Verde, Nizanda (Oaxaca), México

    OpenAIRE

    José Antonio Gallardo Cruz; Meave, Jorge A.; Eduardo A. Pérez García

    2005-01-01

    En este estudio se describe la estructura, la composición florística y los patrones de diversidad de la selva baja caducifolia del Cerro Verde, localizado en Nizanda (Istmo de Tehuantepec, Oaxaca, México). En 30 parcelas de 100 m2 se censaron las plantas leñosas con DAP #8805; 1 cm (estrato alto), y en cinco subcuadros de 4 m2 dentro de cada una se censaron las plantas con DAP 1 cm, pero con altura 30 cm (estrato bajo). Se encontraron 194 especies distribuidas en 52 familias. La riqueza de...

  7. Changes in steam production due to the reservoir conditions in Cerro Prieto, Baja California; Cambios en la produccion de vapor debido a las condiciones del yacimiento en Cerro Prieto, Baja California

    Energy Technology Data Exchange (ETDEWEB)

    Morales Cardenas, Ramon; Rodriguez Rodriguez, Marco H. [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia General de Cerro Prieto, Mexicali, B.C. (Mexico)]. E-mail: marco.rodriguez01@gfe.gob.mx

    2011-07-15

    In more than 35 years of exploitation, thermodynamic conditions have changed in the Cerro Prieto geothermal reservoir. The effects are analyzed of the changes to the reservoir and their consequences to steam production in different field zones. For steam production, the most important features of reservoir fluids are enthalpies and pressures. The evolution of these features is presented in an enthalpy-pressure diagram. Here it can be seen that some reservoir zones have almost reached abandonment conditions. [Spanish] En mas de 35 anos de explotacion el yacimiento geotermico de Cerro Prieto ha experimentado cambios en sus condiciones termodinamicas. En este trabajo se analiza el efecto de esos cambios del yacimiento y su repercusion en la produccion de vapor para las diferentes zonas en las que se ha dividido el campo. Las propiedades mas importantes del fluido en el yacimiento para la produccion de vapor son su entalpia y su presion, por lo que se presenta la evolucion de esas propiedades en un diagrama de presion-entalpia, en el que se observa que hay zonas del yacimiento que estan proximas a alcanzar condiciones de abandono.

  8. Large capacity cnergy from Geo- Plutonic formation for power plants with zero CO2 emissions

    Directory of Open Access Journals (Sweden)

    R.H. Kozłowski

    2010-12-01

    Full Text Available Purpose: The publication presented is a realistic, one of the practicable idea for a substitute to system power plants, consisting in the construction of combined heat and power plants using renewable resources of geo-plutonic energy.Design/methodology/approach: There are various methods of obtaining geothermal energy and various uses for it. The proposed GEO-PLUTONIC ENERGY represents an endless, renewable source of energy coming from nuclear reaction in the Earth’s nucleus, where the temperature reaches 6,000 Centigrade. Mass production of electricity from the Earth’s heat, possible in Iceland due to the volcanic nature of these resources and the shallow depth at which they occur, was difficult in other countries due to the high cost of drilling to greater depths. This barrier has been overcome by us through using a special horizontal drilling technique.Findings: In order to extract and collect the accumulated energy from the area of a large thermal field, a modified shaft/drilling system (called a Super Daisy System equipped with a 3D grate of directional bore-holes called Jet-Stingers fitted with multi-functional heat exchangers is used. The emission-free concept of Geo-Plutonic Energy with the temperature of only over 250ºC, from which we can obtain about 30 MPa of pressure on the turbine. With increased the depth the temperature and heat transmissibility will be raised significantly, which can resulted the yield even to 7-10 MWe (of electricity from one deep heat exchanger.Research limitations/implications: From the rock mass we can collect renewable resources of ,,dry” ascending energy from the paleo heat flow coming from the great atomic furnace – the magma.Originality/value: We are experienced in using the appropriate hydro-thermodynamic theory and its applications which allows us to almost precisely forecast and control the quantity of heat not exceeding 20% of the 100% regeneration capability in the same time range.

  9. Geochemistry and tectonic implications of the trans-Himalayan Lohit plutonic complex, eastern Arunachal Pradesh

    International Nuclear Information System (INIS)

    The Trans-Himalayan Lohit Plutonic Complex occurs to the east of the Eastern Syntaxis in eastern Arunachal Pradesh and the investigations were carried out mainly along the Lohit River section. The plutonic complex intrudes the metavolcanics of probable arc affinity in the west and high-grade metamorphic rocks of the Asian continental margin in the east. It can be sub divided into western and eastern belts, separated by Walong Thrust. The complex consists of multiple intrusions and they are: (I) an early phase of metaluminous, tholeitic to calc- alkaline gabbro and quartz diorites with minor diorites and hybrid rocks; (2) an intermediate phase of calc-alkaline, metaluminous, leucotonalite of high Al-trondhjemitic or adakitic composition; (3) a last phase of peraluminous leucogranite and associated veins of pegmatite and aplite. The enrichment of large-ion-lithophile elements (LILE) relative to high field strength elements (HFSE) of these rock types suggest that they were emplaced in a subduction related environment and derived from different source materials. The major and trace element variations in the early gabbro-quartz diorite, along with the low initial 87Sr/86Sr ratio (0.703-0.704) suggest that they were derived from a parental tholeitic magma, from which the intrusives have been differentiated under increasing water pressure conditions. The geochemical characteristics of the trondhjemites, such as the high Na2O, Al2O3, Sr, Sr/Y ratios and low K2O, Y and depletion of heavy rare earth elements (HREE) are similar to those of adakite and Archaean high Al- trondhjemite. They might have been derived either by melting of the subducted oceanic crust or by partial melting of newly under- plated basaltic crust beneath the thickened continental arc leaving residual garnet and amphibole. The leucogranites with high K2O, Rb, K2O/Na2O, K/Rb, Rb/Sr ratios, and high initial 87Sr/86Sr ratio (0.713), along with depletion in HREE and absence of negative Eu anomaly, suggest

  10. Natural radioactivity and radiation index of the major plutonic bodies in Greece.

    Science.gov (United States)

    Papadopoulos, A; Christofides, G; Koroneos, A; Papadopoulou, L; Papastefanou, C; Stoulos, S

    2013-10-01

    The natural radioactivity of the major plutonic bodies in Greece, as well as the assessment of any potential health hazard due to their usage as decorative building materials is studied. One hundred and twenty one samples from every major plutonic body in Greece, including various rock-types from gabbro to granite, have been measured for their natural radioactivity using γ-spectrometry methodology. According to the experimental results, the natural radioactivity levels were ranged up to 315 Bq kg(-1) for (226)Ra, up to 376 Bq kg(-1) for (232)Th and up to 1632 Bq kg(-1) for (40)K, with arithmetic mean values and standard deviations of 74 (±51), 85 (±54) and 881 (±331) Bq kg(-1) respectively, which are below the international representative mean values for granite stones. The excess on the effective dose received annually indoors due to granite tiles usage is estimated considering a standard room model where granite tiles with 1.5 cm in thickness cover only the floor of the room. The increment on the external γ-radiation effective dose rate shows a Gaussian distribution well dispersed below 0.3 mSv y(-1), presenting a mean value of 0.14 (±0.06) mSv y(-1). In case of the internal α-radiation a log-normal distribution is appeared scattering below 0.5 mSv y(-1) with a mean value 0.19 (±0.13) mSv y(-1), for a well-ventilated living environment. In case of a poor-ventilated room the increment on internal effective dose rate is estimated with a mean value 0.27 (±0.19) mSv y(-1) scattering below 0.8 mSv y(-1). The majority of the samples increase the external as well as the internal dose less than 30% of the maximum permitted limit of the effective dose rate. Therefore, at least from radiological point of view, the plutonic rocks of Greece could be safely used as decorative building materials. PMID:23827232

  11. Magmatic epidote, hornblende barometric estimates, and emplacement of the Conceicao das Creoulas pluton, Alto Pajeu Terrane, NE Brazil

    International Nuclear Information System (INIS)

    The Brasiliano-age magmatic epidote-bearing Conceicao das Creoulas batholith, in the Transversal Zone superterrane in northeastern Brazil, intruded migmatites and metagranitoids of the Riacho do Forno/Recanto Formations. This pluton is composed of porphyritic granodiorite and porphyritic monzogranite. Hornblendes in this pluton solidified between 6-7 Kbar in mafic enclaves and around 8 Kbar for porphyritic granodiorite as estimated by its Al contents. Temperatures for zircon saturation are in the 790-830 deg C range for the mafic enclaves and 800-850 deg C for the porphyritic granodiorite, whereas hornblende-plagioclase pairs yielded temperatures in the 670-690 de C range. In this pluton, epidote, undoubtedly of magmatic origin, with or without allanite cores, included in plagioclase, is rimmed by biotite or is partially resorpted by the magma. Sometimes, patches of hornblende and biotite are present inside epidote. Magmatic epidote compositions vary in the interval 20-25% mole of pistacite, and always exhibit Ti O2 < 0.20% by weight. This compositional range suggested crystallization along the NNO buffer. High initial ratio suggest a significant crustal component in the magma genesis. The magma probably was transported upward by diking and inflated outwards near or at its final site of emplacement, giving to the pluton a diapiric appearance. (author)

  12. Transpressional granite-emplacement model: Structural and magnetic study of the Pan-African Bandja granitic pluton (West Cameroon)

    Science.gov (United States)

    Sandjo, A. F. Yakeu; Njanko, T.; Njonfang, E.; Errami, E.; Rochette, P.; Fozing, E.

    2016-02-01

    The Pan-African NE-SW elongated Bandja granitic pluton, located at the western part of the Pan-African belt in Cameroon, is a K-feldspar megacryst granite. It is emplaced in banded gneiss and its NW border underwent mylonitization. The magmatic foliation shows NE-SW and NNE-SSW strike directions with moderate to strong dip respectively in its northern and central parts. This mostly, ferromagnetic granite displays magnetic fabrics carried by magnetite and characterized by (i) magnetic foliation with best poles at 295/34, 283/33 and 35/59 respectively in its northern, central and southern parts and (ii) a subhorizontal magnetic lineation with best line at 37/8, 191/9 and 267/22 respectively in the northern, central and southern parts. Magnetic lineation shows an `S' shape trend that allows to (1) consider the complete emplacement and deformation of the pluton during the Pan-African D 2 and D 3 events which occurred in the Pan-African belt in Cameroon and (2) reorganize Pan-African ages from Nguiessi Tchakam et al. (1997) compared with those of the other granitic plutons in the belt as: 686 ±17 Ma (Rb/Sr) for D 1 age of metamorphism recorded in gneiss; and the period between 604-557 Ma for D 2-D 3 emplacement and deformation age of the granitic pluton in a dextral ENE-WSW shear movement.

  13. Cuerpos intrusivos asociados a las mineralizaciones polimetálicas del depósito Cerro León, área del anticlinal El Tranquilo, Santa Cruz: evidencias geofísicas Intrusive bodies associated with the polymetallic mineralization of the Cerro León deposit, area of Cerro Tranquilo anticline, Santa Cruz: Geophysical evidence

    OpenAIRE

    G. A Peñalva; S. M. Jovic; C. J. Chernicoff; D.M. Guido; I. Schalamuk

    2008-01-01

    Las características geológicas tales como presencia de cuerpos intrusivos y subvolcánicos someros básicos a intermedios y de las mineralizaciones con alto contenido de sulfuros del área del anticlinal El Tranquilo, son particulares y poco representadas en el macizo del Deseado. El depósito polimetálico vetiforme Cerro León presenta una signatura geoquímica-mineralógica que lo diferencia del clásico modelo epitermal de baja sulfuración característico del macizo del Deseado. Los datos aeromagné...

  14. Analisis neotectónico del área Cerro Salinas, departamento Sarmiento, provincia de San Juan Neotectonic analysis of the Cerro Salinas area, Sarmiento department, province of San Juan

    Directory of Open Access Journals (Sweden)

    Héctor Cisneros

    2010-12-01

    Full Text Available El cerro Salinas es una de las exposiciones más australes del basamento cristalino de las Sierras Pampeanas. Alrededor del mismo han sido reconocidos varios trazos de fallas caracterizados por escarpas rectilíneas de dirección submeridiana, que afectan a depósitos sedimentarios referidos al Terciario y Cuaternario. La actitud espacial de las fallas neotectónicas está controlada por la posición de la estratificación y de los contactos litológicos principales de las unidades terciarias, lo cual se ha interpretado preliminarmente como evidencia del flexodeslizamiento asociado al acortamiento andino. Esta situación guarda mucha similitud con el estilo de deformación de las principales zonas de fallamiento cuaternario de la Precordillera Oriental. Acorde con la distribución espacial de las deformaciones neotectónicas y de la geometría de las mismas, se dividió al área analizada en tres sectores. La principal estructura neotectónica, la falla Cerro Salinas, constituye el límite oeste tanto del cerro Salinas como de los afloramientos precuaternarios circundantes con una longitud reconocida de 15,77 km. Las observaciones realizadas en el área de estudio, principalmente al norte del mismo permiten indicar que la deformación en el frente de falla está vinculada a escarpas asociadas con fallas inversas propagantes. La discriminación cronológica de las unidades morfoestratigráficas cuaternarias se realizó en base a datos de multiparámetros y a la signatura de las superficies aluviales en imágenes Landsat ETM+ y ASTER, mediante procesamiento en base al método de componentes principales. En base a la sumatoria del desplazamiento vertical desarrollado por las escarpas de falla para el Pleistoceno tardío, se ha estimado una tasa de levantamiento mínima de 0,13 mm/año.The so called Cerro Salinas is one of the southernmost expressions of the Sierras Pampeanas crystalline basement. Several fault traces with N-S-trending rectilinear

  15. El lago Chinchaycocha en el mercado de bonos de carbono

    Directory of Open Access Journals (Sweden)

    Wilfredo Bulege Gutiérrez

    2012-12-01

    inviertencapitales en los países subdesarrollados para reducir en su favor las emisiones de GEI. Esta iniciativa ha generado un mercado de compra y venta de certificados de emisiones reducidas (CER. Nuestro país tiene enormes posibilidades para captar estos recursos. Se trata, entonces, de una oportunidad para ingresar a este mercado y generar importantes recursos que pueden ser invertidos en mayor investigación, desarrollo e innovación (I+D+i en los mismos procesos de adaptación y mitigación del cambio climático.

  16. Especialización en baja calidad: España y el mercado internacional del vino, 1950-1990.

    OpenAIRE

    Fernández, Eva

    2012-01-01

    Este artículo estudia los mercados interior e internacional del vino español en el periodo 1950- 1990, mercados que ofrecieron incentivos escasos para la modernización del sector y la inversión en calidad. Hasta los años ochenta, la demanda interna se concentró en vinos ordinarios, que se vendían a granel. En el mercado internacional por su parte, los exportadores españoles también se especializaron en vinos inferiores. El mercado internacional de vinos baratos españoles creció hasta los años...

  17. La estrategia de marketing internacional en mercados emergentes: importancia del análisis de los factores de entorno

    OpenAIRE

    Okazaki, Shintaro; Romero de la Fuente, Jaime; Yagüe Guilén, María Jesús

    2006-01-01

    En este trabajo se aborda la importancia que el análisis de los factores que componen el entorno empresarial tiene para el diseño adecuado del proceso de internacionalización de la empresa en mercados emergentes. La disponibilidad de información relevante sobre las condiciones económicas, demográficas y culturales de los mercados y su incorporación al proceso de decisión constituye un elemento clave para alcanzar el éxito comercial de dichos mercados. Se presenta una aplicación al mercado chi...

  18. Mercados educacionais e a comunidade Education markets and the community

    Directory of Open Access Journals (Sweden)

    Sally Power

    2003-09-01

    Full Text Available Os defensores de abordagens baseadas no mercado para a educação invocam, às vezes, a necessidade de "empoderamento" (empowerment das comunidades nas tomadas de decisão educacionais para justificar a reforma dos sistemas educacionais públicos convencionais. Com base em exemplos da Austrália, da Inglaterra e do País de Gales, da Nova Zelândia e dos eua, este artigo explora as maneiras complexas e contraditórias como as políticas educacionais contemporâneas usam o conceito de envolvimento das comunidades. Ele demonstra mais ainda que o papel e o impacto do envolvimento das comunidades nas escolas nada têm de simples. O artigo conclui que, se o envolvimento das comunidades quer ter efeitos progressistas, ele deve ser articulado com uma política de educação democrática mais ampla.The proponents of market-based approaches to education have sometimes invoked the need for community empowerment in educational decision-making to justify the reform of conventional state educational systems. Drawing upon examples from Australia, England and Wales, New Zealand and the usa, this paper explores the complex and contradictory ways in which the concept of community involvement is used in contemporary education policy. It further demonstrates that the role and impact of community involvement in schools are by no means straightforward. The paper concludes that, if community involvement is to be progressive in its effects, it will need to be articulated with a broader democratic politics of education.

  19. LA MUJER EN EL MERCADO LABORAL ESPAÑOL

    Directory of Open Access Journals (Sweden)

    Elvira López Díaz

    2013-05-01

    Full Text Available Este estudio tiene por objeto mostrar a grandes rasgos la participación femenina en el mercado laboral español y cuáles son los retos u oportunidades que tienen las mujeres ante sí, resaltando los elementos de cambio y de continuidad observados en los últimos años en nuestra sociedad. Para poder comprender la situación actual en la que se encuentra el colectivo femenino se realiza un análisis partiendo de la normativa aplicable, donde el principal referente es nuestra Constitución Española, que sanciona cualquier tipo de discriminación por razón del sexo, y se describen las reformas estructurales que se han ido produciendo en materia de empleo e igualdad de oportunidades, sin olvidar el papel que, en general, las Administraciones Públicas deben desarrollar en la consecución de una igualdad real y efectiva entre mujeres y hombres, en el marco de un Estado Social y Democrático de Derecho como es el nuestro. The aim of this paper is to show in general terms the female participation in the Spanish labor market and what challenges and opportunities women face, highlighting the elements of change and continuity observed in recent years in our society. To understand the present situation of the female collective, an analysis has been done based on the applicable regulations, where the main reference is our Spanish Constitution which penalizes any discrimination by sex. The analysis describes the structural reforms that have occurred regarding to employment and equal opportunities, not to mention the role that should be developed by the Public Administration in order to ensure equal opportunities between women and men, within the framework of a democratic society governed by the rule of law.

  20. y el Mercado Común del Sur (MERCOSUR

    Directory of Open Access Journals (Sweden)

    Ángel Moros

    2006-01-01

    Full Text Available Se analizan algunos indicadores propuestos por la Cumbre Mundial sobre la Sociedad de la Información con el fin de comparar el desarrollo de las políticas nacionales de información, los niveles de tecnologización y la funcionalidad en los países que conforman los bloques de la Comunidad Andina de Naciones y El Mercado Común del Sur. El primer bloque está constituido por Bolivia, Colombia, Ecuador, Perú y Venezuela y el segundo está conformado por Argentina, Brasil, Paraguay, Uruguay y Venezuela, para los efectos de este artículo también se incluye a Chile. Este estudio se desarrolla bajo las características del paradigma tecnológico preparado por la División Desarrollo Productivo y Empresarial de la CEPAL que reconocen ocho fundamentos, de los cuales, para este trabajo se aplicaron dos, el primero enfoca la exogeneidad de las trayectorias tecnológicas, que por sus características se puede aplicar a gran parte de los países de la región, teniendo en cuenta que sus trayectorias son determinadas fuera de los sistemas de innovación La endogeneidad institucional, política y normativa, se inserta en la complejidad y en la incertidumbre de los sistemas de información, parte de modelos enfrentados a trayectorias tecnológicas exógenas, en los cuales los países tienen sus respectivos grados de libertad y varían según su nivel de desarrollo

  1. Importaciones áticas del siglo V a.C. del Cerro del Prado (Algeciras, Cádiz

    Directory of Open Access Journals (Sweden)

    Cabrera, Paloma

    1996-12-01

    Full Text Available In this paper we analyze a group of Attic imports, found in the excavations of Cerro del Prado, a settlement situated in the Bahía de Algeciras (Cádiz. The great interest of this group lies in the fact that it belongs to a particular chronological period, the last third of the 5th century B.C., as we have not found later imports, and in the almost exclusive presence of black glazed vases, which gives US an idea of a very definitive demand of the punic society of the Iberian Peninsula regarding the trade of greek goods.

    Presentamos en este trabajo un conjunto de importaciones áticas halladas en las excavaciones del Cerro del Prado, situado en la bahía de Algeciras (Cádiz. El interés de este conjunto reside en su pertenencia a un momento cronológico muy concreto: el último tercio del siglo V a.C., no habiéndose hallado importaciones más modernas y en la presencia absoluta de vasos de barniz negro, lo que nos habla de una demanda muy determinada de la sociedad púnica peninsular frente al comercio de productos griegos.

