Sample records for prima facie nature

  1. Prima Facie Questions in Quantum Gravity

    Isham, C J


    The long history of the study of quantum gravity has thrown up a complex web of ideas and approaches. The aim of this article is to unravel this web a little by analysing some of the {\\em prima facie\\/} questions that can be asked of almost any approach to quantum gravity and whose answers assist in classifying the different schemes. Particular emphasis is placed on (i) the role of background conceptual and technical structure; (ii) the role of spacetime diffeomorphisms; and (iii) the problem of time.

  2. Gene alterations at Drosophila inversion breakpoints provide prima facie evidence for natural selection as an explanation for rapid chromosomal evolution.

    Guillén, Yolanda; Ruiz, Alfredo


    Chromosomal inversions have been pervasive during the evolution of the genus Drosophila, but there is significant variation between lineages in the rate of rearrangement fixation. D. mojavensis, an ecological specialist adapted to a cactophilic niche under extreme desert conditions, is a chromosomally derived species with ten fixed inversions, five of them not present in any other species. In order to explore the causes of the rapid chromosomal evolution in D. mojavensis, we identified and characterized all breakpoints of seven inversions fixed in chromosome 2, the most dynamic one. One of the inversions presents unequivocal evidence for its generation by ectopic recombination between transposon copies and another two harbor inverted duplications of non-repetitive DNA at the two breakpoints and were likely generated by staggered single-strand breaks and repair by non-homologous end joining. Four out of 14 breakpoints lay in the intergenic region between preexisting duplicated genes, suggesting an adaptive advantage of separating previously tightly linked duplicates. Four out of 14 breakpoints are associated with transposed genes, suggesting these breakpoints are fragile regions. Finally two inversions contain novel genes at their breakpoints and another three show alterations of genes at breakpoints with potential adaptive significance. D. mojavensis chromosomal inversions were generated by multiple mechanisms, an observation that does not provide support for increased mutation rate as explanation for rapid chromosomal evolution. On the other hand, we have found a number of gene alterations at the breakpoints with putative adaptive consequences that directly point to natural selection as the cause of D. mojavensis rapid chromosomal evolution.

  3. Gene alterations at Drosophila inversion breakpoints provide prima facie evidence for natural selection as an explanation for rapid chromosomal evolution

    Guillén Yolanda


    Full Text Available Abstract Background Chromosomal inversions have been pervasive during the evolution of the genus Drosophila, but there is significant variation between lineages in the rate of rearrangement fixation. D. mojavensis, an ecological specialist adapted to a cactophilic niche under extreme desert conditions, is a chromosomally derived species with ten fixed inversions, five of them not present in any other species. Results In order to explore the causes of the rapid chromosomal evolution in D. mojavensis, we identified and characterized all breakpoints of seven inversions fixed in chromosome 2, the most dynamic one. One of the inversions presents unequivocal evidence for its generation by ectopic recombination between transposon copies and another two harbor inverted duplications of non-repetitive DNA at the two breakpoints and were likely generated by staggered single-strand breaks and repair by non-homologous end joining. Four out of 14 breakpoints lay in the intergenic region between preexisting duplicated genes, suggesting an adaptive advantage of separating previously tightly linked duplicates. Four out of 14 breakpoints are associated with transposed genes, suggesting these breakpoints are fragile regions. Finally two inversions contain novel genes at their breakpoints and another three show alterations of genes at breakpoints with potential adaptive significance. Conclusions D. mojavensis chromosomal inversions were generated by multiple mechanisms, an observation that does not provide support for increased mutation rate as explanation for rapid chromosomal evolution. On the other hand, we have found a number of gene alterations at the breakpoints with putative adaptive consequences that directly point to natural selection as the cause of D. mojavensis rapid chromosomal evolution.

  4. In defence of moral imperialism: four equal and universal prima facie principles.

    Dawson, A; Garrard, E


    Raanan Gillon is a noted defender of the four principles approach to healthcare ethics. His general position has always been that these principles are to be considered to be both universal and prima facie in nature. In recent work, however, he has made two claims that seem to present difficulties for this view. His first claim is that one of these four principles, respect for autonomy, has a special position in relation to the others: he holds that it is first among equals. We argue that this claim makes little sense if the principles are to retain their prima facie nature. His second claim is that cultural variation can play an independent normative role in the construction of our moral judgments. This, he argues, enables us to occupy a middle ground between what he sees as the twin pitfalls of moral relativism and (what he calls) moral imperialism. We argue that there is no such middle ground, and while Gillon ultimately seems committed to relativism, it is some form of moral imperialism (in the form of moral objectivism) that will provide the only satisfactory construal of the four principles as prima facie universal moral principles.

  5. Getting to First Base: Prima Facie Arguments for Propositions of Value.

    Tuman, Joseph S.


    Argues that few clear standards exist for value debate. Defines values as instrumental or terminal, and identifies four prima facie burdens necessary for affirming a value resolution: value identification; value criteria; value hierarchy; and topicality through relevance. Examines the role of presumption and burden of proof in value debate. (MM)

  6. Objective justification and Prima Facie anti-competitive unilateral conduct : an exploration of EU Law and beyond

    Vijver, Tjarda Desiderius Oscar van der


    The prohibition of anti-competitive unilateral conduct by firms with market power is not absolute, but allows for derogation. For the purposes of EU law, the ECJ has accepted that a so-called ‘objective justification’ plea may be invoked in the case of a prima facie abuse of dominance. Even though t

  7. 直觉主义伦理中的显见义务论%Ross' View on the Prima Facie Duty



    直觉主义伦理学家罗斯试图通过提出显见义务论来解决道德冲突问题。显见义务就是正确的、有约束力的、应该被履行的、没有与之竞争的义务。在遇有道德冲突时,由于显见义务不证自明的特性,人们凭直觉就可以直接知道应该履行哪一种义务。然而,由于作为显见义务及其基础——直觉本身的缺陷,显见义务论并没有达到它解决道德冲突的目的。%Ross, a scholar of intuitionalist ethics, tried to settle the moral conflict by bringing forward the view of prima facie duty. The prima facie duty is the right, promissory, ought to be performed, no-competitive duty. Due to the self-evidence of the prima facie duty, the people can know directly to ought to perform which duty by intuition as meeting the moral conflict. However, the prima facie duty has not reached its goal of settling the moral conflict because of the drawbacks of it and its foundation--the intuition itself.

  8. Nature and origin of fluids in granulite facies metamorphism

    Newton, R. C.


    The various models for the nature and origin of fluids in granulite facies metamorphism were summarized. Field and petrologic evidence exists for both fluid-absent and fluid-present deep crustal metamorphism. The South Indian granulite province is often cited as a fluid-rich example. The fluids must have been low in H2O and thus high in CO2. Deep crustal and subcrustal sources of CO2 are as yet unproven possibilities. There is much recent discussion of the possible ways in which deep crustal melts and fluids could have interacted in granulite metamorphism. Possible explanations for the characteristically low activity of H2O associated with granulite terranes were discussed. Granulites of the Adirondacks, New York, show evidence for vapor-absent conditions, and thus appear different from those of South India, for which CO2 streaming was proposed. Several features, such as the presence of high-density CO2 fluid inclusions, that may be misleading as evidence for CO2-saturated conditions during metamorphism, were discussed.

  9. Genetic Types of Meter-Scale Cyclic Sequences and Fabric Natures of Facies Succession


    Different genetic types of meter-scale cyclic sequences in stratigraphic records result from episodic accumulation of strata related to Milankovitch cycles. The distinctive fabric natures of facies succession result from the sedimentation governed by different sediment sources and sedimentary dynamic conditions in different paleogeographical backgrounds, corresponding to high-frequency sea-level changes. Naturally, this is the fundamental criterion for the classification of genetic types of meter-scale cyclic sequences. The widespread development in stratigraphic records and the regular vertical stacking patterns in long-term sequences, the evolution characters of earth history and the genetic types reflected by specific fabric natures of facies successions in different paleogeographical settings, all that show meterscale cyclic sequences are not only the elementary working units in stratigraphy and sedimentology, but also the replenishment and extension of parasequence of sequence stratigraphy. Two genetic kinds of facies succession for meter-scale cyclic sequence in neritic-facies strata of carbonate and clastic rocks, are normal grading succession mainly formed by tidal sedimentation and inverse grading succession chiefly made by wave sedimentation, and both of them constitute generally shallowing upward succession, the thickness of which ranges from several tens of centimeters to several meters. The classification of genetic types of meter-scale cyclic sequence could be made in terms of the fabric natures of facies succession, and carbonate meter-scale cyclic sequences could be divided into four types: L-M type, deep-water asymmetrical type, subtidal type and peritidal type. Clastic meter-scale cyclic sequences could be grouped into two types: tidal-dynamic type and wave-dynamic type. The boundaries of meter-scale cyclic sequences are marked by instantaneous punctuated surface formed by non-deposition resulting from high-frequency level changes, which include

  10. Seismic facies; Facies sismicas

    Johann, Paulo Roberto Schroeder [PETROBRAS, Rio de Janeiro, RJ (Brazil). Exploracao e Producao Corporativo. Gerencia de Reservas e Reservatorios]. E-mail:


    The method presented herein describes the seismic facies as representations of curves and vertical matrixes of the lithotypes proportions. The seismic facies are greatly interested in capturing the spatial distributions (3D) of regionalized variables, as for example, lithotypes, sedimentary facies groups and/ or porosity and/or other properties of the reservoirs and integrate them into the 3D geological modeling (Johann, 1997). Thus when interpreted as curves or vertical matrixes of proportions, seismic facies allow us to build a very important tool for structural analysis of regionalized variables. The matrixes have an important application in geostatistical modeling. In addition, this approach provides results about the depth and scale of the wells profiles, that is, seismic data is integrated to the characterization of reservoirs in depth maps and in high resolution maps. The link between the different necessary technical phases involved in the classification of the segments of seismic traces is described herein in groups of predefined traces of two approaches: a) not supervised and b) supervised by the geological knowledge available on the studied reservoir. The multivariate statistical methods used to obtain the maps of the seismic facies units are interesting tools to be used to provide a lithostratigraphic and petrophysical understanding of a petroleum reservoir. In the case studied these seismic facies units are interpreted as representative of the depositional system as a part of the Namorado Turbiditic System, Namorado Field, Campos Basin.Within the scope of PRAVAP 19 (Programa Estrategico de Recuperacao Avancada de Petroleo - Strategic Program of Advanced Petroleum Recovery) some research work on algorithms is underway to select new optimized attributes to apply seismic facies. One example is the extraction of attributes based on the wavelet transformation and on the time-frequency analysis methodology. PRAVAP is also carrying out research work on an

  11. Facies-controlled compositions of petroleum and natural gas in Zechstein carbonates in eastern Germany

    Wehner, H.; Gerling, P. (Bundesanstalt fur Geowissenschaften und Rohstoiffe, Hannover (Germany)); Muller, E.P.; Bleschert, K.H. (Erdol Erdgas Gommern GmbH, Gommern (Germany))


    Petroleum and natural gas are produced from the Stassfurt carbonate (Zechstein 2) at the northern and southern margins of the Zechstein basin in eastern Germany. The following facies types can be distinguished at the basin margins: basin, slope, shelf margin (including carbonate sandbars), sabkha, and lagoon. Especially the high-energy carbonates (grainstones and packstones) of the islands on the shelf and, locally, the carbonate sandbars are considered to be excellent pore reservoirs. The paleomorphological traps are formed by Zechstein salt several hundred meters thick. Suprahydrostatic pressures are common in the traps. The oils are characterized by relatively low concentrations of diasteranes, relatively high biomarker concentrations, and a prevalence of even-numbered n-alkanes. This indicates a moderately mature carbonate source rock. The biomarker patterns and isotope ratios of the oil differ, however, providing an indication of the organic precursor material and the sedimentation environment. The Zechstein 2 source rock samples usually contained less than 0.3% total organic carbon; a maximum of 1.65% was measured. The extractable organic material was determined to have a moderate maturity; the [delta][sup 13]C values of the kerogens are between -25.8 and -24.4$, and the biomarkers indicate a carbonate matrix. On the north side of the Zechstein basin, the oils show a good correlation with the analyzed source rocks. One the south side, only the oils from the sandbar and slope areas correlate with Zechstein 2 source rocks. Source rocks from lagoonal environments are apparently characterized by another organic facies. The associated gases contain considerable nitrogen (17-68 vol.%); CO[sub 2] concentrations lie below 1%. The carbon and hydrogen isotope ratios of the hydrocarbons in these gases are typical of gases associated with oils from marine source rocks. On the basis of their isotope values, the genesis of the nitrogen and CO[sub 2] will be discussed.

  12. Prima Vista toob pargiraamatukogu


    5. ja 6. mail 2005 toimub teine Tartu kirjandusfestival "Prima Vista". Avatakse pargiraamatukogu, kus esinevad 5. mail Jürgen Rooste, Merca, Aapo Ilves, Peep Ilmet, Marko Martinson, Jüri Kaldmaa, Jaan Pehk

  13. UHT granulite-facies metamorphism in Rogaland, S Norway, is polyphase in nature

    Laurent, Antonin; Duchene, Stéphanie; Bingen, Bernard; Seydoux-Guillaume, Anne-Magali; Bosse, Valérie


    Propensity of metamorphic assemblages to remain metastable after melt extraction complicates singularly the petrologist's task to discriminate between a single granulite-facies P-T path and a polyphase one. Using an integrated petrological and in-situ geochronological approach in key rock-samples, we reconstruct the pressure-temperature-time path of Sveconorwegian metamorphism across a 30 km-wide metamorphic gradient ranging from upper amphibolite facies to ultra-high temperature (UHT) granulite-facies in Rogaland, S. Norway. Thermodynamic modelling of phase equilibria in the Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O-Ti2O-O2 chemical system (PerpleX code) are carried out with an emphasis on moderately oxidized, spinel-bearing assemblages resulting from either garnet or sapphirine breakdown. Geochronological U-(Th)-Pb data acquired on both monazite (LA-ICP-MS) and zircon (SIMS) are complemented by minor- and trace-elements signatures of both minerals, to monitor REE distribution through time and to evaluate garnet apparition or demise. Coupling field, petrological and geochronological data lead to a polyphase metamorphic history, lasting about 100 My. The onset of regional granulite facies metamorphism at 1035 Ma is associated with the emplacement of large volumes of granitic magmas in the amphibolite to granulite facies transition zone. In the deeper part of the crustal section, localized sapphirine-bearing restitic lithologies testify to UHT temperatures (900-920 °C). These conditions were reached at ca. 1010 Ma following a tight clockwise P-T path associated with minor exhumation (7 to 5.5 kbar) and subsequent cooling to 700 °C. A distinct thermal episode, initiated at ca. 950 Ma, reached UHT granulite-facies conditions with the intrusion of massif-type anorthosite plutons at ca. 930 Ma producing a 5-km wide aureole. The aureole is delimited by the presence of osumilite in high Fe-Al rocks yielding quantitative estimates of 900-950 °C at a maximum pressure of 5 kbar

  14. Laulvad kirjanikud Prima Vistal


    Kirjandusfestivalist Prima Vista 8.-11. maini Tartus ja laulvate kirjanike kontsertidest: 9. mail Tõnu Trubetsky kontsert ansambliga The Flovers of Romance, 10. mail Villu Tamme, Mathura, Lauri Sommer, Kaarel B. Väljamäe, Andreas Kalkuni, Kauksi Ülle, Merca ja Aapo Ilves

  15. Laulvad kirjanikud Prima Vistal


    Kirjandusfestivalist Prima Vista 8.-11. maini Tartus ja laulvate kirjanike kontsertidest: 9. mail Tõnu Trubetsky kontsert ansambliga The Flovers of Romance, 10. mail Villu Tamme, Mathura, Lauri Sommer, Kaarel B. Väljamäe, Andreas Kalkuni, Kauksi Ülle, Merca ja Aapo Ilves

  16. Pennsylvanian coniferopsid forests in sabkha facies reveal the nature of seasonal tropical biome

    Falcon-Lang, H. J.; Jud, N.A.; John, Nelson W.; DiMichele, W.A.; Chaney, D.S.; Lucas, S.G.


    Pennsylvanian fossil forests are known from hundreds of sites across tropical Pangea, but nearly all comprise remains of humid Coal Forests. Here we report a unique occurrence of seasonally dry vegetation, preserved in growth position along >5 km of strike, in the Pennsylvanian (early Kasimovian, Missourian) of New Mexico (United States). Analyses of stump anatomy, diameter, and spatial density, coupled with observations of vascular traces and associated megaflora, show that this was a deciduous, mixed-age, coniferopsid woodland (~100 trees per hectare) with an open canopy. The coniferopsids colonized coastal sabkha facies and show tree rings, confirming growth under seasonally dry conditions. Such woodlands probably served as the source of coniferopsids that replaced Coal Forests farther east in central Pangea during drier climate phases. Thus, the newly discovered woodland helps unravel biome-scale vegetation dynamics and allows calibration of climate models. ?? 2011 Geological Society of America.

  17. Diane Di Prima

    Livingston, McKenzie


    Diane di Prima was one of the few female Beat writers, but she was just as prolific as her male contemporaries. Her writing style reflected the social upheavals of the day - like the other Beats, she dabbled in stream of consciousness and spontaneous prose, but gradually moved to more structured verse, like Haiku, published in 1967. She experimented heavily with form and diction to set herself apart from the male poets - exemplified in her epic poem, Loba. Her early texts focused heavily on p...

  18. Prima Power Virtual Machine


    Opinnäytetyön tavoitteena oli rakentaa toimiva yhteys Visual Components 3DCreate -simulointiohjelman ja Beckhoff TwinCAT 3 -ohjauksen välille. Tavoitteena oli yhteyden avulla ohjata Prima Power SGe6 -levyntyöstökoneen 3D-simulointimallia fyysisen SGe6-koneen ohjauksella. Työn toimeksiantajana toimi Kauhavalla sijaitseva Finn-Power Oy. Virtuaalikonetta tullaan hyödyntämään virtuaalisessa koulutus- ja testausympäristössä. Työssä oli kartoitettava mitä virtuaalikoneen valmistamiseen vaaditaa...

  19. Philosophia prima como repraesentatio na filosofia natural de Hobbes: exame de fundamentos metafísico-cognitivos como complementos teóricos de seu materialismo mecanicista

    Cláudio R. C. Leivas


    Full Text Available O ponto de partida da Philosophia prima de Hobbes tem como referência a Física e a Metafísica de Aristóteles. O desenvolvimento posterior de sua Philosophia prima, porém, põe em marcha uma crítica da metafísica aristotélica que conduzirá a um remanejamentoteórico de uma série de princípios e conceitos herdados da tradição. Considerada em seu conjunto, a filosofia primeira hobbesiana é constituída por uma definição ampla, isto é, a metafísica definida como ciência do ente enquanto ente (ao invés da clássica definição de ciência do ser enquanto ser, sobre a qual duas definições strictu sensu são erigidas: a metafísica como física geral - dizer o ente (ens é dizer o corpo (corpus - e a metafísica como representação. Este paper é um esforço no sentido de compreender essas e outras questões concernentes aos estudos hobbesianos sobre a forma como conhecemos o mundo, as coisas e nós mesmos.

  20. Carbon isotope characteristics, origin and distribution of the natural gases from the Tertiary salty lacustrine facies in the West Depression Region in the Qaidam Basin

    张晓宝; 胡勇; 马立元; 孟自芳; 段毅; 周世新; 彭德华


    The Tertiary in the West Depression Region of the Qaidam Basin has the typical inland salty lacustrine deposits in China. 34 natural gas samples were collected from 13 oil fields in the West Depression Region in the basin, the chemical compositions and carbon isotopes of methane, ethane, propane, and butane were measured. According to the carbon isotope characteristics of natural gases in combination with geochemical characteristics of the source rocks and crude oils, the natural gases can be divided into sapropelic associated gas, mixed organic matter-derived associated gas, coal-derived gas and mixed gas. The carbon isotope characteristics, origin and distribution of the natural gases are considered to be related with the types and distribution of organic inputs in lake environments with different salinities. The lake salinity can regionally forecast the distribution of the different genetic types of natural gas. Compared with the different genetic types of natural gas from other Chinese basins, the carbon isotopes of the heavy hydrocarbons of the natural gas from the Tertiary salt lacustrine facies in the Qaidam Basin are extremely heavier. Therefore, this should be considered when natural gases are genetically classified in the basin.

  1. PRIMA-X Final Report

    Lorenz, Daniel [German Research School for Simulation Sciences GmbH, Aachen (Germany); Wolf, Felix [German Research School for Simulation Sciences GmbH, Aachen (Germany)


    The PRIMA-X (Performance Retargeting of Instrumentation, Measurement, and Analysis Technologies for Exascale Computing) project is the successor of the DOE PRIMA (Performance Refactoring of Instrumentation, Measurement, and Analysis Technologies for Petascale Computing) project, which addressed the challenge of creating a core measurement infrastructure that would serve as a common platform for both integrating leading parallel performance systems (notably TAU and Scalasca) and developing next-generation scalable performance tools. The PRIMA-X project shifts the focus away from refactorization of robust performance tools towards a re-targeting of the parallel performance measurement and analysis architecture for extreme scales. The massive concurrency, asynchronous execution dynamics, hardware heterogeneity, and multi-objective prerequisites (performance, power, resilience) that identify exascale systems introduce fundamental constraints on the ability to carry forward existing performance methodologies. In particular, there must be a deemphasis of per-thread observation techniques to significantly reduce the otherwise unsustainable flood of redundant performance data. Instead, it will be necessary to assimilate multi-level resource observations into macroscopic performance views, from which resilient performance metrics can be attributed to the computational features of the application. This requires a scalable framework for node-level and system-wide monitoring and runtime analyses of dynamic performance information. Also, the interest in optimizing parallelism parameters with respect to performance and energy drives the integration of tool capabilities in the exascale environment further. Initially, PRIMA-X was a collaborative project between the University of Oregon (lead institution) and the German Research School for Simulation Sciences (GRS). Because Prof. Wolf, the PI at GRS, accepted a position as full professor at Technische Universität Darmstadt (TU

  2. Production of mullite from natural raw materials using mechanical activation; Obtencao de mulita a partir de materias-primas naturais utilizando ativacao mecanica

    Feitosa, G.; Pinheiro, D.G.; Chinelatto, A.L.; Chinelatto, A.S.A [Universidade Estadual de Ponta Grossa (UEPG), PR (Brazil). Programa de Pos-Graduacao em Engenharia e Ciencia de Materiais


    Mullite, ceramic structure consisting by alumina and silica, is present in different ceramic industry, as refractory, white ceramic, titles and advanced ceramics. This is because this material presents high resistance mechanical and high resistance in high temperatures, beyond low expansion coefficients and thermal conductivity. On the other hand, the mullite production needs high temperatures. This work had as objective the production of mullite from natural raw materials, using mechanical activation. Bauxite and quartz had been mixed in the stoichiometric composition and the mixture was submitted to high energy milling for different times. Then non milled powders and milled powders had been sintered in different temperatures. The characterization was made by X Ray diffraction and scanning electronic microscopy. The results demonstrated that the high energy milling affects the mullite formation, decreasing the temperature in that it is formed. (author)

  3. The PRIMA Fringe Sensor Unit

    Sahlmann, Johannes; Abuter, Roberto; Accardo, Matteo; Mottini, Sergio; Delplancke, Francoise


    The Fringe Sensor Unit (FSU) is the central element of the Phase Referenced Imaging and Micro-arcsecond Astrometry (PRIMA) dual-feed facility and provides fringe sensing for all observation modes, comprising off-axis fringe tracking, phase referenced imaging, and high-accuracy narrow-angle astrometry. It is installed at the Very Large Telescope Interferometer (VLTI) and successfully servoed the fringe tracking loop during the initial commissioning phase. Unique among interferometric beam combiners, the FSU uses spatial phase modulation in bulk optics to retrieve real-time estimates of fringe phase after spatial filtering. A R=20 spectrometer across the K-band makes the retrieval of the group delay signal possible. The FSU was integrated and aligned at the VLTI in summer 2008. It yields phase and group delay measurements at sampling rates up to 2 kHz, which are used to drive the fringe tracking control loop. During the first commissioning runs, the FSU was used to track the fringes of stars with K-band magnitu...

  4. PRIMA: A new, competitive small satellite platform

    Galeazzi, Claudio


    ASI, the Italian Space Agency, is going to finance a developing of a small satellite platforms production line called PRIMA (Piattaforma Riconfigurabile Italiana Multi-Applicativa) with Alenia Aerospazio partnership as Prime Contractor and sub-contractors preferably chosen within the Italian Space Industries. The main objective of the program is to develop a multi-mission, easily adaptable Platform for LEO orbits, allowing rapid, efficient and low cost bus for applicative and scientific missions. The Italian national space plan foresees for the enf of 2001 the build up of the Skymed/Cosmo constellation as applicative Earth observation program plus a number of small scientific spacecraft with a rate of 2 missions each three years. To fulfil these schedules, the PRIMA platform should complete its development and qualification program in order to be ready for the first unit (protoqualification flight) to interface the first payload (Science or Applicative). The intrinsic modularity of PRIMA should allow it to adapt itself to a large variety of missions in LEO orbits with minor modifications. The design will be conducted in order to get an advanced Platform able to meet a large set of missions, payloads and launcher specifications. The platform will be completed by a ground control centre adapted to the monitoring of PRIMA based satellites. PRIMA thus offers a very attractive alternative to large-scale missions in terms of costs and completion time. The paper will describe the technical aspects of PRIMA Platform, with particular emphasis put onto its flexibility and reconfigurability for different missions. The System and S/S architectures will also be presented and defined in view of selected mission cases. The AIV/AIT aspects will be discussed, with a discussion of the applicability of Globalstar™ approaches, facility and heritage. Finally, a brief overview of PRIMA first applications /SkyMed/COSMO and David) will be given.

  5. Planejamento experimental aplicado à otimização de massas cerâmicas contendo matérias-primas naturais Experimental design applied to the optimization of ceramic pastes obtained from natural raw materials

    F. R. Albuquerque


    Full Text Available A otimização da composição é uma etapa de fundamental importância no processamento cerâmico. Neste trabalho, planejamento experimental foi aplicado a fim de se avaliar a relação entre propriedade e a composição de um sistema obtido a partir de matérias-primas naturais extraídas no Pegmatito do Seridó, na região fronteiriça RN-PB. Para o estudo do sistema ternário foram combinadas variáveis de processo (temperatura: 1100 e 1200 ºC; patamar de calcinação: 0 e 2 h, com a utilização de planejamento de misturas, de acordo com o planejamento simplex centróide. Os percentuais mínimos de cada componente na mistura foram de 10% v/v. Foram avaliadas as propriedades reológicas de suspensões aquosas das misturas com 50% v/v, otimizadas com PAA-Na. Determinou-se a porosidade aparente e massa específica aparente, além da retração de queima. A composição mineralógica das peças cerâmicas obtidas a 1200 ºC foi basicamente mulita e quartzo. O estudo permitiu especificar a região de composição que leva à maior densidade após sinterização, com um número relativamente pequeno de amostras.The optimization of the composition is an important step in the development of ceramic products. In this work, experimental design was used in order to evaluate the relationship between properties and the composition of a system obtained from mixtures of natural raw materials extracted from "Pegmatito do Seridó", located near the border of the RN and PB states in Brazil. The processing variables (temperature: 1100 and 1200º C and calcinations time: 0 and 2 h and simplex centroid design were combined for the study of the ternary system. The smallest percentage of each component in the mixture was of 10% v/v. The rheological properties of aqueous suspensions obtained with 50% w/w were optimized with PAA-Na. The apparent porosity and apparent specific gravity were determined, besides retraction, after thermal treatment. The mineralogical

  6. The strategic importance of the natural gas as raw material for the Camacari, Bahia, Brazil, industrial pole; A importancia estrategica do gas natural como materia-prima para o polo industrial de Camacari, BA

    Grassi, Monica Oliveira; Caruso, Carlos Alberto da Rocha; Domingues, Suzana Marques; Pereira, Antonio Constantino [Braskem S.A., Camacari, BA (Brazil). Unidade de Insumos Basicos], e-mails:;;;


    This work emphasizes the importance and the benefit of the application of natural gas from Manati, Brazil, as raw material for the petrochemical, chemical and fertilizers industries at the Camacari industrial pole, Bahia, Brazil, allowing they are more competitive in their actuation area. Initially, it is presented the world overview as far the raw material diversification on the petrochemical processes, face the present scenery of high competitiveness and low practiced margins, according to a general view of the offer and demand of gas in Brazil and northeastern area, focusing the Manati, Bahia, Brazil, the main source of gas to the Bahia state. From this point on, a strategy of raw material flexibilization for ethene production, via gaseous route, is presented. A development of viability study for amplification and modernization of a existent unity for ethane recovering from the natural gas of Manati is presented, with quality and types of contaminant different from the original project.

  7. On Ross' prima facie duty%罗斯的自明义务论




  8. Narrow-angle astrometry with PRIMA

    Sahlmann, J; Mérand, A; Zimmerman, N; Abuter, R; Chazelas, B; Delplancke, F; Henning, T; Kaminski, A; Köhler, R; Launhardt, R; Mohler, M; Pepe, F; Queloz, D; Quirrenbach, A; Reffert, S; Schmid, C; Schuhler, N; Schulze-Hartung, T


    The Extrasolar Planet Search with PRIMA project (ESPRI) aims at characterising and detecting extrasolar planets by measuring the host star's reflex motion using the narrow-angle astrometry capability of the PRIMA facility at the Very Large Telescope Interferometer. A first functional demonstration of the astrometric mode was achieved in early 2011. This marked the start of the astrometric commissioning phase with the purpose of characterising the instrument's performance, which ultimately has to be sufficient for exoplanet detection. We show results obtained from the observation of bright visual binary stars, which serve as test objects to determine the instrument's astrometric precision, its accuracy, and the plate scale. Finally, we report on the current status of the ESPRI project, in view of starting its scientific programme.

  9. Facies Constrained Elastic Full Waveform Inversion

    Zhang, Z.


    Current efforts to utilize full waveform inversion (FWI) as a tool beyond acoustic imaging applications, for example for reservoir analysis, face inherent limitations on resolution and also on the potential trade-off between elastic model parameters. Adding rock physics constraints does help to mitigate these issues. However, current approaches to add such constraints are based on averaged type rock physics regularization terms. Since the true earth model consists of different facies, averaging over those facies naturally leads to smoothed models. To overcome this, we propose a novel way to utilize facies based constraints in elastic FWI. A so-called confidence map is calculated and updated at each iteration of the inversion using both the inverted models and the prior information. The numerical example shows that the proposed method can reduce the cross-talks and also can improve the resolution of inverted elastic properties.

  10. PRIMA: An apparatus for medical application

    Sipala, V., E-mail: [Dipartimento di Fisica e Astronomia, Universita degli Studi di Catania (Italy); INFN, sezione di Catania (Italy); Brianzi, M. [INFN, sezione di Firenze (Italy); Bruzzi, M. [INFN, sezione di Firenze (Italy); Dipartimento di Energetica, Universita degli Studi di Firenze (Italy); Bucciolini, M. [Dipartimento di Fisiopatologia Clinica, Universita degli Studi di Firenze (Italy); INFN, sezione di Firenze (Italy); Cirrone, G.A.P. [Laboratori Nazionali del Sud-INFN, Catania (Italy); Civinini, C. [INFN, sezione di Firenze (Italy); Cuttone, G. [Laboratori Nazionali del Sud-INFN, Catania (Italy); Lo Presti, D. [Dipartimento di Fisica e Astronomia, Universita degli Studi di Catania (Italy); INFN, sezione di Catania (Italy); Pallotta, S. [Dipartimento di Fisiopatologia Clinica, Universita degli Studi di Firenze (Italy); Randazzo, N. [INFN, sezione di Catania (Italy); Romano, F. [Laboratori Nazionali del Sud-INFN, Catania (Italy); Stancampiano, C. [INFN, sezione di Catania (Italy); Scaringella, M. [INFN, sezione di Firenze (Italy); Dipartimento di Energetica, Universita degli Studi di Firenze (Italy); Talamonti, C. [Dipartimento di Fisiopatologia Clinica, Universita degli Studi di Firenze (Italy); INFN, sezione di Firenze (Italy); Tesi, M. [Dipartimento di Energetica, Universita degli Studi di Firenze (Italy)


    In this paper a proton Computed Radiography (pCR) apparatus for medical applications, realized by PRIMA (PRoton IMAging) Italian Collaboration, is described. The system is oriented to acquire tomography images and meets clinical demands for the use of protons in radiotherapy treatments. The approach proposed here is based on 'single proton tracking' method with Most Likely Path (MLP) reconstruction of the single particle. A pCR prototype, with a field of view of about 5 Multiplication-Sign 5 cm{sup 2} and an acquisition time of the order of 10 s (10 kHz, 10{sup 5} events), has been developed and tested with a 62 MeV proton beam at the INFN-Laboratori Nazionali del Sud (LNS). The apparatus architecture will be described and first proton radiographies will be shown.

  11. Diferenciando “primação afectiva” de “primação cognitiva”



    Este artigo procura definir o fenómeno da “primação afectiva” (affective priming) discutindo a sua interpretação como sendo a de um fenómeno afectivo vs. um fenómeno cognitivo. Para tal são apresentados dois breves estudos que utilizam como estímulo-primo (prime) afectivo uma happy-face. O primeiro estudo demonstra a capacidade deste estímulo activar o fenómeno de primação afectiva. O segundo demonstra a sua capacidade de induzir nos participantes um estado de espírito positivo. A interpretaç...

  12. ESPRI: Astrometric planet search with PRIMA at the VLTI

    Ségransan D.


    Full Text Available The ESPRI consortium will conduct an astrometric survey for extrasolar planets, using the PRIMA facility at the Very Large Telescope Interferometer. Our scientific goals include determining orbital inclinations and masses for planets already known from radial-velocity surveys, searches for planets around nearby stars of all masses, and around young stars. The consortium has built the PRIMA differential delay lines, developed an astrometric operation and calibration plan, and will deliver astrometric data reduction software.

  13. From chemistry to consciousness the legacy of Hans Primas

    Müller-Herold, Ulrich


    This book reflects on the significant and highly original scientific contributions of Hans Primas. A professor of chemistry at ETH Zurich from 1962 to 1995, Primas continued his research activities until his death in 2014. Over these 50 years and more, he worked on the foundations of nuclear magnetic resonance spectroscopy, contributed to a number of significant issues in theoretical chemistry, helped to clarify central topics in quantum theory and the philosophy of physics, suggested innovative ways of addressing interlevel relations in the philosophy of science, and introduced cutting-edge approaches in the flourishing young field of scientific studies of consciousness. His work in these areas of research and its continuing impact is described by noted experts, colleagues, and collaborators of Primas. All authors contextualize their contributions to facilitate the mutual dialog between these fields.

  14. PRIMAS materials – IBL teaching and professional development materials

    Doorman, Michiel|info:eu-repo/dai/nl/126974764


    The project PRIMAS regroups 14 teams from 12 different countries. It aims to effect a change across Europe in the teaching and learning of mathematics and science with teachers supported to develop inquiry-based learning (IBL) pedagogies so that students gain experience of IBL approaches. Ultimately

  15. Al CERN prima fase sistema gestione dati LHC


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

  16. PRIMAS materials – IBL teaching and professional development materials

    Doorman, Michiel


    The project PRIMAS regroups 14 teams from 12 different countries. It aims to effect a change across Europe in the teaching and learning of mathematics and science with teachers supported to develop inquiry-based learning (IBL) pedagogies so that students gain experience of IBL approaches. Ultimately

  17. PRIMAS materials – IBL teaching and professional development materials

    Doorman, Michiel


    The project PRIMAS regroups 14 teams from 12 different countries. It aims to effect a change across Europe in the teaching and learning of mathematics and science with teachers supported to develop inquiry-based learning (IBL) pedagogies so that students gain experience of IBL approaches.

  18. Prima Vistale tuleb tuntud kirjanikke mitmest Euroopa riigist / Kaarel Kressa

    Kressa, Kaarel, 1983-


    Prima Vista kirjandusfestivali külalisi: Leonie Swann, Attila Bartis, Dmitri Bõkov, Zinaida Lindén, Mihhail Šiškin, Fay Weldon, Jason Goodwin, Rosa Maria Rodríguez Magda, Inga Gaile, Juris Kronbergs, Guntars Godinš, Liana Langa

  19. Prima Vistale tuleb tuntud kirjanikke mitmest Euroopa riigist / Kaarel Kressa

    Kressa, Kaarel, 1983-


    Prima Vista kirjandusfestivali külalisi: Leonie Swann, Attila Bartis, Dmitri Bõkov, Zinaida Lindén, Mihhail Šiškin, Fay Weldon, Jason Goodwin, Rosa Maria Rodríguez Magda, Inga Gaile, Juris Kronbergs, Guntars Godinš, Liana Langa

  20. Outcropping gravitational and deformational sedimentary facies of the Maracangalha formation and their importance for the exploitation of the Reconcavo basin; Facies sedimentares gravitacionais e deformacionais da Formacao Maracangalha em afloramento e sua importancia na exploracao da Bacia do Reconcavo

    Guerra, Gabriel Soares [Shell Brasil Ltda., Rio de Janeiro, RJ (Brazil)]. E-mail:; Borghi, Leonardo [Universidade Federal, Rio de Janeiro, RJ (Brazil). Inst. de Geociencias. Dept. de Geologia]. E-mail:


    The Maracangalha Formation (Reconcavo Basin, Early Cretaceous) shows gravitational and deformational facies (Caruacu beds and Pitanga Member), which constitute gas reservoirs in the Candeias - Maracangalha petroleum system. Ten sedimentary facies of this nature were described in this formation - 3 previously defined by Mutti (Turbidite sandstones, 1992), and 2 by Mutti et alii (Estr. Mem. Sci. Geol., 28, 1996) - which were organized in 'ramp' and 'shelf-slope' facies associations. The ramp facies association divides itself in 'turbidite' and 'inundite' facies tracts, and the shelf-slope facies association is divided into 'sandy' and 'heterolithic'. The proposed depositional paleoenvironment evolves lacustrine deltas dominated by river flooding, which evolves from a ramp morphology to a shelf and slope one. Electrical logs and seismofacies patterns are suggested for the facies associations. (author)

  1. Coal facies studies in Spain

    Suarez-Ruiz, Isabel [INCAR (CSIC), Ap. Co., 73, 33080, Oviedo (Spain); Jimenez, Amalia [Geology, University of Oviedo, 33005, Oviedo (Spain)


    This work is a synthesis of the distribution of the main coal basins and sub-basins in Spain as well as the research carried out on their coal facies. The coal fields are distributed through the Paleozoic (mainly Pennsylvanian), Mesozoic (Cretaceous) and Cenozoic times. Peats also exist in the southeast Spain (Granada area), although these types of deposits are not included in this review. Spanish coal basins are both of a paralic and intramontane type and the coal rank is highly variable, from lignite in the case of the younger coal seams to anthracite for those of Carboniferous age.

  2. Coal facies studies in Australia

    Crosdale, Peter J. [Coalseam Gas Research Institute, School of Earth Sciences, James Cook University, Townsville, Qld 4814 (Australia)


    Despite the economic importance of coal to the Australian economy, detailed studies of controls on variation in coal type are remarkably few. However, important contributions have been made in the understanding of coal facies development. Tertiary lignite deposits of the Gippsland Basin provide key insights into the development of lithotype cyclicity and its relationship to relative sea-level changes, with individual paling-up cycles being correlated to parasequences. Studies of Permian hard coals have identified relationships between coal type and surrounding sediments. Unfortunately, these relationships have been widely over-interpreted in a manner that has diminished their real value.

  3. Coal facies studies in Canada

    Kalkreuth, Wolfgang D. [Laboratorio de Carvao e de Petrologia Organica, Instituto de Geociencias, Universidade Federal do Rio Grande do Sul (UFRGS), Av. Bento Goncalves, 9500, 91501-970 Porto Alegre, RS (Brazil)


    The present study is a compilation of published data on coal facies studies in Canada based on coal petrological and other methods. The geological age of the coals range from the Devonian coal deposits in Arctic Canada to coals of Tertiary age in the Western Canada Sedimentary Basin, intermontane British Columbia and Arctic Canada. In terms of rank, the coal deposits studied range from lignite to low volatile bituminous. Coal petrological methods include maceral and microlithotype analyses, frequently integrated with data from palynological and geochemical analyses. Most recently, a number of studies have applied sequence stratigraphic concepts to the coal-bearing strata including the interpretation of coal petrological data in the context of this concept.

  4. PRIMA-1Met suppresses colorectal cancer independent of p53 by targeting MEK.

    Lu, Tao; Zou, Yanmei; Xu, Guogang; Potter, Jane A; Taylor, Garry L; Duan, Qiuhong; Yang, Qin; Xiong, Huihua; Qiu, Hong; Ye, Dawei; Zhang, Peng; Yu, Shiying; Yuan, Xianglin; Zhu, Feng; Wang, Yihua; Xiong, Hua


    PRIMA-1Met is the methylated PRIMA-1 (p53 reactivation and induction of massive apoptosis) and could restore tumor suppressor function of mutant p53 and induce p53 dependent apoptosis in cancer cells harboring mutant p53. However, p53 independent activity of PRIMA-1Met remains elusive. Here we reported that PRIMA-1Met attenuated colorectal cancer cell growth irrespective of p53 status. Kinase profiling revealed that mitogen-activated or extracellular signal-related protein kinase (MEK) might be a potential target of PRIMA-1Met. Pull-down binding and ATP competitive assay showed that PRIMA-1Met directly bound MEK in vitro and in cells. Furthermore, the direct binding sites of PRIMA-1Met were explored by using a computational docking model. Treatment of colorectal cancer cells with PRIMA-1Met inhibited p53-independent phosphorylation of MEK, which in turn impaired anchorage-independent cell growth in vitro. Moreover, PRIMA-1Met suppressed colorectal cancer growth in xenograft mouse model by inhibiting MEK1 activity.Taken together, our findings demonstrate a novel p53-independent activity of PRIMA-1Met to inhibit MEK and suppress colorectal cancer growth.

  5. PRIMA-1met (APR-246) inhibits growth of colorectal cancer cells with different p53 status through distinct mechanisms.

    Li, Xiao-Lan; Zhou, Jianbiao; Chan, Zit-Liang; Chooi, Jing-Yuan; Chen, Zhi-Rong; Chng, Wee-Joo


    PRIMA-1met (APR-246) is a methylated derivative and structural analog of PRIMA-1 (p53 re-activation and induction of massive apoptosis). PRIMA-1met has been reported to restore both the wild type (wt) structure and function of mutant p53. Here, we show that PRIMA-1met is highly effective at limiting the growth of CRC cells regardless of p53 status. However, PRIMA-1met induces robust apoptosis only in CRC cells with mutant p53. Upregulation of Noxa, a proapoptotic molecule, is crucial for PRIMA-1met mediated activity. In human xenograft model of disease, PRIMA-1met effectively suppresses CRC tumor growth. Our results uncover distinct mechanisms of PRIMA-1met in CRC with different p53 status, thus providing a mechanistic rationale to evaluate the clinical efficacy of PRIMA-1met in CRC patients with different p53 status.

  6. The Marketing strategy of FTV Prima s.r.o. in the enviroment of the czech television market

    Malá, Kateřina


    This thesis focuses on the topic of marketing strategy of FTV Prima s.r.o. in the television market. The main objective of this thesis is the definition of marketing activities and the use of marketing tools by FTV Prima, a company operating nationwide TV broadcast television stations Prima, Prima COOL, Prima Love and Prima ZOOM, leading to a better position in the television market. The theoretical part of the thesis is the application of marketing mix 4P in the television as a media. The pr...


    Ivano Paccagnella


    Full Text Available La prima edizione del Vocabolario milanese-italiano di Francesco Cherubini (1814 si ispira alle teorie del Cesarotti, che considerava i dialetti come importante fonte per l’arricchimento della lingua nazionale. Il saggio mette a confronto i criteri e gli orientamenti lessicografici del Vocabolario di Cherubini con i vocabolari settecenteschi di altre aree dialettali da lui utilizzati e ne evidenzia elementi comuni ed elementi di novità. Cherubini (1814 in the history of the first dialect lexicographyThe first edition of the Milanese-Italian Dictionary by Francesco Cherubini (1814 was inspired by the theories of Cesarotti, who considered dialects to be an important source for the enrichment of the national language. The essay compares the lexicographical criteria and guidelines of Cherubini’s Dictionary with Dialect Dictionaries from the eighteenth century from other dialect areas that he used, and identifies common and new elements.

  8. Pengembangan Aplikasi E-Crm pada PT Trafoindo Prima Perkasa

    Honni Honni


    Full Text Available Various surveys show that the key to corporate success lies not only on the product or service being offered but how far the company’s efforts to satisfy the needs of its customers. Companies have to provide products or services that match customer needs and wants, and then maintain close relations with customers. Customer loyalty will be the key to success, not only in the short term but sustainable competitive advantage. This is because customer loyalty has strategic value for the company. One way that proved effective and successful to meet and satisfy customer needs is through the CRM (Customer Relationship Management. CRM is not new in the business world. Customer Relationship has long been applied by traditional businessmen. Technology in the form of a web can be utilized as a catalyst in improving the quality of CRM. Combining Technology and CRM in a business called E-CRM. E-CRM application development web based on PT Trafoindo Prima Perkasa aims to analyze and design company and customer needs. The research method used in this writing is descriptive survey method primarily associated with the customer. The analysis tool used is the model porter five forces and industry analysis: CPM Matrix, the External Factor Evaluation Matrix (EFE, the Internal Factor Evaluation Matrix (IFE, SWOT Matrix, IE Matrix, SPACE Matrix, and Grand Strategy Matrix to identify alternative strategies can be applied. Alternative strategy is then measured with a Matrix QSP charm, coupled with the approach of Object Oriented Analysis and Design as the basis for the development of E-CRM application based on web. Conclusions obtained are E-CRM applications have produced work as expected.Keywords: development, application of E-CRM, Trafoindo Prima Perkasa

  9. Facies studies of bituminous coals in Poland

    Nowak, Grzegorz J. [Polish Geological Institute, Lower Silesian Branch, al. Jaworowa 19, 53-122, Wroclaw (Poland)


    Polish bituminous coal basins are associated exclusively with Carboniferous deposits, differing in origin and geological structure. This paper presents only short review of papers of Polish authors on coal facies studies of Carboniferous coals occurring in the Lower Silesian Coal Basin (LSCB), Upper Silesian Coal Basin (USCB) and Lublin Coal Basin (LCB) of Poland. Facies investigations of Carboniferous coals of Poland have been in progress over 20 years. The results of these studies have provided new information on such subjects as: (1) recognition of main depositional conditions in paleomires, (2) determine prevailing paleoplant communities, (3) appraisal of peat-forming environment reconstruction-types and characteristics of paleomires. These facies analyses are connected to results of such studies as: pure coal petrology, using maceral and microlithotype composition as parameters of the environment of coal deposition, combined results of petrological, palynological and sedimentological studies.

  10. Correlation of Upper Devonian and Lower Carboniferous Depositional Sequences in Different Facies Belts on Southern Margin of Upper Yangtze Platform


    A fundamental problem in sequence stratigraphy is whether the sequences are global in extent and whether the sea level changes are eustatic in nature. Study on the Upper Devonian and Lower Carboniferous depositional sequences in different facies belts on the southern margin of the Upper Yangtze platform shows that different orders of sequences possess distinctive distribution and correlation in space, although the sea level changes in various orders of sequences may be primarily global in nature. The present paper regards the distribution in space, especially in different facies belts, as a criterion for defining and recognizing the various orders of sequences. The orthosequence (third-order sequence) is probably global in nature, which may be discerned in various depositional facies belts on the continental margin and can be correlated over long distances, sometimes maybe worldwide. Commonly, correlation of the subsequences (fourth-order sequences with time interval of 0.5 Ma to 1.5 Ma) is difficult in different facies belts, although some of them are probably also worldwide in distribution. A subsequence should be distinguishable and correlatable within at least one facies belt. The higher-order sequences, including parasequences (fifth-order sequences) and microsequences (sixth-order sequences), are regional or local in distribution. They may have reflected the longer and shorter Milankovitch cycles respectively. Orthosequences and subsequences are usually recognizable in different facies belts, while parasequences and microsequences may be distinguished only in shallow marine deposits, but not in slope and basin facies deposits.

  11. Investigating the Nexus of Climate, Energy, Water, and Land at Decision-Relevant Scales: The Platform for Regional Integrated Modeling and Analysis (PRIMA)

    Kraucunas, Ian P.; Clarke, Leon E.; Dirks, James A.; Hathaway, John E.; Hejazi, Mohamad I.; Hibbard, Kathleen A.; Huang, Maoyi; Jin, Chunlian; Kintner-Meyer, Michael C.W.; Kleese van Dam, Kerstin; Leung, Lai-Yung R.; Li, Hongyi; Moss, Richard H.; Peterson, Marty J.; Rice, Jennie S.; Scott, Michael J.; Thomson, Allison M.; Voisin, Nathalie; West, Tristram O.


    The Platform for Regional Integrated Modeling and Analysis (PRIMA) is an innovative modeling system developed at Pacific Northwest National Laboratory (PNNL) to simulate interactions among natural and human systems at scales relevant to regional decision making. PRIMA brings together state-of-the-art models of regional climate, hydrology, agriculture, socioeconomics, and energy systems using a flexible coupling approach. The platform can be customized to inform a variety of complex questions and decisions, such as the integrated evaluation of mitigation and adaptation options across a range of sectors. Research into stakeholder decision support needs underpins the platform's application to regional issues, including uncertainty characterization. Ongoing numerical experiments are yielding new insights into the interactions among human and natural systems on regional scales with an initial focus on the energy-land-water nexus in the upper U.S. Midwest. This paper focuses on PRIMA’s functional capabilities and describes some lessons learned to date about integrated regional modeling.

  12. Prima de Riesgo del Mercado: Histórica, Esperada, Exigida e Implícita

    Pablo Fernández


    Full Text Available Gran parte de la confusión sobre la prima de riesgo del mercado se debe a no distinguir entre sus cuatro acepciones: histórica, esperada, exigida e implícita. Los libros de texto tampoco ayudan: las recomendaciones sobre la prima de riesgo del mercado de 100 libros sobre valoración y finanzas publicados entre 1979 y 2008 oscilan entre 3% y 10%. Varios libros utilizan distintas primas de riesgo en distintas páginas.

  13. Micro-facies of Dead Sea sediments

    Neugebauer, Ina; Schwab, Markus J.; Brauer, Achim; Frank, Ute; Dulski, Peter; Kitagawa, Hiroyuki; Enzel, Yehouda; Waldmann, Nicolas; Ariztegui, Daniel; Drilling Party, Dsddp


    Lacustrine sediments infilling the Dead Sea basin (DSB) provide a rare opportunity to trace changing climates in the eastern Mediterranean-Levant region throughout the Pleistocene and Holocene. In this context, high-resolution investigation of changes in sediment micro- facies allow deciphering short-term climatic fluctuations and changing environmental conditions in the Levant. The Dead Sea is a terminal lake with one of the largest drainage areas in the Levant, located in the Mediterranean climate zone and influenced also by the Saharo-Arabian deserts. Due to drastic climatic changes in this region, an exceptionally large variety of lacustrine sediments has been deposited in the DSB. These sediments, partially the results of changing lake levels, primarily represent changes in precipitation (e.g. Enzel et al., 2008). Evaporites (halite and gypsum) reflect dry climatic conditions during interglacials, while alternated aragonite-detritus (AAD) is deposited during glacial lake level high-stands. Here we present the first micro-facies inventory of a ~450 m long sediment profile from the deepest part of the northern DSB (ICDP site 5017-1, ~300 m water depth). The sediment record comprises the last two glacial-interglacial cycles, with mainly AAD facies in the upper part of the Amora Formation (penultimate glacial) and the last glacial Lisan Formation. The last interglacial Samra and the Holocene Zeelim Formations are predominantly characterized by thick bedded halite deposits, intercalated by partly laminated detrital marl sequences. Representative sections of the different facies types have been analyzed for micro-facies on petrographic thin sections, supported by high-resolution µXRF element scanning, magnetic susceptibility measurements and microscopic fluorescence analysis. Furthermore, Holocene sediments retrieved at the deep basin core site have been compared to their shallow-water counterpart at the western margin of the lake (core DSEn; Migowski et al., 2004

  14. PRIMAS: real-time image-based motion measurement system

    Furnee, E. Hans


    The PRIMAS system derives from a long line of development at Delft University of Technology , originating from [1] with subsequent innovations such as strobed illumination (1974) of reflective markers, to obtain the simultaneous, equidistant, periodic sampling of all marker positions; real-time estimation of the marker centroids from the full, digitized, contours (1984) to retain the on-line data reduction, while enhancing the resolution; interfacing to industry-standard AT type personal computers, with modest disk requirements and no buffering, even for long data runs; 100 Hz, 0.1 ms integration time, electronically-shuttered TV cameras, to get an optimum marker contrast in high ambient or outdoor light conditions (1986). System specifications include a precision of typ. 1:18000 (X) for 2-D coordinate noise or repeatability. With the 100 Hz sample rate this implies an unprecedented spatio-temporal resolution [2]. This favors 3-D reconstruction, as well as a low noise propagation in the estimation of first and higher order derivatives, as are routinely required in biomechanics analysis. The latest feature is real-time marker identification by a software module within the data acquisition program. This option, for the not too complex situations, is feasible only by the data reduction inherent in on-line marker centroid processing. The 3-D calibration, reconstruction and further analytical and display programs are available in the ASYST 3.2 Scientific Language System. A source code option caters for customer extensions. The internal VME/VSB system bus allows the basic dual or quad camera 3-D systems to be readily expanded to larger configurations.

  15. Alisitos Formation, calcareous facies: Early Cretaceous episode of tectonic calm

    Suarez-Vidal, F.


    The Alisitos Formation (Aptian-Albian), shaped as a marine volcanic arc, crops out along the western side of the peninsula of Baja California bounding the Peninsular Range batholith. Lithologically, this formation is formed by volcanic-breccias, porphyritic flows, biohermal limestones, and tuffaceous and pyroclastic sediments. The distribution of the different facies depends on the nature of volcanism and the distance from a volcanic center, although the presence of massive biohermal limestone indicates that in the Early Cretaceous (during the tectonic episodes), the volcanic activity decreased to the level that the environmental conditions were favorable for the development of an organic reef barrier, behind an island arc. Such conditions existed south of the Agua Blanca fault and extended to El Arco, Baja California. Based upon field observations and petrological analysis of the Alisitos limestone, an attempt is made to recreate the environmental condition in the Punta China and San Fernando, Baja California, sites.

  16. Multi-waveform classification for seismic facies analysis

    Song, Chengyun; Liu, Zhining; Wang, Yaojun; Li, Xingming; Hu, Guangmin


    Seismic facies analysis provides an effective way to delineate the heterogeneity and compartments within a reservoir. Traditional method is using the single waveform to classify the seismic facies, which does not consider the stratigraphy continuity, and the final facies map may affect by noise. Therefore, by defining waveforms in a 3D window as multi-waveform, we developed a new seismic facies analysis algorithm represented as multi-waveform classification (MWFC) that combines the multilinear subspace learning with self-organizing map (SOM) clustering techniques. In addition, we utilize multi-window dip search algorithm to extract multi-waveform, which reduce the uncertainty of facies maps in the boundaries. Testing the proposed method on synthetic data with different S/N, we confirm that our MWFC approach is more robust to noise than the conventional waveform classification (WFC) method. The real seismic data application on F3 block in Netherlands proves our approach is an effective tool for seismic facies analysis.

  17. A Method for Determining Sedimentary Micro-Facies Belts Automatically

    Linfu Xue; Qitai Mei; Quan Sun


    It is important to understand the distribution of sedimentary facies, especially the distribution of sand body that is the key for oil production and exploration. The secondary oil recovery requires analyzing a great deal of data accumulated within decades of oil field development. At many cases sedimentary micro-facies maps need to be reconstructed and redrawn frequently, which is time-consuming and heavy. This paper presents an integrated approach for determining the distribution of sedimentary micro-facies, tracing the micro-facies boundary, and drawing the map of sedimentary micro-facies belts automatically by computer technique. The approach is based on the division and correlation of strata of multiple wells as well as analysis of sedimentary facies. The approach includes transform, gridding, interpolation, superposing, searching boundary and drawing the map of sedimentary facies belts, and employs the spatial interpolation method and "worm" interpolation method to determine the distribution of sedimentary micro-facies including sand ribbon and/or sand blanket. The computer software developed on the basis of the above principle provides a tool for quick visualization and understanding the distribution of sedimentary micro-facies and reservoir. Satisfied results have been achieveed by applying the technique to the Putaohua Oil Field in Songliao Basin, China.

  18. Los frutos de las cactáceas y su potencial como materia prima

    Patricia Esquivel


    Los frutos de las Cactáceas y su potencial como materia prima. Se presenta información sobre las características generales, así como usos actuales y potenciales de los miembros más importantes, desde un punto de vista comercial, de la familia de las cactáceas.

  19. Prima-1 induces apoptosis in bladder cancer cell lines by activating p53

    Camila B. Piantino


    Full Text Available OBJECTIVES: Bladder cancer represents 3% of all carcinomas in the Brazilian population and ranks second in incidence among urological tumors, after prostate cancer. The loss of p53 function is the main genetic alteration related to the development of high-grade muscle-invasive disease. Prima-1 is a small molecule that restores tumor suppressor function to mutant p53 and induces cancer cell death in various cancer types. Our aim was to investigate the ability of Prima-1 to induce apoptosis after DNA damage in bladder cancer cell lines. METHOD: The therapeutic effect of Prima-1 was studied in two bladder cancer cell lines: T24, which is characterized by a p53 mutation, and RT4, which is the wild-type for the p53 gene. Morphological features of apoptosis induced by p53, including mitochondrial membrane potential changes and the expression of thirteen genes involved in apoptosis, were assessed by microscopic observation and quantitative real-time PCR (qRT-PCR. RESULTS: Prima-1 was able to reactivate p53 function in the T24 (p53 mt bladder cancer cell line and promote apoptosis via the induction of Bax and Puma expression, activation of the caspase cascade and disruption of the mitochondrial membrane in a BAK-independent manner. CONCLUSION: Prima-1 is able to restore the transcriptional activity of p53. Experimental studies in vivo may be conducted to test this molecule as a new therapeutic agent for urothelial carcinomas of the bladder, which characteristically harbor p53 mutations.

  20. Las facies Keuper al SW de la provincia de Soria

    Hernando, S.


    Full Text Available This paper deals with the sedimentological analysis of the materials that correspond to the Keuper facies in the area situated between the Iberian Ranges and the Central System. Acording to the obtained data, two main aspects are emphasized: - During the Upper Triassic, a c1ear retreat of the roast line towards the East took place, since this area constituted the litoral zone during the sedimentation of the Rot and Muschelkalk. - Facies change lateraly from West to East as proximal alluvial Can sediments pass into facies interpreted as distal alluvial fans and continental sabkha environment.Se analizan, desde el punto de vista sedimentológico, unos materiales correspondientes a las facies Keuper entre la Cordillera Ibérica y el Sistema Central. Dos aspectos resaltan tras este análisis: - Desplazamiento de la línea de costa (que durante la sedimentación del Rot y del Muschelkalk estaba situada en esta zona hacia el Este. - Marcado cambio lateral de facies desde el Oeste hacia el Este, pasando de unas facies proximales-medias de abanico aluvial a unas facies distales y ambiente de sabkha continental.

  1. Coupling among Microbial Communities, Biogeochemistry, and Mineralogy across Biogeochemical Facies

    Stegen, James C.; Konopka, Allan; McKinely, Jim; Murray, Christopher J.; Lin, Xueju; Miller, Micah D.; Kennedy, David W.; Miller, Erin A.; Resch, Charles T.; Fredrickson, Jim K.


    Physical properties of sediments are commonly used to define subsurface lithofacies and these same physical properties influence subsurface microbial communities. This suggests an (unexploited) opportunity to use the spatial distribution of facies to predict spatial variation in biogeochemically relevant microbial attributes. Here, we characterize three biogeochemical facies—oxidized, reduced, and transition—within one lithofacies and elucidate relationships among facies features and microbial community biomass, diversity, and community composition. Consistent with previous observations of biogeochemical hotspots at environmental transition zones, we find elevated biomass within a biogeochemical facies that occurred at the transition between oxidized and reduced biogeochemical facies. Microbial diversity—the number of microbial taxa—was lower within the reduced facies and was well-explained by a combination of pH and mineralogy. Null modeling revealed that microbial community composition was influenced by ecological selection imposed by redox state and mineralogy, possibly due to effects on nutrient availability or transport. As an illustrative case, we predict microbial biomass concentration across a three-dimensional spatial domain by coupling the spatial distribution of subsurface biogeochemical facies with biomass-facies relationships revealed here. We expect that merging such an approach with hydro-biogeochemical models will provide important constraints on simulated dynamics, thereby reducing uncertainty in model predictions.

  2. Partial melting of metavolcanics in amphibolite facies regional metamorphism

    Alan Bruce Thompson


    Metavolcanic rocks containing low-Ca amphiboles (gedrite, cummingtonite) and biotite can undergo substantial dehydration-melting. This is likely to be most prominent in Barrovian Facies Series (kyanite-sillimanite) and occurs at the same time as widespread metapelite dehydration- melting. In lower pressure facies series, metavolcanics will be represented by granulites rich in orthopyroxene when dehydration occurs at much lower temperatures than melting. In higher pressure facies series it is not well known whether metavolcanic rocks dehydrate or melt at temperatures lower or similar to that of metapelites.

  3. Coal facies studies in the eastern United States

    Hower, James C. [Center for Applied Energy Research, University of Kentucky, 2540 Research Park Drive, Lexington, KY 40511-8433 (United States); Eble, Cortland F. [Kentucky Geological Survey, University of Kentucky, Lexington, KY 40506 (United States)


    Coals in the eastern United States (east of the Mississippi River) have been the subject of a number of coal facies studies, going back to the 19th century. Such studies would not necessarily fall within a strict modern classification of coal facies studies, but if a study encompassed some aspects of paleobotany, palynology, petrology, geochemistry, or sedimentology, we assumed that some data and interpretations may be of use in evaluations of the facies. References are presented, as a guide for further research, with annotation in the tables.

  4. PRIMA Platform capability for satellite missions in LEO and MEO (SAR, Optical, GNSS, TLC, etc.)

    Logue, T.; L'Abbate, M.


    PRIMA (Piattaforma Riconfigurabile Italiana Multi Applicativa) is a multi-mission 3-axis stabilized Platform developed by Thales Alenia Space Italia under ASI contract.PRIMA is designed to operate for a wide variety of applications from LEO, MEO up to GEO and for different classes of satellites Platform Family. It has an extensive heritage in flight heritage (LEO and MEO Satellites already fully operational) in which it has successfully demonstrated the flexibility of use, low management costs and the ability to adapt to changing operational conditions.The flexibility and modularity of PRIMA provides unique capability to satisfy different Payload design and mission requirements, thanks to the utilization of recurrent adaptable modules (Service Module-SVM, Propulsion Module-PPM, Payload Module-PLM) to obtain mission dependent configuration. PRIMA product line development is continuously progressing, and is based on state of art technology, modular architecture and an Integrated Avionics. The aim is to maintain and extent multi-mission capabilities to operate in different environments (LEO to GEO) with different payloads (SAR, Optical, GNSS, TLC, etc.). The design is compatible with a wide range of European and US equipment suppliers, thus maximising cooperation opportunity. Evolution activities are mainly focused on the following areas: Structure: to enable Spacecraft configurations for multiple launch; Thermal Control: to guarantee thermal limits for new missions, more demanding in terms of environment and payload; Electrical: to cope with higher power demand (e.g. electrical propulsion, wide range of payloads, etc.) considering orbital environment (e.g. lighting condition); Avionics : AOCS solutions optimized on mission (LEO observation driven by agility and pointing, agility not a driver for GEO). Use of sensors and actuators tailored for specific mission and related environments. Optimised Propulsion control. Data Handling, SW and FDIR mission customization

  5. Nueva materia prima borácica como componente de esmaltes cerámicos. Estudio de su solubilidad en suspensiones acuosas concentradas

    Galindo, M.


    Full Text Available This paper presents an alternative to the use of conventional ceramic frits as raw materials that contribute boron to glaze compositions: a new semi-processed borate (patent pending (WO 2007/148101. The solubility of this new raw material is analysed and compared with that exhibited by conventional ceramic frits and other, natural and processed borates. This comparative analysis has been performed by determining the boron percentage present in the liquid phase of several glaze compositions prepared with each of these raw materials, modifying the type of deflocculant used and the solid/liquid contact time. The results of this study demonstrate the low solubility of the new semi-processed borate and its suitability for use in ceramic glaze formulation.

    En el presente trabajo se presenta una alternativa a la utilización de fritas cerámicas convencionales como materias primas que aportan boro a las composiciones de esmalte: un nuevo borato sintético (patente pendiente WO2007/148101. Se ha estudiado y comparado la solubilidad de esta nueva materia prima con la que exhiben las fritas cerámicas convencionales y otros boratos, tanto naturales como sintéticos. Para ello, se ha determinado el porcentaje de boro presente en la fase líquida de varios esmaltes preparados con cada una de dichas materias primas, modificando el tipo de desfloculante utilizado y el tiempo de contacto sólido/líquido. El resultado de este trabajo ha puesto de manifiesto la baja solubilidad que presenta el nuevo borato sintético y su aptitud para ser usado en la formulación de esmaltes cerámicos.

  6. Facies-controlled volcanic reservoirs of northern Songliao Basin, NE China


    Volcanic rocks of the late Mesozoic are very important reservoirs for the commercial natural gases including hydrocarbon, carbon dioxide and rare gases in the northern Songliao Basin. The reservoir volcanic rocks include rhyolite,andesite, trachyte, basalt and tuff. Facies of the volcanic rocks can be classified into 5 categories and 15 special types.Porosity and permeability of the volcanic reservoirs are facies-controlled. Commercial reservoirs were commonly found among the following volcanic subfacies: volcanic neck (Ⅰ1), underground-explosive breccia (Ⅰ3), pyroclastic-bearing lava flow (Ⅱ3), upper effusive (Ⅲ3) and inner extrusive ones (Ⅳ1). The best volcanic reservoirs are generally evolved in the interbedded explosive and effusive volcanics. Rhyolites show in general better reservoir features than other types of rocks do.

  7. Status of PRIMA, the test facility for ITER neutral beam injectors

    Sonato, P.; Antoni, V.; Bigi, M.; Chitarin, G.; Luchetta, A.; Marcuzzi, D.; Pasqualotto, R.; Pomaro, N.; Serianni, G.; Toigo, V.; Zaccaria, P.; ITER International Team


    The ITER project requires additional heating by two neutral beam injectors, each accelerating to 1MV a 40A beam of negative deuterons, delivering to the plasma about 17MW up to one hour. As these requirements have never been experimentally met, it was decided to build a test facility, PRIMA (Padova Research on ITER Megavolt Accelerator), in Italy, including a full-size negative ion source, SPIDER, and a prototype of the whole ITER injector, MITICA, aiming to develop the heating injectors to be installed in ITER. The Japan and the India Domestic Agencies participate in the PRIMA enterprise; European laboratories, such as KIT-Karlsruhe, IPP-Garching, CCFE-Culham, CEA-Cadarache and others are also cooperating. In the paper the main requirements are discussed and the design of the main components and systems are described.

  8. Analisis Pengaruh Keterlibatan Kerja dan Kepuasan Kerja terhadap Organizational Citizenship Behavior di PT Prima Graphia Digital

    Andrew Adi Saputra


    Full Text Available PT Prima Graphia Digital is a company engaged in the area of digital printing, locates at Kalibaru Timur Street IV No 5-7, Senen, Central Jakarta, Indonesia, 10460. The purpose of this research is to analyze the effect of job involvement and work satisfaction towards Organizational Citizenship Behavior in PT. Prima Graphia Digital. Research used associative method. Data used were primary and secondary data obtained through observation, interview and questionnaire distribution to 86 staffs of the company as respondents. After obtaining the data, then data were processed using Pearson correlation, simple and multiple regression. Results showed that job involvement has positive effect and is significant towards Organizational Citizenship Behavior. Similarly, work satisfaction does also have a positive effect and is significant towards Organizational Citizenship Behavior. Furthermore, job involvement and work satisfaction simultaneously have a significant effect towards Organizational Citizenship Behavior.

  9. Mini Review: Innovation technology cultivaion of Citrus Tangerines Borneo Prima in East Kalimantan



    Full Text Available Abstract. Widyawati AT, Nurbani. 2017. Mini Review: Innovation technology cultivaion of Citrus Tangerines Borneo Prima in East Kalimantan. Pros Sem Nas Masy Biodiv Indon 3: 127-131. The demand for high-value commodities such as oranges continues to increase every year. One of the qualities of orange that can not be met by domestic manufacturers is the color of a citrus peel. Most consumers like citrus orange, like mandarin oranges and other citrus imports. Efforts to reduce the national citrus imports is to improve the productivity and quality of citrus orange in Indonesia. Citrus Tangerines Borneo Prima is one of the featured horticultural commodities in East Kalimantan, which has the advantage of being low lying tangerine with orange rind. It Is indispensable citrus cultivation technique is good and right, so that the citrus plant can develop optimally so that later can produce citrus fruit both in quality and quantity.

  10. Caracterización de algunas materias primas nacionales empleadas en alimentos para animales

    Alvaro E. Obando R.


    Full Text Available El objeto de este trabajo fue desarrollar especificaciones y normalizar la nomenclatura de las materias primas colombianas más utilizadas en la fabricación de alimentos concentrados para animales. Se estudiaron los siguientes productos básicos: arroz , sorgo, maíz, trigo y torta de soya, con sus respectivos subproductos, los cuales constituyen el 84% del volumen de demanda. El muestreo, efectuado a nivel nacional, comprendió 55 fabricas que representan cerca de un 90% de la producción nacional. Las especificaciones se hicieron con base en el análisis proximal incluyendo el 99.7% de la población, (X±3S. Se optimizó ei tamaño muestral utilizando un sistema estadístico secuencial. Algunas materias primas son reportadas por primera vez.