  2. Exploring the plutonic crust at a fast-spreading ridge:new drilling at Hess Deep

    Energy Technology Data Exchange (ETDEWEB)

    Gillis, Kathryn M. [Univ. of Victoria, BC (Canada). School of Earth and Ocean Sciences; Snow, Jonathan E. [Univ. of Houston, Houston, TX (United States). Earth & Atmospheric Sciences; Klaus, Adam [Texas A & M Univ., College Station, TX (United States). Integrated Ocean Drilling Program (IODP). United States Implementing Organization.; Guerin, Gilles [Lamont-Doherty Earth Observatory of Columbia Univ., Palisades, NY (United States). Borehole Research Group; Abe, Natsue [Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka (Japan). Inst. for Research on Earth Evolution (IFREE); Akizawa, Norikatsu [Kanazawa Univ. (Japan). Dept. of Earth Sciences; Ceuleneer, Georges [Univ. Paul Sabatier, Toulouse (France). Observatoire Midi-Pyrenees (UMS 831), CNRS; Cheadle, Michael J. [Univ. of Wyoming, Laramie, WY (United States). Dept. of Geology and Geophysics; Adriao, Alden de Brito [Federal Univ. of Rio Grande do Sul, Porto Alegre (Brazil). Geology Inst. (IGEO); Faak, Kathrin [Ruhr Univ., Bochum (Germany). Geological Inst.; Falloon, Trevor J. [Univ. of Tasmania, Hobart, TAS (Australia). Inst. for Marine and Antarctic Studies; Friedman, Sarah A. [Southern Illinois Univ., Carbondale, IL (United States). Dept. of Geology; Godard, Marguerite M. [Univ. Montpellier II (France). Geosciences Montpellier-UMR 5243; Harigane, Yumiko [National Inst. of Advanced Industrial Science and Technology (AIST), Tsukuba (Japan). Marine Geology Dept.; Horst, Andrew J. [Syracuse Univ., NY (United States). Dept. of Earth Science; Hoshide, Takashi [Tohoku Univ., Sendai (Japan). Graduate School of Science; Ildefonse, Benoit [Univ. Montpellier II (France). Lab. de Tectonophysique; Jean, Marlon M. [Northern Illinois Univ., DeKalb, IL (United States). Dept. of Geology and Environmental Geosciences; John, Barbara E. [Univ. of Wyoming, Laramie, WY (United States). Dept. of Geology and Geophysics; Koepke, Juergen H. [Univ. of Hannover (Germany). Inst. of Mineralogy; Machi, Sumiaki [Kanazawa Univ. (Japan). Dept. of Earth Sciences; Maeda, Jinichiro [Hokkaido Univ., Sapporo (Japan). Dept. of Natural History Sciences; Marks, Naomi E. [Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States). Chemistry and Material Sciences Dept.; McCaig, Andrew M. [Univ. of Leeds (United Kingdom). School of Earth and Environment; Meyer, Romain [Univ. of Bergen (Norway). Dept. of Earth Science and Centre for Geobiology; Morris, Antony [Univ. of Plymouth (United Kingdom). School of Earth, Ocean & Environmental Sciences; Nozaka, Toshio [Okayama Univ. (Japan). Dept. of Earth Sciences; Python, Marie [Hokkaido Univ., Sapporo (Japan). Dept. of Earth and Planetary Sciences; Saha, Abhishek [Indian Inst. of Science (IISC), Bangalore (India). Centre for Earth Sciences; Wintsch, Robert P. [Indiana Univ., Bloomington, IN (United States). Dept. of Geological Sciences

    2013-02-28

    Integrated Ocean Drilling Program (IODP) Hess Deep Expedition 345 was designed to sample lower crustal primitive gabbroic rocks that formed at the fast-spreading East Pacific Rise (EPR) in order to test models of magmatic accretion and the intensity of hydrothermal cooling at depth. The Hess Deep Rift was selected to exploit tectonic exposures of young EPR plutonic crust, building upon results from ODP Leg 147 as well as more recent submersible, remotely operated vehicle, and near-bottom surveys. The primary goal was to acquire the observations required to test end-member crustal accretion models that were in large part based on relationships from ophiolites, in combination with mid-ocean ridge geophysical studies. This goal was achieved with the recovery of primitive layered olivine gabbros and troctolites with many unexpected mineralogical and textural relationships, such as the abundance of orthopyroxene and the preservation of delicate skeletal olivine textures.

  3. MCROC - a model to estimate time-dependent microcracking in plutonic rock due to heat

    International Nuclear Information System (INIS)

    Atomic Energy of Canada Limited is studying the disposal of nuclear-fuel waste in a vault in plutonic rock. An important part of this study is to develop models to assess the rate of escape of waste components to the biosphere. Time-dependent changes in the system are important. One such change is the increase in temperature of the rock mass surrounding the vault. Differential thermal expansion between rock constituents (crystals) and the expansion of trapped water will produce microcracking and, hence, possibly changes in intact-rock elastic modulus and permeability. This report describes a model (MCROC) devised to estimate the extent of microcracking and consequent changes in rock elastic modulus and permeability. The model is discussed in detail and is illustrated by various calculations pertinent to a vault designed to accept Canadian nuclear fuel waste. 18 refs

  4. Storm Water Quality in Los Alamos Canyon following the Cerro Grande Fire

    Energy Technology Data Exchange (ETDEWEB)

    M. Johansen; B. Enz; B. Gallaher; K. Mullen; D. Kraig

    2001-04-01

    In May 2000, the Cerro Grande Fire burned about 7400 acres of forest on the Los Alamos National Laboratory (LANL) and about 10,000 acres in watersheds above LANL on Santa Fe National Forest lands. The resulting burned landscapes raised concerns of increased storm water runoff and transport of contaminants by runoff in the canyons traversing LANL. On June 2 and 3, 2000, rain fell in the Los Alamos Canyon watershed generating storm water runoff in the canyon bottom. This event was important in that it was the first significant runoff on LANL following the fire and occurred in a canyon containing known legacy waste sites. Samples from this runoff were analyzed for radionuclide, metal, inorganic, and organic constituents. Results show radionuclide concentrations at or below previous (pre-fire) maximum levels at locations on LANL and downstream. However, greater concentrations of some fallout-associated radionuclides (cesium-137 and strontium-90) were seen arriving on LANL from upstream areas compared to pre-fire conditions. Tests indicate most of the radionuclides in the samples were bound to sediments, not dissolved in water. Most radionuclide concentrations in sediments were below LANL Screening Action Levels, with cesium-137 and strontium-90 as exceptions. Most radionuclide concentrations in samples taken at LANL's downstream boundary were greater than those taken upstream, indicating the presence of contributing sources on LANL. For comparison purposes, doses were calculated on a mrem per liter of unfiltered water basis for 11 radionuclides commonly associated with atmospheric fallout and with LANL operations. The maximum dose was 0.094 mrem per liter unfiltered water and was largely associated with plutonium-239/240. In contrast, all filtered samples had total doses less than 0.001 mrem per liter. Compared to past data, potential doses were not increased by the fire during this initial runoff event. Of the 25 metals tested for, seven were above pre

  5. Analysis and simulatin of rock avalanche sequence in the Cerro Caquilluco landslide (Tacna, Peru)

    Science.gov (United States)

    Crosta, Giovanni B.; Frattini, Paolo; Valbuzzi, Elena; Hermanns, Reginald L.

    2014-05-01

    The Cerro Caquilluco (Tacna, Peru) rock avalanche complex has a total volume of about 15 km3 and a length of 43 km, extending from 3900 m a.s.l to 530 m a.s.l.. Based on geomorphological interpretation and lithological evidences, we reconstructed a possible rock-avalanches sequence consisting of at least nine major events. For each event, we calculated the mobilized volumes through the comparison of pre- and post-failure morphology. We argue that the first rock avalanche event corresponds to the Cerrillos Negros rock avalanche, characterized by a distal tongue shaped lobe, 11 km long, 3 km wide and 25 to 60 m thick (rough volume estimate 1.15 km3), deposited along the piedmont surface (average slope: 2° ). The reconstruction of pristine pre-failure morphology was accomplished by mimicking the preserved morphology close to the source area, and by removing the deposited volumes from the rock avalanche path. For this, we made the hypothesis that the old paleosurface was already eroded by valleys progressively moving upstream during a wetter climate, as suggested by Hoke et al (2007) for similar conditions in northern Chile. The reconstruction of the pre-event morphology required several attempts to fit the eroded and the deposited volumes. Finally, a total mobilized volume of about 10.2 km2 was obtained for this event. For the successive scenarios of slide retrogression, we used the morphologies obtained by previous scenarios as pre-failure morphologies, and we calculated, by difference with current topography, the lobe volumes. The volumes of single rock avalanche episodes decrease from the first to the last event, roughly following a power-law decay. This behavior is comparable to that described by Utili and Crosta (2011) for retrogressive instabilities in rocky cliffs. The rock-avalanche events have been simulated, to verify the different scenarios in terms of spreading area and maximum runout, by using SPH (Smooth Particle Hydrodynamics) and Finite Element codes

  6. El megadeslizamiento del cerro Uritorco, ladera occidental de la Sierra chica de Córdoba

    Directory of Open Access Journals (Sweden)

    Claudio A Carignano

    2014-03-01

    Full Text Available En el extremo norte de la Sierra Chica de Córdoba, sobre el flanco oeste del cerro Uritorco (1.949 m s.n.m., se ha identificado un megadeslizamiento (30°49'55,46"S y 64°29'50,31"O. Los materiales movilizados del frente del escarpe de la falla Sierra Chica, han cubierto parcialmente el granito de Capilla del Monte y los abanicos aluviales pleistocenos del piedemonte. El lóbulo y bloques rotados del deslizamiento conforman un alto topográfico que oficia de límite entre los valles de Punilla (al sur y de Charbonier (al noroeste. Mediante técnicas de procesamiento e interpretación de imágenes satelitales multiespectrales de media (Landsat-ETM y muy alta resolución (GeoEye-1, análisis digital del terreno a partir de modelos de elevación (SRTM y Aster-GDEM y el correspondiente control de campo, se ha delimitado y caracterizado esta megageoforma nunca antes advertida. Dada la elevada sismicidad actual e histórica de la zona y los indicios morfotectónicos que señalan como activas a las fallas Sierra Chica y Pajarillo-Copacabana-Masa, se estima que este deslizamiento posiblemente fue gatillado por un evento sísmico, acontecido en alguna de esas estructuras. Tanto el depósito del deslizamiento como su cicatriz de despegue presentan un significativo grado de erosión hídrica. Por análisis comparativos con otros deslizamientos ya datados y de características similares, situados en el escarpe occidental de las Sierras de San Luis, se le asigna una edad pleistocena medio-tardía. Por su volumen y características (2,1 x109 m³ se estableció que se trata de un megadeslizamiento único en las Sierras de Córdoba y constituye uno de los deslizamientos de mayor tamaño entre los registrados hasta el presente en Argentina.

  7. U-Pb geochronology of Gangdese (Transhimalaya) plutonism in the Lhasa-Xigaze region, Tibet

    International Nuclear Information System (INIS)

    A series of different plutons from the Lhasa-Xigaze segment of the Gangdese (Transhimalaya) belt has been studied by high-resolution U-Pb analyses of zircon (using zircon fractions of 5-100 grains each, selected upon specific grain characteristics). For two diorites, located east of Xigaze (Dazhuka), the zircons yield concordant ages of 93.4 +- 1.0 and 94.2 +- 1.0 m.y., respectively. Also concordant ages of 41.1 +- 0.4 and 41.7 +- 0.4 m.y. have been obtained for two granodiorites, collected southwest of Lhasa (Qushui). The precision on the ages of two granites from the Xigaze and Lhasa area, is limited by two factors: the presence of inherited radiogenic lead and the occurrence of subsequent lead loss. However, some concordant zircons, detected in both granites, define approximate ages of about 67 and 53 m.y., respectively. The inherited lead components show the melting of Precambrian material was involved in magma genesis. The U-Pb ages substantiate a magmatic activity lasting from mid-Cretaceous (Cenomanian) to Eocene (Lutetian) time. Such a period of plutonism at the southern margin of Eurasia, as well as the occurrence of magma generation from continental crust, suggest that the Gangdese range results from the subduction of Tethys oceanic lithosphere (Indian plate) underneath Eurasia (Eurasian plate). If this model is true, the collision of India with Eurasia (Along the Lhasa-Xigaze sector) postdates the emplacement of the 41 m.y. old Gangdese granodiorites, i.e. the collision occurred after Lutetian time. (orig.)

  8. The geology and geochronology of the Belmont pluton and microgranite dykes from the Margate area

    International Nuclear Information System (INIS)

    Field, petrographic, geochemical and Rb-Sr isotope data are presented for two granitic units which are considered to represent amongst the youngest intrusive rocks in the Natal Metamorphic Province. These are the Belmont granite pluton and a suite of unfoliated biotite microgranite dykes from the Margate area. The data suggest that these rocks do not form part of a consanguineous suite as previously envisaged. It is concluded that the Belmont pluton (1055 ± 60Ma) should be assigned to the garnet leucogranite phase of the syntectonic Margate Suite, and that the dykes (∼965 Ma) represent the products of a discrete, late-stage magmatic event which took place towards the end of the Natal orogenesis. Furthermore, the high initial Sr isotopic ratio (∼0,715) of the dykes suggests that they were derived from the melting of pre-existing radiogenic crust. The termination of major tectono-magmatic events in the Late Proterozoic Namaqua-Natal Belt apparently youngs from west to east across South Africa. Reconstructions of Gondwanaland place the Falkland Plateau and the Maudheim Province of Antarctica off the southeast of Africa. Dates obtained from this region range from ∼1000Ma to ∼500Ma, suggesting a continued decrease in age of tectono-magmatic activity eastwards. The microgranite dykes described here are unequivocally amongst the youngest post-tectono-metamorphic intrusions of southern Natal, yet they do not preserve any whole-rock indication of Pan-African isotopic disturbances. Sparse Rb-Sr mineral isotopic data support this indication that there was no significant Pan-African activity in the Natal Metamorphic Province. 8 figs., 7 tabs., 38 refs

  9. Land subsidence in the Cerro Prieto Geothermal Field, 1 Baja California, Mexico, from 1994 to 2005. An integrated analysis of DInSAR, levelingand geological data.

    Energy Technology Data Exchange (ETDEWEB)

    Sarychikhina, O; Glowacka, E; Mellors, R; Vidal, F S

    2011-03-03

    Cerro Prieto is the oldest and largest Mexican geothermal field in operation and has been producing electricity since 1973. The large amount of geothermal fluids extracted to supply steam to the power plants has resulted in considerable deformation in and around the field. The deformation includes land subsidence and related ground fissuring and faulting. These phenomena have produced severe damages to infrastructure such as roads, irrigation canals and other facilities. In this paper, the technique of Differential Synthetic Aperture Radar Interferometry (DInSAR) is applied using C-band ENVISAR ASAR data acquired between 2003 and 2006 to determine the extent and amount of land subsidence in the Mexicali Valley near Cerro Prieto Geothermal Field. The DInSAR results were compared with published data from precise leveling surveys (1994- 1997 and 1997-2006) and detailed geological information in order to improve the understanding of temporal and spatial distributions of anthropogenic subsidence in the Mexicali Valley. The leveling and DInSAR data were modeled to characterize the observed deformation in terms of fluid extraction. The results confirm that the tectonic faults control the spatial extent of the observed subsidence. These faults likely act as groundwater flow barriers for aquifers and reservoirs. The shape of the subsiding area coincides with the Cerro Prieto pull-apart basin. In addition, the spatial pattern of the subsidence as well as changes in rate are highly correlated with the development of the Cerro Prieto Geothermal Field.

  10. An integrated model for the natural flow regime in the Cerro Prieto hydrothermal system based upon petrological and isotope geochemical criteria

    Energy Technology Data Exchange (ETDEWEB)

    Elders, W.A.; Williams, A.E.; Hoagland, J..

    1981-01-01

    Studies of cuttings and cores at Cerro Prieto have now been extended to more than 50 boreholes. The aims of this petrological and isotopic work are to determine the shape of the reservoir, its physical properties, and its temperature distribution and flow regime before the steam field was produced.

  11. 40Ar/39Ar geochronology and palynology of the Cerro Negro formation, South Shetland Islands, Antarctica: a new radiometric tie for cretaceous terrestrial biostratigraphy in the southern hemisphere

    International Nuclear Information System (INIS)

    The upper part of the Jurassic-Cretaceous Byers Group, exposed on Byers Peninsula in the South Shetland Islands, Antarctica, consists of 1.4 km of non-marine strata assigned to the Cerro Negro Formation. Silicic pyroclastic units close to the base of the formation have yielded new 40Ar/39Ar ages of 120.3 ± 2.2 Ma on plagioclase from one horizon, and 119.4 ± 0.6 and 119.1± 0.8 Ma on biotite and plagioclase from a second horizon. Plagioclase from a welded ignimbrite close to the topmost exposed part of the formation has given an 40Ar/39Ar age of 119 ± 3.0 Ma. These ages indicate that the Cerro Negro Formation was deposited during a relatively short period in early Aptian times. The identification of palynomorph taxa has enabled us to propose correlations for the Cerro Negro Formation with spore/pollen zonations of South America and Australia. The presence of Interulobites pseudoreticulatus, Appendicisporites and F. wonthaggiensis in the Cerro Negro Formation supports correlation with the Interulobites-Foraminisporis and the lower part of the tectifera-corrugatus zones in southern South America. The presence of Foraminisporis asymmetricus and other palynomorphs suggests correlation with the Cyclosporites hughesii Interval Zone of early to late Aptian age in Australia. These data represent a valuable addition to the few radiometric ties available for Mesozoic terrestrial palyno-stratigraphy in the Southern Hemisphere. Copyright (1999) Blackwell Science Pty Ltd

  12. El frente de corrimiento andino al nivel de los cerros Penitentes y Visera (alta Cordillera de Mendoza: aspectos cronológicos y cartográficos

    Directory of Open Access Journals (Sweden)

    Jean-Claude Vicente

    2009-10-01

    Full Text Available El hallazgo de una iportante fauna de invertebrados marinos del Tithoniano superior a espaldas del cerro Penitentes en la secuencia carbonática basal de la primera escama del frente de corrimiento andino, confirma la lógica tectónica de un despegue de esta unidad a nivel del Yeso Principal y lleva a invalidar ciertas correlaciones litoestratigráficas y bosquejos paleogeográficos asignados a la Formación La Manga. Por otro lado, el análisis de algunos perfiles claves en torno al cerro Penitentes entre la quebrada Vargas y el cerro Visera permite presentar una reinterpretación tectónica del sector. Esta se sustenta en el reconocimiento y la diferenciación de las unidades terciarias básicas representadas por los Conglomerados Penitentes (Mioceno inferior y los Aglomerados Santa María (Mioceno superior en una relación muy similar a la descrita anteriormente al norte de Puente del Inca. El estudio permite seguir las interferencias, en un contexto polifásico, entre las reactivaciones del corrimiento Penitentes de piel fina y un cabalgamiento frontal de piel gruesa que repite la secuencia terciaria. La discordancia entre las secuencias terciarias y el emplazamiento de una klippe de Malm sobre los Conglomerados Penitentes del sinclinal del cerro Visera, conduce a otorgar cierta importancia a la fase del final del Mioceno inferior.

  13. As políticas ativas de mercado de trabalho no Mercosul

    Directory of Open Access Journals (Sweden)

    Maria Cristina Cacciamali

    2005-12-01

    Full Text Available AS POLÍTICAS ativas de mercado de trabalho constituem instrumentos da política pública que têm como objetivo diminuir os mecanismos concentradores do mercado de trabalho e/ou a sua eficiência alocativa. Todas as modalidades de políticas ativas de mercado de trabalho são realizadas pelos governos da região do Mercosul, permitindo a troca de experiência, o aprimoramento operacional dos programas e o estabelecimento de uma agenda comum.ACTIVE labour market programs aim to correct market imperfections and to improve its allocative efficiency. All the types of active labour market policies are implemented by the governments of the Mercosur, allowing the change of experiences, the operational improvement of the programmes and the definition of a common agenda.

  14. Repensar la profundización financiera: estabilidad y crecimiento en los mercados emergentes

    Directory of Open Access Journals (Sweden)

    Ratna Sahay

    2015-12-01

    Full Text Available En este escrito se usa una nueva medida del desarrollo financiero para mostrar que la mayoría de los mercados emergentes aún puede obtener beneficios de crecimiento y estabilidad con un mayor desarrollo financiero. Primero define el desarrollo financiero como una combinación de profundidad, acceso y eficiencia. Luego muestra que el crecimiento económico se debilita a mayores niveles de desarrollo financiero y que el ritmo del desarrollo financiero es importante; además propone una nueva manera de ver los “tradeoffs” de la regulación financiera. Concluye que no hay una secuencia única en el desarrollo de las instituciones y los mercados financieros, aunque se observa cuando las economías se desarrollan los beneficios relativos de las instituciones disminuyen y los de los mercados aumentan.

  15. Indústria solar térmica em Cabo Verde : potencialidade do mercado

    OpenAIRE

    Nascimento, Cláusia Maria Fonseca da Rocha

    2008-01-01

    O presente trabalho pretende fazer uma análise do potencial do mercado Cabo-verdiano para a utilização da energia solar, através de algumas ferramentas de análise de mercado já conhecidas, nomeadamente as cinco forças de Porter, o Diamante de Porter, a análise PESTEL e a análise SWOT. O primeiro ponto que se pretende esclarecer é a questão: Será que Cabo Verde reúne as condições para ser considerado uma potencial mercado para a produção/ venda de sistemas solares para o a...

  16. Inserção dos jovens no mercado de trabalho

    OpenAIRE

    ANSELMO LUIS DOS SANTOS; DENIS MARACCI GIMENEZ

    2015-01-01

    resumo O objetivo deste trabalho é analisar o padrão de inserção do jovem no mercado de trabalho brasileiro entre 2004 e 2015. A análise parte da caracterização do padrão histórico de inserção dos jovens no mercado de trabalho brasileiro e nas décadas de relativa estagnação econômica entre 1981 e 2003. Em seguida, considerando as transformações demográficas, a elevação do ritmo de crescimento econômico, as políticas sociais e voltadas para o mercado de trabalho, o trabalho procura mostrar com...

  17. A re-appraisal of the stratigraphy and volcanology of the Cerro Galán volcanic system, NW Argentina

    Science.gov (United States)

    Folkes, Christopher B.; Wright, Heather M.; Cas, Ray A.F.; de Silva, Shanaka L.; Lesti, Chiara; Viramonte, Jose G.