  11. Mullite preparation from natural raw materials; Preparacao de mulita a partir de materias-primas naturais

    Sales, Lindemberg Felismino; Almeida Filho, Humberto Dias de; Goncalves, Joao de Freitas; Macedo, Daniel Araujo de [Universidade Federal da Paraiba (UFPB), Joao Pessoa, PB (Brazil). Departamento de Engenharia de Materiais


    The mullite (3Al2O3.2SiO2) has emerged as one of the most important refractory ceramics today. In this work, kaolin, and mixtures of coffee husk ash, a residue arising from the burning of coffee husks were studied in order to obtain the mullite ceramic base. Ceramic formulations with different maximum percentage (1%, 5% and 10%) of the residue were shaped by uniaxial pressing at 250 MPa and sintered between 1100 and 1400 ° C for 1 h. The technological properties were determined on the basis of residue content and sintering temperature. The phase transformations and microstructure were examined by XRD and SEM. The bulk density (MEA) samples containing 1% by mass of coffee residue, and sintered at 1350 ° C was 2.7 g / cm3. (author)

  12. Fine-Grained Turbidites: Facies, Attributes and Process Implications

    Stow, Dorrik; Omoniyi, Bayonle


    Within turbidite systems, fine-grained sediments are still the poor relation and sport several contrasting facies models linked to process of deposition. These are volumetrically the dominant facies in deepwater and, from a resource perspective, they form important marginal and tight reservoirs, and have great potential for unconventional shale gas, source rocks and seals. They are also significant hosts of metals and rare earth elements. Based on a large number of studies of modern, ancient and subsurface systems, including 1000s of metres of section logging, we define the principal genetic elements of fine-grained deepwater facies, present a new synthesis of facies models and their sedimentary attributes. The principal architectural elements include: non-channelised slope-aprons, channel-fill, channel levee and overbank, turbidite lobes, mass-transport deposits, contourite drifts, basin sheets and drapes. These comprise a variable intercalation of fine-grained facies - thin-bedded and very thin-bedded turbidites, contourites, hemipelagites and pelagites - and associated coarse-grained facies. Characteristic attributes used to discriminate between these different elements are: facies and facies associations; sand-shale ratio, sand and shale geometry and dimensions, sand connectivity; sediment texture and small-scale sedimentary structures; sediment fabric and microfabric; and small-scale vertical sequences of bed thickness. To some extent, we can relate facies and attribute characteristics to different depositional environments. We identify four distinct facies models: (a) silt-laminated mud turbidites, (b) siliciclastic mud turbidites, (c) carbonate mud turbidites, (d) disorganized silty-mud turbidites, and (e) hemiturbidites. Within the grainsize-velocity matrix turbidite plot, these all fall within the region of mean size < 0.063mm, maximum grainsize (one percentile) <0.2mm, and depositional velocity 0.1-0.5 m/s. Silt-laminated turbidites and many mud

  13. Materia prima

    La Croce, Ernesto


    La originalidad del esquema aristotélico está dada por la postulación del sustrato, que al asegurar la permanencia del proceso permite resolver las célebres aporías que el cambio y el movimiento habían despertado entre los griegos. Ahora bien, cuando se tra­ta de un cambio accidental (alteración, aumento o translación), el sustrato material se ex­hibe a nuestra percepción con toda evidencia. Porque, siendo accidentales la forma que se abandona y la forma que se acoge, entonces su correlato ma...

  14. Prima Klima

    Czeskleba-Dupont, Rolf


    for vedvarende energi. En kritisk tilgang til vedvarende energi er anbefalet for at kunne undgå et nyt træfyrings-feber. Visdommen i Stern rapporten fra 2006 med sin konklusion om at det kan betale sig med tidlig handling mod den globale opvarmning bliver relateret til situationen for 20 år siden, hvor en...

  15. The PRIMA collaboration: Preliminary results in FBP reconstruction of pCT data

    Vanzi, Eleonora, E-mail: [Fisica Medica, Azienda Ospedaliero-Universitaria Careggi, Firenze (Italy); Bruzzi, Mara [INFN-Sezione di Firenze, Firenze (Italy); Dipartimento di Energetica, Università degli Studi di Firenze, Firenze (Italy); Bucciolini, Marta [Fisica Medica, Azienda Ospedaliero-Universitaria Careggi, Firenze (Italy); INFN-Sezione di Firenze, Firenze (Italy); Dipartimento di Fisiopatologia Clinica, Università degli Studi di Firenze, Firenze (Italy); Cirrone, G.A. Pablo [INFN-Laboratori Nazionali del Sud, Catania (Italy); Civinini, Carlo [INFN-Sezione di Firenze, Firenze (Italy); Cuttone, Giacomo [INFN-Laboratori Nazionali del Sud, Catania (Italy); Lo Presti, Domenico [INFN-Sezione di Catania, Catania (Italy); Dipartimento di Fisica, Università degli Studi di Catania, Catania (Italy); Pallotta, Stefania [Fisica Medica, Azienda Ospedaliero-Universitaria Careggi, Firenze (Italy); INFN-Sezione di Firenze, Firenze (Italy); Dipartimento di Fisiopatologia Clinica, Università degli Studi di Firenze, Firenze (Italy); Pugliatti, Cristina [INFN-Sezione di Catania, Catania (Italy); Dipartimento di Fisica, Università degli Studi di Catania, Catania (Italy); Randazzo, Nunzio [INFN-Sezione di Catania, Catania (Italy); Romano, Francesco [INFN-Laboratori Nazionali del Sud, Catania (Italy); Centro Studi e Ricerche e Museo Storico della Fisica, Roma (Italy); Scaringella, Monica [Dipartimento di Energetica, Università degli Studi di Firenze, Firenze (Italy); Sipala, Valeria [Dipartimento di Chimica e Farmacia, Università degli Studi di Sassari, Sassari (Italy); INFN-Sezione di Cagliari, Cagliari (Italy); Stancampiano, Concetta [INFN-Laboratori Nazionali del Sud, Catania (Italy); and others


    A first prototype of proton Computed Tomography (pCT) scanner, made of four planes and a calorimeter, has been developed by the PRIMA (PRoton IMAging) Italian collaboration and first results concerning tomographic image reconstruction of experimentally acquired data are discussed in this paper. The Filtered Back-Projection (FBP) algorithm was used to reconstruct projections of a phantom acquired with a 62 MeV proton beam. Image noise and spatial resolution were assessed for different parameters of the filter used, with and without selection strategies on proton directions. A satisfactory image quality (0.88 mm resolution and 2.5% noise) was achieved even when the backprojection line was defined using only the line connecting the impact points on the second and third planes and all the data were used, irrespective of the proton direction and residual energy. Probably due to the specific detector-phantom arrangement used in this experiment and due to the substantial reduction of the number of useful events, cuts on proton directions did not increase the image resolution significantly. The results confirm the good performances of the PRIMA scanner prototype. They also demonstrate that FBP can produce images of sufficient quality to be used for patient positioning and to initialize iterative pCT reconstruction methods. -- Highlights: •pCT data have been acquired with the PRIMA scanner and 62 MeV protons. •FBP reconstruction strategies have been analyzed in terms of resolution and noise. •Even the simplest strategy for data rebinning gave <1mm resolution and <3% noise. •FBP image quality could be sufficient for patient positioning verification.

  16. Plant integration of MITICA and SPIDER experiments with auxiliary plants and buildings on PRIMA site

    Fellin, Francesco, E-mail:; Boldrin, Marco; Zaccaria, Pierluigi; Agostinetti, Piero; Battistella, Manuela; Bigi, Marco; Palma, Samuele Dal Bello Mauro Dalla; Fiorentin, Aldo; Luchetta, Adriano; Maistrello, Alberto; Marcuzzi, Diego; Ocello, Edoardo; Pasqualotto, Roberto; Pavei, Mauro; Pomaro, Nicola; Rizzolo, Andrea; Toigo, Vanni; Valente, Matteo; Zanotto, Loris; Calore, Luca; and others


    Highlights: • Focus on plant integration work supporting the realization of SPIDER and MITICA fusion experiments hosted in PRIMA buildings complex in Padova, Italy. • Huge effort of coordination and integration among many stakeholders, taking into account several constrains coming from experiments requirements (on-going) and precise time schedule and budget on buildings construction. • The paper also deals of interfaces management, coordination and integration of many competences, problems solving to find best solution also considering other aspects like safety and maintenance. - Abstract: This paper presents a description of the PRIMA (Padova Research on ITER Megavolt Accelerator) Plant Integration work, aimed at the construction of PRIMA Buildings, which will host two nuclear fusion test facilities named SPIDER and MITICA, finalized to test and optimize the neutral beam injectors for ITER experiment. These activities are very complex: inputs coming from the experiments design are changing time to time, while the buildings construction shall fulfill precise time schedule and budget. Moreover the decision process is often very long due to the high number of stakeholders (RFX, IO, third parties, suppliers, domestic agencies from different countries). The huge effort includes: forecasting what will be necessary for the integration of many experimental plants; collecting requirements and translating into inputs; interfaces management; coordination meetings with hundreds of people with various and different competences in construction and operation of fusion facilities, thermomechanics, electrical and control, buildings design and construction (civil plants plus architectural and structural aspects), safety, maintenance and management. The paper describes these activities and also the tools created to check and to validate the building design, to manage the interfaces and the organization put in place to achieve the required targets.

  17. Maurizio Ferraris, Documentare la documentalità prima del collasso ontologico

    Guglielmo Feis


    Full Text Available Recensiamo l’ultimo lavoro di Maurizio Ferraris, dedicato all’ontologia sociale: Documentalità. Perché è necessario lasciar tracce.  Nel primo paragrafo sono esposte quelle che Ferraris caratterizza come le tesi portanti del suo lavoro, che quindi sono presentate nel secondo paragrafo. Il terzo e il quarto paragrafo sono dedicati alle critiche: prima quelle che Ferraris fa a Barry Smith e a John Searle servendosi della sua teoria e poi, tenendo conto del dibattito e delle recensioni seguite all’uscita del libro, quelle a Ferraris e alla sua teoria.

  18. Matéria-prima da formação Corumbataí na região do pólo cerâmico de Santa Gertrudes, SP, com características naturais para fabricação de argila expandida Sedimentary rocks from Corumbataí formation (Paraná basin, Brazil with natural characteristics to produce expanded clay lightweight aggregate

    M. M. T. Moreno


    Full Text Available Estudou-se um material da base da Formação Corumbataí, proveniente de uma mineração de argila, que apresenta restrições de uso em cerâmica devido à sua dureza e, principalmente, ao alto conteúdo de matéria orgânica. Verificou-se que o material apresenta características naturais ótimas para a fabricação de argila expandida diretamente a partir de fragmentos de rocha, mostrando comportamento piroplástico com expansão significativa se submetido à queima rápida. A caracterização da matéria-prima e do produto foi realizada mediante análise de carbono orgânico, difração de raios X, microscopia ótica e testes de queima. Foram determinadas as condições de queima para obter argila expandida utilizando forno de queima rápida e forno a rolos, ambos de laboratório, obtendo corpos com densidade variável (que podem chegar a valores menores que 0,5 até o limite de expansão. Esta densidade é obtida devido à formação de poros fechados e uma película externa vítrea, que proporcionam uma resistência mecânica alta aos fragmentos expandidos.This paper refers to the study of the material of the base of the Corumbataí formation (Parana Basin, Brazil of a clay mine, which presents limits for its use in ceramic tiles in dry grinding process due to its hardness and, especially, the high content of organic matter in relation to the clay overlaid. The characterization of the raw material and the product was accomplished by organic carbon analysis, X-ray diffraction, optical microscopy and test-firing. Firing conditions were determined to get expanded clay, using fast firing static kiln and a continuous roller kiln, both from laboratory equipment, getting samples with variable density up to the limit of expansion, with density that can reach values lower than 0.5 because of the formation of closed pores and an external vitreous foil which provide a high mechanical resistance to the particles.

  19. Organic facies applied to petroleum exploration; Facies organica: conceitos, metodos e estudos de casos na industria do petroleo

    Menezes, Taissa Rego; Araujo, Carla Viviane; Souza, Igor Viegas Alves F. de [PETROBRAS, Rio de Janeiro, RJ (Brazil). Centro de Pesquisas (CENPES). Gerencia de Geoquimica,]. E-mail:; Mendonca Filho, Joao Graciano; Mendonca, Joalice de Oliveira [Universidade Federal do Rio de Janeiro (UFRJ), Rio de Janeiro, RJ (Brazil). Dept. de Geologia


    The concept of organic facies, as well as the definitions and means of the different facies became a very important tool to petroleum exploration. The application of this concept is the best way to integrate microscopy and geochemical techniques to study kerogen contained in sedimentary rocks. Thus, palynofacies analysis and bulk geochemical methods are used to characterize the total particulate organic matter. Palynofacies analysis involves the integrated study of all aspects of the kerogen assemblage: identification of the individual particulate components, assessment of their absolute and relative proportions and preservation states. The correlation between palynofacies and geochemical data provides the organic facies models that point out the depositional environmental conditions and hydrocarbon source rock potential. (author)

  20. The potential role of fluids during regional granulite-facies dehydration in the lower crust

    Daniel E. Harlov


    Full Text Available High-grade dehydration of amphibolite-facies rocks to granulite-facies is a process that can involve partial melting, fluid-aided solid-state dehydration, or varying degrees of both. On the localized meter scale, solid-state dehydration, due to CO2-rich fluids traveling along some fissure or crack and subsequently outwards along the mineral grain boundaries of the surrounding rock, normally is the means by which the breakdown of biotite and amphibole to orthopyroxene and clinopyroxene occur. Various mineral textures and changes in mineral chemistry seen in these rocks are also seen in more regional orthopyroxene-clinopyroxene-bearing rocks which, along with accompanying amphibolite-facies rocks, form traverses of lower crust. This suggests that solid-state dehydration during high-grade metamorphism could occur on a more regional scale. The more prominent of these fluid-induced textures in the granulite-facies portion of the traverse take the form of micro-veins of K-feldspar along quartz grain boundaries and the formation of monazite inclusions in fluorapatite. The fluids believed responsible take the form of concentrated NaCl- and KCl- brines from a basement ultramafic magma heat source traveling upwards along grain boundaries. Additional experimental work involving CaSO4 dissolution in NaCl-brines, coupled with natural observation of oxide and sulfide mineral associations in granulite-facies rocks, have demonstrated the possibility that NaCl-brines, with a CaSO4 component, could impose the oxygen fugacity on these rocks as opposed to the oxygen fugacity being inherent in their protoliths. These results, taken together, lend credence to the idea that regional chemical modification of the lower crust is an evolutionary process controlled by fluids migrating upwards from the lithospheric mantle along grain boundaries into and through the lower crust where they both modify the rock and are modified by it. Their presence allows for rapid mass and

  1. Sensibilidade à secagem da matéria-prima cerâmica da Formação Corumbataí na região do Polo Cerâmico de Santa Gertrudes, SP

    A. A. Azzi


    Full Text Available As argilas provenientes da Formação Corumbataí são atualmente a principal fonte de matéria-prima para as indústrias do Polo Cerâmico de Santa Gertrudes. 73% das indústrias desse polo que utilizam o processo de secagem via seca são hoje alvo de crescente pressão dos órgãos de controle ambiental devido à emissão de partículas (poeira associado ao processo de secagem da matéria-prima. Neste trabalho, foram realizados quatro diferentes testes de secagem em três tipos de matéria-prima (D, I e M da Formação Corumbataí, com umidades naturais iniciais de 8%, 18% e 19%, respectivamente, para poder avaliar a sensibilidade à secagem. Dentre os testes analisados neste trabalho estão o processo natural de secagem ao sol, secagem ao vento, secagem ao sol combinado a uma corrente de vento, e secagem ao sol com matéria-prima previamente umedecida em água corrente. Os testes foram ainda correlacionados à análise termogravimétrica. A análise por difração de raios X, juntamente com as análises química e petrográfica mostrou que as amostras D, I e M contêm predominantemente filossilicatos 2:1 como illitas (25-30% e esmectitas (15-25%, e em menor quantidade caulinita (0-15% e clorita (0-5%. Os resultados dos experimentos de secagem associados à mineralogia mostram que entre 100 °C e 200 °C nos gráficos de termogravimetria pode indicar de modo rápido a sensibilidade à secagem que o material apresenta, uma vez que a maior perda de umidade obtida nesta faixa indica a maior quantidade de minerais do grupo das esmectitas, que por sua vez conferem ao material menor sensibilidade à secagem. Além disso, os procedimentos de secagem natural sugerem que secar separadamente a matéria-prima pode resultar em maior eficiência do processo de secagem.

  2. Pectina: da matéria-prima ao produto final Pectin: from raw material to the final product

    Maria H. G. Canteri


    Full Text Available A pectina, provavelmente a mais complexa macromolécula natural, é um heteropolissacarídeo contendo predominantemente resíduos de ácido galacturônico. Este polímero, do grupo das fibras dietéticas, é amplamente utilizado como geleificante e estabilizante na indústria de alimentos. O principal processo industrial para obtenção de pectina está baseado na solubilização da protopectina do bagaço de maçã e casca de frutos cítricos, realizada em condições levemente ácidas sob aquecimento. Estudos recentes têm reportado a extração de pectina de novas matérias-primas sob diferentes condições, com influência sobre a qualidade e sobre o rendimento do produto final, para aumentar sua qualidade reológica. Esta revisão descreve a estrutura, as fontes, as aplicações, o processo de extração industrial assim como as principais técnicas de caracterização da pectina.Pectin, probably the most complex macromolecule in nature is a hetero-polysaccharide containing predominantly residues of galacturonic acid (GalA. This polymer, which belongs to a group of dietary fibers, is widely used as a gelling agent and stabilizer in the food industry. The main industrial processing to obtain pectin is based on the solubilization of protopectin from apple pomace and citrus peels, which is done under low acidity and heated conditions. Recent studies have reported the extraction of pectin from new raw materials and using different extraction conditions, which influence the yield and quality of the final product, and may improve the rheological properties. This review describes the structure, sources, applications and industrial extraction processes, as well as the analysis methods of physicochemical characterization of pectin.

  3. Progress in the realization of the PRIMA neutral beam test facility

    Toigo, V.; Boilson, D.; Bonicelli, T.; Piovan, R.; Hanada, M.; Chakraborty, A.; Agarici, G.; Antoni, V.; Baruah, U.; Bigi, M.; Chitarin, G.; Dal Bello, S.; Decamps, H.; Graceffa, J.; Kashiwagi, M.; Hemsworth, R.; Luchetta, A.; Marcuzzi, D.; Masiello, A.; Paolucci, F.; Pasqualotto, R.; Patel, H.; Pomaro, N.; Rotti, C.; Serianni, G.; Simon, M.; Singh, M.; Singh, N. P.; Svensson, L.; Tobari, H.; Watanabe, K.; Zaccaria, P.; Agostinetti, P.; Agostini, M.; Andreani, R.; Aprile, D.; Bandyopadhyay, M.; Barbisan, M.; Battistella, M.; Bettini, P.; Blatchford, P.; Boldrin, M.; Bonomo, F.; Bragulat, E.; Brombin, M.; Cavenago, M.; Chuilon, B.; Coniglio, A.; Croci, G.; Dalla Palma, M.; D'Arienzo, M.; Dave, R.; De Esch, H. P. L.; De Lorenzi, A.; De Muri, M.; Delogu, R.; Dhola, H.; Fantz, U.; Fellin, F.; Fellin, L.; Ferro, A.; Fiorentin, A.; Fonnesu, N.; Franzen, P.; Fröschle, M.; Gaio, E.; Gambetta, G.; Gomez, G.; Gnesotto, F.; Gorini, G.; Grando, L.; Gupta, V.; Gutierrez, D.; Hanke, S.; Hardie, C.; Heinemann, B.; Kojima, A.; Kraus, W.; Maeshima, T.; Maistrello, A.; Manduchi, G.; Marconato, N.; Mico, G.; Moreno, J. F.; Moresco, M.; Muraro, A.; Muvvala, V.; Nocentini, R.; Ocello, E.; Ochoa, S.; Parmar, D.; Patel, A.; Pavei, M.; Peruzzo, S.; Pilan, N.; Pilard, V.; Recchia, M.; Riedl, R.; Rizzolo, A.; Roopesh, G.; Rostagni, G.; Sandri, S.; Sartori, E.; Sonato, P.; Sottocornola, A.; Spagnolo, S.; Spolaore, M.; Taliercio, C.; Tardocchi, M.; Thakkar, A.; Umeda, N.; Valente, M.; Veltri, P.; Yadav, A.; Yamanaka, H.; Zamengo, A.; Zaniol, B.; Zanotto, L.; Zaupa, M.


    The ITER project requires additional heating by two neutral beam injectors, each accelerating to 1 MV a 40 A beam of negative deuterium ions, to deliver to the plasma a power of about 17 MW for one hour. As these requirements have never been experimentally met, it was recognized as necessary to setup a test facility, PRIMA (Padova Research on ITER Megavolt Accelerator), in Italy, including a full-size negative ion source, SPIDER, and a prototype of the whole ITER injector, MITICA, aiming to develop the heating injectors to be installed in ITER. This realization is made with the main contribution of the European Union, through the Joint Undertaking for ITER (F4E), the ITER Organization and Consorzio RFX which hosts the Test Facility. The Japanese and the Indian ITER Domestic Agencies (JADA and INDA) participate in the PRIMA enterprise; European laboratories, such as IPP-Garching, KIT-Karlsruhe, CCFE-Culham, CEA-Cadarache and others are also cooperating. Presently, the assembly of SPIDER is on-going and the MITICA design is being completed. The paper gives a general overview of the test facility and of the status of development of the MITICA and SPIDER main components at this important stage of the overall development; then it focuses on the latest and most critical issues, regarding both physics and technology, describing the identified solutions.

  4. The PRIMA Test Facility: SPIDER and MITICA test-beds for ITER neutral beam injectors

    Toigo, V.; Piovan, R.; Dal Bello, S.; Gaio, E.; Luchetta, A.; Pasqualotto, R.; Zaccaria, P.; Bigi, M.; Chitarin, G.; Marcuzzi, D.; Pomaro, N.; Serianni, G.; Agostinetti, P.; Agostini, M.; Antoni, V.; Aprile, D.; Baltador, C.; Barbisan, M.; Battistella, M.; Boldrin, M.; Brombin, M.; Dalla Palma, M.; De Lorenzi, A.; Delogu, R.; De Muri, M.; Fellin, F.; Ferro, A.; Fiorentin, A.; Gambetta, G.; Gnesotto, F.; Grando, L.; Jain, P.; Maistrello, A.; Manduchi, G.; Marconato, N.; Moresco, M.; Ocello, E.; Pavei, M.; Peruzzo, S.; Pilan, N.; Pimazzoni, A.; Recchia, M.; Rizzolo, A.; Rostagni, G.; Sartori, E.; Siragusa, M.; Sonato, P.; Sottocornola, A.; Spada, E.; Spagnolo, S.; Spolaore, M.; Taliercio, C.; Valente, M.; Veltri, P.; Zamengo, A.; Zaniol, B.; Zanotto, L.; Zaupa, M.; Boilson, D.; Graceffa, J.; Svensson, L.; Schunke, B.; Decamps, H.; Urbani, M.; Kushwah, M.; Chareyre, J.; Singh, M.; Bonicelli, T.; Agarici, G.; Garbuglia, A.; Masiello, A.; Paolucci, F.; Simon, M.; Bailly-Maitre, L.; Bragulat, E.; Gomez, G.; Gutierrez, D.; Mico, G.; Moreno, J.-F.; Pilard, V.; Kashiwagi, M.; Hanada, M.; Tobari, H.; Watanabe, K.; Maejima, T.; Kojima, A.; Umeda, N.; Yamanaka, H.; Chakraborty, A.; Baruah, U.; Rotti, C.; Patel, H.; Nagaraju, M. V.; Singh, N. P.; Patel, A.; Dhola, H.; Raval, B.; Fantz, U.; Heinemann, B.; Kraus, W.; Hanke, S.; Hauer, V.; Ochoa, S.; Blatchford, P.; Chuilon, B.; Xue, Y.; De Esch, H. P. L.; Hemsworth, R.; Croci, G.; Gorini, G.; Rebai, M.; Muraro, A.; Tardocchi, M.; Cavenago, M.; D'Arienzo, M.; Sandri, S.; Tonti, A.


    The ITER Neutral Beam Test Facility (NBTF), called PRIMA (Padova Research on ITER Megavolt Accelerator), is hosted in Padova, Italy and includes two experiments: MITICA, the full-scale prototype of the ITER heating neutral beam injector, and SPIDER, the full-size radio frequency negative-ions source. The NBTF realization and the exploitation of SPIDER and MITICA have been recognized as necessary to make the future operation of the ITER heating neutral beam injectors efficient and reliable, fundamental to the achievement of thermonuclear-relevant plasma parameters in ITER. This paper reports on design and R&D carried out to construct PRIMA, SPIDER and MITICA, and highlights the huge progress made in just a few years, from the signature of the agreement for the NBTF realization in 2011, up to now—when the buildings and relevant infrastructures have been completed, SPIDER is entering the integrated commissioning phase and the procurements of several MITICA components are at a well advanced stage.

  5. Polypharmacy in chronic diseases-Reduction of Inappropriate Medication and Adverse drug events in older populations by electronic Decision Support (PRIMA-eDS): study protocol for a randomized controlled trial.

    Sönnichsen, Andreas; Trampisch, Ulrike S; Rieckert, Anja; Piccoliori, Giuliano; Vögele, Anna; Flamm, Maria; Johansson, Tim; Esmail, Aneez; Reeves, David; Löffler, Christin; Höck, Jennifer; Klaassen-Mielke, Renate; Trampisch, Hans Joachim; Kunnamo, Ilkka


    Multimorbidity is increasing in aging populations with a corresponding increase in polypharmacy as well as inappropriate prescribing. Depending on definitions, 25-50 % of patients aged 75 years or older are exposed to at least five drugs. Evidence is increasing that polypharmacy, even when guidelines advise the prescribing of each drug individually, can potentially cause more harm than benefit to older patients, due to factors such as drug-drug and drug-disease interactions. Several approaches reducing polypharmacy and inappropriate prescribing have been proposed, but evidence showing a benefit of these measures regarding clinically relevant endpoints is scarce. There is an urgent need to implement more effective strategies. We therefore set out to develop an evidence-based electronic decision support (eDS) tool to aid physicians in reducing inappropriate prescribing and test its effectiveness in a large-scale cluster-randomized controlled trial. The "Polypharmacy in chronic diseases-Reduction of Inappropriate Medication and Adverse drug events in older populations" (PRIMA)-eDS tool is a tool comprising an indication check and recommendations for the reduction of polypharmacy and inappropriate prescribing based on systematic reviews and guidelines, the European list of inappropriate medications for older people, the SFINX-database of interactions, the PHARAO-database on adverse effects, and the RENBASE-database on renal dosing. The tool will be evaluated in a cluster-randomized controlled trial involving 325 general practitioners (GPs) and around 3500 patients across five study centres in the United Kingdom, Germany, Austria and Italy. GP practices will be asked to recruit 11 patients aged 75 years or older who are taking at least eight medications and will be cluster-randomized after completion of patient recruitment. Intervention GPs will have access to the PRIMA-eDS tool, while control GPs will treat their patients according to current guidelines (usual care

  6. Analisis dan Perancangan Sistem Informasi Eksekutif Pemasaran pada Distributor Alat Tulis Kantor: Studi Kasus pada Benza Prima

    Mohammad Subekti


    Full Text Available Executive information system (EIS has been widely used in enterprises and institutions to help the executives make decisions quickly and accurately for the organization's business needs. A research is conducted to create a marketing executive information system that can produce analytic reports and comparison reports for the executive of Benza Prima. For information search the fact finding techniques is utilized by conducting surveys directly to the company to study the company needs and the running procedures. The executive information system design uses Object Oriented Analysis and Design (OOAD methodology. The research results in an executive information system that produces report in forms of pivot tables and charts to help the Benza Prima executives make decisions. The marketing executive information system design is expected to provide analytic information that can be used by the Benza Prima executive as an analytic tool in planning marketing strategies. 

  7. Penerapan Best Practice IT Service Management dalam Perbaikan IT Service Desk: Studi Kasus PT. Matahari Putra Prima

    Hendra Hendra


    Full Text Available Information Technology (IT grows very rapidly and affects every aspect of business life to support competition with other companies that have the same field. PT. Matahari Putra Prima has implemented a computerized system as one of its business strategy in achieving the company's business objectives. With the implementation of IT in the company, the role of Service Desk is indispensable in providing services to users. This study aims to identify and analyze the implementation of IT Service Desk of PT. Matahari Putra Prima to the users. This research is expected to increase and improve the quality of IT Service Desk PT. Matahari Putra Prima based on the IT Service Management (ITSM. 

  8. Uranium, rare metals, and granulite-facies metamorphism

    Michel Cuney


    The Tranomaro metasomatized marbles recrystallizing under granulite-facies conditions represent a demonstrative example of fluid transfer from granulite-facies supracrustals to traps represented by regional scale skarns. Such fluids may be at the origin of the incompatible element enrichment detected in leucosomes of migmatites from St Malo in Brittany (France and Black Hills in South Dakota. The northern French Massif Central provides us with an example of a potential association between incompatible element enrichment of granitic melts and granulite-facies metamorphism. U- and F-enriched fine-grained granites are emplaced along a crustal scale shear zone active during the emplacement within the St Sylvestre peraluminous leucogranitic complex. We propose that during granulite-facies metamorphism dominated by carbonic waves in a deep segment of the continental crust, these shear zones control: (i the percolation of F-, LILE-, rare metal-rich fluids liberated primarily by the breakdown of biotite; (ii the enhancement of partial melting by F-rich fluids at intermediate crustal levels with the generation of F-, LILE-, rare metal-rich granitic melts; (iii their transfer through the crust with protracted fractionation facilitated by their low viscosity due to high F-Li contents; and finally (iv their emplacement as rare metal intrusions at shallow crust levels.

  9. Predicted seafloor facies of Central Santa Monica Bay, California

    Dartnell, Peter; Gardner, James V.


    Summary -- Mapping surficial seafloor facies (sand, silt, muddy sand, rock, etc.) should be the first step in marine geological studies and is crucial when modeling sediment processes, pollution transport, deciphering tectonics, and defining benthic habitats. This report outlines an empirical technique that predicts the distribution of seafloor facies for a large area offshore Los Angeles, CA using high-resolution bathymetry and co-registered, calibrated backscatter from multibeam echosounders (MBES) correlated to ground-truth sediment samples. The technique uses a series of procedures that involve supervised classification and a hierarchical decision tree classification that are now available in advanced image-analysis software packages. Derivative variance images of both bathymetry and acoustic backscatter are calculated from the MBES data and then used in a hierarchical decision-tree framework to classify the MBES data into areas of rock, gravelly muddy sand, muddy sand, and mud. A quantitative accuracy assessment on the classification results is performed using ground-truth sediment samples. The predicted facies map is also ground-truthed using seafloor photographs and high-resolution sub-bottom seismic-reflection profiles. This Open-File Report contains the predicted seafloor facies map as a georeferenced TIFF image along with the multibeam bathymetry and acoustic backscatter data used in the study as well as an explanation of the empirical classification process.

  10. [Vaginal ecology, climate, landscapes and populations (xenoecies and facies)].

    Nicoli, J M; Nourrit, J; Michel-Nguyen, A; Sempe, M; Nicoli, R M


    Brief study of vaginal populations, the human vagina being considered as a biotopic cavity. Allusion to dynamic aspects ("vaginal climate", "landscapes") and to various bacterial populations. Introduction of the concept of xenoecies and of facies. This study is preceded by essential definitions of terms widely used in ecology.

  11. Impacto de la prima de riesgo de la deuda soberana sobre el coste de la deuda de las empresas

    Pampín Pazos, Lucía


    Traballo de Fin de Grao en Administración e Dirección de Empresas. Curso 2014-2015 La crisis reciente en el mercado de deuda soberana europea ha disparado el importe de la prima de riesgo, en particular en los países periféricos de la UE. Este hecho podría tener consecuencia sobre las condiciones de financiación de las empresas privadas. En este trabajo analizamos las implicaciones de los cambios en la prima de riesgo de la deuda soberana en España sobre el coste de la deuda de las empresa...


    José María Felipe Mendoza


    Full Text Available Both in his comments on the Sententiae of Peter Lombard and in his Summa Theologiae, Thomas Aquinas uses the term philosophia prima. Although it is not used by Aquinas frequently, this term marks the technical sense which links theologia and metaphysica as the first sciences with the second sciences, like physics. Against this background, this article attempts to clarify: (1 the need of first philosophy to exist, (2 the Thomistic position which claims that there is only one supreme science which, though possessing three names, has God as its only subiectum, and (3 the meaning of the term philosophia prima.

  13. Surficial Sediment Facies features near Shorty's Island on the Kootenai River near Bonners Ferry, ID

    U.S. Geological Survey, Department of the Interior — The surficial bed-sediment facies, herein after referred to as the sediment facies, quantitatively describes the dominant sediment substrate on the surface of the...

  14. Psychotherapy, biological psychiatry, and the nature of matter: a view from physics.

    Berger, L S


    Biological psychiatry has marginalized psychotherapy, and it is difficult for psychotherapists to counter its hegemony. The reductionist/materialist position seems incontrovertible and self-evident. An important factor in maintaining this stance is the belief that the physical world is understandable, solid, unproblematic, especially when compared to the realm of the psychological. Developments in quantum and relativity theories, however, cast doubt on that belief. They show the fundamental nature of the material world to be problematic, enigmatic, paradoxical, impossible to understand or conceptualize in terms of everyday experience. This insight weakens the prima facie case for privileging the material over the psychological, and alternative (i.e., nonneurobiological) approaches to mental health matters should, therefore, be able to compete on an equal footing. However, the materialist-reductionist stance is kept in place by powerful forces and is well defended; rational arguments alone are unlikely to have an impact. This pervasive ideological resistance to rational, often well-founded critiques of physical reductionism continues to be a major impediment to changing the present materialist climate. That resistance has to be addressed before any significant shift in orientation can be expected to occur.

  15. Assessing linkages between spatial facies changes and dimensional variations of glaciers in the upper Indus Basin, western Himalaya

    Ali, Iram; Shukla, Aparna; Romshoo, Shakil A.


    The present study provides an insight into the heterogeneous response of 45 glaciers in the Lidder and Sindh river basins, western Himalaya, and explores the linkages between glacier facies variability and changing glacier parameters. Results show that the region has undergone an overall deglaciation of 12 ± 1.5% (11.9 ± 1.4 km2) from 1996 to 2014. Fluctuations in the temperature and precipitation patterns seem to be the primary factor controlling the changes in glacier dimensions (R2 > 0.82 in all cases). Glacier facies changes suggest depletion in snow-ice cover ( 18 ± 2.3%) and an increase in ice-mixed debris ( 4 ± 1.4%), supraglacial debris ( 6 ± 1.5%), and periglacial debris ( 17 ± 1.2%). These glacier facies transitions are possibly the result of ice-melting; however, its relative rate and elevation decides the nature of facies conversion. An increase in the proportion of supraglacial debris has led to the conversion of 11 clean glaciers to sparsely debris-covered glaciers and 5 sparsely debris-covered glaciers to debris-covered glaciers. The size of the glaciers greatly influenced the rate of conversion of glaciers, and glaciers glaciers also experienced maximum shrinkage. Further, the glaciers with varying supraglacial debris cover respond differently, as sparsely debris-covered glaciers exhibit the highest rates of retreat (25 ± 7.3 m/y), followed by clean (23.7 ± 7.3 m/y) and debris-covered glaciers (13.1 ± 7.3 m/y). Thus, the findings of this work clearly show that the climate change driven dimensional changes of glaciers and variations in the spatial distribution of glacier facies have strong mutual control on each other.

  16. Facies composition and scaling relationships of extensional faults in carbonates

    Bastesen, Eivind; Braathen, Alvar


    Fault seal evaluations in carbonates are challenged by limited input data. Our analysis of 100 extensional faults in shallow-buried layered carbonate rocks aims to improve forecasting of fault core characteristics in these rocks. We have analyzed the spatial distribution of fault core elements described using a Fault Facies classification scheme; a method specifically developed for 3D fault description and quantification, with application in reservoir modelling. In modelling, the fault envelope is populated with fault facies originating from the host rock, the properties of which (e.g. dimensions, geometry, internal structure, petrophysical properties, and spatial distribution of structural elements) are defined by outcrop data. Empirical data sets were collected from outcrops of extensional faults in fine grained, micro-porosity carbonates from western Sinai (Egypt), Central Spitsbergen (Arctic Norway), and Central Oman (Adam Foothills) which all have experienced maximum burial of 2-3 kilometres and exhibit displacements ranging from 4 centimetres to 400 meters. Key observations include fault core thickness, intrinsic composition and geometry. The studied fault cores display several distinct fault facies and facies associations. Based on geometry, fault cores can be categorised as distributed or localized. Each can be further sub-divided according to the presence of shale smear, carbonate fault rocks and cement/secondary calcite layers. Fault core thickness in carbonate rocks may be controlled by several mechanisms: (1) Mechanical breakdown: Irregularities such as breached relays and asperities are broken down by progressive faulting and fracturing to eventually form a thicker fault rock layer. (2) Layer shearing: Accumulations of shale smear along the fault core. (3) Diagenesis; pressure solution, karstification and precipitation of secondary calcite in the core. Observed fault core thicknesses scatter over three orders of magnitude, with a D/T range of 1:1 to 1

  17. La memoria alla barocca ne L’isola del giorno prima di Umberto Eco

    Agnieszka Piwowarska


    Full Text Available In his third novel The Island of the Day Before (L’isola del giorno prima Umberto Eco narrates a story of an unusual castaway named Roberto who – instead of being on a desert island – finishes up on an abandoned (but only at first sight ship. The article aims to analyze how the book’s main character, during his loneliness, reminisces about events from his past. And because the novel is set in the Baroque, Roberto´s memories respect the spirit of that time : numerous flashbacks are evoked by unexpected metaphors that link very distant things. The ship, which is for a young man a cumbersome prison, becomes a real Theatre of Memory, according to Giulio Camillo’s idea.

  18. First results from fringe tracking with the PRIMA fringe sensor unit

    Sahlmann, J; Menardi, S; Schmid, C; Di Lieto, N; Delplancke, F; Frahm, R; Gomes, N; Haguenauer, P; Leveque, S; Morel, S; Mueller, A; Duc, T Phan; Schuhler, N; van Belle, G; 10.1117/12.856896


    The fringe sensor unit (FSU) is the central element of the phase referenced imaging and micro-arcsecond astrometry (PRIMA) dual-feed facility for the Very Large Telescope interferometer (VLTI). It has been installed at the Paranal observatory in August 2008 and is undergoing commissioning and preparation for science operation. Commissioning observations began shortly after installation and first results include the demonstration of spatially encoded fringe sensing and the increase in VLTI limiting magnitude for fringe tracking. However, difficulties have been encountered because the FSU does not incorporate real-time photometric correction and its fringe encoding depends on polarisation. These factors affect the control signals, especially their linearity, and can disturb the tracking control loop. To account for this, additional calibration and characterisation efforts are required. We outline the instrument concept and give an overview of the commissioning results obtained so far. We describe the effects of...

  19. Study of fuel element characteristic of SM and SMP (SM-PRIMA) fuel assemblies

    Klinov, A.V.; Kuprienko, V.A.; Lebedev, V.A.; Makhin, V.M.; Tuchnin, L.M.; Tsykanov, V.A. [Research Institute of Atomic Reactors, Dimitrovgrad (Russian Federation)


    The paper discusses the techniques and results of reactor tests and post-reactor investigations of the SM reactor fuel elements and fuel elements developed in the process of designing the specialized PRIMA test reactor with the SM reactor fuel elements used as a prototype and which are referred to as the SMP fuel elements. The behavior of fuel elements under normal operating conditions and under deviation from normal operating conditions was studied to verify the calculation techniques, to check the calculation results during preparation of the SM reactor safety substantiation report and to estimate the possibility of using such fuel elements in other projects. During tests of fuel rods under deviation from normal operating conditions their advantages were shown over fuel elements, the components of which were produced using the Al-based alloys. (author)

  20. David Frapiccini, L’età aurea di Giulio II. Arti, cantieri e maestranze prima di Raffaello

    Giuseppe Capriotti


    Full Text Available Recensione / Book review Frapiccini D. (2014, L’età aurea di Giulio II. Arti, cantieri e maestranze prima di Raffaello, Roma, Gangemi Editore («Helicona. Collana di monografie di storia dell’arte», a cura di Marco Gallo, 206 pp.

  1. Petrology of blueschist facies metamorphic rocks of the Meliata Unit

    Faryad Shah Wali


    Full Text Available Meliata blueschists originated from basalts, limestones, pelites, psammitic and amphibolite facies basement rocks. Compositionally, the metabasalts have a geochemical signature mostly indicative of a transitional arc-MORB origin, but some mafic rocks having affinity with within plate basalts also present. The mafic blueschists consist of blue amphibole, epidote and albite, rarely also garnet, Na-pyroxene and chloritoid. Apart from phengite and quartz the metapelites and metapsammites contain one or more of the minerals: chloritoid, paragonite, glaucophane, albite, chlorite, occasionally also Na-pyroxene and garnet. Amphibolite facies rocks contain relic garnet, plagioclase and hornblende, the latter two replaced by albite and blue amphibole, respectively. The zoning patterns of blue amphibole, garnet and chloritoid suggest their formation during prograde stage of metamorphism. P-T conditions of meta-morphism are estimated to be about 350-460 oC and 10-12 kbar.

  2. Bayesian inversion for facies detection: An extensible level set framework

    Cardiff, M.; Kitanidis, P. K.


    In many cases, it has been assumed that the variability in hydrologic parameters can be adequately described through a simple geostatistical model with a given variogram. In other cases, variability may be best described as a series of "jumps" in parameter behavior, e.g., those that occur at geologic facies contacts. When using indirect measurements such as pump tests to try to map such heterogeneity (during inverse modeling), the resulting images of the subsurface are always affected by the assumptions invoked. In this paper, we discuss inversion for parameter fields where prior information has suggested that major variability can be described by boundaries between geologic units or facies. In order to identify such parameter fields, we propose a Bayesian level set inversion protocol framework, which allows for flexible zones of any shape, size, and number. We review formulas for defining facies locations using the level set method and for moving the boundaries between zones using a gradient-based technique that improves fit through iterative deformation of the boundaries. We describe the optimization algorithm employed when multiple level set functions are used to represent a field with more than two facies. We extend these formulas to the investigation of the inverse problem in a Bayesian context in which prior information is taken into account and through which measures of uncertainty can be derived. We also demonstrate that the level set method is well suited for joint inversion problems and present a strategy for integrating different data types (such as hydrologic and geophysical) without assuming strict petrophysical relations. Our framework for joint inversion also contrasts with many previous methods in that all data sources (e.g., both hydrologic and geophysical) contribute to boundary delineation at once.




    Full Text Available Este artículo presenta los resultados de una simulación de flujo de agua subterránea en rocas fracturadas. Se emplea un enfoque estocástico (modelo estocástico equivalente en medio poroso fracturado para construir el modelo conceptual y para usar este último en la roca de baja permeabilidad encontrada en el sitio elegido como caso de estudio (Olkiluoto, Finlandia. La roca que se investiga se encuentra localizada alrededor de un grupo de pozos de sondeo y cubre un área de algunas hectáreas. Las mediciones de campo de pruebas de interferencia hidráulica se utilizan para calibrar el modelo de flujo de agua subterránea. Múltiples combinaciones de facies estocásticos se consideran para evaluar el impacto de la distribución y del número de facies en las cargas hidráulicas y en los caudales. Este estudio cuantifica la variabilidad de los resultados numéricos, lo cual es importante para el análisis de la incertidumbre en los sistemas hidrogeológicos. Por otra parte, este estudio muestra que el modelo conceptual de facies estocásticos es una alternativa adecuada a los modelos conceptuales de redes de fracturas discretas.

  4. Multiparameter Elastic Full Waveform Inversion With Facies Constraints

    Zhang, Zhendong


    Full waveform inversion (FWI) aims fully benefit from all the data characteristics to estimate the parameters describing the assumed physics of the subsurface. However, current efforts to utilize full waveform inversion as a tool beyond acoustic imaging applications, for example in reservoir analysis, faces inherent challenges related to the limited resolution and the potential trade-off between the elastic model parameters. Adding rock physics constraints does help to mitigate these issues, but current approaches to add such constraints are based on including them as a priori knowledge mostly valid around the well or as a boundary condition for the whole area. Since certain rock formations inside the Earth admit consistent elastic properties and relative values of elastic and anisotropic parameters (facies), utilizing such localized facies information in FWI can improve the resolution of inverted parameters. We propose a novel confidence map based approach to utilize the facies-based constraints in both isotropic and anisotropic elastic FWI. We invert for such a confidence map using Bayesian theory, in which the confidence map is updated at each iteration of the inversion using both the inverted models and a prior information. The numerical examples show that the proposed method can reduce the trade-offs and also can improve the resolution of the inverted elastic and anisotropic properties.

  5. Recent benthic foraminifera and sedimentary facies distribution of the Abu Dhabi (United Arab Emirates) coastline

    Fiorini, Flavia; Lokier, Stephen W.


    do not contain living foraminifera and the dead assemblage is mostly composed of a few specimens of coarse-sized Miliolidae with fragmented or abraded tests, probably transported from nearby environments. While the shallow-water settings of the Abu Dhabi coastline continue to be areas of active carbonate sedimentation, there have been significant changes in facies distributions over the last 50 years. In particular: × The opportunistic genera Ammonia and Elphidium have become more abundant. Reophax and Ammobaculites are reported in the area for the first time. × With anthropogenic activities some environments, such as inner lagoons, are lost whilst other areas show resilience to anthropogenic activities with little change in sedimentary facies distribution and foraminiferal assemblage. × No living foraminifera are found in dredged channels. The detailed analysis of these changes in foraminifera distribution and sedimentary facies allows us to further our understanding of the effects of anthropogenic activities on shallow-marine environments. By so doing, we are better able to distinguish between those changes that result from anthropogenic activities and those that are a result of naturally-occurring environmental perturbations.

  6. Relation between facies, diagenesis, and reservoir quality of Rotliegende reservoirs in north Germany

    David, F.; Gast, R.; Kraft, T. (BEB Erdgas Erdol GmbH, Hannover (Germany))


    In north Germany, the majority of Rotliegende gas fields is confined to an approximately 50 km-wide east-west-orientated belt, which is situated on the gently north-dipping flank of the southern Permian basin. Approximately 400 billion m[sup 3] of natural gas has been found in Rotliegende reservoir sandstones with average porosities of depths ranging from 3500 to 5000 m. Rotliegende deposition was controlled by the Autunian paleo-relief, and arid climate and cyclic transgressions of the desert lake. In general, wadis and large dunefields occur in the hinterland, sebkhas with small isolate dunes and shorelines define the coastal area, and a desert lake occurs to the north. The sandstones deposited in large dunefields contain only minor amounts of illite, anhydrite, and calcite and form good reservoirs. In contrast, the small dunes formed in the sebkha areas were affected by fluctuations of the desert lake groundwaters, causing the infiltration of detrital clay and precipitation of gypsum and calcite. These cements were transformed to illite, anhydrite, and calcite-II during later diagenesis, leading to a significant reduction of the reservoir quality. The best reservoirs occur in the shoreline sandstones because porosity and permeability were preserved by early magnesium-chlorite diagenesis. Since facies controls diagenesis and consequently reservoir quality, mapping of facies also indicates the distribution of reservoir and nonreservoir rocks. This information is used to identify play area and to interpret and calibrate three-dimensional seismic data.

  7. Computer vision enhances mobile eye-tracking to expose expert cognition in natural-scene visual-search tasks

    Keane, Tommy P.; Cahill, Nathan D.; Tarduno, John A.; Jacobs, Robert A.; Pelz, Jeff B.


    Mobile eye-tracking provides the fairly unique opportunity to record and elucidate cognition in action. In our research, we are searching for patterns in, and distinctions between, the visual-search performance of experts and novices in the geo-sciences. Traveling to regions resultant from various geological processes as part of an introductory field studies course in geology, we record the prima facie gaze patterns of experts and novices when they are asked to determine the modes of geological activity that have formed the scene-view presented to them. Recording eye video and scene video in natural settings generates complex imagery that requires advanced applications of computer vision research to generate registrations and mappings between the views of separate observers. By developing such mappings, we could then place many observers into a single mathematical space where we can spatio-temporally analyze inter- and intra-subject fixations, saccades, and head motions. While working towards perfecting these mappings, we developed an updated experiment setup that allowed us to statistically analyze intra-subject eye-movement events without the need for a common domain. Through such analyses we are finding statistical differences between novices and experts in these visual-search tasks. In the course of this research we have developed a unified, open-source, software framework for processing, visualization, and interaction of mobile eye-tracking and high-resolution panoramic imagery.

  8. Anachronistic facies in the Lower Triassic of South China and their implications to the ecosystems during the recovery time


    China further indicates that the appearance of anachronistic facies immediately following the mass extinction and the elimination from normal shallow marine facies with the radiation of Mesozoic marine faunas imply the natural response of the sedimentary systems and ecosystems to the great Paleozoic-Mesozoic transitional events and their induced harsh environments. Therefore, the ups and downs of the anachronistic facies may act as a proxy for the evolution of ecosystems independent of fossil analyses.

  9. Anachronistic facies in the Lower Triassic of South China and their implications to the ecosystems during the recovery time

    ZHAO XiaoMing; TONG JinNan; YAO HuaZhou; ZHANG KeXin; ZQ CHEN


    that the appearance of anachronistic facies immediately following the mass extinction and the elimination from normal shallow marine facies with the radiation of Mesozoic marine faunas imply the natural response of the sedimentary systems and ecosystems to the great Paleozoic-Mesozoic transitional events and their induced harsh environments.Therefore,the ups and downs of the anachronistic facies may act as a proxy for the evolution of ecosystems independent of fossil analyses.

  10. Gres porcelánico esmaltado producido por vía seca: materias primas fundentes

    Boschi, A. O.


    densificación y, por consiguiente, determinan la temperatura de cocción y la deformación piroplástica. Los agentes fundentes que se usan habitualmente en las composiciones de gres porcelánico son: feldespatos, filitas (usadas en Brasil y nefelinas. Estas materias primas no son solubles al agua, lo que las hace particularmente adecuadas para las composiciones de gres porcelánico tradicional producido por vía húmeda. Sin embargo, existe un gran grupo de materias primas solubles que también tienen un gran potencial como fundentes y que podrían utilizarse en los procesos de vía seca. En este contexto, el objetivo de este trabajo ha sido determinar el potencial fundente de las materias primas solubles al agua, o parcialmente solubles al agua, en una composición de gres porcelánico. La efectividad de varios boratos, es decir, la colemanita, la ulexita, la hidroboracita, así como el carbonato sódico, fueron ensayados en un estudio de tipo comparativo. Los resultados de este estudio indican que la incorporación de pequeñas cantidades de estos fundentes es suficiente para reducir la temperatura de cocción de forma importante, sin causar una alta deformación piroplástica de los soportes. Los mejores resultados se obtuvieron con las composiciones que contenían hidroboracita. Este resultado es especialmente relevante para la creación de composiciones alternativas de piezas de gres porcelánico producidas por vía seca. El proceso de vía seca es, en la actualidad, un tema de especial interés, debido a las cuestiones medioambientales y económicas.


    Indah Tri Lestari


    Full Text Available Tujuan dari penelitian ini adalah untuk mengetahui efektivitas metode pembelajaran role playing pada pokok bahasan mendeskripsikan pelayanan prima untuk meningkatkan hasil belajar siswa kelas X Administrasi Perkantoran SMK Hidayah Semarang. Subjek penelitian ini adalah siswa kelas X AP SMK Hidayah Semarang Tahun Ajaran 2011/2012. Prosedur penelitian ini merupakan siklus kegiatan pembelajaran yang terdiri dari dua siklus, dimana setiap siklus meliputi perencanaan, pelaksanaan tindakan, pengamatan dan refleksi. Instrumen pengumpulan data dalam penelitian ini adalah tes evaluasi yang berupa tes objektif pada tiap akhir siklus dan lembar observasi untuk aktivitas siswa dan kinerja guru. Hasil belajar kognitif siswa pada siklus I sebesar 74,5 dengan ketuntasan klasikal 66,7%. Rata-rata hasil belajar siklus II sebesar 82,5 dengan ketuntasan klasikal 96,7%. Adapun sikap siswa terhadap pembelajaran pada siklus I sebesar 55% dan pada siklus II mencapai peningkatan sebesar 87,5%. Sedangkan kinerja guru pada siklus I mencapai 58,3% dan pada siklus II meningkat menjadi 93,1%. Penerapan metode pembelajaran role playing pada pokok bahasan mendeskripsikan pelayanan prima efektif untuk meningkatkan hasil belajar siswa kelas X Administrasi Perkantoran SMK Hidayah Semarang. Abstract ___________________________________________________________________ The purpose from this research was to determine effectiveness of role playing in describing excellent service to improve students� result class X AP Hidayah Vocational School of Semarang year 2011/2012. The subject of this research is the class X AP of Hidayah Vocational School of Semarang year 2011/2012. The procedure of this research is a cycle of learning activities that consists of two cycles, in which each cycle includes planning, implementation of the action, observation and reflection. Instrument of data collection is the evaluation tests in the form of objective tests at each end of the cycle and observation

  12. 8 CFR 1245.8 - Adjustment of status as a special immigrant under section 101(a)(27)(K) of the Act.


    ... a prima facie determination regarding eligibility for naturalization benefits if the applicant is to... residence fails to complete his or her total active duty service obligation for reasons other than...

  13. 8 CFR 245.8 - Adjustment of status as a special immigrant under section 101(a)(27)(K) of the Act.


    ... a prima facie determination regarding eligibility for naturalization benefits if the applicant is to... residence fails to complete his or her total active duty service obligation for reasons other than...

  14. Facies patterns and depositional environments of Palaeozoic cephalopod limestones

    Wendt, J.; Aigner, T.


    In the eastern Anti-Atlas (Morocco) a platform and basin topography was established during the late Devonian, probably as a result of early Variscan tensional tectonics. Cephalopod limestones were deposited on shallow pelagic platforms, platform slopes and shallow, slowly subsiding basins. On the platform a transition from land areas into nearshore quartzose brachiopod coquinas, crinoidal limestones, condensed cephalopod limestones and finally into nodular limestones is observed. The latter often become disintegrated into incipient debris flows which pass into nodular limestone/marl alternations of a shallow basin. Deeper basins with shale sedimentation lack cephalopod limestones. Similar facies types also occur in the late Devonian of the Montagne Noire (France), Rheinisches Schiefergebirge (West Germany), Moravian Karst (Czechoslovakia), Holy Cross Mountains (Poland) and in the early Carboniferous of the Cantabrian Mountains (Spain). Due to strong late Variscan compressional tectonics and limited outcrops, detailed facies patterns could not be mapped in these regions, but the same facies types as in the eastern Anti-Atlas suggest similar coast/platform, slope and shallow basin topographies. During cephalopod limestone deposition water depth on the platforms was in the order of several tens to about one hundred metres, as is inferred from repeated subaerial exposures and distinctive depositional and faunal/floral features. Water depth in the adjacent shallow basins might have reached several hundreds of metres. Cephalopod limestones represent a typical stage in the evolution of geosynclines, characterized by extremely low sedimentation rates (1-5 m m.y. -1). This stage is preceded by deposition of thick neritic clastics and/or carbonates and is succeeded by deposition of deep-water clastics or flysch.

  15. Coal facies studies in Brazil. A short review

    Correa da Silva, Zuleika Carretta [Rua Eca de Queiroz, 682/402, 90670-020, Porto Alegre RS (Brazil)


    Coal facies studies in Brazil have been done for south Brazilian coal measures over the last 20 years using different methods for reconstructing paleoenvironments of peat formation and deposition. The first studies were based on Teichmuller's concept of macerals; from 1984 to 1993, microlithotypes and palynomorphs were used according to the methodology described by Hacquebard and Donaldson. In the 1990s, a new method of interpreting paleoenvironments implementing organic geochemistry, sequence stratigraphy and the use of biomarkers has become more common in the literature, as well as the use of Diessel's Gelification Index (GI) and Tissue Preservation Index (TPI)

  16. The ESPRI project: astrometric exoplanet search with PRIMA I. Instrument description and performance of first light observations

    Sahlmann, J; Queloz, D; Quirrenbach, A; Elias, N M; Launhardt, R; Pepe, F; Reffert, S; Segransan, D; Setiawan, J; Abuter, R; Andolfato, L; Bizenberger, P; Baumeister, H; Chazelas, B; Delplancke, F; Derie, F; Di Lieto, N; Duc, T P; Fleury, M; Graser, U; Kaminski, A; Koehler, R; Leveque, S; Maire, C; Megevand, D; Merand, A; Michellod, Y; Moresmau, J -M; Mohler, M; Mueller, A; Muellhaupt, P; Naranjo, V; Sache, L; Salvade, Y; Schmid, C; Schuhler, N; Schulze-Hartung, T; Sosnowska, D; Tubbs, B; van Belle, G T; Wagner, K; Weber, L; Zago, L; Zimmerman, N


    The ESPRI project relies on the astrometric capabilities offered by the PRIMA facility of the Very Large Telescope Interferometer for the discovery and study of planetary systems. Our survey consists of obtaining high-precision astrometry for a large sample of stars over several years and to detect their barycentric motions due to orbiting planets. We present the operation principle, the instrument's implementation, and the results of a first series of test observations. A comprehensive overview of the instrument infrastructure is given and the observation strategy for dual-field relative astrometry is presented. The differential delay lines, a key component of the PRIMA facility which was delivered by the ESPRI consortium, are described and their performance within the facility is discussed. Observations of bright visual binaries are used to test the observation procedures and to establish the instrument's astrometric precision and accuracy. The data reduction strategy for astrometry and the necessary correc...

  17. El tratamiento actuarial de los periodos de carencia y el contraseguro de primas en el seguro de dependencia.

    Ricote Gil, Fernando.


    Full Text Available La dependencia es un estado en el que se encuentran las personas que por razones ligadas a la falta o la pérdida de autonomía física, psíquica o intelectual tienen necesidad de asistencia y/o atención significativa para la realización los actos corrientes de la vida diaria. Dentro de la iniciativa privada, el sector asegurador juega un importante papel para la prestación de garantías derivadas de esta cobertura. Un aspecto fundamental en el estudio de esta cobertura es la consideración de los periodos de carencia y el tratamiento del contraseguro de primas durante los mismo. Se analiza el riesgo actuarial y su tratamiento en esta cobertura y la incidencia en la valoración actuarial de las primas por prestaciones de dependencia.

  18. L'universo prima del Big Bang cosmologia e teoria delle stringhe

    Gasperini, Maurizio


    Termini come "universo in espansione", "big bang", "singolarità iniziale" sono ormai entrati a far parte del linguaggio comune. L'idea che l'universo che oggi osserviamo abbia avuto origine da una grossa esplosione (big bang) è ormai ampiamente diffusa e accettata nella moderna cultura popolare, a tutti i libelli. Ma cosa c'era prima del big bang? E ha senso porsi questo interrogativo in un contesto scientifico? I recenti progressi della fisica teoria, e in particolare della cosiddetta teoria delle stringhe, suggeriscono una risposta a questa domanda, fornendo degli strumenti matematici capaci, in linea di principio, di ricostruire la storia dell'universo spingendosi anche oltre l'istante del big bang. Ne emerge un possibile scenario cosmologico nel quale l'universo, anzichè essere "appena nato" al momento del big bang, era piuttosto nel punto di mezzo della sua evoluzione, di durata probabilmente infinita. In questo libro si cerca di illustrare tale scenario usando un linguaggio non troppo tecnico, rivolt...

  19. Estimasi Nilai Pasar Wajar Ekuitas PT Prima Layanan Nasional Enjiniring Dalam Persiapan Initial Public Offering (IPO

    Ahmad Rizani


    Full Text Available PT Prima Layanan Nasional Enjiniring (PT PLN Enjiniring plans to conduct an initial public offering in 2012 that is intended for business development. Purpose of this research was to estimate the fair market value of equity of PT PLN Enjiniring in the framework of an initial public offering. Fair market value of equity of PT PLN Enjiniring is acquired by using discounted cash flow-free cash flow to equity method. Information used for this research come from two secondary data from financial reports and other information contained in the annual report 2008-2010 PT PLN Enjiniring years audited by public accountants, comperative financial reports, and company’s stock data comparison. The estimated fair market value of equity of PT PLN Enjiniring per December 31st 2011 by using the method of discounted cash flow-free cash flow to equity is obtained indication the fair market value of equity amounting to Rp2.583.155.716.515.

  20. Is the turbidite facies association scheme valid for interpreting ancient submarine fan environments?

    Shanmugam, G.; Damuth, J. E.; Moiola, R. J.


    Although turbidite facies reflect only processes of deposition, turbidite facies associations are routinely used to identify ancient submarine-fan subenvironments (e.g., upper fan, channel, lobe, etc.). The assumption that process of deposition also reflects environment of deposition may not be valid for the following reasons: (1) Mutti and Ricci Lucchi's facies association scheme for submarine fans has been developed exclusively from ancient turbidite sequences; however, the true relationship between such turbidite facies associations and related fan subenvironments has not been confirmed from modern fans; (2) individual channel-levee systems of many modern submarine fans are in many cases large enough to contain the entire ancient fan systems on which these facies associations are based; (3) large channel-levee systems comparable to those of modern fans have not been recognized in outcrops. Consequently, the validity of turbidite facies associations for interpreting ancient submarine-fan subenvironments must be considered tenuous until confirmed in modern fans.

  1. Facies del subfondo del canal Beagle, Tierra del Fuego Sub-bottom facies of the Beagle Channel, Tierra del Fuego

    Gustavo Bujalesky


    Full Text Available El canal Beagle conecta los océanos Pacífico y Atlántico en el extremo meridional de Sudamérica y se ubica en el ambiente subantártico. Conforma una cuenca de unos 300 m de profundidad máxima y está separada del océano Atlántico por un umbral de 30 m de profundidad. El canal es un valle tectónico que fue completamente cubierto por el hielo glacial durante la última glaciación. Posteriormente, el canal fue ocupado por un lago glacial desde los 12.000 a los 8.000 años A.P., cuando fue invadido por el mar que alcanzó un nivel máximo entre los 6.000 y 5.000 años A.P. Con el objetivo de analizar las facies sedimentarias superficiales y del subfondo del canal se realizó un relevamiento geofísico con sonar de barrido lateral y un perfilador de 3,5 kHz. Sobre un basamento constituido por rocas metamórficas del Mesozoico, se identificaron depósitos de till y secuencias granodecrecientes que representan distintos estadios del retroceso glaciar, evidenciando hacia la sección superior facies lacustres y por encima depósitos de la transgresión marina del Holoceno. Además, se han identificado paleocauces y secuencias fluviales cubiertas por sedimentos marinos transgresivos.The Beagle Channel connects the Pacific and Atlantic oceans in the southernmost part of South America, and has a subantarctic environment. It is a deep basin (300 m depth separated from the Atlantic Ocean by a shallow sill (30 m depth. The Beagle Channel is a tectonic valley that was completely covered by ice during the Last Glaciation. Later, it was occupied by a glacial lake from 12,000 to 8,000 years B.P. and then flooded by the sea, reaching a maximum sea level between 6,000 and 5,000 years B.P. A geophysical survey (side scan sonar and 3.5 kHz profiler was carried out in the channel to analyze the sea-bed and sub-bottom sedimentary facies. Metamorphic Mesozoic basement rocks are overlain by glacial deposits (till and fining upwards sequences. These sequences

  2. A review of 35 cases of asymmetric crying facies.

    Caksen, H; Odabaş, D; Tuncer, O; Kirimi, E; Tombul, T; Ikbal, M; Ataş, B; Ari Yuca, S


    A review of 35 cases of asymmetric crying facies: Congenital asymmetric crying facies (ACF) is caused by congenital hypoplasia or agenesis of the depressor anguli oris muscle (DAOM) on one side of the mouth. It is well known that this anomaly is frequently associated with cardiovascular, head and neck, musculoskeletal, respiratory, gastrointestinal, central nervous system, and genitourinary anomalies. In this article we report 35 ACF patients (28 children and 7 adults) and found additional abnormalities in 16 of them (i.e. 45%). The abnormalities were cerebral and cerebellar atrophy, mega-cisterna magna, mental motor retardation, convulsions, corpus callosum dysgenesis, cranial bone defect, dermoid cyst, spina bifida occulta, hypertelorism, micrognatia, retrognatia, hemangioma on the lower lip, short frenulum, cleft palate, low-set ears, preauricular tag, mild facial hypoplasia, sternal cleft, congenital heart defect, renal hypoplasia, vesicoureteral reflux, hypertrophic osteoarthropathy, congenital joint contractures, congenital hip dislocation, polydactyly, and umbilical and inguinal hernia. Besides these, one infant was born to a diabetic mother, and had atrial septal defect and the four other children had 4p deletion, Klinefelter syndrome, isolated CD4 deficiency and Treacher-Collins like facial appearance, respectively Although many of these abnormalities were reported in association with ACF, cerebellar atrophy, sternal cleft, cranial bone defect, infant of diabetic mother, 4p deletion, Klinefelter syndrome, isolated CD4 deficiency and Treacher-Collins like facial appearance were not previously published.

  3. Sedimentology and clast fabric of subaerial debris flow facies in a glacially-influenced alluvial fan

    Eyles, N.; Kocsis, S.


    A large alluvial fan (2 km 2), constructed between 11,000 and 7000 years B.P. at the mouth of Cinquefoil Creek in interior British Columbia, Canada, is identified as "glacially-influenced, debris flow-dominated". The fan was rapidly constructed during and immediately after deglaciation when large volumes of glacial debris were resedimented downslope; fans of this type are widespread in the glaciated portion of the North American Cordillera. Diamict facies, deposited as debris flows, account for 48% of the fan volume, sheetflodd gravels 37%, and other facies 15%. Diamicts show three facies types; crudely-bedded facies containing rafts of soft sediment that are attributed to downslope collapse and mixing of heterogeneous glacial deposits. These occur within the core of the fan. Massive and weakly graded (inverse to normal) diamict facies, derived from the downslope flow of weathered volcanic bedrock, occur within a well-defined bed that can be traced across the entire fan. The occurrence of weakly graded facies as lateral equivalents to massive facies within the same bed, implies the partial development of turbulent, high-velocity "streams" within a viscous debris flow moving over a slope of 6°. Clast fabrics in these facies show weakly-clustered a-axes dipping up and downslope comparable to other debris flows and lahars. The Cinquefoil fan, its internal structure and facies, provides a good "modern" analogue for ancient diamictite sequences deposited in areas of active uplift, rifting and glaciation.

  4. natural

    Elías Gómez Macías


    Full Text Available Partiendo de óxido de magnesio comercial se preparó una suspensión acuosa, la cual se secó y calcinó para conferirle estabilidad térmica. El material, tanto fresco como usado, se caracterizó mediante DRX, área superficial BET y SEM-EPMA. El catalizador mostró una matriz de MgO tipo periclasa con CaO en la superficie. Las pruebas de actividad catalítica se efectuaron en lecho fijo empacado con partículas obtenidas mediante prensado, trituración y clasificación del material. El flujo de reactivos consistió en mezclas gas natural-aire por debajo del límite inferior de inflamabilidad. Para diferentes flujos y temperaturas de entrada de la mezcla reactiva, se midieron las concentraciones de CH4, CO2 y CO en los gases de combustión con un analizador de gases tipo infrarrojo no dispersivo (NDIR. Para alcanzar conversión total de metano se requirió aumentar la temperatura de entrada al lecho a medida que se incrementó el flujo de gases reaccionantes. Los resultados obtenidos permiten desarrollar un sistema de combustión catalítica de bajo costo con un material térmicamente estable, que promueva la alta eficiencia en la combustión de gas natural y elimine los problemas de estabilidad, seguridad y de impacto ambiental negativo inherentes a los procesos de combustión térmica convencional.


    Yusi Rosalina


    Full Text Available This study was conducted to collect information regarding carbon storage, particularly the carbon stored in the aboveground biomass as well as in the peat soil. The study site was in a conservation area of the PT National Sago Prima belonging to the PT Sampoerna Agro Tbk. Group. The work was undertaken in January-February 2012. The total aboveground biomass and carbon storage in the research site indicates  that the conservation area is a secondary peat swamp forest, with the biomass of 149.18 ton/ha and carbon stock of 70.12 ton C/ha. The aboveground biomass and carbon consisted of biomass and carbon of tree (83.97 ton/ha containing 39.47 ton C/ha, respectively, saplings (20.69 ton/ha containing 9.72 ton C/ha and seedlings and undergrowth plants (0.03 ton/ha containing 0.01 ton C/ha, wood  necromass (24.06 ton/ha containing 11.31 ton C/ha, and litter (20.44 ton/ha containing 9.61 ton C/ha. An allometric equation was developed for Pandanus atrocarpus Griff. providing an estimated total biomass and carbon of 5.16 ton/ha containing 2.42 ton C/ha. The underground C with the mean peat depth of 5.5 m, mean bulk density of  0.18 g/cm3, and the mean organic C of 46.6 % was 464.895,94 ton C/ha. In the entire conservation forest area of 541 ha the total aboveground biomassa and carbon storage was estimated to be  80,708.64 ton and 37,934.00 ton C, while the total underground carbon was 238,96 million MT C.

  6. Latest Jurassic-early Cretaceous regressive facies, northeast Africa craton

    van Houten, F.B.


    Nonmarine to paralic detrital deposits accumulated in six large basins between Algeria and the Arabo-Nubian shield during major regression in latest Jurassic and Early Cretaceous time. The Ghadames Sirte (north-central Libya), and Northern (Egypt) basins lay along the cratonic margin of northeastern Africa. The Murzuk, Kufra, and Southern (Egypt) basins lay in the south within the craton. Data for reconstructing distribution, facies, and thickness of relevant sequences are adequate for the three northern basins only. High detrital influx near the end of Jurassic time and in mid-Cretaceous time produced regressive nubian facies composed largely of low-sinuosity stream and fahdelta deposits. In the west and southwest the Ghadames, Murzuk, and Kufra basins were filled with a few hundred meters of detritus after long-continued earlier Mesozoic aggradation. In northern Egypt the regressive sequence succeeded earlier Mesozoic marine sedimentation; in the Sirte and Southern basins correlative deposits accumulated on Precambrian and Variscan terranes after earlier Mesozoic uplift and erosion. Waning of detrital influx into southern Tunisia and adjacent Libya in the west and into Israel in the east initiated an Albian to early Cenomanian transgression of Tethys. By late Cenomanian time it had flooded the entire cratonic margin, and spread southward into the Murzuk and Southern basins, as well as onto the Arabo-Nubian shield. Latest Jurassic-earliest Cretaceous, mid-Cretaceous, and Late Cretaceous transgressions across northeastern Africa recorded in these sequences may reflect worldwide eustatic sea-level rises. In contrast, renewed large supply of detritus during each regression and a comparable subsidence history of intracratonic and marginal basins imply regional tectonic control. 6 figures.

  7. Facies del subfondo del canal Beagle, Tierra del Fuego

    Gustavo Bujalesky


    Full Text Available El canal Beagle conecta los océanos Pacífico y Atlántico en el extremo meridional de Sudamérica y se ubica en el ambiente subantártico. Conforma una cuenca de unos 300 m de profundidad máxima y está separada del océano Atlántico por un umbral de 30 m de profundidad. El canal es un valle tectónico que fue completamente cubierto por el hielo glacial durante la última glaciación. Posteriormente, el canal fue ocupado por un lago glacial desde los 12.000 a los 8.000 años A.P., cuando fue invadido por el mar que alcanzó un nivel máximo entre los 6.000 y 5.000 años A.P. Con el objetivo de analizar las facies sedimentarias superficiales y del subfondo del canal se realizó un relevamiento geofísico con sonar de barrido lateral y un perfilador de 3,5 kHz. Sobre un basamento constituido por rocas metamórficas del Mesozoico, se identificaron depósitos de till y secuencias granodecrecientes que representan distintos estadios del retroceso glaciar, evidenciando hacia la sección superior facies lacustres y por encima depósitos de la transgresión marina del Holoceno. Además, se han identificado paleocauces y secuencias fluviales cubiertas por sedimentos marinos transgresivos.

  8. Research on Diageneses of Cambrian Shoal Facies Carbonate Rocks in the Xiadong Area, Hubei Province

    张秀莲; 蒋凌志


    With continuous outcrops, developed shoal facies rocks, complete types of diagenesis and changeable diagenetic environments, Cambrian strata are well developed in the Xiadong area, Yichang, Hubei Province. Under the combined influence of numerous diageneses, secondary pores can be formed, which result in better reservoir properties of the rock strata. The Cambrian rocks in this area consist of mainly carbonate rocks and secondarily detrital rocks. The carbonate rocks are dominated by grainstones including wormkalk, calcirudite-calcarenite, oolitic limestone and oncolitic limestone. Graded bedding and cross bedding are well developed in the strata, which indicates that the formation environment is of a high-energy shoal facies. In this area, there has developed a sequence of stable Cambrian platform carbonate deposition. The evolution trend is as follows: open sea shelf facies? intertidal low-energy restricted sea facies? intertidal high-energy shoal facies? coastal shoal facies? evaporite tidal-flat facies. The diageneses that the strata have experienced mainly include dolomitization, dedolomitization and dissolution, which are constructive diageneses for the formation of secondary pores, such as intercrystal pores, intercrystal solution pores, gypsum mold pores and caverns of dolomite. The diagenetic facies intervals can be divided into the unitary and the compound ones, totalling 22 in the area. In the early atmospheric fresh-water diagenetic environment and the late epidiagenetic environment, Cambrian rocks, especially dolomite of the Middle and Upper Cambrian, experienced extensive and profound fresh water corrosion, forming pore intervals with a porosity ranging from 5% to 15%.