    2011-01-01

    From detailed fieldwork and biotite 40Ar/39Ar dating correlated with paleomagnetic analyses of lithic clasts, we present a revision of the stratigraphy, areal extent and volume estimates of ignimbrites in the Cerro Galán volcanic complex. We find evidence for nine distinct outflow ignimbrites, including two newly identified ignimbrites in the Toconquis Group (the Pitas and Vega Ignimbrites). Toconquis Group Ignimbrites (~5.60–4.51 Ma biotite ages) have been discovered to the southwest and north of the caldera, increasing their spatial extents from previous estimates. Previously thought to be contemporaneous, we distinguish the Real Grande Ignimbrite (4.68 ± 0.07 Ma biotite age) from the Cueva Negra Ignimbrite (3.77 ± 0.08 Ma biotite age). The form and collapse processes of the Cerro Galán caldera are also reassessed. Based on re-interpretation of the margins of the caldera, we find evidence for a fault-bounded trapdoor collapse hinged along a regional N-S fault on the eastern side of the caldera and accommodated on a N-S fault on the western caldera margin. The collapsed area defines a roughly isosceles trapezoid shape elongated E-W and with maximum dimensions 27 × 16 km. The Cerro Galán Ignimbrite (CGI; 2.08 ± 0.02 Ma sanidine age) outflow sheet extends to 40 km in all directions from the inferred structural margins, with a maximum runout distance of ~80 km to the north of the caldera. New deposit volume estimates confirm an increase in eruptive volume through time, wherein the Toconquis Group Ignimbrites increase in volume from the ~10 km3 Lower Merihuaca Ignimbrite to a maximum of ~390 km3 (Dense Rock Equivalent; DRE) with the Real Grande Ignimbrite. The climactic CGI has a revised volume of ~630 km3 (DRE), approximately two thirds of the commonly quoted value.

  18. Analisis neotectónico del área Cerro Salinas, departamento Sarmiento, provincia de San Juan

    Directory of Open Access Journals (Sweden)

    Héctor Cisneros

    2010-12-01

    Full Text Available El cerro Salinas es una de las exposiciones más australes del basamento cristalino de las Sierras Pampeanas. Alrededor del mismo han sido reconocidos varios trazos de fallas caracterizados por escarpas rectilíneas de dirección submeridiana, que afectan a depósitos sedimentarios referidos al Terciario y Cuaternario. La actitud espacial de las fallas neotectónicas está controlada por la posición de la estratificación y de los contactos litológicos principales de las unidades terciarias, lo cual se ha interpretado preliminarmente como evidencia del flexodeslizamiento asociado al acortamiento andino. Esta situación guarda mucha similitud con el estilo de deformación de las principales zonas de fallamiento cuaternario de la Precordillera Oriental. Acorde con la distribución espacial de las deformaciones neotectónicas y de la geometría de las mismas, se dividió al área analizada en tres sectores. La principal estructura neotectónica, la falla Cerro Salinas, constituye el límite oeste tanto del cerro Salinas como de los afloramientos precuaternarios circundantes con una longitud reconocida de 15,77 km. Las observaciones realizadas en el área de estudio, principalmente al norte del mismo permiten indicar que la deformación en el frente de falla está vinculada a escarpas asociadas con fallas inversas propagantes. La discriminación cronológica de las unidades morfoestratigráficas cuaternarias se realizó en base a datos de multiparámetros y a la signatura de las superficies aluviales en imágenes Landsat ETM+ y ASTER, mediante procesamiento en base al método de componentes principales. En base a la sumatoria del desplazamiento vertical desarrollado por las escarpas de falla para el Pleistoceno tardío, se ha estimado una tasa de levantamiento mínima de 0,13 mm/año.

  19. Chatkalita, nekrasovita y otros minerales del grupo de la estannita de Veta María Eugenia, Cerro Atajo, Catamarca Chatkalita, nekrasovita y otros minerales del grupo de la estannita de veta María Eugenia, Cerro Atajo, Catamarca

    OpenAIRE

    M. F. Márquez-Zavalía; M. A. Galliski

    2007-01-01

    En veta María Eugenia, Cerro Atajo, Catamarca, se encontró una asociación de minerales de estaño integrada por: chatkalita Cu6Fe2+Sn2S8, nekrasovita Cu26V2(Sn,As,Sb)6S32, colusita Cu26V2(As,Sn,Sb)6S32, kësterita Cu2(Zn,Fe)SnS4 y estannoidita Cu8(Fe,Zn)3Sn2S12. Estos minerales, incluidos en watanabeíta, están acompañados principalmente por pirita, esfalerita, calcopirita, tetraedrita, bornita y galena; aikinita, enargita, luzonita, marcasita, arsenopirita y pirrotina participan como minerales ...

  20. Hydraulic model of the steam-lines network of the Cerro Prieto, B.C., geothermal field; Modelo hidraulico de la red de vaporductos del campo geotermico de Cerro Prieto, B.C.

    Energy Technology Data Exchange (ETDEWEB)

    Salaices, E; Garcia, A; Martinez J I; Ovando, R; Cecenas, M; Hernandez A F [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: salaices@iie.org.mx; Canchola, I; Mora, O; Miranda, C; Herandez, M; Lopez, S; Murillo, I [Comision Federal de Electricidad, B.C (Mexico)

    2007-01-15

    The steam-line network of the Cerro Prieto geothermal field is composed of 184 wells, and 162 of the wells are integrated and connected by pipes. Thirteen power units, with an installed electrical capacity of 720 MW, are fed by that network. The network length is 120 km, including pipes of several diameters with branches and interconnections. The extension and complexity of the steam-line system make it difficult to analyze the transport and supply of steam to the power plants. For that it was necessary to have a tool capable of analyzing the system and the performance of the network as a whole, as well as the direction and flow volumes in each part of the system. In this paper, a hydraulic model of the Cerro Prieto steam-line network is presented. The model can determine the performance of the whole network by quantifying the pressure drops, flows and heat losses of the components. The model analyses the consequences of changes in operating conditions, steam production, maintenance activities and design (such as the integration of new wells). The model was developed using PIPEPHASE 9.0, a numeric simulator of multi-phase flow in steady state with heat transfer. It is used to model systems and pipe networks for steam- and condensate-transport. [Spanish] La red de vaporductos del campo geotermico de Cerro Prieto esta compuesta por un conjunto de 184 pozos, de los cuales 162 son pozos integrados, interconectados entre si a traves de una red de tuberias. Por medio de esta red se alimentan 13 unidades generadoras de electricidad con una capacidad total instalada de 720 MWe. La red tiene una longitud aproximada de 120 kilometros y esta compuesta por tuberias de diferentes diametros, ramales, interconexiones, etc. La complejidad y extension del sistema de vaporductos hace muy dificil el analisis del transporte y suministro de vapor a las plantas generadoras. Lo anterior creo la necesidad de contar con una herramienta que ayudara en el analisis del sistema con el fin de

  1. PROGRESO TÉCNICO Y PODER DE MERCADO EN LA INDUSTRIA FARMACÉUTICA

    Directory of Open Access Journals (Sweden)

    JOSÉ GALLEGO

    2009-01-01

    Full Text Available En este artículo se presenta la estimación del poder de mercado en la industria farmacéutica colombiana durante 1982 - 2004. El resultado se compara con las estimaciones realizadas para los Estados Unidos y Finlandia. La conclusión fundamental es la confirmación de la existencia de poder de mercado, al estimarse un índice de Lerner mayor que cero y un markup de Hall mayor que uno; la estimación es equivalente al 0.92 y 0.95 del poder presente en Estados Unidos y Finlandia, respectivamente.

  2. El Mercado Alternativo Bursátil: una novedosa oportunidad para las empresas familiares

    OpenAIRE

    Duréndez Gómez Guillamón, Antonio Luis; García Pérez De Lema, Domingo; Mariño Garrido, Teresa

    2014-01-01

    Con la entrada en funcionamiento del Mercado Alternativo Bursátil en España, las empresas familiares de menor capitalización tienen la posibilidad de cotizar en un mercado bursátil diseñado para pymes. Actualmente, con una profunda crisis de origen financiero, el MAB gana una especial relevancia como estrategia alternativa para conseguir financiación y así superar la fuerte restricción en el acceso al crédito bancario. No obstante, las empresas familiares no se podrán ben...

  3. Estrategias óptimas de generadores eólicos en mercados de electricidad

    OpenAIRE

    Gallego Gallego, Jesús

    2009-01-01

    En este proyecto, se han estudiado distintas estrategias de ofertar al mercado eléctrico para intentar mejorar los resultados obtenidos con las herramientas de predicción. De esta forma, además de los pronósticos de estas herramientas, se han tenido en cuenta datos históricos de predicción y generación, estimaciones de los precios futuros de la energía y del coste de los desvíos. En los algoritmos utilizados también se han tenido en cuenta las reglas del mercado eléctrico, d...

  4. Condiciones de trabajo y salud de vendedores informales estacionarios del mercado de bazurto, en cartagena

    OpenAIRE

    Castillo Avila, Irma Yolanda; Gomez Palencia, Isabel Patricia; Banquez Salas, Annia Patricia; Castro Ortega, Audrey Julieth; Lara Escalante, Hilda Rosa

    2013-01-01

    Objetivo Determinar las condiciones de trabajo y salud de vendedores informales estacionarios del mercado de Bazurto de Cartagena. Metodología Población: 1210 vendedores informales estacionarios del mercado de la ciudad. Muestra: 584 vendedores. Se utilizó una lista de chequeo para des­cribir las condiciones de trabajo. Para determinar las condiciones de salud se utili­zó el cuestionario de alteraciones de salud referida a trabajadores, el cuestionario de síntomas neurotóxicos (Q16) y fue val...

  5. Análise Estatística e Atuarial do Mercado de Seguro DPVAT

    OpenAIRE

    Filipe Coelho de Lima Duarte; Luiz Carlos Santos Júnior

    2015-01-01

    O seguro analisado pelo presente estudo, o DPVAT, foi criado em 1974 para proteger vítimas de Danos Pessoais Causados por Veículos Automotores de Via Terrestre. Objetivou-se nesse trabalho analisar o mercado brasileiro do seguro DPVAT sob a ótica da Modelagem Estatística e Atuarial, com base nos dados mensais de janeiro de 2002 a dezembro de 2014. Para isso, foram utilizados índices de análise de mercado securitário, tais quais coeficientes de penetração e densidade; um modelo de série tempor...

  6. ¿Fabricar o comprar? Enfoques de la integración de mercados financieros

    OpenAIRE

    Michael Gavin; Ricardo Hausmann

    1997-01-01

    (Disponible en idioma inglés únicamente) Las grandes diferencias entre los mercados financieros que hay actualmente en América Latina y cuánto cabe anticipar que cambien en un marco de integración total sugiere que las limitaciones financieras al desarrollo económico de América Latina tienen mucho que ver con lo incompleto de la integración de los mercados financieros de la región al sistema financiero mundial. En este trabajo se sugiere que la causa subyacente de la limitada integración de A...

  7. Los mercados públicos en la ciudad contemporánea : el caso de Barcelona

    OpenAIRE

    Guàrdia Bassols, Manuel; Oyón Bañales, José Luis

    2007-01-01

    La historia de los mercados ha sido escasamente estudiada, aunque exista un notable consenso de que han sido la fuerza modeladora de las ciudades europeas desde el medioevo. En la ciudad contemporánea las formas comerciales han atraído fundamentalmente por su novedad. Han interesado así en los distintos momentos históricos los pasajes, los grandes almacenes, los autoservicios, los supermercados o los centros comerciales. Pasada la primera fase de construcción de los nuevos los mercados metáli...

  8. Los mercados públicos en la ciudad contemporánea

    OpenAIRE

    Guàrdia Bassols, Manuel; Oyón Bañales, José Luis

    2007-01-01

    La historia de los mercados ha sido escasamente estudiada, aunque exista un notable consenso de que han sido la fuerza modeladora de las ciudades europeas desde el medioevo. En la ciudad contemporánea las formas comerciales han atraído fundamentalmente por su novedad. Han interessado así en los distintos momentos históricos los pasajes, los grandes almacenes, los autoservicios, los supermercados o los centros comerciales. Pasada la primera fase de construcción de los nuevos los mercados metál...

  9. Estrategia de cobertura con productos derivados para el mercado energético colombiano

    OpenAIRE

    Jhon Alexis Díaz Contreras; Gloría Inés Macías Villalba; Edgar Luna González

    2014-01-01

    El desarrollo que ha presentado el mercado mayorista de energía en Colombia ha permitido que hoy en día se estén negociando futuros de electricidad en el mercado de capitales local. Este trabajo tiene como objetivo dise ̃ nar un producto derivado en el que subyace el precio de la electricidad. Para esto, se analiza la serie de tiempo del precio de la electricidad para modelar su volatilidad ; y a partir de esta, se dise ̃ na una opción exótica tipo barrera que muestra cómo se pueden usar este...

  10. Mercado interbancario colombiano y manejo de liquidez del Banco de la República

    OpenAIRE

    Pamela cardozo Ortiz; Carlos A. Huertas Campos; Julián A.Parra Polanía; Lina V. Patiño ECheverri

    2011-01-01

    El documento tiene como objetivo describir algunos de los elementos fundamentales del mercado interbancario colombiano y del manejo de liquidez por parte del Banco de la República (BR). El documento explica las diferencias entre las principales operaciones en este mercado y describe los mecanismos a través de los cuales el BR suministra liquidez o recoge excesos de la misma en el sistema financiero (SF); entre otros, describe la subasta diaria de expansión realizada por el BR y la determinaci...

  11. Empresa bajo incertidumbre en el precio: modelo con dos destinos y un mercado de futuros

    Directory of Open Access Journals (Sweden)

    Álvarez López, Alberto A.

    2008-01-01

    Full Text Available En este trabajo se desarrolla un modelo para una empresa competitiva que produce una cantidad determinada de un bien, la cual debe repartir entre dos fines distintos, para los que se tienen diferentes precios. La empresa debe decidir la cantidad que destinará a cada fin antes de conocer el precio para uno de ellos; para este fin, existe además un mercado de futuros, por lo que también debe decidir la cantidad que venderá en ese mercado. Tras presentar el modelo, se interpretan económicamente las diferentes soluciones del problema, y se estudian algunas de sus propiedades.

  12. Endeudamiento y competencia en el mercado: Evidencia de las empresas en México.

    OpenAIRE

    Manuel Sánchez Valadez

    2009-01-01

    Motivado por la importancia que tiene el análisis de las decisiones de las empresas en los diversos mercados donde interactúan, y considerando distintas perspectivas al examinar sus causas o efectos, o ambos, el presente documento plantea que las decisiones financieras de las empresas son influidas por la competencia que éstas enfrentan en los mercados reales. El objetivo principal de este trabajo es aportar evidencia que ayude a cubrir la falta de estudios empíricos acerca de esta interacció...

  13. Comportamiento del Consumidor, Competencia en los Mercados y Estrategia Comercial de las Empresas

    OpenAIRE

    Cebollada Calvo, Jos?? Javier

    1996-01-01

    En un contexto din??mica, en el que los consumidores compran repetidamente los productos, la estructura competitiva est?? influida por la experiencia pasada de los compradores, manifestada en forma de lealtad a las marcas que compiten. En la tesis se lleva a cabo un estudio te??rico y emp??rico de la influencia de la lealtad en la formaci??n de precios y cuotas de mercado. La aplicaci??n emp??rica se desarrolla sobre el mercado de detergentes dom??sticos, con datos desdagragados de compras r...

  14. Estudo de mercado: "A satisfação dos franchisados em Portugal"

    OpenAIRE

    Fialho, Maria Cristina Grilo

    2013-01-01

    Este relatório de estágio foi realizado no âmbito do Mestrado em Matemática e Aplicações, com especialização em Estatística e Investigação Operacional, da Universidade de Aveiro, e o estágio foi realizado no GEMEO (Gabinete de Estudos de Mercado e Opinião do IPAM). Foram desenvolvidas várias atividades relacionadas com os Estudos de Mercado, e uma dessas atividades é sobre o Franchising, onde se pretende avaliar o perfil e satisfação do Franchisado em Portugal. Para isso, fo...

  15. FORMAÇÃO DO MERCADO INFORMAL EM KINSHASA (REPUBLICA DEMOCRÁTICA DO CONGO)

    OpenAIRE

    Mukenge Shay

    2010-01-01

    Trata-se deum ensaio sobre os dois circuitos da economia urbana (especificamente o mercado informal) em Kinshasa, capital da República Democrática do Congo. Este ensaio está baseado em dados e experiências da realidade desta cidade, onde buscou-se iluminar, com nova luz, um importante aspecto dos países do Terceiro Mundo: a construção social do trabalho. O estudo dos dois circuitos da economia urbana, proposto por Milton Santos (1979), valoriza os fenômenos da pobreza e do mercado informal co...

  16. Comercialización de Asturias como destino en el mercado chino

    OpenAIRE

    Mou, Juan

    2012-01-01

    Este trabajo tiene como objeto analizar el mercado turístico chino, el desarrollo turístico entre China y Europa, especialmente entre China y España, para promover el Principado de Asturias como un destino turístico a explotar el mercado chino. Desarrolla el proyecto, además, las experiencias de éxito de los destinos; retos y oportunidades del desarrollo y el modelo de negocio de las agencias de viajes chinas, para analizar la medida asturiana de atraer al turista china

  17. A orientação para o mercado do sector corticeiro português

    OpenAIRE

    Rios, Hugo Daniel Oliveira

    2010-01-01

    Com a globalização das economias, o elevado desenvolvimento da tecnologia, e o acelerar dos fluxos económicos dos últimos tempos obrigam a que as organizações pensem de forma mais exigente acerca da sua forma de estar e de agir. Segundo Slater e Narver (1994:46), sendo a orientação para o mercado uma geração e disseminação da informação de mercado que é composta pela informação sobre as necessidades actuais e futuras dos clientes e os factores exógenos que influenciam essas ...

  18. Progreso técnico y poder de mercado en la industria farmacéutica

    OpenAIRE

    JOSÉ GALLEGO

    2010-01-01

    En este artículo se presenta la estimación del poder de mercado en la industria farmacéutica colombiana durante 1982 - 2004. El resultado se compara con las estimaciones realizadas para los Estados Unidos y Finlandia. La conclusión fundamental es la confirmación de la existencia de poder de mercado, al estimarse un índice de Lerner mayor que cero y un markup de Hall mayor que uno; la estimación es equivalente al 0.92 y 0.95 del poder presente en Estados Unidos y Finlandia, respectivamente....

  19. Financiación para proyectos de inversión: capital riesgo y mercados financieros

    OpenAIRE

    San Millán Fernández, José María

    2014-01-01

    RESUMEN: En la actualidad, tras la grave recesión que ha golpeado al sistema financiero mundial, el otorgamiento de financiacion tanto para emprender un negocio como para expandir el mismo se ha visto reducido considerablemente, en especial para las pequeñas y medianas empresas. En este contexto, las empresas de capital riesgo y los mercados secundarios inglés y español, Alternative Investment Market –en adelante AIM- y Mercado Alternativo Bursátil –en adelante MAB- respectivamente, son alter...

  20. Análisis del comportamiento de mercado de la pitahaya (Hylocereus undatus) en Costa Rica

    OpenAIRE

    Olman Quirós Madrigal

    2010-01-01

    La pitahaya (Hylocereus undatus) es una planta que pertenece a la familia de las cactaceae, que se puede consumir como fruta fresca o procesada como pulpa; sin embargo, en Costa Rica su uso no está muy difundido, por lo que el mercado meta es la población de origen nicaragüense residente en el país, quienes catalogan el producto como de consumo tradicional o masivo.Es por esto que resulta importante retomar el estudio de los componentes del mercado, en donde se destaca no sólo por ser una fru...

  1. ISIS: Un Indicador Sintético Integral de los Servicios de mercado

    OpenAIRE

    Luis Julián Álvarez González; Javier Jareño Morago

    2002-01-01

    A pesar de la enorme importancia del sector servicios de mercado en el conjunto de la economía nacional, la información estadística coyuntural de esta rama se encuentra en clara desventaja con respecto a la industria o a la construcción. En efecto, mientras que el sector secundario dispone de indicadores coyunturales representativos del conjunto de sus ramas, no existen estadísticas globales sobre los servicios de mercado, por lo que el análisis coyuntural debe basarse en un conjunto de indic...

  2. Mercado metropolitano de trabajo y desigualdades sociales en el Gran Santiago: ¿Una ciudad dual?

    OpenAIRE

    de Mattos, Carlos A.

    2002-01-01

    Los cambios estructurales en los mercados metropolitanos de trabajo bajo los procesos de reestructuración-informacionalización-globalización, se han situado como un tema central para el estudio de la transformación de las ciudades durante las últimas décadas. Desde esta perspectiva, el presente trabajo analiza los impactos que los procesos de modernización capitalista en Chile han tenido sobre su mercado de trabajo y sobre la evolución de la distribución del ingreso, y sobre esta base, observ...

  3. Presión en el mercado cambiario para el caso venezolano (1984-2003)

    OpenAIRE

    Pedauga, Luis Enrique; Noguera, Carlos

    2006-01-01

    Esta investigación presenta una propuesta para medir el indicador de presión del mercado cambiario para el caso de Venezuela, haciendo uso de análisis de componentes principales. Por su parte, se presenta un modelo monetario ampliado con la riqueza del sector no financiero y la dinámica entre las tasas de interés domésticas y foráneas, para contrastar empíricamente, a través de método econométrico de retardos distribuidos, los determinantes de la presión del mercado cambiario venezolano dentr...

  4. Contrastação empírica do modelo CAPM aplicada ao mercado bolsista português

    OpenAIRE

    Santos, Tânia Cristina Simões de Matos dos

    2012-01-01

    O objectivo deste trabalho é contrastar o modelo CAPM (Capital Asset Pricing Model) para o mercado bolsista português, aplicando-o à análise do individual das carteiras relativas a cada um dos sectores das empresas cotados na Bolsa, e também ao estudo do mercado português no seu todo.

  5. Eruptive history of the youngest Mexican Shield and Mexico's most voluminous Holocene eruption: Cerro El Metate

    Science.gov (United States)

    Oryaëlle Chevrel, Magdalena; Guilbaud, Marie-Noelle; Siebe, Claus

    2016-04-01

    Small to medium-sized shield volcanoes are an important component of many volcanic fields on Earth. The Trans-Mexican Volcanic Belt, one of the most complex and active continental arcs worldwide, displays a large number of such medium-sized volcanoes. In particular the Michoacán-Guanajuato Volcanic Field (MGVF) situated in central Mexico, is the largest monogenetic volcanic field in the world and includes more than 1000 scoria cones and about four hundred medium-sized volcanoes, also known as Mexican shields. The Mexican shields nevertheless represent nearly 70% of the total volume erupted since 1 Ma and hence played a considerable role in the formation of the MGVF. However, the source, storage, and transport as well as the physical properties (density, viscosity, volatile content, etc.) of the magmas involved in these eruptions remain poorly constrained. Here, we focus on Cerro El Metate, the youngest monogenetic andesite shield volcano of the field. New C14 dates for the eruption yield a young age (~AD 1250), which briefly precedes the initial rise of the Tarascan Empire (AD 1350-1521) in this region. This volcano has a minimum volume of ~9.2 km3 DRE, and its viscous lava flows were emplaced during a single eruption over a period of ~35 years covering an area of 103 km2. By volume, this is certainly the largest eruption during the Holocene in Mexico, and it is the largest andesitic effusive eruption known worldwide for this period. Such a large volume of lava erupted in a relatively short time had a significant impact on the environment (modification of the hydrological network, forest fires, etc.), and hence, nearby human populations probably had to migrate. Its eruptive history was reconstructed through detailed mapping, and geochemical and rheological analyses of its thick hornblende-bearing andesitic flows. Early and late flows have distinct morphologies, chemical and mineralogical compositions, and isotopic signatures which show that these lavas were fed by

  6. Cost model for geothermal wells applied to the Cerro Prieto geothermal field case, BC Abstract; Modelo de costeo de pozos geotermicos aplicado para el caso del campo geotermico de Cerro Prieto, BC

    Energy Technology Data Exchange (ETDEWEB)

    Vaca Serrano, Jaime M.E [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: jaime.vaca@cfe.gob.mx

    2008-01-15

    A project for drilling geothermal wells to produce electrical energy can be defined as a sequence of plans to get steam or geothermal fluids to satisfy a previously known demand, and, under the best possible conditions, to obtain payment. This paper presents a cost model for nine wells drilled at the Cerro Prieto geothermal field in 2005 and 2006 to supply steam to the power plants operating in the field. The cost model is based on the well cost, the initial steam production, the annual decline of steam, the drilling schedule and the break-even point for each well. The model shows the cost of steam by the ton and the sale price needed to determine the discount rate and the investment return time. [Spanish] Un proyecto de perforacion de pozos geotermicos puede definirse como una secuencia o sucesion de planes para obtener vapor o fluidos geotermicos destinados a satisfacer una demanda previamente determinada, que se emplearan principalmente para generar energia electrica, bajo las mejores condiciones para obtener un pago. Este trabajo presenta un modelo de costeo para nueve pozos en el campo geotermico de Cerro Prieto, que fueron perforados entre 2005 y 2006 como parte del suministro de vapor para las plantas generadoras que operan en este campo. El modelo de costeo se basa en el costo por pozo, la produccion inicial de vapor, la declinacion anual de vapor, los intereses de las obras de perforacion y el punto de equilibrio para cada pozo. Los resultados permiten conocer el costo de la tonelada de vapor y el precio de venta para determinar la tasa de descuento y el tiempo de retorno de la inversion.

  7. Noise reduction in steam-vent points at the Cerro Prieto geothermal field, BC; Reduccion del ruido en puntos de desfogue en el campo geotermico de Cerro Prieto, BC

    Energy Technology Data Exchange (ETDEWEB)

    Miranda Herrera, Carlos A [Comision Federal de Electricidad, Residencia General de Cerro Prieto, Mexicali, B.C (Mexico)]. E-mail: carlos.miranda02@cfe.gob.mx

    2008-01-15

    Steam silencers have been placed on the power units regulation system of the Cerro Prieto geothermal field, but not where the steam-pipes vent high-pressure steam (rupture disks). Moreover, the power-unit silencers are large and their abilities to reduce noise depend on an external, uncontrollable factor: pores sizes in the volcanic rocks they are made of. Thus a compact, economic and relatively easy to construct metallic silencer was designed to be used at several points of dry-steam venting to minimize the noise. The design was based on orifice-plate equations and a prototype was constructed and tested. It proved capable of reducing noise by 30 decibels for atmospheric discharges of primary steam at operating pressures. The size of the silencer can be adjusted to the particular needs of each vent case. [Spanish] En el campo geotermico de Cerro Prieto solo existen silenciadores de vapor en el sistema de regulacion de las plantas generadoras, pero no en los sitios de desfogue de vapor a alta presion en los vaporductos (discos de ruptura). Ademas, los silenciadores de las plantas son muy robustos y su capacidad de reduccion del ruido depende de un factor externo no controlable, como es el tamano del poro de la roca volcanica con el que estan construidos. Por lo tanto, se diseno un silenciador metalico compacto, economico y relativamente facil de fabricar, para utilizarse en diversos puntos de descarga de vapor seco a fin de minimizar el ruido. El diseno se realizo con base en las ecuaciones de la placa de orificio. Se construyo un prototipo cuyas pruebas demostraron que es capaz de reducir el ruido hasta en 30 decibeles, al descargar desde la presion de operacion de vapor primario hacia la presion atmosferica. Las dimensiones del silenciador pueden ajustarse a las necesidades particulares de cada caso de desfogue.

  8. Composition of coarse-grained magnetite from pegmatite dikes related to plutons of quartz monzonite in the Jabal Lababa area, Kingdom of Saudi Arabia

    Science.gov (United States)

    Overstreet, William C.; Mousa, Hassan; Matzko, John J.

    1985-01-01

    Crystals of magnetite as large as 30 mm long and 7 mm thick are locally present in quartz-rich zones of interior and exterior pegmatite dikes related to plutons of quartz monzonite in the Jabal Lababa area. Niobium, tin, and yttrium are strongly enriched in six specimens of magnetite from interior pegmatite dikes in a small pluton where these elements form geochemical anomalies in nonmagnetic heavy-mineral concentrates from wadi sediment. Less abundant anomalous elements in the magnetite are molybdenum, lead, and zirconium, which also tend to be present in anomalous amounts in the nonmagnetic concentrates from the niobium-bearing pluton. The most anomalous trace element in the magnetite is zinc, which is at least 10 times as abundant as it is in the quartz monzonite plutons or in the nonmagnetic concentrates. The capacity of magnetite to scavenge molybdenum, zinc, niobium, lead, tin, yttrium, and zirconium suggests the possible utility of magnetite as a geochemical sample medium.

  9. Desigualdades en el mercado laboral : el colectivo de personas ex reclusas y su inserción en el mercado laboral

    OpenAIRE

    Martínez Cívico, Laura

    2013-01-01

    El acceso al mercado laboral no es igual para todos ni ofrece las mismas oportunidades. Existen ciertos colectivos de la sociedad que presentan grandes dificultades de acceso debido en parte a estigmas o prejuicios asociados a ellos por la sociedad. El colectivo de personas ex reclusas es uno de ellos. Existen multitud de factores tanto a nivel individual como social que inciden en la posterior reinserción laboral de este colectivo, que ponen de relieve la necesaria existencia de mecanismos d...

  10. Perspectivas del Mercado de Derivados en Colombia Retraso derivado del desconocimiento Perspectivas del Mercado de Derivados en Colombia Retraso derivado del desconocimiento

    Directory of Open Access Journals (Sweden)

    Natalia Cañas Arboleda

    2006-12-01

    Full Text Available El mercado de derivados representa la evolución de los mercados financieros enel mundo, debido a la capacidad que tiene el primero de ofrecer cobertura a losparticipantes del mercado, función importante en el actual contexto de globalización.Por lo anterior, en el país se desarrollan, aunque un poco tarde, diversos proyectospara la incorporación de futuros y opciones, como nuevas alternativas de inversióny financiación que redunden en menor incertidumbre para los inversionistas dediferentes sectores de la economía. A partir de allí, se muestra la situación actualdel mercado de derivados en Colombia y los esfuerzos realizados por diferentesinstituciones, encaminados al desarrollo del mismo.The derivative market represents the evolution of financial markets in the world, given the capacity that the former has for offering coverage to market participants, which is an important feature in the present context of globalization. For this reason, some projects are being developed in our country, though  a bit late, for the incorporation of futures and options, as new investment and financing alternatives, which may result in a reduced uncertainty for the investors in different sectors of the economy. This article shows the current situation of the derivative market in Colombia and the efforts made by different institutions, aimed at the development of such a market.

  11. A paleomagnetic and stable isotope study of the pluton at Rio Hondo near Questa, New Mexico: Implications for CRM related to hydrothermal alteration

    International Nuclear Information System (INIS)

    Paleomagnetic and rock magnetic data combined with stable isotope data from the middle Tertiary pluton along the Rio Hondo in northern New Mexico suggest that its magnetic remanence has both thermal (TRM) and high-temperature chemical (CRM) components. Oxygen isotope temperatures indicate that magnetite associated with the more rapidly cooled higher levels of the pluton, and with mafic inclusions and cogenetic rhyolitic dikes sampled at lower levels of exposure, ceased subsolidus recrystallization and isotopic exchange above its Curie temperature (5800C) in the presence of a magmatic fluid. Continued cooling imparted a TRM to these portions of the pluton. The more slowly cooled granodiorite at lower levels has quartz-magnetite isotopic temperatures that are below the Curie temperature of magnetite implying that its magnetization is high-temperature CRM. Sub-Curie isotopic temperatures for other granitic plutons in the western U.S.A. suggest that CRM may be commonly derived from subsolidus interactions between magnetite and magmatic fluids in plutonic rocks. A meteoric-hydrothermal system generated by the cooling Rio Hondo pluton, and not by younger adjacent intrusions, resulted in limited alteration along zones of high permeability near the southern margin of the Rio Hondo pluton, and in more prevasive alteration of the pluton to the north. The meteoric-hydrothermal alteration occurred at relatively high temperatures (>3500C) and, with the exception of local chloritization, caused little visible alteration of the rocks. The isotopic ratios indicate that little of the magnetite could have grown from or exchanged with a meteoric-hydrothermal fluid. (orig.)

  12. A paleomagnetic and stable isotope study of the pluton at Rio Hondo near Questa, New Mexico: implications for CRM related to hydrothermal alteration

    Science.gov (United States)

    Hagstrum, J.T.; Johnson, C.M.

    1986-01-01

    Paleomagnetic and rock magnetic data combined with stable isotope data from the middle Tertiary pluton along the Rio Hondo in northern New Mexico suggest that its magnetic remanence has both thermal (TRM) and high-temperature chemical (CRM) components. Oxygen isotope temperatures indicate that magnetite associated with the more rapidly cooled higher levels of the pluton, and with mafic inclusions and cogenetic rhyolitic dikes sampled at lower levels of exposure, ceased subsolidus recrystallization and isotopic exchange above its Curie temperature (580??C) in the presence of a magmatic fluid. Continued cooling imparted a TRM to these portions of the pluton. The more slowly cooled granodiorite at lower levels has quartz-magnetite isotopic temperatures that are below the Curie temperature of magnetite implying that its magnetization is high-temperature CRM. Sub-Curie isotopic temperatures for other granitic plutons in the western U.S.A. suggest that CRM may be commonly derived from subsolidus interactions between magnetite and magmatic fluids in plutonic rocks. A meteoric-hydrothermal system generated by the cooling Rio Hondo pluton, and not by younger adjacent intrusions, resulted in limited alteration along zones of high permeability near the southern margin of the Rio Hondo pluton, and in more prevasive alteration of the pluton to the north. The meteoric-hydrothermal alteration occurred at relatively high temperatures (> 350??C) and, with the exception of local chloritization, caused little visible alteration of the rocks. The isotopic ratios indicate that little of the magnetite could have grown from or exchanged with a meteoric-hydrothermal fluid. ?? 1986.

  13. Mineralogical, chemical and isotopic diversity in plutonic rock suites from the Coastal Maine Magmatic Province:the role of source region heterogeneity, tectonic setting and magmatic processes

    OpenAIRE

    Hogan, John Patrick

    1990-01-01

    This dissertation represents an investigation of the mid-Paleozoic tectono-thermal and kinematic evolution of the crust in eastern coastal Maine as recorded by the plutonic rocks of this region. The first chapter describes the plutonic rocks of the Coastal Maine Magmatic Province. A tectonic model is developed in which late Ordovician-Silurian bimodal magmatism is interpreted to reflect crustal melting as a result of intraplating of mantle melts at high crustal levels during...

  14. Petro-structural study of volcano-plutonic rocks of Yaoure Mountains: Contribution to understanding the metallotectic gold mineralization (Central Côte d'Ivoire)

    OpenAIRE

    Barthelemy Gnammytchet KOFFI; Gbele Ouattara; Alain Nicaise KOUAMELAN; Jean Paul DEROIN

    2013-01-01

    The petrographic study of rocks and some few outcrops revealed the great diversity of volcano-plutonic formations. Indeed, magmatism of the Yaouré Mountains is quite differentiated, ranging from basic terms (basalts) to acidic terms (rhyolites), passing to neutral terms (rhyodacites, andesites and dacites). The study also identifies several varieties of plutonic igneous rocks, including diorites, granodiorites, gabbros and sub-volcanic (microgranites). Diorites and granodiorites are dykes or ...

  15. Chemistry and petrology of the Apennine Front, Apollo 15. I - KREEP basalts and plutonic rocks. II - Impact melt rocks

    Science.gov (United States)

    Simon, S. B.; Papike, J. J.; Laul, J. C.

    1988-01-01

    The mineralogy, petrology, and chemistry of rock fragments for the Apennine Front coarse fines (10-4 and 4-2 mm) have been determined. The data are consistent with a single eruptive event that produced several flows. It is found that most of the plutonic rocks are ferroan in nature, with a few belonging to the Mg-suite. The mineral and bulk chemistry of KREEP basalts and the composition of ferroan anorthosites are discussed. Petrographic studies of 21 impact melts are also presented, showing a variety of textures. It is found that the Apollo 15 impact melts are mixtures of low-K Fra Mauro, KREEP, and plutonic components. The Ni/Ir ratios of the melt rocks are shown to be greater than chondritic values, indicating ancient and/or iron meteorite components.

  16. Evaluation of the Cerro Solo nuclear ore, province of Chubut. On the economic parameters of the deposit. Pt. 3

    International Nuclear Information System (INIS)

    Preliminary results of the resources estimation carried out in the Cerro Solo uranium ore deposit, located in the Chubut Province, 1900 km SW from Buenos Aires and 380 Km W from Trelew, presented in tonnes of uranium recoverable at costs up to U$S 80/kgU, are as follows: a) Reasonable assured resources (indicated): 800 tU; b) Estimates Additional Resources (inferred): 2200 tU. Economic evaluation at the order-of-magnitude level, performed using the grade-tonnage model of the deposit, resulted a useful tool in the different stages of the project to identify the influence of technical parameters on the potential profitability. Research about feasibility of in-situ leaching method of exploitation for this deposit introduces an interesting alternative for future uranium production in the country. (Author)

  17. IMPACT OF ADDITIONALS CONTAMINANTS DUE TO ACID MINE DRAINAGE IN TRIBUTARIES OF THE PILCOMAYO RIVER FROM CERRO RICO, POTOSÍ, BOLIVIA

    Directory of Open Access Journals (Sweden)

    William H.J. Strosnider

    2014-09-01

    Full Text Available Intensive mining and processing of the polymetallic sulfide ore body of Cerro Rico de Potosí (Bolivia has occurred since 1545. To further investigate acid mine drainage (AMD discharges and their link to downstream contamination, data were gathered during two sampling events during the most extreme periods of the dry and wet seasons of one year. Concentrations of Ag, B, Ba, Mo, Sb, Se, Sn and V in AMD and receiving streams were greater than Bolivian discharge limits and receiving water body guidelines as well as international agricultural use standards. High concentrations of rare earth metals have been documented in this area. Results indicate that contamination from mining has a larger scope than previously thought and underscore the importance of remediation.

  18. Charnockitic ortho gneisses and mafic granulites of Cerro Olivo complex, proterozoic basement of SE Uruguay, Part 1: Geology

    International Nuclear Information System (INIS)

    Charnockitic ortho gneisses and mafic granulite s exposed in the Cerro Bori Block, in the center of Punta del Este terrain, were the first document occurrence of granulitic rocks from SE sector of the Uruguayan Shield. We present here their main geological features, with the purpose to suggest some petrologic and structural interesting problems for a future lithogeochemical, mineral chemistry, stable isotopes and fluid inclusion studies about these rocks. We propose some speculation form field-based studies considering a cognate magmatic origin of both kinds of rocks, previous to a homogeneous granulitic metamorphism. Some structural evidences indicate that after their uplift, these rocks were located on over thickened crust, at great to medium deepness. A cataclasis during anatexis and amphibolite-facies mineral association stabilization are common phenomena. Other evidences suggest a polycyclic character for the regional geologic evolution

  19. Notes on the ecology of Phyllodactylus reissi (Phyllodactylidae: Sauria in Parque Nacional Cerros de Amotape (Tumbes, Peru

    Directory of Open Access Journals (Sweden)

    Juan Carlos Jordán Arizmendi

    2012-02-01

    Full Text Available Some basics aspects on the ecology of the nocturnal gecko Phyllodactylus reissi from Parque Nacional Cerros de Amotape (Tumbes, Peru are described. This species used rock boulders (57,4% and trees (31,9% as microhabitats primarily, exhibiting a nocturnal activity pattern, with a peak between 2100-2200 hours, remaining active until midnight. Body temperature (mean 24,4 ºC was correlated with both air and substrate temperature, with the last variable affecting in higher degree (47% the body temperature of this species. The slightly high body temperature of Phyllodactylus reissi, compared to other Phyllodactylus geckos, could be related to nocturnal microhabitat use and diurnal retreat site selection. More studies on lizard ecology from this endangered ecosystem are needed.

  20. Estudio de la líqueno flora encontrada en el Cerro de Quininí, Tibacuy, Cundinamarca

    Directory of Open Access Journals (Sweden)

    Hormaza Francisco

    2000-12-01

    Full Text Available

    Se realizó un muestreo de la liquen o flora del cerro de Quininí, Tibacuy, Cundinamarca para estudiar las características morfológicas externas de los géneros de líquenes encontrados en el. A su vez se hizo la revisión bibliográfica acerca de dichos géneros, datando así la riqueza de líquenes en la zona con 8 géneros en total y con respecto al papel de bioindicadores se mostró el grado de intervención para el lugar.

  1. Characterizing fractured plutonic rocks of the Canadian shield for deep geological disposal of Canada's radioactive wastes

    International Nuclear Information System (INIS)

    Since 1978 AECL has been investigating plutonic rocks of the Canadian Shield as a potential medium for the disposal of Canada's nuclear fuel waste. During the last two years this study has been continued as part of Ontario Hydro's used fuel disposal program. Methods have been developed for characterizing the geotechnical conditions at the regional scale of the Canadian Shield as well as for characterizing conditions at the site scale and the very near-field scale needed for locating and designing disposal vault rooms and waste emplacement areas. The Whiteshell Research Area (WRA) and the Underground Research Laboratory (URL) in southeastern Manitoba have been extensively used to develop and demonstrate the different scales of characterization methods. At the regional scale, airborne magnetic and electromagnetic surveys combined with LANDSAT 5 and surface gravity survey data have been helpful in identifying boundaries of the plutonic rocks , overburden thicknesses, major lineaments that might be geological structures, lithological contacts and depths of the batholiths. Surface geological mapping of exposed rock outcrops, combined with surface VLF/EM, radar and seismic reflection surveys were useful in identifying the orientation and depth continuity of low-dipping fracture zones beneath rock outcrops to a depth of 500 to 1000 m. The surface time-domain EM method has provided encouraging results for identifying the depth of highly saline pore waters. The regional site scale investigations at the WRA included the drilling of twenty deep boreholes (> 500 m) at seven separate study areas. Geological core logging combined with borehole geophysical logging, TV/ATV logging, flowmeter logging and full waveform sonic logging in these boreholes helped to confirm the location of hydro geologically important fractures, orient cores and infer the relative permeability of some fracture zones. Single-hole radar and crosshole seismic tomography surveys were useful to establish the

  2. Los marsupiales (Mammalia del Mioceno Superior de la Formación Cerro Azul (Provincia de La Pampa, Argentina

    Directory of Open Access Journals (Sweden)

    Visconti, G.