  9. Comparison of geostatistical kriging algorithms for intertidal surface sediment facies mapping with grain size data.

    Park, No-Wook; Jang, Dong-Ho


    This paper compares the predictive performance of different geostatistical kriging algorithms for intertidal surface sediment facies mapping using grain size data. Indicator kriging, which maps facies types from conditional probabilities of predefined facies types, is first considered. In the second approach, grain size fractions are first predicted using cokriging and the facies types are then mapped. As grain size fractions are compositional data, their characteristics should be considered during spatial prediction. For efficient prediction of compositional data, additive log-ratio transformation is applied before cokriging analysis. The predictive performance of cokriging of the transformed variables is compared with that of cokriging of raw fractions in terms of both prediction errors of fractions and facies mapping accuracy. From a case study of the Baramarae tidal flat, Korea, the mapping method based on cokriging of log-ratio transformation of fractions outperformed the one based on cokriging of untransformed fractions in the prediction of fractions and produced the best facies mapping accuracy. Indicator kriging that could not account for the variation of fractions within each facies type showed the worst mapping accuracy. These case study results indicate that the proper processing of grain size fractions as compositional data is important for reliable facies mapping.

  10. Comparison of Geostatistical Kriging Algorithms for Intertidal Surface Sediment Facies Mapping with Grain Size Data

    No-Wook Park


    Full Text Available This paper compares the predictive performance of different geostatistical kriging algorithms for intertidal surface sediment facies mapping using grain size data. Indicator kriging, which maps facies types from conditional probabilities of predefined facies types, is first considered. In the second approach, grain size fractions are first predicted using cokriging and the facies types are then mapped. As grain size fractions are compositional data, their characteristics should be considered during spatial prediction. For efficient prediction of compositional data, additive log-ratio transformation is applied before cokriging analysis. The predictive performance of cokriging of the transformed variables is compared with that of cokriging of raw fractions in terms of both prediction errors of fractions and facies mapping accuracy. From a case study of the Baramarae tidal flat, Korea, the mapping method based on cokriging of log-ratio transformation of fractions outperformed the one based on cokriging of untransformed fractions in the prediction of fractions and produced the best facies mapping accuracy. Indicator kriging that could not account for the variation of fractions within each facies type showed the worst mapping accuracy. These case study results indicate that the proper processing of grain size fractions as compositional data is important for reliable facies mapping.

  11. Facies discrimination in a mixed fluvio-eolian setting using elemental whole rock geochemistry

    Svendsen, Johan; Friis, Henrik; Stollhofen, Harald


    performed on the geochemical data has enabled discrimination of seven of the eight facies types. Furthermore, the facies discrimination method allowed a quantitative estimate of the degree of fluvial reworking of eolian sand. We believe that the method presented here, when calibrated to a reference well...

  12. Marine habitat mapping of the Milford Haven Waterway, Wales, UK: Comparison of facies mapping and EUNIS classification for monitoring sediment habitats in an industrialized estuary

    Carey, Drew A.; Hayn, Melanie; Germano, Joseph D.; Little, David I.; Bullimore, Blaise


    A detailed map and dataset of sedimentary habitats of the Milford Haven Waterway (MHW) was compiled for the Milford Haven Waterway Environmental Surveillance Group (MHWESG) from seafloor images collected in May, 2012 using sediment-profile and plan-view imaging (SPI/PV) survey techniques. This is the most comprehensive synoptic assessment of sediment distribution and benthic habitat composition available for the MHW, with 559 stations covering over 40 km2 of subtidal habitats. In the context of the MHW, an interpretative framework was developed that classified each station within a 'facies' that included information on the location within the waterway and inferred sedimentary and biological processes. The facies approach provides critical information on landscape-scale habitats including relative location and inferred sediment transport processes and can be used to direct future monitoring activities within the MHW and to predict areas of greatest potential risk from contaminant transport. Intertidal sediment 'facies' maps have been compiled in the past for MHW; this approach was expanded to map the subtidal portions of the waterway. Because sediment facies can be projected over larger areas than individual samples (due to assumptions based on physiography, or landforms) they represent an observational model of the distribution of sediments in an estuary. This model can be tested over time and space through comparison with additional past or future sample results. This approach provides a means to evaluate stability or change in the physical and biological conditions of the estuarine system. Initial comparison with past results for intertidal facies mapping and grain size analysis from grab samples showed remarkable stability over time for the MHW. The results of the SPI/PV mapping effort were cross-walked to the European Nature Information System (EUNIS) classification to provide a comparison of locally derived habitat mapping with European-standard habitat

  13. A short report of the investigations made on the facies of German coal deposits

    Dehmer, Janet [An den Rothen 96, D-97080 Wurzburg (Germany)


    In 1996, Commission II of the ICCP set up a coal facies working group. The first step was to collate literature on coal facies analysis for different countries. This report provides an overview on the investigations made on the facies interpretations of German coal deposits over the last 50 years with an emphasis on Tertiary coals. It outlines the major deposits present in Germany and gives the main facies interpretations of coals of lignite and bituminous rank. Furthermore, it points out that there lies a certain ambiguity in the interpretation of specific maceral associations, which could confuse facies analyses without the support of interdisciplinary studies and thus suggests that the working group should address this point for future work.

  14. Control of facies/potential on hydrocarbon accumulation:a geological model for Iacustrine rift basins

    Chen Dongxia; Pang Xiongqi; Zhang Shanwen; Wang Yongshi; Zhang Jun


    The formation and distribution of hydrocarbon accumulations are jointly controlled by"stratigraphic facies"and"fluid potential",which can be abbreviated in"control of facies/potential on hydrocarbon accumulation".Facies and potential control the time-space distribution of hydrocarbon accumulation macroscopically and the petroliferous characteristics of hydrocarbon accumulation microscopically.Tectonic facies and sedimentary facies control the time-space distribution.Lithofacies and petrophysical facies control the petroliferous characteristics.Favorable facies and high porosity and permeability control hydrocarbon accumulation in the lacustrine rift basins in China.Fluid potential is represented by the work required,which comprises the work against gravity,pressure,interfacial energy and kinetic energy.Hydrocarbon migration and accumulation are controlled by the joint action of multiple driving forces,and are characterized by accumulation in the area of low potential.At the structural high,low geopotential energy caused by buoyancy control anticlinal reservoir.The formation of lithological oil pool is controlled by low interfacial energy caused by capillary force.Low compressive energy caused by overpressure and faulting activity control the formation of the faulted block reservoir.Low geopotential energy of the basin margin caused by buoyancy control stratigraphic reservoir.The statistics of a large number of oil reservoirs show that favorable facies and low potential control hydrocarbon accumulation in the rift basin.where over 85% of the discovered hydrocarbon accumulations are distributed in the trap with favorable facies and lOW potentials.The case study showed that the prediction of favorable areas by application of the near source-favorable facies-low potential accumulation model correlated well with over 90% of the discovered oil pools' distribution of the middle section of the third member of the Shahejie Formation in the Dongying Depression,Bohai Bay

  15. Materias primas no tradicionales en la industria cerámica

    Caligaris, R.


    cerámicos con el fin de mejorar sus propiedades finales. Todos los compactos, obtenidos por prensado uniaxial de estos polvos, recibieron tratamientos térmicos adecuados a sus composiciones, para luego ser caracterizados por diversas técnicas entre las que se pueden mencionar: dilatometría, difracción de rayos X, porosidad, microdureza, microscopías óptica y electrónica de barrido y análisis por dispersión de energías. Del análisis de los resultados obtenidos en estos estudios, se concluyó que los materiales ensayados constituyen una potencial fuente de materia prima para la industria cerámica.

  16. Performance Refactoring of Instrumentation, Measurement, and Analysis Technologies for Petascale Computing. The PRIMA Project

    Malony, Allen D. [Univ. of Oregon, Eugene, OR (United States). Dept. of Computer and Information Science; Wolf, Felix G. [Wilhelm-Johnen-Strasse, Julich (Germany). Forschungszentrum Julich GmbH


    The growing number of cores provided by today’s high-­end computing systems present substantial challenges to application developers in their pursuit of parallel efficiency. To find the most effective optimization strategy, application developers need insight into the runtime behavior of their code. The University of Oregon (UO) and the Juelich Supercomputing Centre of Forschungszentrum Juelich (FZJ) develop the performance analysis tools TAU and Scalasca, respectively, which allow high-­performance computing (HPC) users to collect and analyze relevant performance data – even at very large scales. TAU and Scalasca are considered among the most advanced parallel performance systems available, and are used extensively across HPC centers in the U.S., Germany, and around the world. The TAU and Scalasca groups share a heritage of parallel performance tool research and partnership throughout the past fifteen years. Indeed, the close interactions of the two groups resulted in a cross-­fertilization of tool ideas and technologies that pushed TAU and Scalasca to what they are today. It also produced two performance systems with an increasing degree of functional overlap. While each tool has its specific analysis focus, the tools were implementing measurement infrastructures that were substantially similar. Because each tool provides complementary performance analysis, sharing of measurement results is valuable to provide the user with more facets to understand performance behavior. However, each measurement system was producing performance data in different formats, requiring data interoperability tools to be created. A common measurement and instrumentation system was needed to more closely integrate TAU and Scalasca and to avoid the duplication of development and maintenance effort. The PRIMA (Performance Refactoring of Instrumentation, Measurement, and Analysis) project was proposed over three years ago as a joint international effort between UO and FZJ to

  17. Performance Refactoring of Instrumentation, Measurement, and Analysis Technologies for Petascale Computing: the PRIMA Project

    Malony, Allen D. [Department of Computer and Information Science, University of Oregon; Wolf, Felix G. [Juelich Supercomputing Centre, Forschungszentrum Juelich


    The growing number of cores provided by today’s high-end computing systems present substantial challenges to application developers in their pursuit of parallel efficiency. To find the most effective optimization strategy, application developers need insight into the runtime behavior of their code. The University of Oregon (UO) and the Juelich Supercomputing Centre of Forschungszentrum Juelich (FZJ) develop the performance analysis tools TAU and Scalasca, respectively, which allow high-performance computing (HPC) users to collect and analyze relevant performance data – even at very large scales. TAU and Scalasca are considered among the most advanced parallel performance systems available, and are used extensively across HPC centers in the U.S., Germany, and around the world. The TAU and Scalasca groups share a heritage of parallel performance tool research and partnership throughout the past fifteen years. Indeed, the close interactions of the two groups resulted in a cross-fertilization of tool ideas and technologies that pushed TAU and Scalasca to what they are today. It also produced two performance systems with an increasing degree of functional overlap. While each tool has its specific analysis focus, the tools were implementing measurement infrastructures that were substantially similar. Because each tool provides complementary performance analysis, sharing of measurement results is valuable to provide the user with more facets to understand performance behavior. However, each measurement system was producing performance data in different formats, requiring data interoperability tools to be created. A common measurement and instrumentation system was needed to more closely integrate TAU and Scalasca and to avoid the duplication of development and maintenance effort. The PRIMA (Performance Refactoring of Instrumentation, Measurement, and Analysis) project was proposed over three years ago as a joint international effort between UO and FZJ to accomplish

  18. The earthing system of the PRIMA Neutral Beam Test Facility based on the Mesh Common Bonding Network topology

    Pomaro, Nicola, E-mail:; Boldrin, Marco; Lazzaro, Gabriele


    Highlights: • We designed a high performance earthing system for the ITER Neutral Beam Test Facility. • The system is based on the Mesh Common Bonded Network topology. • Careful bonding of all metallic structures allowed to obtain a well meshed system. • Special care was dedicated to improve EMC performance of critical areas like control rooms. • The facility experimental results will be representative also of the ITER situation. - Abstract: PRIMA is a large experimental facility under realization in Padova, aimed at developing and testing the Neutral Beam Injectors for ITER. The operation of these devices involves high RF power and voltage up to 1 MV. Frequent and high voltage electrical breakdowns inside the beam sources occur regularly. The presence of a distributed carefully optimized earthing system is of paramount importance to achieve a satisfying disturbances immunity for equipment and diagnostics. The paper describes the design and the realization of the earthing system of the PRIMA facility, which is based on the MESH-Common Bonding Network (MESH-CBN) topology, as recommended by IEC and IEEE standards for installations with high levels of Electromagnetic Interferences (EMI). The principles of the MESH-CBN approach were adapted to the PRIMA layout, which is composed by several buildings, that are independent for seismic and architectural reasons, but are linked by many electrical conduits and hydraulic pipelines. The availability of huge foundations, with a large number of poles and pillars, was taken into account; building parts dedicated to host control rooms and sensitive equipment were treated with particular care. Moreover, the lightning protection system was integrated and harmonized with the earthing system.

  19. Producción de etanol a partir de diferentes materias primas. Un análisis comparativo

    Miguel A. Otero; Gustavo Saura; Julio A. Martínez-Valdivielso


    Se analizan los indicadores de eficiencia de la producción de etanol a partir de diferentes fuentes de carbono en uso actual o perspectivo en la industria alcoholera. Los rendimientos de producción de etanol por hectárea de tierra sembrada y por tonelada de cosecha se discuten para maíz, caña, remolacha azucarera y yuca (Manihot utilísima), resultando que en términos de rendimiento en litros/t de materia prima, el maíz supera al resto de los productos analizados en más del doble, alcanzando 4...

  20. Predicción de precios de materias primas por medio del seguimiento de indicadores económicos

    Gómez Gómez, Daniel


    La predicción del comportamiento de la economía mundial se ha hecho más compleja con la globalización de las últimas décadas -- Al tener acceso a información en vivo, todos los fenómenos económicos se transmiten fácilmente de un lado del planeta al otro, afectando los mercados e industrias a un mayor ritmo que anteriormente -- Además de esto, esta sinergia ha llevado a una alta volatilidad de precios de las materias primas -- Sin embargo, existen métodos que permiten hacer un acercamiento a e...

  1. 论显要义务理论在酒店人力资源管理中的应用%The Use of the Theory of the Prima Facie Duty in Hotel Human Resources Management




  2. Surficial Sediment Facies features near the Myrtle Bend Confluence with the Kootenai River near Bonners Ferry, ID

    U.S. Geological Survey, Department of the Interior — The surficial bed-sediment facies, herein after referred to as the sediment facies, quantitatively describes the dominant sediment substrate on the surface of the...

  3. Distribution and composition of verdine and glaucony facies from the sediments of the western continental margin of India

    Thamban, M.; Rao, V.P.

    Investigations on green grains from sediments of the western continental margin of India, between Ratnagiri and Cape Comorin, (water depth 37-330 m) indicate the presence of verdine and glaucony facies. Verdine facies occurs over an area of about...

  4. Distinguishing fluvio-deltaic facies by bulk geochemistry and heavy minerals: an example from the Miocene of Denmark

    Olivarius, Mette; Rasmussen, Erik S.; Siersma, Volkert Dirk


    Interpretations of seismic profiles, gamma-ray logs and sediment descriptions were used to classify seven facies in Miocene fluvio-deltaic deposits ofDenmark. An impartial approach was adopted by not including analytical data in the facies definition. This approach allowed identification...... is found from the delta slope facies offshore to the delta toe and shelf facies. This trend is interpreted as a result of sorting by turbidity currents. The mixed origin of the transgressive lag facies is shown by the poorer sorting in this facies. By indicating the amount of alteration the sediments have...... been exposed to, the Ti-mineral maturity has proven useful in characterizing the facies. This systematic approach of tying depositional environments to a well-calibrated sequence stratigraphic model has generated analytical results which are valid as reference levels for future facies identifications....

  5. Assessing Biogenecity of Stromatolites: Return to the Facies

    Shapiro, R. S.; Jameson, S.; Rutter, A.; McCarthy, K.; Planavsky, N. J.; Severson, M.


    The discovery of richly microfossiliferous cherty stromatolites near Schreiber and Kakabeka Falls, Ontario, in the 1.9 Ga Gunflint Iron Formation, firmly established the field of pre-Cambrian paleontology. In the half-century since this discovery, paradigm shifts in the ecology of the microfossils as well as the utility of stromatolites as biological markers has caused a re-evaluation of our understanding of the pre-Cambrian fossil record. This research summarizes facies evaluation of the two stromatolite marker beds in the Gunflint-correlative Biwabik Iron Formation of Minnesota. The centimeter-scale microstratigraphy of cores drilled through the central and eastern Mesabi Iron Range was coupled with field descriptions of outcrops and mines in both the Biwabik and Gunflint iron formations. Eight lithologic facies associated with the stromatolites are identified: A) Pebble conglomerate clasts ranging in size of 0.5-3 cm, syneresis cracks, and septarian nodules with medium to coarse grain matrix; B) siltstone with subparallel sub-mm to 5 cm magnetitic and non-magnetic bands; C) stromatolitic boundstone comprising stratiform, pseudocolumnar, domal, undulatory, flat-laminated, dendritic, columnar, and mico-digitate forms and oncoids 0.5 to 2 cm diameter; D) grainstone with medium to coarse siliceous and carbonate ooids and peloids; E) massive green crystalline beds with bands of magnetite, quartz, calcite, disseminated pyrite and localized ankerite; F) autobreccicated fabric of 0.3 to 10 mm clasts; G) medium to coarse sandstone; H) quartzite. Correlation between 11 cores near Hoyt Lakes and 9 cores through the basal stromatolite layer at the MinnTac Mine near Virginia revealed that stromatolites formed both on conglomerate and medium quartz sandstone. Multiple forms of stromatolite may occur in a vertical succession (flat-laminated to undulatory to psuedocolumnar to columnar) or a core may be dominated by one type, typically columnar-stratiform. Where stromatolites do

  6. Early Childhood Development And Education Through Nature-Child Interactions: A Conceptual Paper

    Acar, İbrahim H.


    The present paper addresses following research questions: RQ1: How does nature or nature-based activities help children’s cognitive development? RQ2: How does nature or nature-based activities help children’s social and prosocial behavior development? RQ3: How does nature or nature-based activities enhance children’s learning abilities? To address these research questions, this paper will explore how nature helps young children’s cognitive, social, prosocial behavior development through prima...

  7. Facies discrimination in a mixed fluvio-eolian setting using elemental whole rock geochemistry

    Svendsen, Johan; Friis, Henrik; Stollhofen, Harald


    Fluvio-eolian successions are generally characterized by a high degree of complexity and internal heterogeneity. Quantifying the rapid facies changes in time and space is a major challenge to hydrocarbon reservoir characterisation.We present a method for facies discrimination in fluvio-eolian suc......Fluvio-eolian successions are generally characterized by a high degree of complexity and internal heterogeneity. Quantifying the rapid facies changes in time and space is a major challenge to hydrocarbon reservoir characterisation.We present a method for facies discrimination in fluvio......-eolian successions. The method is developed on the modern fluvio-eolian sediments from the Skeleton Coast dune field, Namibia. The examined sediments comprise eight different facies types; eolian dune sands, inter dune fluvial channel sands, intra erg mass flow deposits, intra erg hyperconcentrated flow deposits...... performed on the geochemical data has enabled discrimination of seven of the eight facies types. Furthermore, the facies discrimination method allowed a quantitative estimate of the degree of fluvial reworking of eolian sand. We believe that the method presented here, when calibrated to a reference well...




    Full Text Available The only occurrence of Tertiary (Oligocene sediments in the Dolomites at Monte Parei results from a complex tectonic and sedimentary history. The Tertiary marine clastic succession is sealing the Dinaric (Late Cretaceous to Paleogene deformed basement. The basin-fill can be differentiated into four lithofacies which show extensive lateral interfingering: ,local scarp breccias with giant blocks (facies A, chaotic breccias of debris flow origin (facies B, balanid and shell coquina beds (facies C and conglomeratic grain and debris flows with sandstone intercalations (facies D. Transport directions (imbricate clasts and cross bedding and petrographic composition indicate two different source areas. Sediments of facies B were shed from a structural high in the SW, while carbonate-siliciclastic debris of facies C and D originated from a pebbly or rocky shore in the N. Lithofacies and facies interrelationships clearly indicate the control by synsedimentary tectonic activity. Neoalpine closure of the basin by overthrusting lead to the preservation of the sediments. 

  9. Sedimentary facies of Maastrichtian to Danian deposits in Amur River area, Russian Far East

    Shigeyuki Suzuki; Abdul R. Ashraf; Hakuyu Okada


    Sedimentary facies of the Tsagayan Formation is distributed in the eastern Zeya-Bureya Basin has been analyzed. The formation is of the Maastrichtian to Danian in age and characterized by the cyclicity of the fining-upwards successions. Analysis of environmental changes during the K/T boundary is the focus of this study. Five facies have been identified: Facies A, thick and laterally extensive coarse-grained to medium-grained sandstone units, interpreted as channelfill deposits; Facies B, parallel-laminated to massive mudstone units interpreted as interchannel lakes and flood plain deposits; Facies C, sheet-like medium-grained to fine-grained sandstones interpreted as crevasse splay deposits;Facies D, coal to coaly mudstone beds interpreted as deposits ofpeatlands; Facies E, very poorly sorted sandy mudstone beds interpreted as debris flow deposits. Fluvial environments with the low-relief flat topography was inferred. A channel transported large volumes of clasts, and a flood basin with interchannel lakes and peatlands was deciphered. Any distinct change of sedimentary environments has not been identified throughout the Tsagayan Formation (including the K/T boundary). However, two beds of debris flow deposits were identified. The one occurs at the uppermost part of the lower Tsagayan Subformation and contains dinosaur fossils. The other is intercalated in the upper Tsagayan Subformation.

  10. Early Tertiary subsidence and sedimentary facies - Northern Sirte Basin, Libya

    Gumati, Y.D.; Kanes, W.H.


    The subsidence curves and subsidence rate curves for the Sirte basin, constructed from the stratigraphic record, show that subsidence was continuous throughout Late Cretaceous and Tertiary times, reaching a maximum during the Paleocene and Eocene, when a major reactivation of faults occurred. Shales and carbonates were deposited during all of the Late Cretaceous and Tertiary. Abrupt lateral facies changes occur from the platform areas toward the deeper troughs along with steep downdip thickening. The absence of upper Paleozoic and lower Mesozoic sediments suggests that the area was domed, faulted, and eroded during the late Mesozoic. As a result of crustal extension during the Paleocene, a marked lithologic and structural change occurred. The Heira Shale succeeded the Kalash Limestone in the Marada trough. Reactivation of the earlier faults, accompanied by an increase in the sediment supply from the south, caused these lower Paleocene shales to cover the entire area, with the exception of the old highs where carbonate deposition continued. An intercalation of shales and carbonates provides a sensitive indicator of change of depth and sediment type. 14 figures.

  11. Early Tertiary subsidence and sedimentary facies - northern Sirte Basin, Libya

    Gumati, Y.D.; Kanes, W.H.


    The subsidence curves and subsidence rate curves for the Sirte basin, constructed from the stratigraphic record, show that subsidence was continuous throughout Late Cretaceous and Tertiary times, reaching a maximum during the Paleocene and Eocene, when a major reactivation of faults occurred. Shales and carbonates were deposited during all of the Late Cretaceous and Tertiary. Abrupt lateral facies changes occur from the platform areas toward the deeper troughs along with steep downdip thickening. These conditions were probably assisted by contemporaneous faulting along structurally weak hinge lines where the dominant structural elements are normal step faults. The absence of upper Paleozoic and lower Mesozoic sediments suggests that the area was domed, faulted, and eroded during the late Mesozoic. As a result of crustal extension during the Paleocene, a marked lithologic and structural change occurred. The Heira Shale succeeded the Kalash Limestone in the Marada trough. Reactivation of the earlier faults, accompanied by an increase in the sediment supply from the south, caused these lower Paleocene shales to cover the entire area, with the exception of the old highs where carbonate deposition continued. An intercalation of shales and carbonates provides a sensitive indicator of change of depth and sediment type.

  12. Middle Eocene seagrass facies from Apennine carbonate platforms (Italy)

    Tomassetti, Laura; Benedetti, Andrea; Brandano, Marco


    Two stratigraphic sections located in the Latium-Abruzzi (Monte Porchio, Central Apennines, Central Italy) and in the Apulian carbonate platform (S. Cesarea-Torre Tiggiano, Salento, Southern Italy) were measured and sampled to document the sedimentological characteristic and the faunistic assemblages of Middle Eocene seagrass deposits. The faunistic assemblages are dominated by porcellaneous foraminifera Orbitolites, Alveolina, Idalina, Spiroloculina, Quinqueloculina, Triloculina and abundant hooked-shaped gypsinids, associated with hooked red algae and green algae Halimeda. Fabiania, rotaliids and textulariids as well as nummulitids are subordinated. The samples were assigned to Lutetian (SBZ13-16) according to the occurrence of Nummulites cf. lehneri, Alveolina ex. gr. elliptica, Idalina berthelini, Orbitolites complanatus, Slovenites decastroi and Medocia blayensis. At Santa Cesarea reticulate nummulites occur in association with Alveolina spp. and Halkyardia minima marking the lower Bartonian (SBZ17). Three main facies associations have been recognised: I) larger porcellaneous foraminiferal grainstones with orbitolitids and alveolinids deposited into high-energy shallow-water settings influenced by wave processes that reworked the sediments associated with a seagrass; II) grainstone to packstone with small porcellaneous foraminifera and abundant permanently-attached gypsinids deposited in a more protected (e.g., small embayment) in situ vegetated environment; III) bioclastic packstone with parautochthonous material reworked from the seagrass by rip currents and accumulated into rip channels in a slightly deeper environment. The biotic assemblages suggest that the depositional environment is consistent with tropical to subtropical vegetated environments within oligotrophic conditions.


    Luis Fernando Melo Velandia


    Full Text Available En este documento se estima una medida de compensación inflacionaria (Break Even Inflation usando los rendimientos de los bonos de deuda del gobierno colombiano (TES en pesos e indizados a unidades de valor real (UVR para el periodo comprendido entre enero de 2003 y noviembre de 2009. Esta medida se descompone en expectativas de inflación y prima por riesgo inflacionario. Las expectativas de inflación se calculan con base en la representación de estado espacio de un modelo afín de estructura a término extendido. Con objeto de mejorar los pronósticos, este modelo incorpora las expectativas de inflación a 12 meses de la encuesta mensual del Banco de la República. Los resultados muestran una tendencia a la baja tanto de las expectativas de inflación como de la prima por riesgo inflacionario. Esto puede deberse al aumento de la confianza en la política monetaria por parte de los agentes. Además, los resultados indican que a corto plazo, la compensación inflacionaria es un buen indicador de expectativas de inflación.

  14. Organic facies characteristics of the Carboniferous Pamucakyayla Formation, western Taurus, Antalya Nappes, Kemer (Antalya/Turkey)

    Bertan Gulludag, Cevdet; Altunsoy, Mehmet; Ozcelik, Orhan


    The study area is located in the western part of the Taurus Belt (SW Turkey). This region exhibits a complex structure involving two autochthonous units surrounded and imbricated with three allochthonous complexes. Antalya Nappes is a complex tectonic imbricate structure including sedimantary and ultrabasic rocks. In this study, organic facies characteristics of Carboniferous coaly units in the Pamucakyayla region (Kemer, Antalya-Turkey) were examined. The Carboniferous Pamucakyayla Formation, which is characterized by sandstone, claystone, marl and coaly units. This units includes different levels of coal seams in different thicknesses. Organic matter is composed predominantly of woody and amorphous material, with a minor contribution of planty and coaly material. Kerogen in the deposits is type II/III, as indicated by organic petrographic observations and Rock-Eval data. Total organic carbon (TOC) values are generally between 0.01 and 1.44 %, but reach 5.81 % in the formation. Tmax values vary between 446 and 451 °C and indicate mature zone (Based on the value of 0.25 % TOC). Organic facies type BC, C and CD were identified in the investigated units. Organic facies BC is related sandstoneand marl lithofacies. This facis is deposited under an anoxic water column in a fine grained clastics, where rapid deposition creates anoxia in the sediments after deposition. This facies is characterized by average values of HI around 317 (equivalent to type II kerogene), TOC around 0.02 %, and an average of S2 of 0.04 mg HC/g of rock. Organic facies C is related to sandstone, marl and coal lithofacies. This facies is characterized by average values of HI around 176 (equivalent to type III kerogene), TOC around 0.19 %, and an average of S2 of 0.03 mg HC/g of rock. The organic matter is partly oxidized, and terrestrial. Organic facies C is the "gas-prone" facies. Organic facies CD is related to limestone, marl and coal lithofacies. This facies is characterized by average values

  15. Calculo y comparacion de la prima de un reaseguro de salud usando el modelo de opciones de Black-Scholes y el modelo actuarial

    Luis Eduardo Giron


    Full Text Available La presente investigación pretende calcular y comparar la prima de un reaseguro  usando el modelo de opciones de Black-Scholes y el modelo clásico actuarial tradicional. El período de análisis va desde enero de 2011 hasta diciembre de 2012. Los resultados obtenidos muestran que el modelo de Black-Scholes, que se utiliza normalmente para valorar opciones financieras, puede ser también usado para la estimación de primas de reaseguros de salud; y que la prima neta estimada a partir de este modelo se aproxima a las establecidas por el método actuarial, excepto cuando el deducible del reaseguro es muy alto (por encima de $200.000.000.

  16. PET/CT assessment in follicular lymphoma using standardized criteria: central review in the PRIMA study

    Tychyj-Pinel, Christelle [Service de Medecine Nucleaire, Hospices Civils de Lyon, Centre Hospitalier Lyon Sud, Pierre-Benite (France); Ricard, Fabien [Service de Medecine Nucleaire, Hospices Civils de Lyon, Centre Hospitalier Lyon Sud, Pierre-Benite (France); Universite de Lyon, Faculte de Medecine, UCB Lyon 1, Lyon (France); Fulham, Michael [Royal Prince Alfred Hospital, Department of PET and Nuclear Medicine, Sydney (Australia); University of Sydney, Sydney Medical School, Sydney (Australia); Fournier, Marion [Centre Hospitalier Lyon Sud, The Lymphoma Academic Research Organisation (LYSARC), Pierre-Benite (France); Meignan, Michel [CHU Henri Mondor, Medicine Nucleaire, Creteil (France); Lamy, Thierry [Service d' Hematologie, CHU, Rennes (France); Vera, Pierre [Centre Henri Becquerel, Service de Medecine Nucleaire, Rouen (France); Rouen University, QuantIF (Litis EA4108), Rouen (France); Salles, Gilles [Universite de Lyon, Faculte de Medecine, UCB Lyon 1, Lyon (France); Service d' Hematologie, Hospices Civils de Lyon, Centre Hospitalier Lyon Sud, Pierre-Benite (France); Trotman, Judith [University of Sydney, Sydney Medical School, Sydney (Australia); Concord Hospital, Department of Haematology, Concord, NSW (Australia)


    We aimed to compare the standardized central review of {sup 18}F-fluorodeoxyglucose (FDG) positron emission tomography (PET)/CT scans performed after induction therapy for follicular lymphoma (FL) in the PRIMA study (Salles et al., Lancet 377:42-51, 2011; Trotman et al., J Clin Oncol 29:3194-3200, 2011) to scan review at local centres. PET/CT scans were independently evaluated by two nuclear medicine physicians using the 2007 International Harmonization Project (IHP) criteria (Cheson et al., J Clin Oncol 25:579-586, 2007; Juweid et al., J Clin Oncol 25:571-578, 2007; Shankar et al., J Nucl Med 47:1059-1066, 2006) and Deauville 5-point scale (5PS) criteria (Meignan et al., Leuk Lymphoma 50:1257-1260, 2009; Meignan et al., Leuk Lymphoma 51:2171-2180, 2010; Barrington et al., Eur J Nucl Med Mol Imaging 37:1824-1833, 2010). PET/CT status was compared with prospectively recorded patient outcomes. Central evaluation was performed on 119 scans. At diagnosis, 58 of 59 were recorded as positive, with a mean maximum standardized uptake value (SUV{sub max}) of 11.7 (range 4.6-35.6). There was no significant association between baseline SUV{sub max} and progression-free survival (PFS). Sixty post-induction scans were interpreted using both the IHP criteria and 5PS. Post-induction PET-positive status failed to predict progression when applying the IHP criteria [p = 0.14; hazard ratio (HR) 1.9; 95 % confidence interval (CI) 0.8-4.6] or 5PS with a cut-off ≥3 (p = 0.12; HR 2.0; 95 % CI 0.8-4.7). However, when applying the 5PS with a cut-off ≥4, there was a significantly inferior 42-month PFS in PET-positive patients of 25.0 % (95 % CI 3.7-55.8 %) versus 61.4 % (95 % CI 45.4-74.1 %) in PET-negative patients (p = 0.01; HR 3.1; 95 % CI 1.2-7.8). The positive predictive value (PPV) of post-induction PET with this liver cut-off was 75 %. The 42-month PFS for patients remaining PET-positive by local assessment was 31.1 % (95 % CI 10.2-55.0 %) vs 64.6 % (95 % CI 47.0-77.6 %) for PET

  17. Sobre producción de la materia prima (leche en el altiplano de Bolivia

    Apaza-Huallpa Yesenia


    Full Text Available Por la falta de mercados para acomodar la producción nacional de leche, muchos productores locales están reduciendo significativamente el número de sus vacas lecheras, que están siendo comercializadas como vacuno corriente en ferias o mataderos a un tercio del precio que tenían pocos años atrás. Actualmente existe una sobreproducción de leche en el departamento de La Paz y cada vez se reduce la demanda de la población, así los agricultores se quedan con el producto teniendo que darle otra finalidad, pero en muchos casos se vuelve inevitable por las grandes cantidades de materia prima, para regular esta crisis, que se ha visto agudizada, por los bajos precios internacionales de este alimento de primera necesidad, situación que estaría impulsando el ingreso de leche y productos procedentes de las países vecinos, de ahí que, es necesario realizar esfuerzos e inversiones para innovar y producir nuevas variedades de artículos lácteos, pue permitan ampliar el mercado, y así competir en mejores condiciones respecto a los productos foráneos. Sería iniciativas que necesitan apoyo del Estado para su materialización, por ejemplo con dotación de infraestructura industrial, fuentes de energía, exenciones impositivas a la importación de tecnología, mayor flexibilidad fiscal y laboral, facilidades de financiamiento, medidas orientadas a fomentar la producción láctea del país en particular y la industria nacional en general. El mercado de la leche se ve afectado por la presencia de leche en polvo de contrabando o legalmente importada, situación que un paquete de leche importada en polvo cuesta hasta 20 Bs., mientras que la Planta Industrializadora de Leche (PIL-Andina comercializa en 41.70 Bs. La leche es un nutrimento fundamental para la salud humana, su aporte en proteínas, calcio y vitaminas es absolutamente importante, sin embargo hay una tendencia muy arraigada, que la leche no le gusta a la población. Esta es una posici

  18. The Natural Antimicrobial Enzyme Lysozyme is Up-Regulated in Gastrointestinal Inflammatory Conditions

    Carlos A. Rubio


    Full Text Available The cells that line the mucosa of the human gastrointestinal tract (GI, that is, oral cavity, oesophagus, stomach, small intestine, large intestine, and rectum are constantly challenged by adverse micro-environmental factors, such as different pH, enzymes, and bacterial flora. With exception of the oral cavity, these microenvironments also contain remnant cocktails of secreted enzymes and bacteria from upper organs along the tract. The density of the GI bacteria varies, from 103/mL near the gastric outlet, to 1010/mL at the ileocecal valve, to 1011 to 1012/mL in the colon. The total microbial population (ca. 1014 exceeds the total number of cells in the tract. It is, therefore, remarkable that despite the prima facie inauspicious mixture of harmful secretions and bacteria, the normal GI mucosa retains a healthy state of cell renewal. To counteract the hostile microenvironment, the GI epithelia react by speeding cell exfoliation (the GI mucosa has a turnover time of two to three days, by increasing peristalsis, by eliminating bacteria through secretion of plasma cell-immunoglobulins and by increasing production of natural antibacterial compounds, such as defensin-5 and lysozyme. Only recently, lysozyme was found up-regulated in Barrett’s oesophagitis, chronic gastritis, gluten-induced atrophic duodenitis (coeliac disease, collagenous colitis, lymphocytic colitis, and Crohn’s colitis. This up-regulation is a response directed to the special types of bacteria recently detected in these diseases. The aim of lysozyme up-regulation is to protect individual mucosal segments to chronic inflammation. The molecular mechanisms connected to the crosstalk between the intraluminal bacterial flora and the production of lysozyme released by the GI mucosae, are discussed. Bacterial resistance continues to exhaust our supply of commercial antibiotics. The potential use of lysozyme to treat infectious diseases is receiving much attention.