    2000-04-01

    Full Text Available We describe the most complete South American marsupial association of Huayquerian Age (late Miocene. Specimens were recovered from several new localities of central and northern La Pampa province (central Argentina, at levels assignable to Cerro Azul Fm.: Bajo Giuliani, Quehué, Telén, El Guanaco, and Laguna Chillhué. Loessoid sediments studied from this formation are indicative of lacustrine deposits overlaid by eolian levels bearing evidences of pedogenesis. A study of these levels at each one of the new localities led to their correlation in an integrated profile of Cerro Azul Fm. This formation corresponds to «Epecuén Fm.», at least in Salinas Grandes de Hidalgo, and probably also to the upper levels of Arroyo Chasicá Fm. The studied marsupials are representative of almost all major lineages (orders of South American Neogene marsupials. The marmosine didelphid Zygolestes tatei sp. nov. differs from the type species of the genus in its larger size, unreduced third lower premolar, and in the less reduction of the metaconid in the last lower molar. Another marmosine, Thylamys pinei sp. nov., differs from other Marmosini in the twinning of the para- and metaconid in the lower molars, and in the wider talonid of the m4. The Monodelphini marmosines Thylatheridium hudsoni y T. dolgopolae are abundant in several localities of this formation; their study confirms close affinities between this genus and Monodelphis. The didelphines Hyperdidelphys pattersoni and an indeterminate species of Lutreolina are also represented by a few specimens. A mandibular fragment including part of the last molar may represent the oldest record of a Sparassocynidae in central Argentina. The Borhyaenidae and Thylacosmilidae (Sparassodonta are also recorded by a few, fragmentary specimens. Pliolestes venetus sp. nov. (Paucituberculata, Caenolestidae differs from the type species of the genus in its smaller size and in the larger, less displaced metaconid in the

  3. Constraining the Paleogene of South America: Magnetostratigraphy and paleoclimate proxy records from Cerro Bayo (Provincia de Salta, Argentina)

    Science.gov (United States)

    Hyland, E.; Cotton, J. M.; Sheldon, N. D.

    2012-12-01

    Records of rapid climatic and ecological shifts in the past are crucial for understanding global systems and for predicting future impacts of climate change. Transient and broad scale hyperthermal events during the Paleogene, such as the Paleocene-Eocene Thermal Maximum (PETM) and Early Eocene Climatic Optimum (EECO), have been studied extensively through both marine records and a significant terrestrial record from North America. Despite this, little evidence exists from the climatic and ecological histories of other major landmasses, which limits the effectiveness of global climate response predictions. Here we present an integrated paleoenvironmental reconstruction of the early Paleogene from a site in central South America (Cerro Bayo, Argentina), including a new magnetostratigraphic age model, pedological and sedimentological interpretation, whole rock geochemical climate proxies, isotopic environmental proxies, and microfloral assemblages. Cerro Bayo is a 235-meter terrestrial section that exposes the Tunal, Mealla, and Maiz Gordo Formations, and based on magnetostratigraphic interpolation spans roughly 58—50 Mya, including both the PETM and EECO events. These formations are composed primarily of reddish sandstone and siltstone, much of which exhibits features characteristic of a moderate degree of pedogenesis (i.e., Inceptisols and Alfisols). High-resolution climate proxies derived from paleosol geochemical compositions highlight rapid increases in mean annual temperature (>5°C) and precipitation (>300 mm yr-1) during the PETM, as well as more gradual increasing temperature and precipitation trends leading up to the EECO. Carbon isotope stratigraphy through the section also indicates a sizable negative excursion (~4‰) during the PETM, and generally positive isotopic trends during the early Eocene. Phytolith biostratigraphy also details changes in local vegetation composition during climatic events that corresponds to similar patterns seen in terrestrial

  4. Development of the Cerro solo deposit and uranium favorability of the San Jorge Gulf Basin, province of Chubut

    International Nuclear Information System (INIS)

    In the future the uranium exploration activities of CNEA would tend to improve the knowledge of geology and uranium favorability; to perform prospection tasks, and research and development in exploration technologies, to contribute to be in a position to meet the requirements of the country in the long term. On the other hand, a strong growth of nuclear capacity is expected in the first two decades of the next century. Based on its promising grade, the Cerro Solo uranium ore deposit was selected in 1990 by the CNEA to carry out an assessment project. The intensive exploration level was accomplished, as follows: definition of general characteristics of the main orebodies; detailed geologic studies; estimation of resources with adequate data; and preliminary selection of mining-milling methods to estimate the potential profitability of the project. The deposit belongs to the sandstone type. The mineralized layers are distributed into the fluvial sandstones and conglomerates of the cretaceous Chubut Group, lying 50 to 130 m deep Resources of the deposit, with an average grade of 0.3% U, in tonnes of recoverable uranium at costs of up to $80/kg U, are: Reasonable Assured Resources (RAR): 800 t U, Estimated Additional Resources, Category I (EAR-I): 2100 t U. Follow-up drilling programmes are being performed at present in some of the target sites defined in the paleochannel that hosts the Cerro Solo deposit, in order to establish the hypothetical resources of the area. The sites were determined as a result of the exploration that CNEA conducted in the Pichinan uranium district. Recently a regional research project was formulated, for the detailed exploration in the San Jorge Gulf Basin, where the Chubut Group is distributed. 17 refs, 4 figs

  5. Petrogenesis of the Dengzhazi A-type pluton from the Taihang-Yanshan Mesozoic orogenic belts, North China Craton

    Science.gov (United States)

    Xiaolu, Niu; Bin, Chen; Xu, Ma

    2011-05-01

    The voluminous Mesozoic monzonitic to monzogranitic rocks in the north China craton (NCC) mostly show high-K calc-alkaline and I-type granitoids features. The Dengzhazi granitic pluton, however, shows features typical of A-type granites. The A-type pluton was emplaced in the Taihang-Yanshan orogenic belts of the northern margin of the NCC, with zircon U-Pb ages of around 140 Ma. The Dengzhazi A-type granites are characterized by high SiO 2 (70.2-77.7 wt.%), K 2O + Na 2O, Zr, Nb, Ga, Zn, and Y contents as well as high Ga/Al ratios, and extremely low CaO, Ba, Sr. In addition, they show high zircon saturation temperatures (870-950 °C), low water and low oxygen fugacity. All these features are consistent with the A-type affinity of the pluton. In situ Hf isotopic analyses for the dated zircons show relatively small range of ɛHf( t) (-13 to -17). They also have homogeneous initial Nd isotopic compositions with ɛNd( t) ranging from -15.1 to -16.3. The Hf and Nd isotopic data suggest that the Dengzhazi A-type granites originated from a homogeneous crustal source, probably the Archean mafic-intermediate granulites. Taking into account the high temperatures, the low H 2O and fO 2 of the magma system, we believe that partial melting of the granulites should have been triggered by underplating of mantle-derived magmas at the base of the mafic lower crust in an extensional regime. The Dengzhazi A-type granite is the oldest pluton of the Taihang-Yanshan Mesozoic magma belts, signifying the commencement of extensive underplating of mafic magmas, and thus of lithospheric thinning in the northern NCC.

  6. The Ajo Mining District, Pima County, Arizona--Evidence for Middle Cenozoic Detachment Faulting, Plutonism, Volcanism, and Hydrothermal Alteration

    Science.gov (United States)

    Cox, Dennis P.; Force, Eric R.; Wilkinson, William H.; More, Syver W.; Rivera, John S.; Wooden, Joseph L.

    2006-01-01

    Introduction: The Ajo porphyry copper deposit and surrounding Upper Cretaceous rocks have been separated from their plutonic source and rotated by detachment faulting. Overlying middle Cenozoic sedimentary and volcanic rocks have been tilted and show evidence for two periods of rotation. Following these rotations, a granitic stock (23.7?0.2 Ma) intruded basement rocks west of the Ajo deposit. This stock was uplifted 2.5 km to expose deep-seated Na-Ca alteration.

  7. Map showing distribution and classification of felsic plutonic rocks in the eastern Arabian Shield, Kingdom of Saudi Arabia

    Science.gov (United States)

    Du Bray, E.A.

    1983-01-01

    This 1:500,000-scale compilation shows the distribution of felsic plutonic rocks, lithologic types, and associated mineralization in an area between lat 21° and 24°30’ N., long 43°30’ and 46° E. It is part of a shieldwide compilation being done within the framework of Saudi Arabian Deputy Ministry for Mineral Resources projects 2.04 and 3.12.

  8. Mineral-scale Sr isotope variation in plutonic rocks – a tool for unraveling the evolution of magma systems.

    OpenAIRE

    Davidson, J. P.; Font, L.; Charlier, B.L.A.; Tepley, F.J. III

    2006-01-01

    Isotope ratios of elements such as Sr, Nd, Pb and Hf can be used as tracers of magmatic sources and processes. Analytical capabilities have evolved so that isotope ratios can now be analysed in situ, and isotopic tracers can therefore be used within single minerals to track the changing magmatic environment in which a given mineral grew. This contribution shows that Sr isotope ratios in feldspars that make up plutonic rocks will typically preserve initial isotopic variations, provided precise...

  9. Paleoproterozoic structural frame of the Yetti domain (Eglab shield, Algeria): Emplacement conditions of the Tinguicht late pluton from magnetic fabric study

    Science.gov (United States)

    Merabet, Nacer-eddine; Mahdjoub, Yamina; Henry, Bernard; Abtout, Abdeslam; Maouche, Said; Kahoui, Mohamed; Lamali, Atmane; Ayache, Mohamed

    2016-02-01

    The Tinguicht pluton is part of the ˜2.07 Ga post-collisional magmatic suites that intruded the Yetti Paleoproterozoic volcano-sedimentary series of the western part of the Eglab Shield (West African Craton). It represents one of the most recent units of these suites. This pluton, with a NW-SE elliptic shape, is unfoliated, and its deformational structures are practically restricted to fracturing and faulting. New structural, microstructural and aeromagnetic data are presented in order to analyze in particular the relationship between the Tinguicht pluton emplacement and the related NNW-SSE major mega-shear zone, separating the Yetti and Eglab domains. To constrain the context of the regional post-collisional evolution of the Eglab shield, a structural analysis was performed by mapping the magnetic structures (foliation and lineation) using AMS. The combination of the results of all the used approaches leads to a new and enriched image of this granitic pluton and of its tectonic emplacement context. The elliptic shape of the granitic body and the AMS strain pattern are consistent with the presence of a NNW-SSE major structure. NNW-SSE is also one of the major directions highlighted by the aeromagnetic data. This study thus evidences the role of the pre-existing major shear zones in controlling emplacement of post-collisional Paleoproterozoic plutons like Tinguicht, as shown for Drissa pluton in the Eglab domain earlier.

  10. “LAS AUDIENCIAS DE LA CALLE” ENTRE MERCADOS, CALLES Y MÚSICA EN PERÚ

    Directory of Open Access Journals (Sweden)

    Franklin Cornejo Urbina

    2008-01-01

    Full Text Available Cuando se habla de audiencias de los medios de comunicación entendemos también que ellas cambian en los contextos, donde los televidentes y radioescuchas usan los medios con modos y fines diferentes. Así y como parte de la diversidad de las audiencias he ubicado bajo la definición “audiencias de la calle” a un grupo social, más bien de origen humilde y de rutinas cotidianas colectivo-comunitarias, que incluyen a ex campesinos, niños de la calle, comerciantes ambulantes e inmigrantes empobrecidos que se reúnen, trabajan y pasan gran parte del día en mercados de zonas urbano marginales de Lima, en Perú. El mercado popular es un lugar para las grandes mayorías donde hay encuentros y tensiones entre lo urbano y rural por viejas diferencias étnicas, regionales, locales y comunitarias entre andinos y costeños. La pobreza, la urbanización y el crecimiento de las ciudades han convertido al mercado en un lugar de sobrevivencia, trabajo, y un espacio para afrontar la vida de la ciudad. El presente artículo aborda el tema de los estudios de audiencia desde el mercado popular peruano, sus medios y comunicaciones.

  11. Testing a Threshold: An Approximate Replication of Johnson, Mercado & Acevedo 2012

    Science.gov (United States)

    Johnson, Mark D.; Nicodemus, Christine L.

    2016-01-01

    In order to better understand the role of working memory in second language (L2) written production, this study contributes to recent research attempting to apply Kellogg's model of working memory in first language (L1) writing to L2 writing research (Ellis & Yuan 2004; Ong & Zhang 2010; Johnson, Mercado & Acevedo 2012). This paper…

  12. La repercusión de las transformaciones territoriales en el mercado de tierras

    OpenAIRE

    Martinoli, María Érica

    2000-01-01

    En este trabajo se indaga sobre la lógica de funcionamiento del mercado de tierras, los actores involucrados y los nuevos productos inmobiliarios derivados del actual proceso de concentración económica, exclusión social y fragmentación territorial

  13. China, inversiones extranjeras en servicios: el mercado gastronómico

    OpenAIRE

    Zottele de Vega, Esteban; Universidad Veracruzana

    2013-01-01

    En el presente artículo se describen las características del mercado gastronómico chino, enfatizando en la importancia de la adaptabilidad y del guanxi, como elementos indispensables para aquellos empresarios extranjeros que aspiran a invertir en China. Asimismo, se ofrecen ejemplos de inversiones extranjeras en China, en el ámbito de la gastronomía.

  14. Estrategia, Orientación al Mercado y Desempeño Organizacional

    Directory of Open Access Journals (Sweden)

    Carmen Berenice Ynzunza Cortés

    2013-01-01

    Full Text Available La pequeña industria desempeña una función crucial en la economía y el desarrollo de los países. De acuerdo con datos del Instituto Nacional de Estadística y Geografía [1], la PYME en México representa el 99.1% de la estructura empresarial. Sin embargo, el nivel de desarrollo alcanzado, producto de la globalización, ha sido bajo en comparación a otros países. Por ello, dentro de los objetivos de investigación planteados en este trabajo están el analizar el impacto que las fuerzas de mercado tienen sobre las estrategias competitivas prospectoras y analizadoras; y determinar el vínculo existente entre las capacidades de orientación al mercado, la estrategia competitiva y el desempeño organizacional, en 116 Pymes del sector industrial del Estado de Querétaro, mediante un modelo estructural con un muestreo de conveniencia no probabilístico. Los resultados indican que las fuerzas del mercado afectan las estrategias competitivas prospectoras y analizadoras y que éstas favorecen la creación de las capacidades necesarias para generar una ventaja competitiva como la orientación al mercado, encontrándose que ésta capacidad organizacional es un factor importante para el crecimiento y el desempeño organizacional.

  15. Análisis del comportamiento de mercado de la pitahaya (Hylocereus undatus en Costa Rica

    Directory of Open Access Journals (Sweden)

    Olman Quirós Madrigal

    2010-10-01

    Full Text Available La pitahaya (Hylocereus undatus es una planta que pertenece a la familia de las cactaceae, que se puede consumir como fruta fresca o procesada como pulpa; sin embargo, en Costa Rica su uso no está muy difundido, por lo que el mercado meta es la población de origen nicaragüense residente en el país, quienes catalogan el producto como de consumo tradicional o masivo.Es por esto que resulta importante retomar el estudio de los componentes del mercado, en donde se destaca no sólo por ser una fruta con componentes nutricionales que aportan beneficios a la salud humana, sino tambien porque suple una demanda latente y su cultivo puede ser una actividad alternativa para productores de zonas con condiciones agroecológicas adversas. En relación con el abastecimiento del producto en el mercado nacional, se enfatiza que su procedencia es nacional pero principalmente se importa como fruta fresca y pulpa de Nicaragua y, en menor grado, de Colombia.El precio de la pitahaya en el mercado nacional está estrechamente relacionado con los precios de importación, ya que la oferta principal proviene del producto importado, por lo que ha tenido un comportamiento creciente al pasar, de US$0,574 en el año 2003, a US$1,18 por kg en el 2007.

  16. El sector de manufacturas en Guanajuato y su participación en el mercado nacional

    Directory of Open Access Journals (Sweden)

    Roberto Escalante

    2011-01-01

    Full Text Available El objetivo del presente artículo es identificar los determinantes de la producción de la industria de manufacturas en Guanajuato en tres divisiones: alimentos, autopartes y calzado. Los resultados de las estimaciones econométricas muestran que la industria de autopartes es bastante sensible a las condiciones del mercado externo. La industria de alimentos está muy vinculada al mercado interno. La industria del calzado desde principios de la presente década ha enfrentado una crisis derivada de un crecimiento acelerado de las importaciones, y se espera que mantenga esta tendencia negativa en los próximos años. Condiciones favorables en el mercado externo promoverían un mayor crecimiento en las autopartes y el calzado, pero este resultado considera que las empresas tienen una capacidad de respuesta para adaptarse a las nuevas condiciones y mejorar su posicionamiento en el mercado nacional. Factores importantes a considerar en el diseño de una política industrial a nivel estatal.

  17. Cuerpos intrusivos asociados a las mineralizaciones polimetálicas del depósito Cerro León, área del anticlinal El Tranquilo, Santa Cruz: evidencias geofísicas Intrusive bodies associated with the polymetallic mineralization of the Cerro León deposit, area of Cerro Tranquilo anticline, Santa Cruz: Geophysical evidence

    Directory of Open Access Journals (Sweden)

    G. A Peñalva

    2008-03-01

    Full Text Available Las características geológicas tales como presencia de cuerpos intrusivos y subvolcánicos someros básicos a intermedios y de las mineralizaciones con alto contenido de sulfuros del área del anticlinal El Tranquilo, son particulares y poco representadas en el macizo del Deseado. El depósito polimetálico vetiforme Cerro León presenta una signatura geoquímica-mineralógica que lo diferencia del clásico modelo epitermal de baja sulfuración característico del macizo del Deseado. Los datos aeromagnéticos del área del anticlinal El Tranquilo permiten reconocer una conspicua anomalía subcircular que se interpreta como un intrusivo no aflorante, de aproximadamente 9 km de diámetro, que subyace al Grupo El Tranquilo y a la Formación Roca Blanca; su profundidad se estima en 1400 m. Este cuerpo intrusivo genera el domamiento regional del anticlinal El Tranquilo y el fracturamiento radial asociado. La interpretación de la presencia de pequeños cuerpos intrusivos y subvolcánicos o apófisis alimentados por el cuerpo intrusivo mayor, asociados con anomalías magnéticas de menor diámetro y mayor gradiente, está confirmada por datos de perforación. Las principales vetas del depósito Cerro León se ubican asociadas espacialmente con los cuerpos intrusivos y subvolcanicos someros no aflorantes. Esto, sumado al alto contenido de sulfuros y la signatura geoquímica y mineralógica de las vetas, sugiere que posiblemente estén asociadas genéticamente a los cuerpos intrusivos subyacentes y circundantes, y permite utilizar este modelo como una herramienta de prospección para este tipo de depósitos.The geologic characteristics such as presence of basic to intermediate intrusive and subvolcanic bodies, and the mineralization with high sulfide content of the El Tranquilo anticline area are peculiar and poorly represented in the Deseado Massif. The Cerro León polymetallic deposit presents a geochemical and mineralogical signature that is

  18. Formation of lower continental crust by relamination of buoyant arc lavas and plutons

    Science.gov (United States)

    Kelemen, Peter B.; Behn, Mark D.

    2016-03-01

    The formation of the Earth's continents is enigmatic. Volcanic arc magmas generated above subduction zones have geochemical compositions that are similar to continental crust, implying that arc magmatic processes played a central role in generating continental crust. Yet the deep crust within volcanic arcs has a very different composition from crust at similar depths beneath the continents. It is therefore unclear how arc crust is transformed into continental crust. The densest parts of arc lower crust may delaminate and become recycled into the underlying mantle. Here we show, however, that even after delamination, arc lower crust still has significantly different trace element contents from continental lower crust. We suggest that it is not delamination that determines the composition of continental crust, but relamination. In our conceptual model, buoyant magmatic rocks generated at arcs are subducted. Then, upon heating at depth, they ascend and are relaminated at the base of the overlying crust. A review of the average compositions of buoyant magmatic rocks -- lavas and plutons -- sampled from the Aleutians, Izu-Bonin-Marianas, Kohistan and Talkeetna arcs reveals that they fall within the range of estimated major and trace elements in lower continental crust. Relamination may thus provide an efficient process for generating lower continental crust.

  19. Metamorphism and plutonism in the Quetico Belt, Superior Province, N.W. Ontario

    Science.gov (United States)

    Percival, J. A.

    1986-01-01

    The Quetico Belt lies between the metavolcanic Wawa-Shebandowan and Wabigoon Belts. It consists of marginal metasedimentary rocks and central pelitic, gneissic and plutonic rocks. Metamorphism is Barrovian, at depths less than 10 km, and grade increases from margins to core of the belt: the outermost pelites are at chlorite-muscovite grade; inward a garnet-andalusite zone formed throughout the inner margin; and the central zone ranges form garnet-andalusite in the west and garnet-sillimanite-muscovite to garnet-sillimanite-cordierite and rare kyanite 6 to 150 km to the east. This increase is correlated with granitic intrusives. Migmatites in the core have intrusive leucosomes in the west and locally derived ones in the east. Isograd surfaces are steep where the belt is narrow and dip gently where it is wide. The Quetico Park intrusive complex of the central region of the Quetico Belt shows a zonation across it 20 to 50 km width from older, medium grained biotite composition to younger, coarse to pegmatitic granitic composition. Sediment of the Quetico basin had its source in the bordering metavolcanic belts and was deposited ca. 2.75 to 2.70 Ga ago. Boundaries of the belt dip inward, so it essentially is a graben of inter-arc or back-arc type.

  20. Fission Track Geochronology of Xiaonanchuan Pluton and the Morphotectonic Evolution of Eastern Kunlun since Late Miocene

    Institute of Scientific and Technical Information of China (English)

    2006-01-01

    Apatite fission track (AFT) thermochronology of seven samples from the Xiaonanchuan(小南川) pluton in the Kunlun (昆仑) pass area was carried out, for the purpose of determining the timing of cooling and the relation between the exhumation and the morphotectonic processes. The AFT ages yield low denudation rates of 0.020-0.035 mm/ a during the late Miocene, which correspond to a stable geomorphic and weak tectonic uplifting environment. The low denudation rates can be considered as the approximate tectonic uplifting rates. The AFT geochronology shows paroxysmally rapid cooling since the Pliocene and an apparent material unroofing of more than 3 km in the Xiaonanchuan area. This was not the result of simple denudation. The rapid cooling was coupled with the intensive orogeny since the Pliocene, which was driven by tectonic uplifting. The accelerated relief building was accompanied by a series of faulting, which caused the basin and the valley formation and sinking. The space pattern of the AFT ages also shows differential uplifting, which decreases northwardly. This trend is supported by the regional AFT data, which indicate that the exhumation decreases northwardly in eastern Kunlun. This trend also exists in east-west orientation from the western Kunlun range to the eastern. The uplifting trend is also supported by geomorphic characteristics including the elevation and the relief differences as well as the distribution of the Late Cenozoic volcanism.