  19. Sedimentary Facies and Distribution of Reservoir Rocks from the Feixianguan Formation in the Daxian-Xuanhan Region, NE Sichuan


    , solution openings (caves) and minute fissures. Macropores and coarse pore throats are common. The reservoir rocks are apparently controlled by sedimentary facies in distribution patterns. Vertically, they occur dominantly in the second and first members of the Feixianguan Formation, and laterally in the platform exposed shoals and restricted platforms, where good natural gas potential is expected.

  20. Facies and facies association of the siliciclastic Brak River and carbonate Gemsbok formations in the Lower Ugab River valley, Namibia, W. Africa

    Paciullo, F. V. P.; Ribeiro, A.; Trouw, R. A. J.; Passchier, C. W.


    The Neoproterozoic Zerrissene Turbidite Complex of central-western Namibia comprises five turbiditic units. From the base to the top they are the Zebrapüts Formation (greywacke and pelite), Brandberg West Formation (marble and pelite), Brak River Formation (greywacke and pelite with dropstones), Gemsbok River Formation (marble and pelite) and Amis River Formation (greywacke and pelites with rare carbonates and quartz-wacke). In the Lower Ugab River valley, five siliciclastic facies were recognised in the Brak River Formation. These are massive and laminated sandstones, classical turbidites (thick- and thin-bedded), mudrock, rare conglomerate and breccia. For the carbonate Gemsbok River Formation four facies were identified including massive non-graded and graded calcarenite, fine grained evenly bedded blue marble and calcareous mudrock. Most of these facies are also present in the other siliciclastic units of the Zerrissene Turbidite Complex as observed in other areas. The vertical facies association of the siliciclastic Brak River Formation is interpreted as representing sheet sand lobe to lobe-fringe palaeoenvironment with the abandonment of siliciclastic deposition at the top of the succession. The vertical facies association of the carbonate Gemsbok Formation is interpreted as the slope apron succession overlain by periplatform facies, suggesting a carbonate slope sedimentation of a prograding depositional shelf margin. If the siliciclastic-carbonate paired succession would represent a lowstand relative sea-level and highstand relative sea-level, respectively, the entire turbidite succession of the Zerrissene Turbidite Complex can be interpreted as three depositional sequences including two paired siliciclastic-carbonate units (Zebrapüts-Brandberg West formations; Brak River-Gemsbok formations) and an incomplete succession without carbonate at the top (Amis River Formation).

  1. Sensitivity to PRIMA-1MET is associated with decreased MGMT in human glioblastoma cells and glioblastoma stem cells irrespective of p53 status.

    Patyka, Mariia; Sharifi, Zeinab; Petrecca, Kevin; Mansure, Jose; Jean-Claude, Bertrand; Sabri, Siham


    Alterations of the TP53 tumor suppressor gene occur in ~30% of primary glioblastoma (GBM) with a high frequency of missense mutations associated with the acquisition of oncogenic "gain-of-function" (GOF) mutant (mut)p53 activities. PRIMA-1MET/APR-246, emerged as a promising compound to rescue wild-type (wt)p53 function in different cancer types. Previous studies suggested the role of wtp53 in the negative regulation of the DNA repair protein O6-methylguanine-DNA methyltransferase (MGMT), a major determinant in resistance to therapy in GBM treatment. The potential role of MGMT in expression of p53 and the efficacy of PRIMA-1MET with respect to TP53 status and expression of MGMT in GBM remain unknown. We investigated response to PRIMA-1MET of wtp53/MGMT-negative (U87MG, A172), mutp53/MGMT-positive U138, LN-18, T98/Empty vector (T98/EV) and its isogenic MGMT/shRNA gene knockdown counterpart (T98/shRNA). We show that MGMT silencing decreased expression of mutp53/GOF in T98/shRNA. PRIMA-1MET further cleared T98/shRNA cells of mutp53, decreased proliferation and clonogenic potential, abrogated the G2 checkpoint control, increased susceptibility to apoptotic cell death, expression of GADD45A and sustained expression of phosphorylated Erk1/2. PRIMA-1MET increased expression of p21 protein in U87MG and A172 and promoted senescence in U87MG cell line. Importantly, PRIMA-1MET decreased relative cell numbers, disrupted the structure of neurospheres of patient-derived GBM stem cells (GSCs) and enabled activation of wtp53 with decreased expression of MGMT in MGMT-positive GSCs or decreased expression of mutp53. Our findings highlight the cell-context dependent effects of PRIMA-1MET irrespective of p53 status and suggest the role of MGMT as a potential molecular target of PRIMA-1MET in MGMT-positive GSCs.

  2. PRIMA-1Met/APR-246 induces apoptosis and tumor growth delay in small cell lung cancer expressing mutant p53

    Zandi, Roza; Selivanova, Galina; Christensen, Camilla Laulund;


    Small cell lung cancer (SCLC) is a highly malignant disease with poor prognosis, necessitating the need to develop new and efficient treatment modalities. PRIMA-1(Met) (p53-dependent reactivation of massive apoptosis), also known as APR-246, is a small molecule, which restores tumor suppressor...... function to mutant p53 and induces cancer cell death in various cancer types. Since p53 is mutated in more than 90% of SCLC, we investigated the ability of PRIMA-1(Met) to induce apoptosis and inhibit tumor growth in SCLC with different p53 mutations....

  3. Facies architecture within a regional glaciolacustrine basin: Copper River, Alaska

    Bennett, Matthew R.; Huddart, David; Thomas, Geoffrey S. P.


    This paper defines the principal architectural elements present within the Pleistocene, glaciolacustrine basin-fill of the Copper River Basin in Alaska. The Copper River drains an intermontane basin via a single deeply incised trench through the Chugach Mountains to the Gulf of Alaska. This trench was blocked by ice during the last glacial cycle and a large ice-dammed lake, referred to as Lake Atna, filled much of the Copper Basin. Facies analysis within the basin floor allows a series of associations to be defined consistent with the basinward transport of sediment deposited along calving ice margins and at the basin edge. Basinward transport involves a continuum of gravity driven processes, including slumping, cohesive debris flow, hyperconcentrated/concentrated density flows, and turbidity currents. This basinward transport results in the deposition of a series of subaqueous fans, of which two main types are recognised. (1) Large, stratified, basin floor fans, which extend over at least 5 km and are exposed in the basin centre. These fans are composed of multiple lobes, incised by large mega-channels, giving fan architectures that are dominated by horizontal strata and large, cross-cutting channel-fills. Individual lobes and channel-fills consist of combinations of: diamict derived from iceberg rainout and the ice-marginal release of subglacial sediment; multiple units of fining upward gravels which grade vertically into parallel laminated and rippled fine sands and silts, deposited by a range of density flows and currents derived from the subaqueous discharge of meltwater; and rhythmites grading vertically into diamicts deposited from a range of sediment-density flows re-mobilising sediment deposited by either iceberg rainout or the ice-marginal release of sediment. (2) Small, complex, proximal fans, which extend over less than 2 km, and are exposed in the southern part of the basin. These fans are composed of coalescing and prograding lobes of diamict and

  4. Research on 3D Distribution of Meandering River Sand Body Using Sedimentary Facies Method and 3D Geological Modeling

    WU Jian; CAO Dai-yong


    Sedimentary facies study is an important method in describing the property and distribution of reservoir. 3D geological modeling is a powerful tool in 3D characterization of geological bodies. By combining the sedimentary facies study with 3D geological modeling to generate 3D sedimentary facies model, the 3D geometry and distribution feature of sand bodies can be more accurately characterized, particularly in 3D view. In Liuchu oilfield of Jizhong depression, the Ed2IV formation was recognized as meandering river deposition facies and five sedimentary facies were identified, which include point bar sand, levee, channel margin, abandoned channel and floodplain. All the 24 sand body facies in Ed2IV were mapped and the 3D sedimentary facies model established based on 2D facies maps. The result shows that the 3D sedimentary facies model is well matched for the research result of sedimentary facies. Being an extension of traditional sedimentary study, the 3D sedimentary facies model can be used to describe the 3D geometry and distribution orders of a single sand body more reliably and more accurately.

  5. ATL_FAC: usSEABED facies data for the entire U.S. Atlantic Coast

    U.S. Geological Survey, Department of the Interior — The facies data layer (_FAC.txt) is a point coverage of known sediment samplings, inspections, and probings from the usSEABED data collection and integrated using...

  6. Adenoid facies and chronic refractory rhinosinusitis managed by endoscopic-assisted adenoidectomy

    Sudhir M Naik


    Full Text Available Background /Objectives: To study 30 cases of patients of chronic adenoiditis with adenoid facies and refractory chronic rhinosinusitis managed by endoscopic assisted adenoidectomy. Materials and method: 7 cases of adenoid facies and 23 cases of chronic refractory rhinosinusitis with adenoiditis were managed by endoscopic assisted adenoidectomy during the study period of 12 months from August 2012 to July 2013. Result: endoscopic assisted adenoidectomy proves to be more effective in managing adenoid facies and chronic refractory rhinosinusitis with adenoid hyperplasia. Conclusion: visualization of the adenoid mass using endoscope helps complete removal of the diseased adenoids. Endoscopic assisted adenoidectomy is treatment of choice in adenoid facies and chronic refractory rhinosinusitis with adenoid hyperplasia and more effective than conventional adenoidectomy.

  7. Application of micro-seismic facies to coal bed methane exploration

    Li Donghui; Dong Shouhua; Zhang Cong; Deng Shuaiqi; Li Shujie


    A neural network is applied to high-quality 3-D seismic data during micro-seismic facies analysis to perform the waveform analysis and training on single reflection events.Modeled seismic channels are established and the real seismic channels are classified.Thus,a distribution of micro-seismic facies having a high precision over a flat surface was acquired.This method applied to existing geological data allows the distribution of areas rich in coal bed methane to be clearly defined.A distribution map of the micro-seismic facies in the research area is shown.The data accord well with measured methane contents,indicating that the analysis using micro-seismic facies is reliable and effective.This method could be applied to coal bed methane exploration and is of great importance to future exploration work and to an increase in the drilling success rate.

  8. Fluvial facies reservoir productivity prediction method based on principal component analysis and artificial neural network

    Pengyu Gao


    Full Text Available It is difficult to forecast the well productivity because of the complexity of vertical and horizontal developments in fluvial facies reservoir. This paper proposes a method based on Principal Component Analysis and Artificial Neural Network to predict well productivity of fluvial facies reservoir. The method summarizes the statistical reservoir factors and engineering factors that affect the well productivity, extracts information by applying the principal component analysis method and approximates arbitrary functions of the neural network to realize an accurate and efficient prediction on the fluvial facies reservoir well productivity. This method provides an effective way for forecasting the productivity of fluvial facies reservoir which is affected by multi-factors and complex mechanism. The study result shows that this method is a practical, effective, accurate and indirect productivity forecast method and is suitable for field application.

  9. Models for Facies and Compositional Variations in Gale Crater lake sediments, Mars

    Grotzinger, J. P.


    The Murray formation, Gale crater, Mars contains one major depositional facies - laminated mudstone - deposited in a lake; and minor additional facies - ripple cross laminated and trough cross bedded sandstones - representing subaqueous delta foreslope, fluvial, or eolian environments. The persistence of fine lamination, locally with scour and drape truncation surfaces, and absence of desiccation cracks, prism cracks, intraclasts, displacive evaporite crystals and nodules all suggest a perennial lake formed at depths great enough to avoid seasonal desiccation. Possible eolian and fluvial deposits would indicate base level lowering during longer-term lake level oscillation. Two compositional facies are observed based on elemental and mineralogic data, a hematite-sulfate (HS) facies and magnetite-silica (MS) facies. The HS facies comprises the lower few meters of stratigraphy exposed in the foothills of Mt Sharp, and transitions upward without any major change in the physical facies into the MS facies which persists through 10 meters up to higher levels in the Murray formation. Thinning of lamination from 2 mm to 0.5 mm coincides with the compositional facies transition. At the highest stratigraphic levels studied by Curiosity hematitic rocks are encountered again but lack significant sulfates that are not associated with later diagenesis; physical facies are a mixture of finely laminated mudstones and trough crossbedded fine sandstones. Two models best fit the physical and compositional data. In the first case, variations in the composition of fine clastic detritus delivered to the lake via marginal sediment plumes, coupled with redox oscillations in the composition of authigenic minerals precipitated from the lake. In the second model, originally reduced sediments of either detrital or authigenic origin are oxidized during burial diagenesis related to circulation of oxidizing groundwaters, converting reduced species, e.g. magnetite and sulfides, to hematite and Fe

  10. Sedimentary facies and paleoenvironmental interpretation of a Holocene marsh in the Gironde Estuary in France

    WANG Jianhua; MASSE Laurent; TASTET Jean-Pierre


    The Monards Marsh is located on the northeastern bank of the Gironde Estuary in France. Lithological, sedimentological and micropalaeontological investigations were made on four cores to determine the evolution of Holocene sedimentary environments and processes in this area over the last 6 000 a. Three main lithological facies are distinguished from bottom to top: (1) grey laminated silty-sandy clay; (2) homogeneous dark grey silty clay; and (3) compact silty clay. About 26 benthic foraminifera species are identified and divided into six groups according to their ecological characteristics. In association with lithology, sedimentary structures and grainulometry, the distribution of foraminifera group is used to define external slikke, internal slikke, external schorre, internal schorre, and continental marsh facies. Combined with 14C(AMS) dating, these data indicate four successive paleoenvironments in the Monards Marsh: (1) Holocene transgression resulted in the development of a basal schorre facies overlying fluvial deposits that transformed to slikke facies sedimentation; the transgression maximum occurred around 5 600 to 5 400 a BP and was inferred to be associated with the last phase of the rapid Holocene sea-level rise; (2) post-trangressive maximum sedimentation resulted in a regressive sequence of deposits prograding towards the estuary, corresponding to the stabilisation of sea level after 5 400 a BP; (3) a slight positive tendency in the sea level around 2 800 a BP recorded in the central part of the marsh; and (4) the wetland to a continental marsh environment. The sequential pattern for the evolution of wetlands in this estuarine area during the Holocene is fluvial facies-blackish schorre facies-slikke facies-blackish schorre facies-continental marsh facies. Characteristics of sedimentary facies distribution and evolution reveal that the development of Holocene salt marsh in this area was controlled by the sea-level change and tidal range. The


    Mirko Stjepanović


    Full Text Available In the period 1993-1997 investigations were conducted on natural low marshy grassland of facies Arrhenatheretum elatioris alopecurosum located 60 km west of Osijek and 7 km south of the river Drava. Variants of nitrogen fertilization, NPK fertilizers and non-fertilized were comprised in the investigation. Presence of 121 plant species of which 22 grass and grass-like species, 12 legumes and 87 other plant species was determined. On the average of five years grassland fertilization affected changes in density value of all plant groups. The highest grass density was found out with the variant fertilized with N120P12K120 and the highest legumes density appeared to be on non-fertilized variant. In 1997 Centaurea jacea, Cerastium holosteoides and Myosotis arvensis dissapeared from plant density of other species due to fertilization and mowing effect. Grasses Alopercurus pratensis and Poa pratensis var. angustifolia as well as leguminoses Trfolim pratense and Lathyrus pratensis are especially characterized by good fodder and density value.

  12. Adenoid facies and chronic refractory rhinosinusitis managed by endoscopic-assisted adenoidectomy


    Background /Objectives: To study 30 cases of patients of chronic adenoiditis with adenoid facies and refractory chronic rhinosinusitis managed by endoscopic assisted adenoidectomy. Materials and method: 7 cases of adenoid facies and 23 cases of chronic refractory rhinosinusitis with adenoiditis were managed by endoscopic assisted adenoidectomy during the study period of 12 months from August 2012 to July 2013. Result: endoscopic assisted adenoidectomy proves to be more effective in m...

  13. Stratigraphic Correlation of Middle Triassic Sequences among Different Paleogeographic Sedimentary Facies in South China


    Affected by the Indosinian movement, the sediments in the main part of South China, Yangtzeplatform, started to transform from marine to continental during the Middle Triassic. In the meantime, a noticeable paleogeographic and sedimentary facies differentiation occurred in the marginal regions of the platforms and produced completely different lithologic and paleontologicsequences in various paleogeographic gradients and sedimentary facies areas, which brought about the difficulties for the stratigraphic correlation based on the traditional stratigraphies. This paper proposes to use some characteristic environmental events as the markers of the stratigraphic corre lation across various paleogeographic sedimentary facies, considering that some distinctive regionalenvironmental events should have affected at the same time on the entire basin or the connectedsedimentary regions and produced some closely related sedimentary records in the stratigraphic sequences though the affected intensity and recorded pattern might be different among the regions.The change of violent relative sea level (generally water depth) and the alteration of tectonic activity summarized from the dynamic mechanism of sedimentation are the best markers of environmental events for stratigraphic correlation. Based on the analysis and recognition of some significantenvironmental events at the typical stratigraphic sequences from various paleogeographic sedimentary facies and combined with the consideration of the variations in expressed form and strength fthe events among different paleogeographic gradients and sedimentary facies, the stratigraphic sequences from different sedimentary facies can be easily correlated directly. Furthermore, the evolutionary history of the whole sedimentary basin can be clearly established.

  14. On quanta, mind, and matter: Hans Primas in Context. H. Atmanspacher, A. Amann, U. Müller-Herold (Eds), Kluwer, Boston, 1999, pp. 398 + viii, US192.00 £133.56 (hardback), ISBN 0-7923-5696-9

    Halvorson, Hans

    This book consists of a collection of 18 articles by students, colleagues, and friends of the theoretical chemist/philosopher of science, Hans Primas. Although the articles are written in honor of Primas, the editors state that the collection is not a Festschrift, but that it simply 'takes up some of the discussions that Primas has initiated or inspired' (p. 2). Due to the breadth of Primas' intellectual interests, the result is a highly eclectic collection of articles, whose topics range through (i) the historical development of experimental NMR spectroscopy, (ii) Jungian psychology, (iii) a defense of determinism in the rationalistic tradition of Leibniz, to (iv) a mathematical exposition of 'operator trigonometry.' However, since our space-and my expertise-is limited, the following comments will be restricted to those articles that deal with the mathematical and conceptual foundations of physics, a subject to which Primas has made a large contribution.

  15. Tertiary facies architecture in the Kutai Basin, Kalimantan, Indonesia

    Moss, Steve J.; Chambers, John L. C.


    The Kutai Basin occupies an area of extensive accommodation generated by Tertiary extension of an economic basement of mixed continental/oceanic affinity. The underlying crust to the basin is proposed here to be Jurassic and Cretaceous in age and is composed of ophiolitic units overlain by a younger Cretaceous turbidite fan, sourced from Indochina. A near complete Tertiary sedimentary section from Eocene to Recent is present within the Kutai Basin; much of it is exposed at the surface as a result of the Miocene and younger tectonic processes. Integration of geological and geophysical surface and subsurface data-sets has resulted in re-interpretation of the original facies distributions, relationships and arrangement of Tertiary sediments in the Kutai Basin. Although much lithostratigraphic terminology exists for the area, existing formation names can be reconciled with a simple model explaining the progressive tectonic evolution of the basin and illustrating the resulting depositional environments and their arrangements within the basin. The basin was initiated in the Middle Eocene in conjunction with rifting and likely sea floor spreading in the Makassar Straits. This produced a series of discrete fault-bounded depocentres in some parts of the basin, followed by sag phase sedimentation in response to thermal relaxation. Discrete Eocene depocentres have highly variable sedimentary fills depending upon position with respect to sediment source and palaeo water depths and geometries of the half-graben. This contrasts strongly with the more regionally uniform sedimentary styles that followed in the latter part of the Eocene and the Oligocene. Tectonic uplift documented along the southern and northern basin margins and related subsidence of the Lower Kutai Basin occurred during the Late Oligocene. This subsidence is associated with significant volumes of high-level andesitic-dacitic intrusive and associated volcanic rocks. Volcanism and uplift of the basin margins

  16. Stratigraphy and Facies Analysis of a 122 M Long Lacustrine Sequence from Chalco Lake, Central Mexico

    Herrera, D. A.; Ortega, B.; Caballero, M.; Lozano, S.; Pi, T.; Brown, E. T.


    Chalco lake is located SE of the outskirts of Mexico City, at the central part of the Trans Mexican Volcanic Belt. Previous studies show the importance of this lacustrine sequence as an archive of paleoenvironmental and paleoclimatic changes. A set of five cores up to 122 m depth were drilled in the basin, in order to analyze the sedimentary record and to extent the previous knowledge of past environmental changes in central Mexico. As an initial step, in this work we present the identification and classification of sedimentary facies. Preliminary paleomagnetism analyses recognize the possible record of the Blake Event (ca. 120 kyr BP), and suggest that the sequence might span the last 240 kyr. In this case, variations in sedimentary facies could reflect the conditions of the MIS 1-7. The facies are mostly diatom ooze, carbonate mud, organic rich silt and volcaniclastic, both massive and laminated, and massive dark gray to reddish brown silt. From 1 to 8 m depth dominates the organic rich silt facies, which correlates with the MIS 1. Intercalations of reddish brown and grayish brown silt facies, between 8 to 60 m depth, indicate changes occurred during MIS 2 to 5d. Between 60-75 m depth the sequence is characterized by dark grayish silty clay facies, which possibly coincide with the MIS 5e. At 79 m depth (ca. 130 kyr BP) we found struvite (MgNH4PO4.6H2O), which may be related to dry conditions. The laminated diatom ooze facies dominates between 90 to 122 m depth and indicates rhythmic changes in the sediment deposition of the basin. The volcaniclastic facies is represented by lapilli and ash deposits in more than 100 individual tephra layers of both mafic and felsic composition. Some of them correspond to main volcanic eruptions, as the Upper Toluca Pumice (13,500 cal yr BP), from the Nevado de Toluca volcano and the Pómez con Andesita (17,700 cal yr BP) from the Popocatépetl volcano. The carbonate mud facies is composed of calcite and siderite, with frequent

  17. Age and duration of eclogite-facies metamorphism, North Qaidam HP/UHP terrane, Western China

    Mattinson, C.G.; Wooden, J.L.; Liou, J.G.; Bird, D.K.; Wu, C.L.


    Amphibolite-facies para-and orthogneisses near Dulan, at the southeast end of the North Qaidam terrane, enclose minor eclogite and peridotite which record ultra-high pressure (UHP) metamorphism associated with the Early Paleozoic continental collision of the Qilian and Qaidam microplates. Field relations and coesite inclusions in zircons from paragneiss suggest that felsic, mafic, and ultramafic rocks all experienced UHP metamorphism and a common amphibolite-facies retrogression. SHRIMP-RG U-Pb and REE analyses of zircons from four eclogites yield weighted mean ages of 449 to 422 Ma, and REE patterns (flat HREE, no Eu anomaly) and inclusions of garnet, omphacite, and rutile indicate these ages record eclogite-facies metamorphism. The coherent field relations of these samples, and the similar range of individual ages in each sample suggests that the ???25 m.y. age range reflects the duration of eclogite-facies conditions in the studied samples. Analyses from zircon cores in one sample yield scattered 433 to 474 Ma ages, reflecting partial overlap on rims, and constrain the minimum age of eclogite protolith crystallization. Inclusions of Th + REE-rich epidote, and zircon REE patterns are consistent with prograde metamorphic growth. In the Lu??liang Shan, approximately 350 km northwest in the North Qaidam terrane, ages interpreted to record eclogite-facies metamorphism of eclogite and garnet peridotite are as old as 495 Ma and as young as 414 Ma, which suggests that processes responsible for extended high-pressure residence are not restricted to the Dulan region. Evidence of prolonged eclogite-facies metamorphism in HP/UHP localities in the Northeast Greenland eclogite province, the Western Gneiss Region of Norway, and the western Alps suggests that long eclogite-facies residence may be globally significant in continental subduction/collision zones.

  18. Cross-stratified Facies Observed by the Mars Science Laboratory Rover at Gale Crater, Mars

    Edgar, Lauren; Rubin, Dave; Grotzinger, John; Bell, Jim; Calef, Fred; Dromart, Gilles; Gupta, Sanjeev; Kah, Linda; Lewis, Kevin; Mangold, Nicolas; Schieber, Jurgen; Stack, Katie; Sumner, Dawn; MSL Science Team


    The Mars Science Laboratory Curiosity rover has investigated a number of sedimentary rock outcrops since landing in Gale crater. From the Rocknest location, during sols 59 to 100, Curiosity observed a range of cross-bedded deposits spanning more than 60 m in lateral extent. Cross-bedding is best exposed in an ~80-cm-thick outcrop known as Shaler. Observations using the Mast Cameras of cross-bedding both at Shaler and Rocknest enabled the recognition of several distinct cross-bedded facies. Analysis of cross-bedding geometries provides insight into the depositional environment. On the basis of inferred grain size, erosional resistance, color, and sedimentary structures, we have identified four facies: 1) resistant cross-stratified facies, 2) smooth, fine-grained cross-stratified facies, 3) dark gray, pitted facies, and 4) recessive, vertically fractured facies. Sedimentary structures include simple and compound cross-bedding, angular discontinuities between lamina sets, and potential soft-sediment deformation. Trough cross-bedding suggests that bedforms had sinuous crestlines. Cross-bed sets range from centimeter to decimeter in scale. Small cm-scale climbing ripples were identified in the vicinity of Rocknest. Where climbing bedforms are visible, they climb at subcritical angles, resulting in preservation of only the lee slopes. Analysis of cross-bedding dip directions indicate a range of sediment transport directions. Grain transport under turbulent flows was required to produce the observed cross-bedded facies. We consider three possible depositional environments: eolian, fluvial, and pyroclastic surge. Pyroclastic surge deposits often contain bedforms with supercritical angles of climb, evidence for unidirectional transport radially away from a point source, contain volcanic indicators such as bombs and accretionary lapilli, and display distinct trends in grain size and facies from proximal to distal deposits or in vertical section. These characteristics do not

  19. Depositional Model of the Marcellus Shale in West Virginia Based on Facies Analysis

    Bruner, Kathy


    A lithologic analysis of well exposed Marcellus outcrops has identified six different facies in West Virginia and neighboring states: (1) light gray calcareous shale, (2) fossiliferous limestone, (3) black calcareous shale, (4) black noncalcareous shale, (5) dark gray noncalcareous shale, and (6) K-bentonite. Close interbedding of these rock types attests to a complex, ever-changing environment on the eastern foreland ramp of the Appalachian Basin. The environmental setting was clearly not a deep trough, permanently anoxic, salinity stratified, sediment starved, and populated exclusively by phytoplankton—the traditional depositional model. To the contrary, our sedimentary data suggest a rather shallow water depth, intermittent anoxia, normal-marine salinity, a fluctuating input of siliciclastic mud, and faunal communities of low and moderate diversity. Interbedding of the shale and limestone lithofacies as well as the vertical stacking of facies associations is explained most simply by fluctuations in water depth coupled with fluctuations in sediment supply. The sea floor was, at times, immediately below wave base (Facies 1 and 2), around the depth of the thermocline (Facies 2 and 3), or below the thermocline (Facies 4 and 5), relative sea level changing through two sequences of lowstand, transgression, and highstand. Simultaneously the supply of siliciclastic mud was greater at times of lowstand (increased erosion) and highstand (prograding shoreline), and the supply smaller during transgression (sediment stored in distant coastal plain).

  20. Facies development and paleoenvironment of the Hajajah Limestone Member, Aruma Formation, central Saudi Arabia

    El-Sorogy, Abdelbaset S.; Ismail, Abdelmoneim; Youssef, Mohamed; Nour, Hamdy


    The Campanian Hajajah Limestone Member of the Aruma Formation was formed during two regressive episodes. Each of them formed of three depositional facies, from base to top: 1) intra-shelf basin facies, made up of fossiliferous green shale and mudstone with ostracods and badly preserved foraminifers. 2) fore-reef facies, consists of hard, massive, marly coralline limestone. The upper part is rich with low divers, badly to moderate preserved, solitary and colonial corals, and, 3) back reef and near-shore facies, consists of fossiliferous sandy dolomitized, bioturbated limestone with abundant reworked corals, bivalves, gastropods, and aggregate grains. On the basis of field observations, micro-and macrofossils and microfacies analysis, the Hajajah Limestone Member was deposited in distal marine settings below storm wave base in a low-energy environment changed upward to fore-reef framework in an open marine environment with moderate to high energy conditions and terminated with shallow marine facies with accumulation of skeletal grains by storms during regression.

  1. 'Prima furon le cose e poi i nomi'. Riflessioni attorno alla filosofia del linguaggio di Galileo

    Palmerino, C.R.


    This article addresses an aspect of Galileo’s thought that has hitherto attracted little attention, that is to say, his philosophy of language. First of all, we try to show that Galileo’s reflections on the ambiguous and conventional nature of verbal language, though not expounded systematically, pr

  2. 'Prima furon le cose e poi i nomi'. Riflessioni attorno alla filosofia del linguaggio di Galileo

    Palmerino, C.R.


    This article addresses an aspect of Galileo’s thought that has hitherto attracted little attention, that is to say, his philosophy of language. First of all, we try to show that Galileo’s reflections on the ambiguous and conventional nature of verbal language, though not expounded systematically,

  3. Sedimentary facies of the central part of radial tidal sand ridge system of the eastern China coast

    Yong YIN; Xinqin ZOU; Dakui ZHU; Jiaxiang HUANG


    A unique radial tidal sand ridge system (RTSRS) has developed under a complex tidal current field on the eastern China coast between the Yangtze River delta to the south and the abandoned Yellow River (Huanghe) delta to the north. The present study examines the sedimentary evolution of a ridge-channel pair in the central RTSRS. Three cores, with two on the ridges and one in the channel, were drilled to reveal the late Pleistocene-Holocene deposits of the system. Five sedimentary facies were distinguished, i.e. ridge-shallow subtidal facies, ridge-deep subtidal facies, near-surface channel bottom facies, middle tidal flat facies and low tidal flat facies. The ridge-shallow subtidal facies consists of sandy strata with ripple cross bed-dings, horizontal lamina, and massive beddings. Bioturbation seldom occurs. The ridge-deep subtidal facies is primarily characterized by sandy and muddy interlayers with common flaser and lenticular bedding structures. Bioturbation appears abundantly. Massive and graded sediment sequences of storm origin are pre-sent as characterized by rich shell fragments. The near-surface channel bottom facies consists of loose, soft, clayey silt deposits with deformed sedimentary layers. This facies occurs in the deeper part of the active chan-nels. The middle tidal flat and lower tidal flat facies composed of silt-clay couplets prevailed primarily in the tidal flats. Incomplete sedimentary successions show that coastal plain deposits dominate in the study area during 12-13 ka B.P. The sandy ridge and channel facies became dominant during 4 6 ka B.P. when the sea level receded temporarily. Tidal ridge and channel in the study area became active during the last four decades. Sediment reworking due to typhoon and sandy ridge migration plays a key role in shaping the present radial ridge system.

  4. The influence of facies heterogeneity on the doublet performance in low-enthalpy geothermal sedimentary reservoirs

    Crooijmans, R. A.; Willems, C. J L; Nick, Hamid


    A three-dimensional model is used to study the influence of facies heterogeneity on energy production under different operational conditions of low-enthalpy geothermal doublet systems. Process-based facies modelling is utilised for the Nieuwerkerk sedimentary formation in the West Netherlands Basin...... and the energy recovery rate for different discharge rates and the production temperature (Tmin) above which the doublet is working. With respect to the results, we propose a design model to estimate the life time and energy recovery rate of the geothermal doublet. The life time is estimated as a function of N....../G, Tmin and discharge rate, while the design model for the energy recovery rate is only a function of N/G and Tmin. Both life time and recovery show a positive relation with an increasing N/G. Further our results suggest that neglecting details of process-based facies modelling may lead to significant...


    Dyah Agustin Wulandari


    Full Text Available Mutu ikan kaleng tergantung pada kesegaran bahan mentah, cara pengalengan, peralatan dan kecakapan serta pengetahuan pelaksana-pelaksana teknis, sanitasi dan higiene pabrik dan lingkungan.  Kesegaran bahan mentah sangat penting dalam industri perikanan.  Kesegaran adalah tolak ukur untuk membedakan ikan jelek dan bagus kualitasnya.  Bila kualitas bahan mentah bagus, maka produk yang dihasilkan juga bagus.  Untuk mengendalikan mutu produk yang dihasilkan perusahaan diperlukan suatu sistem yang terkendali dan dapat mengendalikan seluruh aktifitas yang mempengaruhi mutu produk. Khusus untuk produk perikanan lahirnya konsep HACCP mendorong negara-negara maju menerapkan sistem pengawasan mutu ini kepada produsen sebagai jaminan mutu produknya. Dari hasi studi pustaka dan penelitian serta pengamatan langsung pada PT. Karya Manunggal Prima Sukses Muncar,  ternyata diketahui bahwa mutu bahan baku dan produk akhir berupa ikan kaleng sardine saus tomat yang dihasilkan sesuai dengan standart mutu SNI 01-3548-1994.  Sedangkan penerapan konsepsi HACCP belum terlaksana dengan baik sehingga diperlukan perbaikan, baik GMP dan SSOP pada unit pengolahan.Kata kunci : Mutu ikan kaleng, HACCP.  The quality of a certain tinned-fish depends on several things; those are the freshness of raw materials, tinning technique, devices, knowledge, and capability of the technicians, sanitation and hygienist of the factory. The freshness of raw materials is important in fishery industries.  Freshness is one of indicators in determining fish quality. If raw materials are in good quality so that the product will be. To maintain quality of a product in certain factory, system that are able to control all of the elements affecting product quality, is absolutely needed. In fishery product, availability of HACCP, encourage the advanced-countries to apply a monitoring system of product quality to the producer as a kind of quality guarantee. From the study of certain literature

  6. La legge civile ecclesiastica ticinese del 1855 nel quadro storico della prima metà dell’ottocento

    Antonio Angelucci


    Full Text Available Il contributo - segnalato dal Prof. Alessandro Ferrari, che ne attesta la scientificità e l’originalità - è destinato alla pubblicazione nella rivista  Il diritto ecclesiastico.  È stato realizzato grazie a un finanziamento della Fondazione Ferdinando e Laura Pica-Alfieri di Lugano.SOMMARIO: PRIMA PARTE – 1. Il contesto storico-politico e la produzione legislativa in materia ecclesiastica antecedente alla legge del 1855 – 2. La prima fase (1803-1829: dall’Atto di Mediazione al progetto di Statuto civile ed ecclesiastico del 1819 – 3. La seconda fase (1830-1839: la Costituzione del 4 luglio 1830 e l’opposizione tra istanze moderate e idee liberal-radicali – 4. La terza fase (1840-1847: il prevalere delle idee liberali – 5. La quarta fase (1848-1855: i provvedimenti antiecclesiastici degli anni tra il 1848 e il 1855 – SECONDA PARTE – 6. La legge civile ecclesiastica del 24 maggio 1855: genesi e contenuto. Dalle prime richieste di una legge al progetto del 1852 – 7. Il 1855: l’iter di formazione della legge – 8. L’intento programmatico della legge: gli articoli 1 e 2 – 9. Il contenuto della legge e la centralità del placet governativo – 10. Conclusioni.ABSTRACT: The essay describes the historical and political context, as well as the law production in Canton Ticino during the first half of the nineteenth-century, which will lead to the Civil Ecclesiastical Law of 1855. The article is structured in two parts. The first part deals with the historical period between 1803 and 1829 and is divided into four sections: from the Act of Mediation to the project of the Civil Ecclesiastical Statute of 1819; the Constitution of 1830; the predominance of liberal ideas and the anti-ecclesiastical measures from 1848 to 1855. The second part is entirely dedicated to the Civil Ecclesiastical Law of 1855 – peak of the historical political process described in the first part – and to the analysis of its origin and the

  7. Immune related transcriptional responses and performance of Litopenaeus vannamei post-larvae fed on dietary probiotic PrimaLac(®).