  1. Elpasolite from hyperalkaline pegmatite of the Khibiny pluton, Kola Peninsula. Symmetry of elpasolite

    Science.gov (United States)

    Pekov, I. V.; Chukanov, N. V.; Kononkova, N. N.; Zubkova, N. V.; Rabadanov, M. Kh.; Pushcharovsky, D. Yu.

    2008-12-01

    Elpasolite, K2NaAlF6, has been found for the first time in a pegmatite related to peralkaline foid syenite at Mt. Koashva, Khibiny alkaline pluton, Kola Peninsula, Russia, as pale pink octahedral crystals up to 2 mm in size within cavities in the natrolite core of pegmatite in association with amicite, sodalite, aegirine, pectolite, catapleiite, sitinakite, lemmleinite-K, and vinogradovite. The chemical composition determined with an electron microprobe is as follows, wt %: 31.53 K; 9.22 Na; 11.20 Al; 47.21 F; total is 99.16. The empirical formula is K1.96Na0.98Al1.01F6.05. The infrared spectrum is given. The crystal structure has been refined to R = 0.030, space group Fm bar 3 m, a = 8.092 Å. The result of a special X-ray powder diffraction study confirmed the suggestion made by Morss (1974) that reflections violating space group Fm bar 3 m in some published X-ray powder patterns of natural elpasolite are Kβ-lines.

  2. Distribution of manganese between coexisting biotite and hornblende in plutonic rocks

    Science.gov (United States)

    Greenland, L.P.; Gottfried, D.; Tilling, R.I.

    1968-01-01

    The distribution of manganese between coexisting biotite and hornblende for 80 mineral pairs from igneous rocks of diverse provenance (including Southern California, Sierra Nevada, Boulder, and Boulder Creek batholiths and the Jemez Mountains volcanics) has been determined by neutron activation analysis. Data on the distribution ratio (Kd = Mnhornblende Mnbiotite) indicate that an equilibrium distribution of Mn is closely approached, though not completely attained, in most samples from plutonic environments. Comparison of Kd values of mineral pairs with bulk chemical composition of host rocks reveals no correlation. Because initial crystallization temperatures vary with rock composition, the lack of correlation of composition with Kd suggests that the equilibrium distribution of Mn between biotite and hornblende reflects exchange at subsolidus temperatures rather than initial crystallization temperatures. The highest Kd values are for volcanic rocks, in which rapid quenching prevents subsolidus redistribution of Mn. For sample pairs from the Southern California and Sierra Nevada batholiths there is a positive correlation of Kd with TiO2 content of biotite. Though the evidence is not compelling, Kd may also correlate with the rate of cooling and/or the presence or absence of sphene in the rock. ?? 1968.

  3. Natural radionuclides in the rocks of the Valle del Cervo Pluton in Piedmont

    International Nuclear Information System (INIS)

    Monitoring of the gamma radiation in Valle del Cervo Pluton was performed by determining U and Th contents in the main rock types cropping out over the entire area and pertaining to the granitic complex, syenitic complex and monzonitic complex. In particular, syenitic rocks were largely used as building and ornamental materials (e.g. Sienite della Balma). All the samples are fresh and do not present joints or fractures filled with U minerals. In the crushed samples the activity of uranium varies from 346 to 764 Bq/kg. Concentration of thorium varies from 202 to 478 Bq/kg. For all the analysed rocks uranium activity is higher than thorium one. The lowest value of radioactive concentration is referred to rocks of the granitic complex. The most active rocks are syenites. The data confirm the high activities of Valle del Cervo rock types, strongly connected with high K content of the source magma (geochemical signature); on the contrary, the activity seems to be not related to the location of the samples. (authors)

  4. An extrusive-plutonic event at Hardy Point and its vicinity - Greenwich Island - Antarctic

    International Nuclear Information System (INIS)

    The volcanic and intrusive rocks at Hardy point and its vicinity were formed mainly during a Mesozoic magmatism. Andesitic-basalt flows and and andesites constitute the volcanic rocks. The intrusive ones were expressed as an epizonal body, with dioritic to granitic composition, and are cogenetic to the volcanic ones. The geochemical patterns indicate that volcanism preceded plutonism. In rare earth elements diagram the intrusive rocks present a further developed pattern, in which all rocks show calc-alkaline affinity, an enrichment in light rare earth diagram the intrusive rocks present a further, in which all rocks show calc-alkaline affinity, an enrichment in light rare earth elements relative to the heavy ones, probably due to partial melting of the mantle. In the spidergram (LILE, HFSE) the same pattern is observed for all rock groups, with strong negative anomalies of ti, p Nb, typical of island arcs, besides a positive anomaly of Ce, which could be related to the assimilation of Ce-enriched marine sediments. (author)

  5. The intrusive complexof the Island of Giglio: geomagnetic characteristics of plutonic facies with low susceptibility contrast

    Directory of Open Access Journals (Sweden)

    R. Cavallini

    1998-06-01

    Full Text Available Two main plutonic facies characterize the intrusive complex of the Island of Giglio, and the trend of their contact at depth has been modelled using a 2D½ analysis based on a detailed geomagnetic survey in order to verify the geological hypothesis of the subsurface geometry of this contact. The magnetic anomaly connected with the discontinuity is quite low, due to the small difference between the magnetic susceptibilities of the two granitic facies. Development of this model of inversion of the magnetic field, which is in good agreement with the geological interpretation, was made possible by: 1 accurate control of the geomagnetic time variations and consequent temporal reduction, 2 a very low level of the artificial magnetic noise, 3 high density of the magnetic survey, 4 detailed knowledge of the mapped geologic contact between facies and of their petrologic characteristics, and 5 direct local measurements of the magnetic susceptibilities of the key lithologies. The model shows the trends of the geological contact, as projected in three E-W sections, that dips eastward in the range between 210 and 540, supporting the geologic hypothesis that the Pietrabona facies represents an external shell of the shallowly emplaced Giglio monzogranite intrusion.

  6. Orientação para o Mercado no Segmento Hoteleiro: o caso português

    Directory of Open Access Journals (Sweden)

    Mario Barata Raposo

    2010-07-01

    Full Text Available Resumo O objectivo deste estudo foi medir o grau de orientação para o mercado dos maiores grupos hoteleiros de Portugal. Após uma breve explanação sobre a orientação para o mercado e o segmento hoteleiro em Portugal apresentou-se um estudo empírico realizado junto dos maiores 20 grupos de hotéis de Portugal, utilizando como instrumento de colecta de dados, a tradicional escala Markor (Market orientation adaptada ao sector hoteleiro. Constatou-se nas organizações investigadas uma boa capacidade de geração de informações de mercado e resposta ao mercado. Porém os resultados obtidos com o constructo da disseminação de informações de mercado ficaram abaixo das expetactivas. Portanto, o desafio actual para as principais redes de hotéis de Portugal é propiciar a melhoria da disseminação interna das informações que os profissionais de marketing recolhem junto ao mercado. Palavras-chave: gestão do marketing; orientação para o mercado; markor; sector hoteleiro em Portugal. Abstract The objective of this study was to measure level of orientation for the market of the largest hotel groups of Portugal. After a brief explanation on the market orientation and the hotel segment in Portugal an empiric study was presented performed with the largest groups of 20 hotels of Portugal, using as an instrument of collection data, the traditional Markor scale (market orientation adapted to the hotel sector. It was found in the investigated organizations a good capacity to generate market information and response to the market. However the results obtained with the construct of the dissemination of market information were below the expectations. So the current challenge for the main networks of hotels in Portugal is to improve the internal dissemination of information that marketing professionals gathered at the market. Keywords: marketing management, orientation to the market, markor, hotel sector in Portugal.

  7. Decree 343/012. Is regulated the servitude established by Decree-Law 10,383, on several lines of electricity conduction -150 KV to be built in the departments of Florida, Cerro Largo, Maldonado, Flores, San Jose and Tacuarembo

    International Nuclear Information System (INIS)

    This decree regulates the establishment of electricity conduction in Florida, Cerro Largo, Maldonado, Flores, San Jose and Tacuarembo towns. These electrical lines are necessary to provide the public service by UTE

  8. Información y Volatilidad en el Mercado Financiero Information and Volatility in Financial Markets

    Directory of Open Access Journals (Sweden)

    Aldo H Alonso

    2006-01-01

    Full Text Available Este trabajo analiza la relevancia que tiene el proceso de información que vincula a las empresas con el mercado financiero y de capitales en particular. Además entrega evidencia empírica recogida en el mercado argentino sobre el impacto de factores específicos de las empresas respecto de la información revelada al mercado y en el comportamiento de las cotizaciones. A partir de la aplicación de un índice que mide la información que las empresas suministran voluntariamente al mercado, y mediante análisis de correlación y regresión, se logra soporte adicional sobre relaciones directas entre características propias de las empresas y el nivel de información que suministran. Los resultados muestran que existe una relación inversa entre información revelada y volatilidad propia de las acciones en el mercado argentino.This study analyzes the relevance of the informational process linking enterprises with financial , and particularly with capital, markets. Empirical evidence is also presented which was gathered in the Argentinean market on the impact of specific factors on enterprises in relation to discretionary information revealed to the market, as well the impact on the behavior of quotations. Based on the application of an index which measures the level of discretionary information that enterprises provide the market, and by correlation and regression analyses, additional support is obtained for direct relations among particular characteristics of the enterprises and the levels of information which they provide. The results show that there is an inverse relation between information revealed and the specific volatility of company shares in the Argentinean market .

  9. El smartphone como herramienta de estudios de mercado : Identificación de factores tecnológicos, de estudio de mercado y de uso personal para la creación de apps

    OpenAIRE

    Bonet Cos, Eduard

    2015-01-01

    En un contexto cada vez más digital e interconectado, la necesidad de reinventar las técnicas tradicionales de investigación de mercados se hace evidente. Aunque ciertos tipos de estudios de mercado online ya son herramientas consolidadas desde hace tiempo, como el cuestionario web, la industria necesita seguir innovando. El reciente auge de los teléfonos inteligentes o smartphones abre nuevas posibilidades en el sector de la investigación de mercados: la capacidad de geolocalización, la inme...

  10. Composición, estructura y diversidad del cerro El Águila, Michoacán, México Composition, structure and diversity of the cerro El Águila, Michoacán, Mexico

    Directory of Open Access Journals (Sweden)

    Luis Eduardo Zacarias-Eslava

    2011-09-01

    Full Text Available Se describe la composición, estructura y diversidad de la vegetación presente en el cerro El Águila, Michoacán. Se reconocieron fisonómicamente 5 tipos de vegetación y en cada uno se establecieron 16 parcelas circulares de 400 m² (3.2 ha para censar los individuos leñosos ≥ 10 cm d.a.p., con una parcela anidada de 100 m² (0.8 ha para los individuos entre 2.5 y 9.9 cm d.a.p. El muestreo incluyó 46 especies agrupadas en 33 géneros y 21 familias. Los bosques tropical caducifolio y de Quercus deserticola tuvieron los valores más bajos de altura promedio ( 11 m y área basal (> 40 m²/ha. La diversidad fue mayor en el bosque tropical caducifolio (S=23 y α =5.4 y menor en el de Quercus-Pinus (S= 13 y α= 2.71. En general, los tipos de vegetación mostraron diferentes especies dominantes y una alta diversidad beta. La composición y estructura de estas comunidades puede asociarse a cambios en altitud y a la perturbación por actividades humanas. No obstante, la zona de estudio aún presenta áreas en buen estado de conservación, particularmente los bosques templados hacia las zonas con mayor altitud, por lo que se sugiere que en un futuro cercano sea incluida dentro de alguna categoría de protección estatal.This study describes composition, structure and diversity of vegetation in the Cerro El Águila, Michoacán. Five plant communities were recognized and for each one all woody individuals ≥10 cm DBH were tallied in sixteen 400 m² circular plots, whereas individuals between 2.5 and 9.9 cm DBH were measured in a 100 m² circular sub-plot centered within each larger plot. A total of 46 species, 33 genera and 21 families were recorded. The tropical deciduous forest and Quercus deserticola forest had low values of mean plant height ( 11 m and basal area (> 40 m²/ha. Diversity was greater in the tropical deciduous forest (S= 23 and α= 5.4, respectively and lower in the oak-pine forest (S= 13 and α= 2.71. All communities displayed

  11. HMV Ingenieros Ltda : un modelo de internacionalización para entrar en el mercado Triángulo Norte

    OpenAIRE

    Marín Cadavid, Carolina

    2012-01-01

    Esta investigación por medio de un estudio de caso estudia el proceso de internacionalización que debería seguir HMV ingenieros Ltda, con el objetivo de ingresar en el mercado Triángulo Norte. Un paso a paso es el modelo que debe llevarse a cabo como guía para incursionar en dicho mercado. Con la experiencia de HMV Ingenieros Ltda, se concluye que presenta una fortaleza para establecer presencia comercial (modo 3) en el mercado de Triángulo Norte. Adicionalmente acorde con las tendencias de l...

  12. Análisis del mercado eléctrico: desde generación hasta comercialización

    OpenAIRE

    Colás Elizalde, Mikel

    2016-01-01

    El objetivo de este trabajo es analizar el sector eléctrico. El análisis incluye una detallada descripción de los principales agentes que interactúan en el sector (generación, transporte, distribución y comercialización), las principales características competitivas del mercado y los principales determinantes del precio de la electricidad. El mercado eléctrico es complejo y todos los actores involucrados tienen problemas económicos que dificultan el análisis. No es un mercado c...

  13. Aplicación del mercado de carbono en pequeñas centrales hidroeléctricas

    OpenAIRE

    Duque Grisales, Eduardo Alexander

    2014-01-01

    Con la creación del Protocolo de Kioto se introdujo en la sociedad una nueva preocupación acerca de la necesidad de limitar la cantidad de emisiones de Gases de Efecto Invernadero (GEI). Esta preocupación ha llevado a la creación de un nuevo mercado: el Mercado de Carbono, escenario a través del cual se desea crear un precio común para este elemento. En este mercado se otorga un tipo de bonos llamados “certificados de reducción de emisiones” (CERs) a los proyectos que por su actividad reducen...

  14. Vulnerabilidad del mercado nacional del maíz (Zea mays L.) ante cambios exógenos internacionales

    OpenAIRE

    González Rojas, Karina

    2010-01-01

    El aumento de las importaciones de maíz (Zea mays L.), la reciente liberación comercial y la actual crisis energética global, pone en situación de vulnerabilidad al mercado nacional del grano. Para cuantificar los efectos que pudieran tener cambios exógenos internacionales en el mercado de maíz en México se formuló un modelo Armington para el año promedio 2004/2006. Los resultados obtenidos indican que el mercado nacional de maíz es vulnerable a cambios en la oferta y demanda mundial. Una red...

  15. La importancia de la inteligencia de mercados en la actividad exportadora de las empresas españolas

    OpenAIRE

    Navarro-García, Antonio; Barrera-Barrera, Ramón; Peris-Ortiz, Marta

    2013-01-01

    El objetivo de la presente investigación es responder al gap investigador existente en la literatura sobre el rol que juega la inteligencia de mercados en la actividad exportadora. Específicamente se pretende conocer los efectos que ejerce la inteligencia de mercados en las interrelaciones entre las distancias de mercados (doméstico vs. extranjeros) percibidas por los responsables de exportación, las decisiones estratégicas de marketing mix (estandarización vs. adaptación) y el...

  16. La invisibilidad de las condiciones laborales y de salud de niños del mercado felipe ángeles

    OpenAIRE

    Orozco Valerio, María de Jesús; Baez Baez, Laura; Méndez Magaña, Ana Cecilia; Celis, Alfredo

    2012-01-01

    Objetivo Identifi car las condiciones de trabajo y salud de los menores que trabajan en el mercado Felipe Ángeles de la Ciudad de Guadalajara. Metodología Se realizó un estudio descriptivo a 198 menores de 18 años de edad que desempeñaban alguna actividad laboral en dicho mercado. Se aplicó una encuesta que incluía variables sociodemográfi cas de los menores, de condiciones del trabajo y de salud. Resultados Los menores de que laboran en este mercado son principalmente hombres (89,9 %) con ed...

  17. A CRISE DA BOLSA DE VALORES CHINESA: UMA ANÁLISE DOS EFEITOS SOBRE MERCADOS ACIONÁRIOS INTERNACIONAIS

    OpenAIRE

    Antônio André Cunha Callado; Aldo Leonardo Cunha Callado; Carla Renata Silva Leitão

    2014-01-01

    Estudos de eventos têm sido amplamente utilizados para investigar a Hipótese dos Mercados Eficientes tem sido amplamente investigada ao longo das últimas duas décadas. O artigo tem como objetivo investigar a reação de índices de diversos mercados acionários ao evento na Bolsa de Valores da China em fevereiro de 2007. Para a realização do estudo foram utilizados 12 índices pertencentes a diversos mercados acionários (Alemanha, Argentina, Austrália, Brasil, Estados Unidos, França, Hong Kong, Ín...

  18. O mercado de carbono no contexto da União Europeia : um caso português

    OpenAIRE

    Cavaleiro, João António Quintela

    2011-01-01

    O presente estudo apresenta os seguintes objectivos de investigação: i) identificar os conceitos de economia ambiental por detrás do mercado de carbono e explicitar esta opção como uma das estratégias possíveis de controlo ambiental; ii) compreender como está a ser estabelecido e regulado o mercado de carbono no seio da União Europeia, em especial em Portugal; iii) identificar as percepções de um dos principais operadores do mercado de carbono em Portugal, a EDP. As metodologias utilizadas na...

  19. La invisibilidad de las condiciones laborales y de salud de niños del mercado Felipe Ángeles

    OpenAIRE

    María de Jesús Orozco-Valerio; María G. Laura-Báez; Ana C. Méndez-Magaña; Alfredo Celis de la Rosa

    2012-01-01

    Objetivo Identificar las condiciones de trabajo y salud de los menores que trabajan en el mercado Felipe Ángeles de la Ciudad de Guadalajara. Metodología Se realizó un estudio descriptivo a 198 menores de 18 años de edad que desempeñaban alguna actividad laboral en dicho mercado. Se aplicó una encuesta que incluía variables sociodemográfi cas de los menores, de condiciones del trabajo y de salud. Resultados Los menores de que laboran en este mercado son principalmente hombres (89,9 %) con eda...

  20. The rules of urban planning and administrative responsibilities in protecting to the vulnerability and risk of Cerro Tapezco in Santa Ana

    International Nuclear Information System (INIS)

    An analysis of regulation is made of land use and administrative management of the Cerro Tapezco to show that as the years have passed it has been verified that the Costa Rican law on town planning has been inadequate for current problems due to lack of updating of various scientific and technical sources also dispersion and proliferation of competences of administrative authorities. The physical setting and planning rules is identified for CerroTapezco and surrounding towns. Local actions are explored in the elaboration of improvement and reform of the regulatory plan of Santa Ana. The administrative entities and institutions with competence in the development and implementation of plans have been identified, assessing deficiencies, inconsistencies and administrative omissions in urban planning of the city of Santa Ana and recommending changes necessary for the proper application of the Costa Rican law

  1. Caracterización arqueométrica de cerámicas ibéricas de los yacimientos de Alarcos y El Cerro de las Cabezas

    OpenAIRE

    Guirao Polo, David

    2014-01-01

    En la presente Tesis Doctoral se han analizado arqueométricamente 146 fragmentos de cerámicas de época ibérica procedentes de los yacimientos del Cerro de Alarcos (Ciudad Real) y de El Cerro de las Cabezas (Valdepeñas, Ciudad Real). A partir del análisis químico-estadístico, mineralógico, térmico y microscópico, se ha identificado la existencia de grupos cerámicos, con características propias e identificativas, que deben vincularse a la producción cerámica de uno y otro poblado. El establecim...

  2. Evaluation of the Cerro Solo nuclear ore, province of Chubut. Geological characteristics of the deposit and of the basin. Pt. 2

    International Nuclear Information System (INIS)

    The Cerro Solo uranium ore deposit, is located 420 km west from Trelew city, Chubut province, in the extra-andean. The geologic environment belongs to the northwest edge portion of the intracratonic San Jorge Gulf Basin. The uraniferous district is named Pichinanes Ridge district. The mineralization lies 25 to 130 m depth, and is hosted by Los Adobes formation aged Aptian-Albian, made up by conglomerates, sandstones, coarse-sandstones and less abundant siltstones and claystones. The Cerro Solo ore deposit that belongs to the sandstone type-uranium occurrences are lenticular or tabular shaped, associated with organic material and pyrite, generally roughly parallel to the bedding (Trend-Type). The uranium minerals are uraninite and coffinite associated with organic material and pyrite, and frequently hematite, goethite, calcite, siderite and barite are observed. (Author)

  3. Effects of the Cerro Grande Fire (Smoke and Fallout Ash) on Soil Chemical Properties Within and Around Los Alamos National Laboratory

    Energy Technology Data Exchange (ETDEWEB)

    Fresquez, P.R.; Velasquez, W.R.; Naranjo, L. Jr.

    2000-11-01

    Soil surface (0- to 2-in. depth) samples were collected from areas within and around Los Alamos National Laboratory (LANL) just after the Cerro Grande fire, analyzed for radionuclides, radioactivity, and trace elements (heavy metals), and compared to soil samples collected in 1999 from the same sites. In addition, many types of organic substances (volatile and semivolatile organic compounds, organochlorine pesticides, polychlorinated biphenyls, high explosives, and dioxin and dioxin-like compounds) were assessed in soils from LANL, perimeter, and regional sites after the fire. Results show that impacts to regional, perimeter, and on-site (mesa top) areas from smoke and fallout ash as a result of the Cerro Grande fire were minimal.

  4. Two-phase characteristics of the feeding fluid of Cerro Prieto IV wells (Mexico) obtained by gas equilibrium; Caracteristicas bifasicas del fluido de alimentacion de pozos de Cerro Prieto IV (Mexico), obtenidas por equilibrio gaseoso

    Energy Technology Data Exchange (ETDEWEB)

    Barragan-Reyes, Rosa Maria; Arellano-Gomez, Victor Manuel; Portugal-Marin, Enrique [Instituto de Investigaciones Electricas (Mexico); De Leon-Vivar, Jesus [Comision Federal de Electricidad, Residencia General de Cerro Prieto, B.C (Mexico)

    2008-10-15

    The gas composition of fluids produced by CP IV geothermal wells from the Cerro Prieto field was studied in order to identify different types of fluids entering the wells by estimating their temperature and excess steam. A method based on the Fischer Tropsch reaction and H2S equilibrium with pyrite-pyrrhotite as mineral buffer (FTHSH3) was used. The results for the reservoir natural state indicated the presence of fluids with heterogeneous reservoir temperature (between 275 and 310 degrees Celsius) and excess steam values, which were found from negative (boiled liquid that has lost steam when flowing to the well) to one (steam phase with zero liquid saturation). The study for individual wells in which boiling processes were identified, showed that through time, the feeding fluids consist of a two-phase mixture with different liquid/steam proportions. Also, the results suggested that a steam phase could occur at CP IV which is added to the feeding fluid, depending on the operation conditions of the wells. The origin of this steam could be the boiling of the deeper liquid due to a pressure drop. [Spanish] Se estudio la composicion gaseosa de los fluidos producidos por pozos geotermicos del sector CP IV del campo de Cerro Prieto para tratar de distinguir aportes de fluidos diferentes mediante la estimacion de su temperatura de yacimiento y del exceso de vapor. Se utilizo un metodo de equilibrio gaseoso basado en la reaccion de Fischer Tropsch y el equilibrio combinado pirita-pirrotita (FT-HSH3). Los resultados obtenidos indican que en el estado inicial del yacimiento existen fluidos que muestran heterogeneidad en los valores de temperatura de yacimiento (entre 275 y 310 grados Celsius), asi como en el exceso de vapor con valores desde negativos (liquido que despues de ebullir ha perdido vapor en su trayecto hacia el pozo) hasta uno (vapor con cero saturacion de liquido). El estudio individual de los pozos con fenomenos de ebullicion muestra que a traves del tiempo

  5. Geological and production analyses focused on exploration of the eastern part of the Cerro Prieto geothermal field, BC; Analisis geologico-productivo enfocado a la exploracion de la parte oriental del campo geotermico de Cerro Prieto, BC

    Energy Technology Data Exchange (ETDEWEB)

    Aguilar Dumas, Alvaro [Comision Federal de Electricidad, Residencia General de Cerro Prieto, B.C (Mexico)]. E-mail: alvaro.aguilar@cfe.gob.mx

    2008-01-15

    The eastern part of the Cerro Prieto geothermal field (CGCP), known as Poligono Nuevo Leon, is an area with proven geothermal resources, as confirmed by seven directional wells located toward the east and by vertical well M-200 located inside the polygon. Well M-200 was drilled in 1984 and has produced about 4 million tons of steam to date. It is integrated into the CP-2 sector, producing 68 t/h of steam. Presently the eastern part of CGCP, representing 25% of the total field area, is producing over half of the steam for the entire field. In the last few years, the steam has come only after increasing the number of production wells located in the eastern zone of CGCP (Rodriguez, 2006), where pressure, enthalpy and temperature conditions are better than in other parts of the field. However in the long term it will be necessary to incorporate Poligono Nuevo Leon into the productive area to expand the productive life of CGCP. This paper includes a geological analysis, plus models for steam production, temperature and enthalpy for Poligono Nuevo Leon. [Spanish] La parte oriental del Campo Geotermico de Cerro Prieto (CGCP), conocida como Poligono Nuevo Leon, representa una area potencial con recursos geotermicos comprobados, lo que demuestran siete pozos direccionales que se han perforado hacia el este, asi como el pozo vertical M-200, localizado dentro del poligono. El pozo M-200 se perforo en 1984 y ha producido a la fecha alrededor de 4 millones de toneladas de vapor, estando integrado al sector CP-2 una produccion de 68 t/h de vapor. Actualmente la parte oriental del CGCP, que representa el 25% del area total del campo, produce mas de la mitad del total de vapor del campo. El suministro de vapor en los ultimos anos se ha logrado cubrir aumentando el numero de pozos en operacion localizados en la zona oriente del CGCP (Rodriguez, 2006), ya que es aqui donde hay condiciones de presion, entalpia y temperatura del yacimiento que son mejores que en otras areas del campo

  6. Studies for recovering injection capacity in wells of the Cerro Prieto, BC, geothermal field; Estudios para recuperar la capacidad de aceptacion en pozos inyectores del campo geotermico de Cerro Prieto, BC

    Energy Technology Data Exchange (ETDEWEB)

    Alvarez Rosales, Julio [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia General de Cerro Prieto, Mexicali, Baja California (Mexico)]. E-mail: julio.alvarez@cfe.gob.mx

    2010-01-15

    As in geothermal fields around the world, at Cerro Prieto geothermal field, Baja California, former exploratory and production wells are used to inject residual brine. Since the 1980s, studies and activities have been carried out to find ways to recharge the reservoir and dispose of brine without harming the environment or underground aquifers. These include infiltration and cold-and-hot injection. Some of the studies are presented here, including analyses of litho-facies; core samples; pressure, temperature and spinner logs; well tests and injection rates-plus some studies on the shallow aquifer. All have been useful in fulfilling requirements made by environmental authorities. Because injection rates constantly decrease due to formation damage, it is proposed an additional technique be used to reduce such damages and prolong the lifetime of cold-and-hot injection wells-while ensuring the environment and shallow aquifers are not affected. [Spanish] Al igual que en diversos campos geotermicos en el mundo, en el de Cerro Prieto, Baja California se han utilizado tanto pozos inyectores perforados ex profeso como antiguos pozos exploratorios y productores para inyectar el fluido residual al subsuelo. Desde la decada de los 80 se han realizado diversos estudios y acciones en ese campo geotermico para recargar al yacimiento y para disponer del fluido residual, sin ocasionar danos al ambiente ni a los cuerpos hidricos del subsuelo, que van desde la infiltracion hasta la inyeccion en frio y en caliente. Este articulo presenta los diferentes estudios realizados con ese objetivo en el campo, incluyendo el analisis de litofacies, de nucleos de formacion, de registros de presion, temperatura y spinner, las pruebas en pozos y analisis de tasas de aceptacion, asi como los efectuados en el acuifero superficial. Todos ellos han sido de utilidad para atender los requerimientos de las autoridades ambientales. Finalmente, y en virtud de que las tasas de aceptacion de los pozos

  7. Estudio petrográfico de las facies piroclásticas de la Formación Cerro Varela en el sur de la Sierra de San Luis Petrographic study of the pyroclastic facies of the Cerro Varela Formation in the south of the Sierra de San Luis

    Directory of Open Access Journals (Sweden)

    Amancay N. Martínez

    2010-11-01

    Full Text Available En la provincia de San Luis, existen tres sub-cuencas denominadas Las Salinas, Beazley y Mercedes. Estas cuencas corresponden a depocentros de rift elongados en sentido NO, que alojan rocas ígneas de edad triásica con espesores que llegan hasta los 4.000 metros. Las rocas ígneas de la Formación Cerro Varela forman parte del cerro homónimo que constituye los últimos asomos australes de la sierra de San Luis. Las riolitas triásicas que afloran en la sierra de Varela se disponen dentro de un esquema estructural extensional asociado a la formación de cuencas de tipo rift. Las unidades analizadas de la Formación Cerro Varela están compuestas por tobas cristalinas tanto de alto grado como de bajo grado de soldadura, de composición riolítica e interpretadas como depósitos originados por flujos piroclásticos. Por su litología, edad y contexto regional, las rocas de la Formación Cerro Varela integran el magmatismo gondwánico del Grupo Choiyoi de edad permotriásica de la Cordillera Frontal de Mendoza y San Juan.In the San Luis province, there are three sub-basins called Las Salinas, Beazley and Mercedes. These basins correspond to elongated rift depocenter with a NO orientation that host Triassic igneous rocks with thicknesses that reach 4,000 meters. The igneous rocks from Cerro Varela Formation, part of the homonym hill, is the last vestige of the southern Sierra San Luis. The Triassic rhyolites that crop up in the sierra de Varela, are placed within a structural pattern associated with the formation of extensional basins. Crystal tuffs of Cerro Varela are corresponds to tuffs with high and low degree of welding, of rhyolitic composition and interpreted as pyroclastic deposits. For its lithology, age and regional context, the rocks of the Cerro Varela Formation integrate the Gondwanic magmatism of Permo-Triassic age, related to the Choiyoi Group of the Cordillera Frontal of Mendoza and San Juan.

  8. Growth of a Large Composite Magma System: the EJB Pluton, Eastern California.

    Science.gov (United States)

    Matty, D. J.; Vervoort, J.; Dufrane, A.; Hart, G.; Student, J.; Morgan, S.

    2008-12-01

    The composite EJB pluton crops out in the White-Inyo Mountains of eastern California, and comprises the Eureka Valley monzonite (EVM), the Joshua Flat quartz monzonite (JFQM), the Beer Creek granite (BCG), and an unnamed diorite. While sometimes equivocal, field relationships suggest that the EVM was emplaced first, followed by the JFQM, and finally the BCG; the diorite predates the BCG. Sylvester and others (GSAB, 1978) reported zircon U-Pb ages of 179±2 Ma for the EVM and 174±5 Ma for the JFQM. Coleman and others (GSAB, 2003) determined a U-Pb age of 179±3 Ma (via Pb-loss trajectory) for the BCG. Because of the uncertainty in the ages and ambiguous field relations, the sequence and duration of EJB magmatism remain unclear. To understand more fully the timing of EJB magmatism, we separated zircons from 12 samples collected from each of the main EJB units. These samples were characterized using light microscopy, SEM and CL techniques. U-Pb ages were determined from individual zircons by LA-ICP-MS following the method of Chang and others (G3, 2006). For the ages reported below, the reported uncertainties are based on factors within the analysis, but do not include external factors such as sample/standard bias or other matrix effects. Overall uncertainty in LA-ICPMS U-Pb geochronology is hard to assess, but we estimate that all ages reported below are subject to a minimum 2% uncertainty. We determined a concordant U-Pb age of 180±2 Ma for the EVM, which agrees with the results of Sylvester and others (1978). The unnamed diorite produced a concordant U-Pb age of 177±3 Ma. Concordant U-Pb ages of 172±2, 172±3, 173±2, 174±2, and 175±2 Ma were determined for individual samples of the JFQM and agree with the age reported by Sylvester and others (1978) of 174±5 Ma. Concordant U-Pb ages of 168±4, 168±3, 169±1, 172±2, and 172±2 Ma were determined for individual BCG samples. Within the reported error, there is no difference in age between individual samples of

  9. Pucarilla-Cerro Tipillas volcanic complex: the oldest recognized caldera in the southeastern portion of central volcanic zone of Central Andes?

    International Nuclear Information System (INIS)

    We recognize the most eastern and oldest collapse caldera structure in the southern portion of the Central Volcanic Zone of the Andes. A description of Middle-Upper Miocene successions related to explosive- effusive events is presented. The location of this centre close to Cerro Galn Caldera attests a recurrence in the volcanism between 12 and 2 Ma in this portion of the Altiplano - Puna Plateau.

  10. Moche social boundaries and settlement dynamics at Cerro Castillo (c. AD 600-1000), Nepeña Valley, Peru Volume 1

    OpenAIRE

    Rengifo, Carlos

    2014-01-01

    This dissertation explores the pre-Columbian occupation at Cerro Castillo, a coastal settlement in the Nepeña Valley, Peru. The study examines the site’s internal organisation as well as its relationship with regional cultural phenomena during its most important period of occupation (circa AD 600-1000). Characterising the Moche presence at the site is one of the main subjects of this investigation. Moche was one of the grandest civilisations that developed in the pre-Columbian ...

  11. Cerro Grande Fire Impact to Water Quality and Stream Flow near Los Alamos National Laboratory: Results of Four Years of Monitoring

    Energy Technology Data Exchange (ETDEWEB)

    B.M. Gallaher; R.J. Koch

    2004-09-15

    In May 2000, the Cerro Grande fire burned about 7400 acres of mixed conifer forest on the Los Alamos National Laboratory (LANL), and much of the 10,000 acres of mountainside draining onto LANL was severely burned. The resulting burned landscapes raised concerns of increased storm runoff and transport of contaminants by runoff in the canyons traversing LANL. The first storms after the fire produced runoff peaks that were more than 200 times greater than prefire levels. Total runoff volume for the year 2000 increased 50% over prefire years, despite a decline in total precipitation of 13% below normal and a general decrease in the number of monsoonal thunderstorms. The majority of runoff in 2000 occurred in the canyons at LANL south of Pueblo Canyon (70%), where the highest runoff volume occurred in Water Canyon and the peak discharge occurred in Pajarito Canyon. This report describes the observed effects of the Cerro Grande fire and related environmental impacts to watersheds at and near Los Alamos National Laboratory (LANL) for the first four runoff seasons after the fire, from 2000 through 2003. Spatial and temporal trends in radiological and chemical constituents that were identified as being associated with the Cerro Grande fire and those that were identified as being associated with historic LANL discharges are evaluated with regard to impacts to the Rio Grande and area reservoirs downstream of LANL. The results of environmental sampling performed by LANL, the New Mexico Environment Department (NMED), and U.S. Geological Survey (USGS) after the Cerro Grande fire are included in the evaluation. Effects are described for storm runoff, baseflow, stream sediments, and area regional reservoir sediment.

  12. Pucarilla-Cerro Tipillas volcanic complex: the oldest recognized caldera in the southeastern portion of central volcanic zone of Central Andes?

    Energy Technology Data Exchange (ETDEWEB)

    Guzman, Silvina; Petrinovic, Ivan [CONICET -IBIGEO. Museo de Cs. Naturales, Universidad de Salta, Mendoza 2 (4400), Salta (Argentina)], E-mail: guzmansilvina@gmail.com

    2008-10-01

    We recognize the most eastern and oldest collapse caldera structure in the southern portion of the Central Volcanic Zone of the Andes. A description of Middle-Upper Miocene successions related to explosive- effusive events is presented. The location of this centre close to Cerro Galn Caldera attests a recurrence in the volcanism between 12 and 2 Ma in this portion of the Altiplano - Puna Plateau.

  13. Report about drilling works made in 13 Anomaly de Taylor and in the N- NE of its, around Fraile Muerto (Cerro Largo district): Uranium project

    International Nuclear Information System (INIS)

    The perforations were carried out to investigate in depth denominated anomaly 13 detected during the Taylor Mission (1975) and extended the punch area of study during you are suitable DINAMIGE-BRGM (Project the present report details the activities realised in the environs Fraile Muerto (Cerro Largo district) by the command team of perforations of the uranium project. Previously and contemporarily to the executed works, prospection became geophysical ground geochemistry geology and, works. (Uranium)

  14. Death Valley turtlebacks: Mesozoic contractional structures overprinted by Cenozoic extension and metamorphism beneath syn-extensional plutons

    International Nuclear Information System (INIS)

    The term turtleback was first coined to describe the curvilinear fault surfaces that produced a distinctive geomorphic form in the Black Mountains east of Death Valley, and although it was decades before their full significance was appreciated, they remain one of the most distinctive features of the extensional structure of the Death Valley region. Historically the interpretation of the features has varied markedly, and misconceptions about their character continue to abound, including descriptions in popular field guides for the area. It the 1990's, however, the full history of the systems began to be apparent from several key data: 1) the dating of the plutonic assemblage associated with the turtlebacks demonstrated that late Miocene, syn-extensional plutonism was fundamental to their formation; 2) the plutonic assemblage forms an intrusive sheet structurally above the turtlebacks, indicating a tie between much of the high grade metamorphism and Cenozoic plutonism; 3) a modern analog for the syn-extensional plutonism in the Black Mountains was recognized beneath Death Valley with the imaging of a mid-crustal magma body; 4) the Neogene structural history was worked out in the turtlebacks showing that folding of early-formed shear zones formed the turtleback anticlinoria but overprinting by brittle faults produced the final form as they cut obliquely across the older structure; and 5) the pre-extensional structural history was clarified, demonstrating that Mesozoic basement-involved thrust systems are present within the turtlebacks, but have been overprinted by the extensional system. An unresolved issue is the significance of Eocene U-Pb dates for pegmatites within the region, but presumably these relate somehow to the pre-extensional history. Miller and Pavlis (2005; E. Sci. Rev.) reviewed many features of the turtlebacks, and our working model for the region is that the turtlebacks originated as mid-crustal ductile-thrust systems within the Cordilleran fold

  15. Investigación del mercado industrial con el fin de desarrollar soluciones de poliuretano para el mercado Ibérico

    OpenAIRE

    Ruiz Peceño, Miguel Javier

    2014-01-01

    El siguiente proyecto consiste en el estudio, evaluación y el desarrollo de varios sectores del mercado industrial Ibérico y Europeo con el fin de identificar oportunidades de crecimiento mediante el desarrollo e implementación de nuevos productos y soluciones. En colaboración con el equipo Técnico Comercial y el departamento de Marketing & Sales se llevó a cabo el proyecto en el negocio de Formulated Systems de The Dow Chemical Company. Dow Formulated Systems se encarga del desarrollo y come...

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

    International Nuclear Information System (INIS)

    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 km2), 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

  17. Geologic and hydrologic controls on the economic potential of hydrothermal systems associated with upper crustal plutons

    Science.gov (United States)

    Weis, Philipp; Driesner, Thomas; Scott, Samuel; Lecumberri-Sanchez, Pilar

    2016-04-01

    Heat and mass transport in hydrothermal systems associated with upper crustal magmatic intrusions can result in resources with large economic potential (Kesler, 1994). Active hydrothermal systems can form high-enthalpy geothermal reservoirs with the possibility for renewable energy production. Fossil continental or submarine hydrothermal systems may have formed ore deposits at variable crustal depths, which can be mined near today's surface with an economic profit. In both cases, only the right combination of first-order geologic and hydrologic controls may lead to the formation of a significant resource. To foster exploration for these hydrothermal georesources, we need to improve our understanding of subsurface fluxes of mass and energy by combining numerical process modelling, observations at both active and fossil systems, as well as knowledge of fluid and rock properties and their interactions in natural systems. The presentation will highlight the role of non-linear fluid properties, phase separation, salt precipitation, fluid mixing, permeability structure, hydraulic fracturing and the transition from brittle to ductile rock behavior as major geologic and hydrologic controls on the formation of high-enthalpy and supercritical geothermal resources (Scott et al., 2015), and magmatic-hydrothermal mineral resources, such as porphyry copper, massive sulfide and epithermal gold deposits (Lecumberri-Sanchez et al., 2015; Weis, 2015). References: Kesler, S. E., 1994: Mineral Resources, economics and the environment, New York, McMillan, 391. Lecumberri-Sanchez, P., Steele-MacInnis, M., Weis, P., Driesner, T., Bodnar, R.J. (2015): Salt precipitation in magmatic-hydrothermal systems associated with upper crustal plutons. Geology, v. 43, p. 1063-1066, doi:10.1130/G37163.1 Scott, S., Driesner, T., Weis, P. (2015): Geologic controls on supercritical geothermal resources above magmatic intrusions. Nature Communications, 6:7837 doi: 10.1038/ncomms8837 Weis, P. (2015): The

  18. Evaluación integral del riesgo volcánico del Cerro Machín, Colombia

    Directory of Open Access Journals (Sweden)

    Leonel Vega Mora

    2013-01-01

    Full Text Available El volcán Cerro Machín (VCM se encuentra situado en la Cordillera Central de Colombia. Por la com- posición química, magnitud y extensión de sus erupciones pasadas, se reconoce como un volcán explosivo de gran potencial de daño, cuya actividad futura podría afectar intensamente durante mucho tiempo (meses hasta años una región muy estratégica para la economía del país, que cubre áreas pertenecientes a los departamentos de Tolima, Quindío, Valle del Cauca y Cundinamarca, en las cuales habitan cerca de un millón de personas. En este artículo se muestra la metodología y resultados del estudio de “Evaluación Integral del Riesgo del Cerro Machín – Colombia”, realizado durante 2009 por el Grupo PIGA de Investigación en Política, Información y Gestión Ambiental de la Facultad de Ingeniería de la Universidad Nacional de Colombia, tomando como punto de partida el estudio de “Evaluación de la Amenaza Volcánica Potencial del Cerro Machín” adelantado en el 2002 por el Servicio Geológico Colombiano (SGC. En consecuencia, se genera y ajusta una nueva ecuación para la determinación del riesgo, basada en la valoración de índices de amenaza intrínseca e índices de vulnerabilidad, los primeros en función del grado de intensidad, duración, extensión y acumulación de las amenazas, y los segundos, en función del grado de exposición espacial y temporal de los elementos (sociales, económicos, institucionales y ecosisté- micos y de su capacidad de respuesta intrínseca y extrínseca ante las amenazas. Con estas ecuaciones y mediante el uso de sistemas de información geográfica (SIG, se realiza para cada escenario de análisis considerando la modelación geoespacial del riesgo a nivel de cada pixel cartográfico del área territorial de estudio. En esta modelación se integra toda la informa- ción territorial del área en estudio, lo que permite obtener, de acuerdo con el marco lógico de evaluación preestablecido