    Miandare, Hamed Kolangi; Yarahmadi, Peyman; Abbasian, Mahdi


    The present study investigated the effects of various levels of multi-strain probiotic on the immune related gene expression, digestive enzyme activity, growth performance, body chemical composition and survival of Litopenaeus vannamei post-larvae. After transferring post-larvae of L. vannamei to indoor conditions and subsequent acclimation to laboratory condition for 14 days, the shrimp were fed multi-strain probiotic at four different doses of 0, 0.25, 0.5 and 1.0 g kg(-1) for eight weeks. Shrimp fed 0.5 and 1.0 g kg(-1) probiotic PrimaLac(®) exhibited significantly (p < 0.05) higher weight gain, specific growth rate, body crude protein as well as lower FCR compared to other groups. Feeding on 0.5 and 1 g kg(-1) dietary multi-strain probiotic significantly (p < 0.05) increased the level of body crude protein. Oral administration of 0.5 and 1.0 g kg(-1) multi-strain probiotic significantly (p < 0.05) decreased body crude lipid and body moisture respectively. 30 days after feeding, protease, amylase and lipase activity increased in groups fed 0.5 and 1.0 g kg(-1) probiotic PrimaLac(®). However, on the 60th day, specific protease and amylase activity in all treatment groups were significantly higher than control group (p < 0.05) but lipase activity was higher (p < 0.05) in groups fed 0.5 and 1.0 g kg(-1) multi-strain probiotic. Oral administration of 1.0 g kg(-1) probiotic increased (p < 0.05) the level of prophenoloxidase and g-type lysozyme gene on day 30th and 60th after treatment. On day 30th and 60th, penaeidin gene expression was significantly higher in all treatment groups compared to the control group (p < 0.05). In general, findings of this study demonstrated that oral administration of 0.5 and 1.0 g kg(-1) multi-strain probiotic improved the performance of the fish and increased the expression of immune related genes.

  8. Facies conditions of the 2. Lusatian seam horizon in the area East of Peitz

    Boenisch, R.; Liskow, C.


    Characterizes the Miocene brown coal deposit in the area Peitz, Jaenschwalde and Guben (GDR) by methods of paleobotany and paleogeography. Results of macropetrographic facies analysis and geophysical borehole measurements were employed in the study. Geologic profiles of the region as well as maps of seam distribution were drawn up. The analysis proves that prehistoric river meanders divide the brown coal moor into a northern and a southern section. A description of the paleoenvironment and the sedimentation process is given. A correlation between coal facies and technological coal quality is pointed out. The study is being used to develop a geologic seam model for this brown coal mining area. 9 refs.

  9. Sequence associations of sedimentary facies in continental basins and their applications to palaeogeographic mapping

    TANG Hua-feng; CHENG Ri-hui; KONG Qing-ying; BAI Yun-feng; YU Ming-feng


    According to the characteristics of sedimentary facies and their vertical associations, sequence association of sedimentary facies can be divided into 2 types and 28 subtypes. The first type (type A) is a sedimentary sequence without volcanic rocks, including 18 subtypes. The second type (type B) is a volcanogenic succession including 10 subtypes.Each subtype may reflect certain filling condition under certain sedimentary environment. Time and space distribution of different types of sequence associations can reflect tectonics that controlled the basin evolution, sedimentary environments and palaeogeography.

  10. Utilización de cenizas volantes y mineralizadores como materia prima en la fabricación de cemento

    Palomo Sánchez, Ángel


    Full Text Available In this research the process of formation of a low energy clinker is studied, when fly-ashes (rich in sulphates and lime and fluorspar are used as raw materials (fly-ashes replaces to the tradicional raw mix partially. The availability of those fly-ashes is shown since clinker at 1.340 °C is obtained. The mineralogical composition, mineralizer capacity and temperature of formation of the new liquid phase is studied.

    En el presente trabajo se estudia el proceso de formación de un clínker de bajo consumo energético, empleando como materia prima cenizas volantes sulfocálcicas (en sustitución parcial del crudo tradicional y fluorita. Se demuestra la validez de dichas cenizas volantes, obteniendo clínker a 1.340 °C. Se estudia la composición mineralógica, capacidad de mineralización y temperatura de formación de la nueva fase líquida.

  11. Il formalismo russo, Roman Jakobson e la linguistica nella prima metà del Novecento

    Benedetta Baldi


    Full Text Available This article addresses the relation between Russian Formalism and linguistic thought in the first decades of the twentieth century. The theory of literary language proposed by the Formalist School assigns a central role to the linguistic devices that characterize a text as poetic or literary; the basic idea is that these devices work as a system, a notion derived from Saussurean linguistics. The leading figure we consider is Roman Jakobson, a key interpreter of Formalism, and, at the same time, an original and influential linguist. In his work the interpretation of poetic language is related to an overall linguistic theory, where the properties of natural languages, crucially phonology, and the use (functions of language have a theoretical characterization.

  12. Teater : Tänavused balletipreemiad. "Prima la Donna". Kontsertetendus "Sina ja mina". Rahvakultuur : Laste murdelaulu ja -luulepäevad tänavu Hageris / Vesta Uuetoa

    Uuetoa, Vesta


    Rahvusooperis laulab "Boheemis" külaline Soomest - Ari Grönthal. Kadrioru lossis antakse üle traditsioonilised balletiauhinnad. 20.-26. V toimub rahvusooperis Estonia ooperi ja balletifestival "Prima la Donna", mille teemaks on saatuslikud, tähelepanuväärsed ja jõulised naised. Kurt Weilli ja Lotte Lenya elu draamas ja muusikas on lavastanud Mart Kampus. 18. ja 19. mail saavad Hageris kokku murdelaulu ja -luulega tegelevad lapsed

  13. Handbook of efficient recommandations: Public Deliverable D6.4, PRIMA collaborative project, EU 7th Framework Programme, contract no. 212345

    Meyer, B.C.; Laplana, R.; Raley, M.; Baqueiro, O.; Kopeva, D.; Hautdidier, B.


    The Deliverable 6.4 “Handbook of efficient recommendations” deals with the main methodological developments in the context of screening, scoping and Sustainability Impact Assessment (SIA) developed and discussed in PRIMA. The main topics of this handbook deal with key aspects of the methodological enhancement of Impact Assessment within the context of experiences in Environmental Impact Assessment and Strategic Environmental Assessment. Key research is linked to the questions abou...

  14. Sedimentology of some facies from the Coris formation (Middle and Upper Miocene), Central Valley, Costa Rica, Central America; Sedimentologia de alunas facies de la formacion Coris (Mioceno Medio, Mioceno superiore), Valle Central, Costa Rica, America Central

    Obando, L.G.; Bottazzi, G.; Alvarado, F. [Universidad de Costa Rica, San Jose (Costa Rica). Escuela Centroamericana de Geologia


    In the Central Valley of Costa Rica exists a principal sandy-quartz sequence (Middle Miocene to Upper Miocene). Occasionally these rocks are interbedded with coal seams (lignite 0.3 to 1m thick) and siltstones very rich in organic matter. New data and reinterpretation of the sequences has permitted definition of the sedimentary facies: silicoclastic platform (mixed facies), open bay facies, bar facies (bar front (middle shoreface) and upper shoreface). Those facies represent a strand plain, generated by Miocene inter-oceanic currents, through the channel genetic related with the sinistral Costa Rica transcurrent fault system. That fault has segmented the national territory and generated the pull-apart basin in the Central Valley. This rapid subsidence accumulated thick shallow deposits. 27 refs., 5 figs.

  15. Facies analysis and paleoenvironmental reconstruction of Upper Cretaceous sequences in the eastern Para-Tethys Basin, NW Iran

    Omidvar, M.; Safari, A.; Vaziri-Moghaddam, H.; Ghalavand, H.


    Upper Cretaceous mixed carbonate-siliciclastic sequences are among the most important targets for hydrocarbon exploration in the Moghan area, located in the eastern Para-Tethys Basin. Despite of their significance, little is known about their facies characteristics and depositional environments. Detailed facies analysis and paleoenvironmental reconstruction of these sequences have been carried out in eight surface sections. Accordingly, four siliciclastic facies, eight carbonate facies and one volcanic facies have been recognized. Detailed facies descriptions and interpretations, together with the results of facies frequency analysis, standard facies models and Upper Cretaceous depositional models of Para-Tethys Basin, have been integrated and a non-rimmed carbonate platform is presented. This platform was affected by siliciclastic influx, in the form of coastal fan delta and submarine fans in the shallow- to deep-marine parts, respectively. This model is interpreted to be shallower in the central and northeastern parts of the Moghan area. Toward the southeast and southwest, this shallow platform turns into deep marine settings along steep slopes without remarkable marginal barriers. (Author)

  16. Identification of hydrochemical facies in the Roswell Artesian Basin, New Mexico (USA), using graphical and statistical methods

    Newman, Brent D.; Havenor, Kay C.; Longmire, Patrick


    Analysis of groundwater chemistry can yield important insights about subsurface conditions, and provide an alternative and complementary method for characterizing basin hydrogeology, especially in areas where hydraulic data are limited. More specifically, hydrochemical facies have been used for decades to help understand basin flow and transport, and a set of facies were developed for the Roswell Artesian Basin (RAB) in a semi-arid part of New Mexico, USA. The RAB is an important agricultural water source, and is an excellent example of a rechargeable artesian system. However, substantial uncertainties about the RAB hydrogeology and groundwater chemistry exist. The RAB was a great opportunity to explore hydrochemcial facies definition. A set of facies, derived from fingerprint diagrams (graphical approach), existed as a basis for testing and for comparison to principal components, factor analysis, and cluster analyses (statistical approaches). Geochemical data from over 300 RAB wells in the central basin were examined. The statistical testing of fingerprint-diagram-based facies was useful in terms of quantitatively evaluating differences between facies, and for understanding potential controls on basin groundwater chemistry. This study suggests the presence of three hydrochemical facies in the shallower part of the RAB (mostly unconfined conditions) and three in the deeper artesian system of the RAB. These facies reflect significant spatial differences in chemistry in the basin that are associated with specific stratigraphic intervals as well as structural features. Substantial chemical variability across faults and within fault blocks was also observed.

  17. Seismic-geometric facies model of lacustrine carbonates of Morro do Chaves Formation, Sergipe-Alagoas Basin; Modelagem sismica-geometrica de facies dos carbonatos lacustres da Formacao Morro do Chaves, Bacia de Sergipe-Alagoas

    Kinoshita, Eliseu Massaaki [Internacional America Latina PETROBRAS Colombia (Colombia). E e P. UN-COL. Gerencia de Ativos Offshore], e-mail:


    Sergipe-Alagoas Basin, to the seismic facies of a high-resolution seismic section (out thrust-1) from the same outcrop This model was based on the interaction of three models: the Integration Facies Model; Stratigraphic- Structural Facies Model and Velocity Facies Model. The first relates the gamma-rays, sonic velocity, porosity and geometry information with the kinds of facies associations. The second is the result of the integration of the first model with the outcrop 3-D Laser-scanner topographic image and the structural geometric observations. The last is the representation of the substitution of the facies associations of the second model for their respective sonic velocities. This last model was the input parameter to the 2-D acoustic model, which produced a synthetic seismic section of the outcrop of a similar standard to the high-resolution section of out thrust-1. The out thrust-1 high-resolution seismic section interpretation, based on the Seismic-Geometric Facies Model, demonstrated that the facies associations found in the shallow drill hole S-217 and well FU-107, both 50m from the seismic line, correlate in the same seismic-stratigraphic level. More importantly, the geometries of the seismic facies found in the stratigraphic and structural positions were consistent with those observed in the outcrop geological structural analysis. This evidence indicates that the seismic model of the coquinas outcrop, Morro do Chaves Formation, may be used as an analogue model in hydrocarbon exploration and production activities, particularly in the coquinas facies reservoirs of the Lagoa Feia Formation, Campos Basin. (author)

  18. The intrusive complexof the Island of Giglio: geomagnetic characteristics of plutonic facies with low susceptibility contrast

    R. Cavallini


    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.

  19. Upper Cretaceous chalk facies and depositional history recorded in the Mona-1 core, Mona Ridge

    Anderskouv, Kresten; Surlyk, Finn


    -slope evolution of debris flows. Debris flows are rep­resented by matrix-supported conglomerates, which form one of the most common facies in the succession. High-concentration, gravity-driven suspension flows passed into dilute visco-plastic flows during the final stages of deposition and resulted...

  20. Facies Analysis of Fahliyan Formation in North Dezful Embayment, Southwest Iran: Implications for Porosity Distribution

    Sabouhi, M.; Jahani, D.; Taati Qurayem, F.; Aminzadeh, A.


    Fahliyan Formation (Neocomian) is one of the important hydrocarbon reservoirs of khami group in south west of Iran. This Formation has 332m thickness in type section and mainly consist of carbonate rocks. In this study, the Fahliyan Formation was investigated in subsurface section of AZN#B Well in the north Dezful Embayment (with281m thickness). Lower boundary of Fahliyan Formation with Garau Formation is continuous and the upper contact with Gadvan formation is conformable According to this study 13 carbonate microfacies and one shaily facies were recognized which are grouped into four facies associations(micro facies group). These facies associations present platform to basin depositional setting and are nominated as : A (Tidal-flat), B (Lagoon), C (Bar) and D (Open marine). Based on available data set including cutting samples, thin sections and well log analysis, it seems the Fahliyan Formation was deposited in a Carbonate shelf setting and the studied profile indicates the shallowest part of the platform. Secondary porosities due to dolomitization and Stylolitization played an important role in increasing reservoir quality of the formation. Other types of porosities occupied by later cementations and had no contribution in reservoir quality.

  1. Fenomenologia in "prima" e in "terza" persona: Searle e Dennett critici di Husserl

    Federica Buongiorno


    Full Text Available “First” and “Third” Person Phenomenology: Searle and Dennett Critics of Husserl - In this paper I compare Searle’s and Dennett’s philosophies of mind with Husserl’s theory of consciousness. My aim is to show how they modified the phenomenological concept of intentionality turning it into a “third-person” model of description. This change leads to problematic consequences concerning mainly (i the distinction between a mental act and its content, and the related criticism of the representational theory of mind; (ii the Cartesian Theater argument and the related Homunculus argument as well as the claim that the notion of subjectivity needs to be dismantled; (iii the rejection of the Unconscious. I my view Searle’s and Dennett’s positions follow from embracing a contradictory notion of reductionism, which is also implicit in the developments of “naturalized phenomenology” and neurophenomenology. These difficulties cannot be solved by adapting or applying the phenomenological method to cognitive sciences, nor even by merely returning to Husserl’s theory. Rather, we need to determine what specific problems can be phenomenologically addressed in a scientific context: for instance the temporal structure of consciousness and the issue of the unconscious contents of mind.

  2. Modern foraminiferal facies in a subtropical estuarine channel, Bertioga, São Paulo, Brazil

    Eichler, P.P.B.; Eichler, B.B.; De Miranda, L. B.; Rodrigues, A.R.


    Numerical analyses of modern foraminiferal abundance and environmental data from the Bertioga Channel (Sa??o Paulo, Brazil) reveal multiple biofacies within an overall paralic setting. Despite its fisheries, mariculture and attraction to tourists, the environmental state of Bertioga Channel remains poorly studied. The present investigation is an attempt to partly fill this gap; the parameters examined include depth, salinity, temperature, organic carbon, sulfur content and bottom sediment type. Muddy sediments with high organic carbon content derived from land drainage are found in the inner parts of the channel, whereas sandy sediment dominates the areas adjacent to the Atlantic Ocean. In the eastern entrance to the channel, sandy sediment contain species of Rotaliida from Facies 1 (including Elphidium discoidale, Elphidium poeyanum, Hanzawaia boueana, Pararotalia cananeiaensis and Nonionella atlantica), reflecting normal marine salinity. Sediments with high percentages of silt and clay in polyhaline and eurybaline environments of the eastern part and Itapanhau?? River contain Facies 2, which includes Ammonia beccarii and Pararotalia cananeiaensis. In the western entrance and central, western and eastern parts, where salinities vary from 18 to 30 psu and the sediments contain both low and high organic carbon, the foraminifera from Facies 3 are dominated by Quinqueloculina milletti, Arenoparrella mexicana, Pararotalia cananeiaensis, Ammonia beccarii, Buliminella elegantissima, Elphidium sp., Elphidium excavatum, Elphidium gunteri and Elphidium poeyanum. In mesohaline and polyhaline waters of the central part, the organic-carbon-rich silt and clay contain Facies 4, which includes Ammonia beccarii, Pararotalia cananeiaensis, Elphidium excavatum and Elphidium sp. Most of organic-carbon-enriched, silty-clay substrates that are subject to the highest fresh-water discharge and high bottom temperatures support two different assemblages: one of mostly Rotaliina and the

  3. Parts-based geophysical inversion with application to water flooding interface detection and geological facies detection

    Zhang, Junwei

    I built parts-based and manifold based mathematical learning model for the geophysical inverse problem and I applied this approach to two problems. One is related to the detection of the oil-water encroachment front during the water flooding of an oil reservoir. In this application, I propose a new 4D inversion approach based on the Gauss-Newton approach to invert time-lapse cross-well resistance data. The goal of this study is to image the position of the oil-water encroachment front in a heterogeneous clayey sand reservoir. This approach is based on explicitly connecting the change of resistivity to the petrophysical properties controlling the position of the front (porosity and permeability) and to the saturation of the water phase through a petrophysical resistivity model accounting for bulk and surface conductivity contributions and saturation. The distributions of the permeability and porosity are also inverted using the time-lapse resistivity data in order to better reconstruct the position of the oil water encroachment front. In our synthetic test case, we get a better position of the front with the by-products of porosity and permeability inferences near the flow trajectory and close to the wells. The numerical simulations show that the position of the front is recovered well but the distribution of the recovered porosity and permeability is only fair. A comparison with a commercial code based on a classical Gauss-Newton approach with no information provided by the two-phase flow model fails to recover the position of the front. The new approach could be also used for the time-lapse monitoring of various processes in both geothermal fields and oil and gas reservoirs using a combination of geophysical methods. A paper has been published in Geophysical Journal International on this topic and I am the first author of this paper. The second application is related to the detection of geological facies boundaries and their deforation to satisfy to geophysica

  4. Facies and depositional architecture according to a jet efflux model of a late Paleozoic tidewater grounding-line system from the Itararé Group (Paraná Basin), southern Brazil

    Aquino, Carolina Danielski; Buso, Victoria Valdez; Faccini, Ubiratan Ferrucio; Milana, Juan Pablo; Paim, Paulo Sergio Gomes


    -laden nature of the flows. At the transitional zone, a hydraulic jump produces a rapid shift of conglomeratic to sandy facies with associated scour features. Towards the distal zones, the jet detaches to originate a vertical turbulent jet characterized by more diluted flows. Discussion of fan facies and architecture within a framework of jet-efflux dynamics provides an improved understanding of grounding-line fans systems that produce coarse-grained strata commonly enclosed by fine-grained rocks. The results have clear implication in terms of prediction of facies tract and geometry of oil and gas reservoirs deposited under similar conditions. And also can be useful to identifying the position of a glacial terminus through time.

  5. Residuos cerámicos para su posible uso como materia prima en la fabricación de clínker de cemento Portland: caracterización y activación alcalina

    Martínez-Ramírez, S.


    Full Text Available The world-wide cement industry is seeking experimental avenues that will lead to cement production that is less energy-intensive, less damaging to the surrounding environment and less prolific in GHG emissions. In Spain and Europe in general, this approach is wholly consistent with the concept of sustainability and compliance with the Kyoto Protocol. The use of different kinds of industrial waste and by-products as alternative materials in cement manufacture has proved to be a very effective way of contributing to such sustainability. These alternative materials may be incorporated during cement production by partial/y replacing conventional fuel and/or the raw materials ground into the raw mix, or by including active additions to the cement and/or clinker.The present paper discusses the preliminary results obtained in a study of the composition and alkali activation of six types of fired ceramic waste with a view to their viability as partial replacements for some of the prime materials used to prepare raw mix for Portland cement.The results show that the chemical and mineralogical composition of the six materials makes them apt for such possible use. They are neither toxic nor radioactive. And as might be expected this type of waste exhibits pozzolanic activity. Alkali activation of the waste, low at the age analyzed (8 days, does not appear to be affected by the vitreous phase content or the nature of the activator. The characterization study conducted on the activated paste shows that the feldspar phases are the ones most susceptible to dissolution and reaction with the alkaline solutions.La industria cementera mundial está buscando vías experimentales que permitan desarrollar cementos que precisen menor energía en su formación, degraden menos los entornos y emitan menos gases contaminantes a la atmósfera. Esta línea, en España y Europa, coincide plenamente con el concepto de sostenibilidad y alcanzar el cumplimiento del Protocolo de

  6. Sulfur Isotope Trends in Archean Microbialite Facies Record Early Oxygen Production and Consumption

    Zerkle, A.; Meyer, N.; Izon, G.; Poulton, S.; Farquhar, J.; Claire, M.


    The major and minor sulfur isotope composition (δ34S and Δ33S) of pyrites preserved in ~2.65-2.5 billion-year-old (Ga) microbialites record localized oxygen production and consumption near the mat surface. These trends are preserved in two separate drill cores (GKF01 and BH1-Sacha) transecting the Campbellrand-Malmani carbonate platform (Ghaap Group, Transvaal Supergroup, South Africa; Zerkle et al., 2012; Izon et al., in review). Microbialite pyrites possess positive Δ33S values, plotting parallel to typical Archean trends (with a Δ33S/δ34S slope of ~0.9) but enriched in 34S by ~3 to 7‰. We propose that these 34S-enriched pyrites were formed from a residual pool of sulfide that was partially oxidized via molecular oxygen produced by surface mat-dwelling cyanobacteria. Sulfide, carrying the range of Archean Δ33S values, could have been produced deeper within the microbial mat by the reduction of sulfate and elemental sulfur, then fractionated upon reaction with O2 produced by oxygenic photosynthesis. Preservation of this positive 34S offset requires that: 1) sulfide was only partially (50­­-80%) consumed by oxidation, meaning H2S was locally more abundant (or more rapidly produced) than O2, and 2) the majority of the sulfate produced via oxidation was not immediately reduced to sulfide, implying either that the sulfate pool was much larger than the sulfide pool, or that the sulfate formed near the mat surface was transported and reduced in another part of the system. Contrastingly, older microbialite facies (> 2.7 Ga; Thomazo et al., 2013) appear to lack these observed 34S enrichments. Consequently, the onset of 34S enrichments could mark a shift in mat ecology, from communities dominated by anoxygenic photosynthesizers to cyanobacteria. Here, we test these hypotheses with new spatially resolved mm-scale trends in sulfur isotope measurements from pyritized stromatolites of the Vryburg Formation, sampled in the lower part of the BH1-Sacha core. Millimeter

  7. A catalogue of Danian gastropods from the Baunekule facies, Faxe Formation, Denmark

    Lauridsen, B.W.


    Full Text Available This catalogue of 194 gastropod taxa is based on the collection of Danian gastropods from the Baunekule facies, Faxe Formation in eastern Denmark. The gastropod fauna is extremely rich and well preserved. Most of the gastropods (106 species are referred to genus level only, 9 morphotypes to even higher taxonomical levels and 79 gastropods are referred to species level. The gastropods are classified following Bouchet & Rocroi (2005 as 4 different clades: Vetigastropoda (represented by 26 species and 10 superfamilies, Caenogastropoda (represented by 142 species and 17 superfamilies, Heterobranchia (represented by 23 species and 5 superfamilies and Opisthobranchia (represented by 1 species and 1 superfamily. The new species Zaclys? nuetzeli n. sp. is introduced. The Faxe Formation is recognised as a cold-water coral ecosystem with interfingering smaller bryozoan mounds. The Baunekule facies is found in the upper part of the coral mound complex of the Faxe Formation, where it forms isolated lensoidal bodies in the flanks of some of the coral mounds. It is characterised by a high diversity invertebrate fauna that occurs in weakly consolidated coraldominated floatstone to rudstone. The diagenesis of the Baunekule facies is of special significance because a high proportion of the originally aragonite-shelled fauna is preserved by recrystallization to calcite during early burial diagenesis. Most of the gastropods are not known from other parts of the Faxe Fm. The fauna is very important for comparative evolutionary studies of fossil and modern gastropods on cold-water coral mounds. Many of the genera have not previously been recorded from Danian strata. None of the gastropod species found in the Baunekule facies are known for certain to range below the Cretaceous–Palaeogene boundary. The fauna is comparable to gastropods found on modern cold-water coral mounds in the North Atlantic. The gastropod fauna from the Baunekule facies is characterised by a


    Albert C. Reynolds; Dean S. Oliver; Fengjun Zhang; Yannong Dong; Jan Arild Skjervheim; Ning Liu


    Knowledge of the distribution of permeability and porosity in a reservoir is necessary for the prediction of future oil production, estimation of the location of bypassed oil, and optimization of reservoir management. But while the volume of data that can potentially provide information on reservoir architecture and fluid distributions has increased enormously in the past decade, it is not yet possible to make use of all the available data in an integrated fashion. While it is relatively easy to generate plausible reservoir models that honor static data such as core, log, and seismic data, it is far more difficult to generate plausible reservoir models that honor dynamic data such as transient pressures, saturations, and flow rates. As a result, the uncertainty in reservoir properties is higher than it could be and reservoir management can not be optimized. The goal of this project is to develop computationally efficient automatic history matching techniques for generating geologically plausible reservoir models which honor both static and dynamic data. Solution of this problem is necessary for the quantification of uncertainty in future reservoir performance predictions and for the optimization of reservoir management. Facies (defined here as regions of relatively uniform petrophysical properties) are common features of all reservoirs. Because the flow properties of the various facies can vary greatly, knowledge of the location of facies boundaries is of utmost importance for the prediction of reservoir performance and for the optimization of reservoir management. When the boundaries between facies are fairly well known, but flow properties are poorly known, the average properties for all facies can be determined using traditional techniques. Traditional history matching honors dynamic data by adjusting petrophysical properties in large areas, but in the process of adjusting the reservoir model ignores the static data and often results in implausible reservoir

  9. Felsic granulite with layers of eclogite facies rocks in the Bohemian Massif; did they share a common metamorphic history?

    Jedlicka, Radim; Faryad, Shah Wali


    High pressure granulite and granulite gneiss from the Rychleby Mountains in the East Sudetes form an approximately 7 km long and 0.8 km wide body, which is enclosed by amphibolite facies orthogneiss with a steep foliation. Well preserved felsic granulite is located in the central part of the body, where several small bodies of mafic granulite are also present. In comparison to other high pressure granulites in the Bohemian Massif, which show strong mineral and textural re-equilibration under granulite facies conditions, the mafic granulite samples preserve eclogite facies minerals (garnet, omphacite, kyanite, rutile and phengite) and their field and textural relations indicate that both mafic and felsic granulites shared common metamorphic history during prograde eclogite facies and subsequent granulite facies events. Garnet from both granulite varieties shows prograde compositional zoning and contains inclusions of phengite. Yttrium and REEs in garnet show typical bell-shaped distributions with no annular peaks near the grain rims. Investigation of major and trace elements zoning, including REEs distribution in garnet, was combined with thermodynamic modelling to constrain the early eclogite facies metamorphism and to estimate pressure-temperature conditions of the subsequent granulite facies overprint. The first (U)HP metamorphism occurred along a low geothermal gradient in a subduction-related environment from its initial stage at 0.8 GPa/460 °C and reached pressures up to 2.5 GPa at 550 °C. The subsequent granulite facies overprint (1.6-1.8 GPa/800-880 °C) affected the rocks only partially; by replacement of omphacite into diopside + plagioclase symplectite and by compositional modification of garnet rims. The mineral textures and the preservation of the eclogite facies prograde compositional zoning in garnet cores confirm that the granulite facies overprint was either too short or too faint to cause recrystallisation and homogenisation of the eclogite

  10. Garnet-bearing Granulite Facies Rock Xenoliths from Late Mesozoic Volcaniclastic Breccia, Xinyang, Henan Province


    This paper presents the primary results of petrologic,mineralogical and petrochemical studies of garnet beating granulite facies rock xenoliths from Xinyang, Henan Province. These xenoliths, which are found in a pipe of late Mesozoic volcaniclastic breccia, are of high density (3.13-3.30 g/cm3) and high seismic velocity (Vp = 7.04-7.31 km/s), being products of underplating of basaltic magmas and had experienced granulite facies metamorphism. The underplating and metamorphism took place before the eruption of the host rock. Petrographical studies and equilibrium T-P calculations show that these xenoliths were captured at a 49 km depth and experienced at least a 16 km uplift before they were captured. The dynamics of the uplift could be related to the continent-continent collision between the North China plate and the Yangtze plate during the Triassic.

  11. Using informative priors in facies inversion: The case of C-ISR method

    Valakas, G.; Modis, K.


    Inverse problems involving the characterization of hydraulic properties of groundwater flow systems by conditioning on observations of the state variables are mathematically ill-posed because they have multiple solutions and are sensitive to small changes in the data. In the framework of McMC methods for nonlinear optimization and under an iterative spatial resampling transition kernel, we present an algorithm for narrowing the prior and thus producing improved proposal realizations. To achieve this goal, we cosimulate the facies distribution conditionally to facies observations and normal scores transformed hydrologic response measurements, assuming a linear coregionalization model. The approach works by creating an importance sampling effect that steers the process to selected areas of the prior. The effectiveness of our approach is demonstrated by an example application on a synthetic underdetermined inverse problem in aquifer characterization.

  12. Vertical Sound Velocity Transition in the Coral Reef Core and its Significance of Indicating Facies

    Li Ganxian; Lu Bo


    On the basis of the sound velocity measurements of the coral reef core from Nanyong No. 1 Well of Yongshu Reef in the Nansha Islands, the paper studies the relations between the vertical sound velocity transition features in the coral reef core and the corresponding stratigraphic depositional facies change as well as stratigraphic gap of erosion,analyses the cause of the sound velocity transition, expounds the concrete process of the sea level change resulting in the stratigraphic gap of erosion and facies change in the coral reef and explains the relations between the vertical sound velocity transition in the coral reef core and the corresponding stratigraphic paleoclimate and the sea level change. This study is of important practical value and theoretical significance to the island and reef engineering construction and the acoustic logging for oil exploration in the reef limestone area as well as the paleoceanographic study of the marginal sea in the western Pacific Ocean.

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



    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.

  14. Episodic subgreenschist facies metamorphism in the Andes of Chile - is it a valid model?

    Bevins, R. E.; Robinson, D.; Aguirre, L.; Vergara, M.


    The Central Andes of Chile are characterized by subgreenschist facies burial metamorphism that is reported as having developed in up to seven episodic cycles of some 40Myr duration. The main evidence in support of the model is reported as mineralogical breaks at major stratigraphic boundaries that are interpreted as documenting sharp breaks in metamorphic grade. Here we test this model by examination of the progressive secondary mineral development, reaction progress in mafic phyllosilicates, and topological variations of the low-grade assemblages in metabasites for Jurassic to Miocene sequences east of Santiago. The mafic phyllosilicates (smectite - mixed-layer chlorite/smectite - chlorite) show increasing reaction progress with stratigraphic age and there is a continuum across the main stratigraphic boundaries, such there is no offset or gap in the reaction progress at these boundaries. There are some differences in mineral assemblages between the various stratigraphic units, such as between prehnite+pumpellyite+/-laumonite or amphibole-bearing and non amphibole bearing rocks, from which contrasting subgreenschist facies can be recognised. However, consideration of the controls on mineral parageneses at subgreenschist facies conditions demonstrates that these different facies cannot be used solely as evidence of sharp breaks in metamorphic grade at unconformities, as has been reported in many previous publications for the Andes. The presently accepted model for the Central Andes, involving repeated cycles of episodic metamorphism developing in extensional basins, is, therefore, partly unfounded. Consideration of the overall tectonic evolution of this part of the Andes concurs that the burial metamorphism developed in extensional settings, but in only two events, namely in mid-late Cretaceous and Late Miocene times respectively. The results from this work suggest that the record of sharp metamorphic breaks and the episodic model of metamorphism reported for many

  15. Low-grade Prehnite-Pumpellyite facies metamorphism in the Bamble sector, SE-Norway

    Velo, Mari Roen


    Low-grade metamorphic minerals have been found within the high-grade terrain in the Bamble sector, SE-Norway. The minerals prehnite and pumpellyite indicative of prehnite-pumpellyite facies conditions have been confirmed around the Kragerø area. The formation of analcime, thomsonite, hydrogarnet, albite and clay minerals is also a part of the low-grade metamorphism. The occurrence of these low-grade minerals is constricted to pseudomorph replacement of earlier mineral phases, hydrothermal vei...

  16. Deep marine facies in the Upper Volgian - Ryazanian of the northern Danish Central Gragen

    Ineson, J.R.; Rasmussen, E.S.


    In the Gertrud Graben, a sub-basin of the Danish Central Graben, the uppermost Farsund Formation (Upper Volgian - Ryazanian) is characterized by organic-rich mudstones interbedded locally with turbidite sandstones. The core presented here, from the Jeppe-1 well (5603/28-3), records the processes active on the western flank of the Graben, adjacent to a Late Jurassic structural high, the Gert Ridge. In this setting, `classical` turbidites are largely restricted to thin sand-mud couplets, deposited by sediment-starved, dilute turbidity currents, possibly representing overbank deposits from an axial turbidite system in the Gertrud Graben. Sand-rich facies typically have a mud matrix and contain mudstone clasts and large contorted rafts of interbedded sandtone and mudstone; these deposits mainly record sliding and bebris flow, but intrusive sediment boidies may also be represented. The facies spectrum is completed by organic-rich, non-bioturbated hemipelagic mudstones which form an important component of the the `hot shales` which cap the cored section although remaining subordinate to mudstone turbidites. Upper Jurassic mudrocks are generally accepted to be the most important hydrocarbon source rocks in the central and northern North Sea. Of particular importance are the `hot shales` that occur in the upper levels of the succession and show abnormally high (`hot`) levels of gamma radioactivity, corresponding to a high content of organic carbon. In certain settings, these rich source rocks interfinger with, or overlie, sand-rich reservoir facies that are commonly of deep-water aspect. The aim here is to present an example of this facies association from the Jeppe-1 well (5603/28-3) in the Danish sector of the Central Graben. (au) 8 fig., 16 refs.

  17. FRBR prima di FRBR


    This paper deals with lack of FRBR-zation of present online catalogues and with a way to organize on the shelves resources by FRBR entities using Colon Classification book number.Main results of this analysis are: categories expressed by FBRB were already identified by Ranganathan in its bibliographic system; Colon classification book number allows a higher degree of arrangement of bibliographic resources, i.e. compliant to FRBR entities; also for this reason, Colon classification book number...

  18. Aardgas is prima trekkerbrandstof

    Hilhorst, G.J.; Timmerman, M.