  19. Paradigmas del mercado financiero rural en países en desarrollo

    Directory of Open Access Journals (Sweden)

    Luis Alberto Fuentes Méndez

    2006-12-01

    Full Text Available Este artículo tiene como objetivos i analizar los paradigmas que explican el funcionamiento del mercado financiero rural en los países en desarrollo y ii evaluar los resultados de las políticas públicas asociadas a cada paradigma en el acceso a los servicios financieros de las familias rurales pobres. El paradigma de las Instituciones Especializadas de Crédito Agrícola señala que, ante las fallas del mercado de crédito en las que los prestamistas informales monopolizan el mercado con tasas de interés de usura y las organizaciones financieras formales no ofrecen suficientes recursos financieros para el desarrollo, el Estado debe intervenir para garantizar el acceso al crédito. Las políticas derivadas son creación de organizaciones públicas especializadas, subsidiar la tasa de interés activa y regular la banca pública y privada para que destine parte de su cartera de créditos al financiamiento agrícola. El paradigma de los Mercados Financieros propone que un mercado sin regulaciones se acerca al modelo de competencia perfecta y por lo tanto sugiere la no intervención del Estado en su funcionamiento para lograr la máxima eficiencia económica. Este paradigma incluye entre sus políticas liberar las tasas de interés, eliminar las carteras de crédito obligatorias y liquidar las organizaciones públicas de financiamiento. El paradigma de la Información Imperfecta señala que el funcionamiento eficiente y equitativo del mercado financiero se basa en el diseño de instituciones y organizaciones que evadan los problemas generados por la existencia de fallas de información (problemas de evaluación, de incentivos y de reembolso. En el marco de este paradigma las organizaciones de financiamiento rural deben diseñar y aplicar tecnologías que aprovechen las experiencias positivas del sector financiero informal y formal, para mejorar la forma en que se capta, procesa y transmite información entre prestatarios y prestamistas y as

  20. Análisis litoestratigráfico de la Formación Cerro Azul (Mioceno Superior en la provincia de La Pampa

    Directory of Open Access Journals (Sweden)

    Graciela Visconti

    2010-10-01

    Full Text Available La Formación Cerro Azul fue definida en 1980 para incluir a las sedimentitas continentales pliocenas (limolitas arenosas y areniscas limosas que afloran de manera discontinua en casi todo el ámbito de la provincia de La Pampa. No obstante, varias investigaciones paleontológicas realizadas a partir de la segunda mitad de la década del 80' han permitido ubicar geocronológicamente a la unidad en el intervalo 10 Ma a 5,8-5,7 Ma. El objetivo del trabajo es realizar un análisis de las características litoestratigráficas de la Formación Cerro Azul de acuerdo al Código Argentino de Estratigrafía. Se propone un lectoestratotipo para la unidad, consistente en el perfil de Algarrobo del Águila y un perfil auxiliar en cerro El Morro. También se establecieron las relaciones estratigráficas con otras formaciones. Se interpreta un paleoambiente depositacional de llanura, donde alternan depósitos de loess con numerosos paleosuelos, detectándose escasos depósitos lacustres en la base y pocos cursos fluviales.

  1. Geographic Information System (GIS) Emergency Support for the May 2000 Cerro Grande Wildfire, Los Alamos, New Mexico, USA

    Energy Technology Data Exchange (ETDEWEB)

    C.R.Mynard; G.N.Keating; P.M.Rich; D.R. Bleakly

    2003-05-01

    In May 2000 the Cerro Grande wildfire swept through Los Alamos, New Mexico, burning approximately 17,400 ha (43,000 acres) and causing evacuation of Los Alamos National Laboratory (LANL) and the communities of Los Alamos and White Rock. An integral part of emergency response during the fire was the use of geographic information system (GIS) technology, which continues to be used in support of post-fire restoration and environmental monitoring. During the fire Laboratory GIS staff and volunteers from other organizations worked to produce maps and provide support for emergency managers, including at an emergency GIS facility in Santa Fe. Subsequent to the fire, Laboratory GIS teams supported the multiagency Burned Area Emergency Rehabilitation (BAER) team to provide GIS data and maps for planning mitigation efforts. The GIS teams continue to help researchers, operations personnel, and managers deal with the tremendous changes caused by the fire. Much of the work is under the auspices of the Cerro Grande Rehabilitation Project (CGRP) to promote recovery from fire damage, improve information exchange, enhance emergency management, and conduct mitigation activities. GIS efforts during the fire provided important lessons about institutional matters, working relationships, and emergency preparedness. These lessons include the importance of (1) an integrated framework for assessing natural and human hazards in a landscape context; (2) a strong GIS capability for emergency response; (3) coordinated emergency plans for GIS operations; (4) a method for employees to report their whereabouts and receive authoritative information during an evacuation; (5) GIS data that are complete, backed-up, and available during an emergency; (6) adaptation of GIS to the circumstances of the emergency; (7) better coordination in the GIS community; (8) better integration of GIS into LANL operations; and (9) a central data warehouse for data and metadata. These lessons are important for planning

  2. Estructura, composición y diversidad de la selva baja caducifolia del Cerro Verde, Nizanda (Oaxaca, México

    Directory of Open Access Journals (Sweden)

    José Antonio Gallardo Cruz

    2005-01-01

    Full Text Available En este estudio se describe la estructura, la composición florística y los patrones de diversidad de la selva baja caducifolia del Cerro Verde, localizado en Nizanda (Istmo de Tehuantepec, Oaxaca, México. En 30 parcelas de 100 m2 se censaron las plantas leñosas con DAP ≥ 1 cm (estrato alto, y en cinco subcuadros de 4 m2 dentro de cada una se censaron las plantas con DAP 30 cm (estrato bajo. Se encontraron 194 especies distribuidas en 52 familias. La riqueza de especies fue idéntica en ambos estratos (145 especies, y cada uno aportó de manera exclusiva ca. 25% de la riqueza total registrada. Leguminosae fue la familia más rica en especies (27, seguida por Asteraceae (20 y Euphorbiaceae (18. Las especies más frecuentes fueron Bursera simaruba + B. aff. cinerea (no distinguidas en el campo, Euphorbia schlechtendalii, Pilosocereus collinsii y Capparis verrucosa. La riqueza específica promedio por cuadro fue de 30 especies. Los índices basados en la riqueza y la abundancia de las especies (Berger-Parker = 0.20; Simpson = 0.09; α de Fisher = 9.47; Shannon = 2.78; equitatividad = 0.82 indican una alta diversidad y una consecuente baja dominancia en esta selva. Los valores extrapolados mostraron una densidad total (estratos alto + bajo de 23,950 ind. ha-1 (830 ind. ha-1 con DAP ≥ 10 cm, una cobertura de 446.7%, y un área basal de 53 m2 ha-1. La altura promedio del 10% de los árboles más altos fue 9.1 m. La estructura de la selva baja del Cerro Verde es semejante a la de otras comunidades vegetales del trópico seco de México y denota un buen estado de conservación. Este hecho, aunado a su particular composición florística, enfatiza la pertinencia de su conservación formal.

  3. O mercado dos detergentes máquina roupa : a pressão promocional

    OpenAIRE

    Róis, Marta Alexandra Grangeiro

    2012-01-01

    Projecto de Mestrado em Economia da Empresa e da Concorrência / Classificação JEL: L81, Q51 O presente estudo tem como objetivo principal analisar a evolução da pressão promocional no mercado dos detergentes máquina roupa, com especial ênfase no canal dinâmico. Para tal foi utilizado o modelo de análise estrutural proposto por Porter (1980), mais conhecido pelo modelo das cinco forças. Com base na informação disponível sobre o mercado foram analisadas as cinco forças das quais foi possí...

  4. Flexibilidad y precarización del mercado de trabajo en México

    Directory of Open Access Journals (Sweden)

    César Armando Salazar

    2014-01-01

    Full Text Available Después del abandono del concepto de “pleno empleo” durante la década de 1970, se ha adoptado la idea de una “tasa de desempleo no acelerado de inflación” (NAIRU. A partir de la misma se ha argumentado que la inexistencia de flexibilidad en el mercado de trabajo es lo que propicia una falta de oferta adecuada. A partir de la argumentación económica ortodoxa se estima que la aplicación de medidas de flexibilidad, como la eliminación de las instituciones reguladoras del factor trabajo, propiciarían una mayor oferta y calidad en el mercado laboral, lo cual no se ha cumplido en el modelo neoliberal.

  5. Mercado de servicios de ajustes del sistema eléctrico : propuestas de mejora

    OpenAIRE

    Justo Rojas, Elisa María

    2013-01-01

    En general, el modelo de mercado eléctrico español y la regulación han fomentado la garantía de suministro de energía eléctrica y su calidad, no obstante la mayor parte del diseño del mismo responde al contexto energético que existía en 1998. En los últimos años se han registrado una serie de cambios importantes que han modificado el escenario y el funcionamiento del mercado eléctrico, como son una importante penetración de las energías renovables no gestionables, la incorporac...

  6. Uma nova realidade do mercado de gás natural : modelo e os processos

    OpenAIRE

    Dias, Raquel Alexandra Guerra

    2010-01-01

    Mestrado em Ciências Empresariais O Gás Natural, como utility que é, constitui uma fonte energética fundamental no panorama energético de qualquer país. Nos últimos anos, o mercado de GN tem vindo a sofrer algumas alterações significativas a nível estrutural, nomeadamente, através da imposição da Directiva Comunitária da União Europeia 98/30/CE, de 2 de Junho de 2008. A referida Directiva estabeleceu regras quanto à liberalização do Mercado. O documento irá centrar a sua análise no conjunt...

  7. Cultura alfabética y mercado cultural en Colombia y en España

    Directory of Open Access Journals (Sweden)

    Ancízar Narváez

    2010-01-01

    Full Text Available En el presente artículo se establece una comparación entre la oferta y la demanda de cultura alfabética a través de la descripción de los sistemas educativos; así mismo, se compararan la oferta y el consumo mediáticos a través de la descripción de los sistemas mediáticos de Colombia y España. Con estos insumos, se intenta establecer las características del mercado cultural en cada uno de los dos países y sus posibilidades de inserción en el mercado global del conocimiento.

  8. A análise do mercado turístico

    OpenAIRE

    Martínez Roget, Fidel

    2013-01-01

    Esta unidade didáctica forma parte da materia «Impacto Económico do Turismo Urbano» que se imparte no primeiro semestre, dentro do máster universitario en Turismo Urbano e Xestión de Empresas Turísticas. Con esta materia preténdese iniciar aos estudantes na análise do impacto económico xerado polo turismo en áreas sub-nacionais, en concreto, en destinos urbanos. Para isto, nunha primeira parte, estúdanse os dous elementos básicos dun mercado, neste caso do mercado turístico, é dicir, a de...

  9. ¿Por qué y cómo regular el mercado educativo?

    OpenAIRE

    Christian Maroy

    2008-01-01

    Desde hace más de una década, las políticas educativas de numerosos países tienden a ampliar las posibilidades de elección de la escuela por parte de los padres, ya sea promoviendo una lógica "cuasi-mercado", o flexibilizando la carte scolaire. Este artículo da cuenta de los debates científicos sobre los efectos de esta promoción del mercado sobre la segregación y desigualdades. Más allá de las controversias en la literatura, parece que la combinación de la elección de los padr...

  10. Frutos y semillas medicinales vendidas en plazas de mercado de Bogotá, Colombia

    Directory of Open Access Journals (Sweden)

    Valderrama-Rincón Natalia María

    2005-12-01

    Full Text Available Se realizó el inventario de los frutos y semillas mediante encuestas semiestructuradas a cerca del uso medicinal y la caracterización de los vendedores, en siete plazas de mercado de Bogotá. Se emplearon técnicas etnobotánicas cuantitativas para determinar la validación social de la información. Se registraron 54 posibles especies pertenecientes a 29 familias y 45 géneros; además, fueron recopilados 80 nombres comunes. Se registraron 33 especies en fruto, 20 en semillas y solo una especie fue comercializada como fruto y semilla. Se establecieron dos tipos de
    plazas de mercado y se crearon cuatro grupos de frutos y semillas medicinales de acuerdo a los índices utilizados.

  11. Segmentação dos mercados nos centros hípicos

    OpenAIRE

    Martins, António Carlos Pereira Rico

    2014-01-01

    O setor equestre e o cavalo desde cedo que acompanham a história de Portugal, mas é um setor com poucos estudos económicos. O presente estudo foca-se nos centros hípicos e estabelece como objetivo geral identificar segmentos de mercado ao nível do público-alvo dos centros hípicos e como objetivos específicos, identificar os critérios e variáveis de segmentação e caracterizar os elementos que compõem cada segmento. O estudo apresenta a fundamentação teórica sobre a segmentação de mercado, p...

  12. Valoración del mercado bursátil basado en percepciones subjetivas

    OpenAIRE

    Rodríguez Castillo, Javier

    2009-01-01

    El proyecto que a continuación voy a exponer trata de ver si la percepción del público sobre la economía (medida en su percepción de las portadas de los periódicos) es un indicador del mercado de valores. La motivación para realizar este proyecto viene de la afición y curiosidad que tengo acerca del mercado de valores y la gran relación existente entre la inversión en bolsa y la estadística, permitiéndome esta última la posibilidad de poder presentar este estudio como proyecto fin de carrera....

  13. ESPECULAÇÃO E ARBITRAGEM NO MERCADO BRASILEIRO DE CÂMBIO FUTURO

    OpenAIRE

    Pedro Rossi

    2014-01-01

    Esse artigo propõe uma metodologia para tratar da formação da taxa de câmbio real/dólar com base na identificação das categorias de agentes responsáveis pela arbitragem e pela especulação no mercado futuro. A análise desenvolvida identifica a correlação entre a posição de câmbio de grupos de agentes na BM&F e a variação cambial no intervalo de um mês. Os resultados encontrados são compatíveis com a hipótese de que os estrangeiros e investidores institucionais formam tendências no mercado de c...

  14. Mercados eficientes e arbitragem: um estudo sob o enfoque das finanças comportamentais

    OpenAIRE

    Tarcísio Saraiva Rabelo Junior; Ricardo Hirata Ikeda

    2004-01-01

    A Hipótese dos Mercados Eficientes (HME) tem se mostrado uma das mais influentes teorias no campo das finanças, sendo base para inúmeros modelos de precificação de ativos, com aplicações que vão desde modelos tradicionais utilizados em Finanças Corporativas até avançadas teorias utilizadas na identificação do preço "justo" de derivativos financeiros. Um dos pilares da HME é a possibilidade da arbitragem como mecanismo de correção de possíveis desvios que o mercado possa sofrer de sua forma ef...

  15. Empleo público en el ejército y el mercado de trabajo

    OpenAIRE

    San Clemente Zúñiga, Ignacio

    2014-01-01

    Este Trabajo de Fin de Grado (TFG), pretende analizar el mercado laboral en el Ejército Español, para ello analizaremos los flujos de entrada en dicho mercado, es decir, las plazas que se convocan cada año, en concreto, para la escala de Tropa y Marinería de las Fuerzas Armadas Españolas y las solicitudes que se presentan para dichas plazas. También se analizará el número de componentes actuales de la escala de Tropa y Marinería, y lo analizaremos comparándolos con la población española y con...

  16. A CRISE DA BOLSA DE VALORES CHINESA: UMA ANÁLISE DOS EFEITOS SOBRE MERCADOS ACIONÁRIOS INTERNACIONAIS

    Directory of Open Access Journals (Sweden)

    Antônio André Cunha Callado

    2014-04-01

    Full Text Available Estudos de eventos têm sido amplamente utilizados para investigar a Hipótese dos Mercados Eficientes tem sido amplamente investigada ao longo das últimas duas décadas. O artigo tem como objetivo investigar a reação de índices de diversos mercados acionários ao evento na Bolsa de Valores da China em fevereiro de 2007. Para a realização do estudo foram utilizados 12 índices pertencentes a diversos mercados acionários (Alemanha, Argentina, Austrália, Brasil, Estados Unidos, França, Hong Kong, Índia, Indonésia, Inglaterra, Japão e México. Os procedimentos referentes ao delineamento do estudo consideraram a definição da janela de tempo, bem como os procedimentos inerentes a um estudo de evento para realçar alterações no comportamento dos retornos dos índices de mercado e investigar a ocorrência de retornos anormais acumulados. Os resultados obtidos demonstram evidências inerentes à reação de alguns dos mercados acionários investigados em relação ao evento ocorrido na Bolsa chinesa. A queda dos Índices de Performance de Sharpe observada em todos os índices de mercado investigados revelam evidências que corroboram o impacto significativo e sistemático decorrente da queda ocorrida no mercado acionário chinês. Este resultado sugere que a importância relativa da China no cenário internacional dos mercados de capitais não deve ser subestimada.

  17. O mercado de luxo e o marketing holístico: o caso dos hotéis de luxo

    OpenAIRE

    Filipe, S.; Simões, D.

    2014-01-01

    No atual contexto económico de crise, o mercado de luxo conseguiu cresceu, porque muitos dos clientes de luxo mantêm o poder financeiro e conservam a sua ambição por luxo. No entanto, num mercado caracterizado por intensa concorrência não é suficiente ter uma marca forte, é imprescindível acrescentar valor e o marketing holístico pode contribuir fortemente para esse resultado. Nesse sentido, o objetivo de...

  18. Relationship between oxosilicate niobium mineralization and organic matter in alkaline pegmatites of the Khibiny pluton, Kola Peninsula

    Science.gov (United States)

    Chukanov, N. V.; Pekov, I. V.; Perepelitsina, E. O.; Ermolaeva, V. N.; Vozchikova, S. A.

    2010-12-01

    In alkaline pegmatites of the Khibiny pluton niobium oxosilicates with (Nb + Ti)/Si ≥ 1 and Nb > Ti occur in intimate fine intergrowths with endogenic organic matter, which makes it possible to assume a genetic relationship between them. Such intergrowths from pegmatites of Mounts Kukisvumchorr and Koashva have been studied by electron microscopy, electron microprobe, IR spectroscopy, and exclusion chromatography. Unsaturated hydrocarbon groups, including aromatic ones, and carboxylate groups are prevalent in the organic matter intergrown with the niobium oxosilicates. The molecular weight distribution in the part of the bitumen soluble in tetrahydrofurane is polymodal, probably due to its formation as a result of parallel reactions on several catalytic centers of polymerization.

  19. Oxygen isotope geochemistry of a potassic porphyritic calc-alkalic composite pluton: the Itaporanga batholith, state of Paraiba, Northeastern Brazil

    International Nuclear Information System (INIS)

    The composite porphyritic, potassic calc-alkaline Itaporanga batholith was intruded between the metasediments of the Cachoeirinha-Salgueiro groups and the gneisses of the basement, in the western portion of the State of Paraiba, Northeastern Brazil. The close interaction of mafic (potassium diorite) with felsic porphyritic rocks (quartz monzonite to granite) forming hybrid ones (monzonite to granodiorite) developed migmatite-like structures (stromatic and, less often, agmatic) suggesting coexistence and mixing of magmas as a major process during the evolution of this pluton. Quartz, known for its resistence to weathering and subsequent oxygen isotope exchange, was used to compare the δ18O values among these rocks. (author)

  20. Structural characterization of the Misajé granitic pluton (NW Cameroon): constraints from magnetic and field observations

    Science.gov (United States)

    Fozing, Eric Martial; Njanko, Théophile; Naba, Séta; Kwékam, Maurice; Njonfang, Emmanuel; Rochette, Pierre

    2015-12-01

    The Misajé granitic pluton, emplaced between 569 and 560 Ma in an amphibolitic and gneissic host rock, comprises four petrographic units namely biotite-hornblende granite (BHG), granodiorite (Gd), biotite granite (BG), and leucocratic granite (LG). Four major tectonic events have been described in the studied area: a D1-early tectonic event, responsible of the E-W flat foliation which has been progressively transposed by a D2 tectonic event. A D2 event has developed heterogeneous simple shear in a dextral transpressive context with moderate to strong dipping NE-SW striking foliation; a D3 tectonic event has lead to a sinistral N-S ductile shear characterized by N- to ENE-striking foliation and E-W strike-slip shear corridors and a D4 tectonic event that developed N-S dextral ductile strike-slip deformation. The magnetic study of the pluton, based on the AMS parameters, reveals the coexistence of both paramagnetic (dominated by iron-bearing silicates; 54 % of sites) and ferromagnetic (due to the occurrence of PSD and MD grains of magnetite or other ferromagnetic minerals; 46 % of sites) behaviors. Magnetic foliation shows best poles at 55/82 for the whole pluton, 95/32 in BHG, and 273/83 in BG, and the magnetic lineation trends are mostly NNE-SSW with best lines at 210/8, 198/19, and 36/3, respectively. The trend of the magnetic lineation in BG indicates an S-shape trajectory, suggesting a sinistral sense of shear motion along discrete E-W corridors situated at the northern and southern ends. Kinematic indicators in BG point to a sinistral sense of shear, suggesting its emplacement during the D3 event. The close relationship between K 1 and K 3 points to a syn-kinematic emplacement and crystallization of the Misajé granitic pluton during the Pan-African event, and the tectonic evolution of the study area is considered to be coeval with the tectonic evolution of the trans-Saharan Pan-African belt of eastern Nigeria.