    Op proefbedrijf De Marke is een trekker (Fendt 306) omgebouwd naar een dual-fuel diesel-aardgas-trekker. De trekker heeft gedurende de onderzoeksperiode technisch goed gefunctioneerd. De lange vultijd van de gastanks op de trekker wordt wel als een praktisch probleem ervaren. Er kan niet snel even

  19. Er praksis prima?

    Holm, Claus


    Tiltroen til praktisk sans er i vækst, mens den teoretiske fornuft møder skepsis. Paradoksalt nok rammer den antiteoretiske bevægelse også universiteterne. To forskere advarer mod, at samfundet forlader sig på praksis....

  20. Variscan terrane of deep-crustal granulite facies in Yushugou area, southern Tianshan

    王润三; 周鼎武; 王居里; 王焰; 刘养杰


    The Yushugou terrane of deep-crustal granulite facies in southern Tianshan consists of two parts, granulite and metaperidotite. The whole terrane is a metamorphism of (high-pressure) granulite facies, and typical mineral associations are: Gt-Cpx-Pl-Tit-Ilm (±Qz) (silica-saturated and oversaturated mafic rocks), Gt-Ky (pseudomorph)-Pl-Ru-Ilm±Qz (metapelitic rocks) and Spi-Opx-Cpx-Ol (meta-ultramafic rocks). The peak-stage P-T conditions are 795—964℃, 0.97—1.42 GPa, which are obtained with mineral chemistry, assemblage analyses and P-T estimation. The Sm-Nd isochron age of peak-stage metamorphic minerals is (315±3.62) Ma. All of these indicate that the terrane is a deep-crustal body, which subduets to the depth of 40—50 km in the middle late-Paleozoic, undergoing metamorphism of (high-pressure) granulite facies, and exhumed again to the surface by tectonic uplifting.

  1. Modern Pearl River Delta and Permian Huainan coalfield, China: A comparative sedimentary facies study

    Suping, P.; Flores, R.M.


    Sedimentary facies types of the Pleistocene deposits of the Modern Pearl River Delta in Guangdong Province, China and Permian Member D deposits in Huainan coalfield in Anhui Province are exemplified by depositional facies of anastomosing fluvial systems. In both study areas, sand/sandstone and mud/mudstone-dominated facies types formed in diverging and converging, coeval fluvial channels laterally juxtaposed with floodplains containing ponds, lakes, and topogenous mires. The mires accumulated thin to thick peat/coal deposits that vary in vertical and lateral distribution between the two study areas. This difference is probably due to attendant sedimentary processes that affected the floodplain environments. The ancestral floodplains of the Modern Pearl River Delta were reworked by combined fluvial and tidal and estuarine processes. In contrast, the floodplains of the Permian Member D were mainly influenced by freshwater fluvial processes. In addition, the thick, laterally extensive coal zones of the Permian Member D may have formed in topogenous mires that developed on abandoned courses of anastomosing fluvial systems. This is typified by Seam 13-1, which is a blanket-like body that thickens to as much as 8 in but also splits into thinner beds. This seam overlies deposits of diverging and converging, coeval fluvial channels of the Sandstone D, and associated overbank-floodplain deposits. The limited areal extent of lenticular Pleistocene peat deposits of the Modern Pearl River Delta is due to their primary accumulation in topogenous mires in the central floodplains that were restricted by contemporaneous anastomosing channels.

  2. Pre-stack-texture-based reservoir characteristics and seismic facies analysis

    Song Cheng-Yun; Liu Zhi-Ning; Cai Han-Peng; Qian Feng; Hu Guang-Min


    Seismic texture attributes are closely related to seismic facies and reservoir characteristics and are thus widely used in seismic data interpretation. However, information is mislaid in the stacking process when traditional texture attributes are extracted from post-stack data, which is detrimental to complex reservoir description. In this study, pre-stack texture attributes are introduced, these attributes can not only capable of precisely depicting the lateral continuity of waveforms between different reflection points but also reflect amplitude versus offset, anisotropy, and heterogeneity in the medium. Due to its strong ability to represent stratigraphics, a pre-stack-data-based seismic facies analysis method is proposed using the self-organizing map algorithm. This method is tested on wide azimuth seismic data from China, and the advantages of pre-stack texture attributes in the description of stratum lateral changes are verifi ed, in addition to the method’s ability to reveal anisotropy and heterogeneity characteristics. The pre-stack texture classification results effectively distinguish different seismic reflection patterns, thereby providing reliable evidence for use in seismic facies analysis.

  3. Materias primas para pavimentos y revestimientos cerámicos en la región de Murcia

    Fernández, C.


    Full Text Available The clay industry of the Murcia Region has never had a relevant industrial importance, with only around ten brick operations in the last few years. Today only only two brid factories are operative having certain size. The extraordinary industrial development currently experienced by the Region has leaded to the development of new initiatives which need institutional backing. In this framework and under the sponsoring of the Council of Technologies, Industry and Commerce of the Autonomic Community, the Spanish Geological Survey (ITGE has carried out a general survey for raw materials for the ceramic industry in the region, mainly aimed to find clays for ceramic gres and glazed tiles, whose results are discussed in this paper. Murcia has a very complicated geology, being carbonated marine sediments the most important lithologies. Due to it, it is difficult to find no-carbonated shales or clays to produce gres tiles. We have found six zones containing different clay types, that reach a few hundreds million tons of resources. With that clays we have produce in the laboratory gres tiles and glazed tiles of commercial quality.

    La industria cerámica de la Región de Murcia no ha tenido gran importancia industrial, limitándose a una decena de fábricas de ladrillos. Hoy en día sólo operan en la región 2 fábricas de ladrillos de cierta entidad. El extraordinario desarrollo industrial que experimenta actualmente la Región suscita nuevas iniciativas empresariales, que precisan del apoyo institucional. En este marco y bajo el auspicio y con la financiación parcial de la Consejería Tecnologías, Industria y Comercio de la Comunidad Autónoma, el Instituto Tecnológico Geominero de España ha realizado en los tres últimos años una investigación general de materias primas para la industria cerámica en la región, especialmente dirigida a localizar arcillas para pavimentos y revestimientos cerámicos, cuyos resultados se exponen en este




    Full Text Available Este articulo proscrita los resultados del proyecto ce Investigación IPP (Innovación ce Procesos y Productos que plantea un análisis profundo y sistémico de las cadenas productivas, basado en el estudio de la productividad y los procesos. Este proyecto se trabajo en 4 fases: Inteligencia, Experimentación. Innovación y Apropiación tecnológica. Estas etapas están dirigidas al mejoramiento continuo ce los procesos, de los productos ce la organización y de las interacciones entre los actores de la cadena productiva de las materias primas minerales y energéticas. En la fase de inteligencia, se estudiaron las características, las ecesidades. el mercado y el entorno de la cadena productiva que son el resultado del aprovechamiento de los recursos naturales y del ambiente En la segunda fase, se caracterizó la formulación, diseño c implantación ce prototipos de procesos y productos que emulen el comportamiento del proceso en un sistema real y sean amigables con el medio ambiente. Teniendo en cuenta las dos primeras fases, la tercera se caracterizó por la formulación y el diseño ce nuevos procesos y productos que mejoren la eficiencia y la productividad. En la última fase del proyecto, se planteó el servicio de apropiación tecnológica que busca transferir innovación y conocimiento de punta a la cadena. Finalmente el resultado ce IPP es la propuesta de un centro de innovación y tecnología en la Universidad Nacional de Colombia, que garantizará la apropiación y adecuación de las soluciones a las cadenas productivas, siendo una innovación para el sector de la minería, los materiales y la energía, y teniendo como principios, productos y procesos amigables con el ambiente.

  5. Chemopreventive Effects of the p53-Modulating Agents CP-31398 and Prima-1 in Tobacco Carcinogen-Induced Lung Tumorigenesis in A/J Mice

    Chinthalapally V. Rao


    Full Text Available Lung cancer is the leading cause of cancer deaths worldwide. Expression of the p53 tumor suppressor protein is frequently altered in tobacco-associated lung cancers. We studied chemopreventive effects of p53-modulating agents, namely, CP-31398 and Prima-1, on 4-(methylnitrosamino-1-(3-pyridyl-1-butanone (NNK-induced lung adenoma and adenocarcinoma formation in female A/J mice. Seven-week-old mice were treated with a single dose of NNK (10 µmol/mouse by intraperitoneal injection and, 3 weeks later, were randomized to mice fed a control diet or experimental diets containing 50 or 100 ppm CP-31398 or 150 or 300 ppm Prima-1 for either 17 weeks (10 mice/group or 34 weeks (15 mice/group to assess the efficacy against lung adenoma and adenocarcinoma. Dietary feeding of 50 or 100 ppm CP-31398 significantly suppressed (P < .0001 lung adenocarcinoma by 64% and 73%, respectively, after 17 weeks and by 47% and 56%, respectively, after 34 weeks. Similarly, 150 or 300 ppm Prima-1 significantly suppressed (P < .0001 lung adenocarcinoma formation by 56% and 62%, respectively, after 17 weeks and 39% and 56%, respectively, after 34 weeks. Importantly, these results suggest that both p53 modulators cause a delay in the progression of adenoma to adenocarcinoma. Immunohistochemical analysis of lung tumors from mice exposed to p53-modulating agents showed a significantly reduced tumor cell proliferation and increased accumulation of wild-type p53 in the nucleus. An increase in p21- and apoptotic-positive cells was also observed in lung tumors of mice exposed to p53-modulating agents. These results support a chemopreventive role of p53-modulating agents in tobacco carcinogen-induced lung adenocarcinoma formation.

  6. Diastolic properties of the Sorin Solo, ATS 3F, Edwards Prima Plus and Medtronic Freestyle stentless valves: an independent in-vitro comparison.

    Weltert, Luca; Nardella, Saverio; Girola, Fabiana; Scaffa, Raffaele; Bellisario, Alessandro; Maselli, Daniele; De Paulis, Ruggero


    Currently, little is known of the diastolic properties of stentless valves that affect stress and strain on leaflets and, hence, their durability. In a pressurized aortic root model, a series of in-vitro tests was conducted to determine how stentless valves behave in diastole, and how they adapt to different annulus-to-sinotubular junction (STJ) ratios. Sixteen 25 mm stentless aortic valves (four each of the Sorin Solo, ATS 3F, Edwards Prima Plus and Medtronic FreeStyle) were sutured into a 32 mm Valsalva graft, suspending the commissures into the expandable region (42 mm). The neoaortic root was pressurized and the size of the STJ progressively reduced by wrapping the neocommissural ridge with Dacron rings. Endoscopic views and ultrasound imaging were used to observe the geometry of the leaflets, regurgitation, and the height and level of leaflet coaptation at different annulus-to-STJ ratios. Pericardial prostheses built to mimic a cylinder (ATS 3F and Sorin Solo) showed the greatest tolerance to STJ dilatation and a larger coaptation surface, but also a tendency to roll in on themselves in an italic S-shape if oversized. Valves built to mimic native aortic leaflets (porcine Prima Plus and Medtronic Freestyle) showed a reduced tolerance to STJ dilatation, resulting in regurgitation and a smaller coaptation surface, but also a reduced tendency to roll if oversized. Despite similar systolic performances, stentless prostheses behave differently during diastole. The 3F and Solo valves benefit from a better tolerance to STJ dilatation, while the Prima Plus and Freestyle benefit from a more stable shape of closure under conditions of oversizing.

  7. Le Visage de la Victoire di Henry De Groux: la riscoperta di un’opera antimilitarista del tempo della Prima guerra mondiale

    Carol Morganti


    Full Text Available Il presente intervento è dedicato a un’importante raccolta di incisioni, oggi riscoperta: Le Visage de la Victoire, eseguita dall’artista belga Henry De Groux. Costituita da oltre 40 incisioni (acqueforti e vernici molli, è stata realizzata nel corso della Prima Guerra Mondiale al fine di denunciare l’inutile massacro in corso. Si tratta di opere di ispirazione visionaria, che rivelano significati universali, mettendo il maestro belga in rapporto di affinità con artisti quali Goya e Otto Dix.

  8. Diseño de la bodega de materia prima del área de calzado en una industria plástica

    Moreno, Paulina; Abad Morán, Jorge Fernando


    La presente tesis se enfoca dentro de la Bodega de Materia Prima del Área de Calzado en una Industria Plástica, la cual presenta problemas como: pasillos no identificados, todos los productos no están codificados, mezcla de productos de alta y baja rotación, stock de productos obsoletos, productos almacenados en otras áreas, no tiene un sistema de manejo y manipuleo. El objetivo principal es organizar los materiales en la bodega, minimizando los tiempos muertos y reduciendo la congestión en ...

  9. Integración de Jatropha curcas L. en agroecosistemas como materia prima para biodiesel en la región centro de Chiapas, México.

    Solís Guzmán, Blanca Flor


    Jatropha curcas L. es una opción de importancia en Chiapas como materia prima para biodiesel y se han establecido alrededor de 10 mil hectáreas, aún con escasa información como cultivo. El objetivo de este trabajo fue determinar el potencial de integración de J. curcas en agroecosistemas de la Región Centro de Chiapas, México. Esta investigación se realizó en tres etapas de 2008 a 2011. Primero se determinaron áreas potenciales con el programa ArcView GIS Ver. 3.2®, en dos escenarios: 1) pend...

  10. Avaliação da qualidade de matérias-primas de ruibarbo utilizadas em formulações farmacêuticas

    O.V. Sousa


    Full Text Available As plantas denominadas de ruibarbo sintetizam antraquinonas e taninos, que são responsáveis pelos efeitos laxante e adstringente, respectivamente. Análises da qualidade de cinco matérias-primas de ruibarbo foram realizadas a fim de detectar adulterações. As reações para antraquinonas e taninos foram positivas. Os constituintes rapônticos foram observados na amostra de Rheum palmatum (2. As medidas de cinzas totais para Rheum palmatum (2 e Ferraria cathartica estão acima do esperado. Conforme resultados, as amostras de Rheum palmatum (2 e Ferraria cathartica devem estar adulteradas.


    Bonifaz, Nancy; Gutiérrez, Francisco


    Es común que la alimentación de los animales en crianza en un hato lechero sea subestimada y conlleve a deficiencias nutricionales que se reflejan en bajas ganancias de peso, animales sin el peso adecuado al primer servicio (16-18 meses de edad) y baja producción de leche cuando alcanzan su etapa productiva. El objetivo de esta investigación fue identificar la calidad nutricional de las principales materias primas que se emplean en la alimentación de bovinos lecheros del cantón Cayam...

  12. Diseño de la bodega de materia prima del área de calzado en una industria plástica

    Moreno, Paulina; Abad Morán, Jorge Fernando


    La presente tesis se enfoca dentro de la Bodega de Materia Prima del Área de Calzado en una Industria Plástica, la cual presenta problemas como: pasillos no identificados, todos los productos no están codificados, mezcla de productos de alta y baja rotación, stock de productos obsoletos, productos almacenados en otras áreas, no tiene un sistema de manejo y manipuleo. El objetivo principal es organizar los materiales en la bodega, minimizando los tiempos muertos y reduciendo la congestión en ...

  13. Recuperación de materias primas secundarias procedentes de residuos de aparatos eléctricos y electrónicos (RAEES)

    Giménez San Andrés, Gerard


    Estudiar la viabilidad técnica y económica de la recuperación de materias primas secundarias, procedentes de los residuos de aparatos eléctricos y electrónicos. Para ello el proyecto se centrara en unos determinados tipos de RAEES y en la recuperación de ciertos materiales empleando unas tecnologías determinadas. Algunos de los factores que se tendrán en cuenta para realizar el análisis técnico y económico son el grado de recuperación, los recursos necesarios para lograrlo y la diferencia de ...

  14. Facies analysis of an Upper Jurassic carbonate platform for geothermal reservoir characterization

    von Hartmann, Hartwig; Buness, Hermann; Dussel, Michael


    The Upper Jurassic Carbonate platform in Southern Germany is an important aquifer for the production of geothermal energy. Several successful projects were realized during the last years. 3D-seismic surveying has been established as a standard method for reservoir analysis and the definition of well paths. A project funded by the federal ministry of economic affairs and energy (BMWi) started in 2015 is a milestone for an exclusively regenerative heat energy supply of Munich. A 3D-seismic survey of 170 square kilometer was acquired and a scientific program was established to analyze the facies distribution within the area ( Targets are primarily fault zones where one expect higher flow rates than within the undisturbed carbonate sediments. However, since a dense net of geothermal plants and wells will not always find appropriate fault areas, the reservoir properties should be analyzed in more detail, e.g. changing the viewpoint to karst features and facies distribution. Actual facies interpretation concepts are based on the alternation of massif and layered carbonates. Because of successive erosion of the ancient land surfaces, the interpretation of reefs, being an important target, is often difficult. We found that seismic sequence stratigraphy can explain the distribution of seismic pattern and improves the analysis of different facies. We supported this method by applying wavelet transformation of seismic data. The splitting of the seismic signal into successive parts of different bandwidths, especially the frequency content of the seismic signal, changed by tuning or dispersion, is extracted. The combination of different frequencies reveals a partition of the platform laterally as well as vertically. A cluster analysis of the wavelet coefficients further improves this picture. The interpretation shows a division into ramp, inner platform and trough, which were shifted locally and overprinted in time by other

  15. Recent benthic foraminifera and sedimentary facies from mangrove swamps and channels of Abu Dhabi (United Arab Emirates)

    Fiorini, Flavia; Odeh, Weaam A. S. Al; Lokier, Stephen W.; Paul, Andreas


    Zonation of Recent mangrove environments can be defined using benthic foraminifera, however, little is known about foraminifera from mangrove environments of the Arabian Gulf. The objective of this study is to produce a detailed micropaleontological and sedimentological analysis to identify foraminiferal associations in several coastline environments (mangrove swamps and channels) located on the eastern side of Abu Dhabi Island (UAE). Detailed sediment sampling collection in mangal environments of Eastern Abu Dhabi was carried out to assess the distribution of living and dead benthic foraminifera in different sedimentary facies in the mangal and in the surrounding area comprising natural environments of the upper and lower intertidal area (mud flats and channels) and areas modified by anthropogenic activities (dredged channels). The fine-grain sediments collected near mangrove (Avicenna marina) roots presented a high abundance of living and dead foraminifera tests. The assemblages in these samples show very low diversity and are almost entirely constituted of small-sized opportunistic species belonging to the genera Ammonia and Elphidium. In particular: • Samples collected on the mud flat and in ponds at the margin of the channel show a foraminiferal assemblage characterised by abundant foraminifera belonging to the genera Ammonia, Elphidium, Triloculina, Quinqueloculina, Peneroplis and Spirolina. • Samples collected in the lower (wet) intertidal area close to Avicenna marina roots, presented a low-diversity assemblage mostly comprising opportunistic foraminifera of the genera Ammonia and Elphidium along with rare miliolidae. • Samples from the upper intertidal area (dry) close to Avicenna marina roots, produced an assemblage exclusively composed of small-sized opportunistic Ammonia and Elphidium, together with abundant specimens belonging to the genera Trochammina. Throchammina specimens have not been previously recorded from Recent sedimentary samples of

  16. Bathymetric and sediment facies maps for China Bend and Marcus Flats, Franklin D. Roosevelt Lake, Washington, 2008 and 2009

    Weakland, Rhonda J.; Fosness, Ryan L.; Williams, Marshall L.; Barton, Gary J.


    The U.S. Geological Survey (USGS) created bathymetric and sediment facies maps for portions of two reaches of Lake Roosevelt in support of an interdisciplinary study of white sturgeon (Acipenser transmontanus) and their habitat areas within Franklin D. Roosevelt Lake, Washington. In October 2008, scientists from the USGS used a boat-mounted multibeam echo sounder (MBES) to describe bathymetric data to characterize surface relief at China Bend and Marcus Flats, between Northport and Kettle Falls, Washington. In March 2009, an underwater video camera was used to view and record sediment facies that were then characterized by sediment type, grain size, and areas of sand deposition. Smelter slag has been identified as having the characteristics of sand-sized black particles; the two non-invasive surveys attempted to identify areas containing black-colored particulate matter that may be elements and minerals, organic material, or slag. The white sturgeon population in Lake Roosevelt is threatened by the failure of natural recruitment, resulting in a native population that consists primarily of aging fish and that is gradually declining as fish die and are not replaced by nonhatchery reared juvenile fish. These fish spawn and rear in the riverine and upper reservoir reaches where smelter slag is present in the sediment of the river lake bed. Effects of slag on the white sturgeon population in Lake Roosevelt are largely unknown. Two recent studies demonstrated that copper and other metals are mobilized from slag in aqueous environments with concentrations of copper and zinc in bed sediments reaching levels of 10,000 and 30,000 mg/kg due to the presence of smelter slag. Copper was found to be highly toxic to 30-day-old white sturgeon with 96-h LC50 concentrations ranging from 3 to 5 (u or mu)g copper per liter. Older juvenile and adult sturgeons commonly ingest substantial amounts of sediment while foraging. Future study efforts in Lake Roosevelt should include sampling of

  17. Comparison of turbidite facies associations in modern passive-margin Mississippi fan with ancient active-margin fans

    Shanmugam, G.; Moiola, R. J.; McPherson, J. G.; O'Connell, S.


    Our comparison of the modern passive-margin Mississippi fan (DSDP Leg 96) with ancient active-margin fans (e.g. Eocene Hecho Group, Spain) reveals major differences in turbidite facies associations (Mutti and Ricci Lucchi scheme) and in seismic characteristics in the lower fan area. The lower (outer) Mississippi fan is composed of channel (Facies B and F) and non-channel facies (C? and D), whereas ancient fans are characterized by non-channelized, thickening-upward, depositional lobe facies (C and D). An absence of depositional lobes in the lower Mississippi fan is also suggested by a lack of convex-upward (mounded) seismic reflections with bidirectional downlap. Continuous seismic reflections of the lower Mississippi fan may represent "sheet sands", but not those of true depositional lobes with mounded character. Extensive channelization in modern passive-margin fans appears to be a product of the lateral shifting of a major sinuous distributary system, developed as a consequence of low gradients and the transport of sediment with a relatively low sand/mud ratio. In contrast, channels in active-margin fans are short and of low sinuosity as a result of high gradients and the transport of sediment with a relatively high sand/mud ratio. The turbidite facies association scheme, which was developed exclusively from ancient active-margin fans, should be applied to mature passive-margin fans with qualifications because of the differences in spatial distribution of turbidite facies and their associations.

  18. Facies and depositional model of Almada Canyon, Almada Basin, Bahia, Brazil; Facies e modelo deposicional do Canyon de Almada, Bacia de Almada, Bahia

    D' Avila, Roberto Salvador Francisco; Souza Cruz, Carlos Emanoel de; Oliveira Filho, Jose Souto; Jesus, Candida Menezes de; Cesero, Pedro de; Dias Filho, Dorval Carvalho; Lima, Claudio Coelho de; Queiroz, Claudia Lima de; Santos, Saulo Ferreira; Ferreira, Eduardo Araripe [PETROBRAS, Santos, SP (Brazil). Unidade de Negocio de Exploracao]. E-mail:


    In the continental portion of the Almada Basin outcrops of canyon filling deposits are represented by turbidite channels and associated facies from Urucutuca Formation. The canyon - semi-exhumated - eroded basement and pre-Cenomanian sedimentary rocks. The field study of the outcrops and cores obtained in adjacent perforations lead to the understanding of the facies and processes that controlled the deposition of these channeled turbidite that can be compared to the reservoirs of many oil fields in Brazil. The Almada canyon is a submarine conduct of tectonic origin that was enlarged by the repeated passing of turbidity currents. During the rift phase and the Albian period, compressive events reactivated old N E and N W faults in the basement as trans current fault systems. The continuation of these stresses, from the Cenomanian to the Maastrichtian, developed normal faults that controlled a submarine canyon that connected the continent, where an estuary was formed between the mountains, to the deep marine region of the basin. The canyon has received sediments brought by catastrophic fluvial floods coming from the surrounding mountains, which formed hyperpicnal flows that have evolved as turbidity currents, thus causing erosion of the substrate and carrying a huge volume of sediments to the basin. A part of that load was deposited in the canyon and formed turbidite channels filled by conglomerates, sandstones and shales. These moderately to highly efficient turbidite are intercalated to pro delta pelites and low density turbid plumes deposits, which have mostly been re mobilized as slump and debris flows (chaotic deposits). Pelites were accumulated mainly in the normal fluvial sedimentation phases, when the sandy sediment was retained next to the canyon head and were reworked by the tides on the upper part of the estuary. (author)

  19. Cribado de microorganismos y materias primas para intensificar la producción de enzimas celulasas en fermentación en estado sólido

    Gualberto León-Revelo


    Full Text Available En el presente trabajo, se llevó a cabo el cribado de hongos filamentosos y la evaluación de las principales materias primas del medio de cultivo para intensificar la producción de enzimas celulasas en Fermentación en Estado Sólido (FES. Entre los microorganismos estudiados, Aspergillus niger presenta la máxima expresión de enzimas celulasas extracelulares con fracción de halo de hidrólisis de 0,5 a las 24 horas. El estudio de concentración de inóculo y las materias primas mostró la mayor actividad, de 51,3 IU/gMs y productividad de 2,13 IU/gMs*h en el tiempo 24 horas, cuando se inocula una concentración de hifas de 28 g/kgMs, sulfato de amonio (0,14 % p/v y extracto de levadura (0,73 % p/v como fuente de nitrógeno inorgánico y orgánico, lactosa (5 g/L como fuente de carbono y afrecho cervecero como material lignocelulósico.

  20. La gestión de las materias primas silíceas en el Pirineo Occidental: la ocupación Magdaleniense de Berroberria (Urdax, Navarra



    Full Text Available La cueva de Berroberria es uno de los yacimientos más representativos del Magdaleniense en el Pirineo Occidental. Se presentan en este caso los resultados del estudio de procedencia de las materias primas líticas empleadas por los grupos del Magdaleniense Medio (alrededor de 14500 cal. BC. La metodología propuesta incluye análisis petrológicos y mineralógicos, mediante los que se identifican los principales afloramientos de sílex de los que se abastecieron. Se ha constatado así la explotación mayoritaria de los recursos silíceos más cercanos, como es el sílex de Flysch, junto con la de recursos regionales, como los sílex de Tercis o Chalosse, y siendo minoritarios pero de gran interés los aportes de materias primas extra-regionales de posible procedencia noraquitana. La gestión de cada una de estas rocas, al igual que su representación, es diferente; pero concuerda con la dinámica observada para esta cronología.

  1. Ahorro de agua y materia prima en los procesos de pelambre y curtido del cuero mediante precipitación y recirculación de aguas



    Full Text Available El principio del proceso de recuperación de cromo, consiste en precipitar el cromo contenido en el licor residual como hidróxido utilizando un álcali; este precipitado se separa por sedimentación y se disuelve nuevamente con ácido sulfúrico. De los resultados obtenidos, se observaron porcentajes de remoción superiores al 99%. Con la recirculación directa de aguas de pelambre fue posible obtener ahorros de agua del 64% y ahorros en materia prima del 32 %, además, con una adecuada selección del tamizador es posible recircular el agua un número máximo de tres veces, sin afectar la calidad del producto final. Así mismo, se comprobó la viabilidad de la recirculación directa de aguas de curtido, con ahorros de materia prima del 17%. Con medidas de este tipo, prácticas y fáciles de implementar, la industria del curtido del cuero podría disminuir considerablemente la contaminación, operar de una forma mas segura y con mayor eficiencia de producción.




    Full Text Available El presente trabajo tiene por objetivo primordial optimizar el consumo energético y reducir la contaminación ambiental asociada, por la liberación de CO2, en una planta de micronización de sílice. La metodología empleada consiste en aplicar la teoría de Bond para la selección de materias primas a tratar en la mencionada planta, la cual dependiendo de las necesidades actuales opera con dos tamaños de molienda d100, 50 y 75μm. Los ensayos experimentales se llevaron a cabo sobre muestras tomadas en la planta, teniendo en cuenta que las tres materias primas son de distinta procedencia y de similares características químicas y mineralógicas. Del análisis de los resultados obtenidos se concluye que el consumo energético de la planta puede reducirse hasta algo más de un 30% en ambos tamaños y evitando las emisiones de CO2 en 293,83 kg y 128,86 kg por hora de funcionamiento respectivamente.

  3. Colonias de corales y facies oncolíticas en el Dogger de las sierras de Cabra y Puente Genil (Subbético externo, provincia de Córdoba

    Molina, J. M.


    Full Text Available The presence of coral colonies and oncoid facies in the Dogger of the External Subbetic is first shown in this paper. It is worthy of remark that the Dogger materials (ooid limestones basically are placed between pelagic formations. Really, they represent a part of a shallowing-upward sequence which beging with the pelagic sediments of the DomerianToarcian. Over these materials a shallow carbonate shelf is established where biohenns, coral colonies, oncoid and ooid facies are developed, caping the sequence a hard-ground of the Upper Bathonian. The Upper Jurassic materials are clearly pelagic with "ammonitico rosso" facies. This work represents a contribution to the scientific controversy about the interpretation of the ooid limestones of the Dogger. In other areas (Venetian Alps, Balearic Islands, etc., these limestones have been interpreted as deep redeposited sediments and attempts to extend this interpretation to all the Dogger ooid limestones of the Alpine realm have been made. The features shown in this paper about the shallow marine nature of these materials in the External Subbetic are conclusives.

    se describen por primera vez, en el Dogger del Subbético externo, colonias de corales y facies oncolíticas, Especial interés tiene, ya que estos materiales del Dogger (calizas oolíticas, se intercalan entre formaciones de carácter marcadamente pelágico. En efecto, se trata de una etapa de somerización de la cuenca; sobre los sedimentos pelágicos del DomerenseToarcense se implanta una plataforma carbonatada marina somera donde se desarrollan colonias de corales y facies oncolíticas, para terminar en un hard-ground del Bathonense superior. El Jurásico superior es claramente pelágico con facies "ammonítico rosso", Se contribuye con este trabajo a la polémica científica planteada en la interpretación de las calizas oolíticas del Dogger. Estas han sido interpretadas como redepositadas en medios profundos en otras

  4. Upper Cretaceous chalk facies and depositional history recorded in the Mona-1 core, Mona Ridge, Danish North Sea

    Finn Surlyk


    Full Text Available The 331 m long core from the Mona-1 well in the Danish North Sea spans almost the entire Upper Cretaceous Chalk Group but only about 10% of Late Cretaceous time is represented. The succession comprises 14 facies representing pelagic deposition, turbidity flow, and mass-transport processes, including mudflow, debris flow, and slumping. Pelagic deposits vary mainly in terms of the concentration of siliciclastic material, the trace-fossil assemblage, and the presence or ab¬sence of primary sedimentary structures. Pelagic sedimentation was probably punctuated by the deposition of thin turbidites, and the resultant deposits were thoroughly bioturbated if deposited during normal oxygenation at the sea floor. Periodic benthic dysoxia resulted in the preservation of primary structures, as represented by laminated chalk which consists of thin pelagic laminae alternating with thin turbidites. In addition to the thin turbidites in the laminated chalk, four dif¬ferent turbidite facies are interpreted as representing high- to low-energy flows. Clast-supported chalk conglomerates have previously not been differentiated from other turbidites, but are here interpreted to be directly related to the down-slope evolution of debris flows. Debris flows are rep¬resented by matrix-supported conglomerates, which form one of the most common facies in the succession. High-concentration, gravity-driven suspension flows passed into dilute visco-plastic flows during the final stages of deposition and resulted in the deposition of structureless chalks. Limited shear deformation produced distinct quasi-facies from which the precursor facies can be deduced, whereas intense or continued shear deformation produced a shear-banded quasi-facies from which the precursor facies cannot be deduced in all cases. A series of major slump packages (14–18 in total are interpreted, forming over 40% of the succession; debrites appear to be the most common precursor facies involved in

  5. Upper Cretaceous chalk facies and depositional history recorded in the Mona-1 core, Mona Ridge, Danish North Sea: Plate 1

    Surlyk, Finn


    Full Text Available The 331 m long core from the Mona-1 well in the Danish North Sea spans almost the entire Upper Cretaceous Chalk Group but only about 10% of Late Cretaceous time is represented. The succession comprises 14 facies representing pelagic deposition, turbidity flow, and mass-transport processes, including mudflow, debris flow, and slumping. Pelagic deposits vary mainly in terms of the concentration of siliciclastic material, the trace-fossil assemblage, and the presence or ab¬sence of primary sedimentary structures. Pelagic sedimentation was probably punctuated by the deposition of thin turbidites, and the resultant deposits were thoroughly bioturbated if deposited during normal oxygenation at the sea floor. Periodic benthic dysoxia resulted in the preservation of primary structures, as represented by laminated chalk which consists of thin pelagic laminae alternating with thin turbidites. In addition to the thin turbidites in the laminated chalk, four dif¬ferent turbidite facies are interpreted as representing high- to low-energy flows. Clast-supported chalk conglomerates have previously not been differentiated from other turbidites, but are here interpreted to be directly related to the down-slope evolution of debris flows. Debris flows are rep¬resented by matrix-supported conglomerates, which form one of the most common facies in the succession. High-concentration, gravity-driven suspension flows passed into dilute visco-plastic flows during the final stages of deposition and resulted in the deposition of structureless chalks. Limited shear deformation produced distinct quasi-facies from which the precursor facies can be deduced, whereas intense or continued shear deformation produced a shear-banded quasi-facies from which the precursor facies cannot be deduced in all cases. A series of major slump packages (14–18 in total are interpreted, forming over 40% of the succession; debrites appear to be the most common precursor facies involved in

  6. Pseudotachylytes of the Deep Crust: Examples from a Granulite-Facies Shear Zone

    Orlandini, O.; Mahan, K. H.; Regan, S.; Williams, M. L.; Leite, A.


    The Athabasca Granulite Terrane is an exhumed section of deep continental crust exposed in the western Canadian shield. The terrane hosts the 1.88 Ga Cora Lake shear zone, a 3-5 km wide sinistral and extensional oblique-slip system that was active at high-pressure granulite-grade conditions ( ~1.0 GPa, >800°C to ~0.8 GPa and 700 °C). Pseudotachylyte, a glassy vein-filling substance that results from frictional melting during seismic slip, is common in ultramylonitic strands of the shear zone, where veins run for tens of meters subparallel to foliation. Some but not all PST veins have been overprinted with the Cora Lake shear zone foliation, and undeformed PST locally bears microlitic garnet. The frictional melts that quench into PST may reach >1400 °C, but are extremely localized and cool to country rock temperatures within minutes, resulting in glass and/or microlitic mineral growths. The melt itself is thought by many to be in disequilibrium with the host rock due to its rapid nature, but during cooling equilibrium is probably reached at small scales. This allows for microprobe analysis of adjacent microlites for thermobarometric calculations. Preliminary results from undeformed (e.g., youngest of multiple generations) PST suggest that quenching occurred in upper amphibolite facies ambient conditions and is compatible with later stages of Cora Lake shear zone activity. Host-rock mylonites contain abundant garnet and pyroxene sigma clasts indicating sinistral shear, and where PST-bearing slip surfaces are found at low angles to the foliation, they display sinistral offset. The host rock contains abundant macroscopic and microscopic sinistral shear fracture systems (e.g., Riedel [R], Y, and P displacement surfaces) within the immediate proximity of PST veins, indicating a complex interplay of brittle and ductile behavior that is interpreted to be genetically related to the formation of the PST. The shear fracture systems are characterized by sharply bounded

  7. Early geomorphological evolution of the North Polar Layered Deposits, Mars, from SHARAD radar-facies mapping

    Nerozzi, Stefano; Holt, John W.


    The north polar layered deposits (NPLD) are the largest accumulation of water ice in the northern hemisphere of Mars. Since their discovery, they are thought to hold a valuable record of recent climate change within their stratigraphy (Murray et al., Icarus, 1972; Cutts, JGR, 1973b), yet little is known about their age and accumulation history. Due to exposures in trough walls, detailed stratigraphy of the uppermost layers and their evolution have been studied extensively since the first Mariner 9 images of the NPLD (e.g. Soderblom et al., JGR, 1973). However, large portions of the polar cap are still unmapped and no detailed studies of the lowermost layered deposits have been performed to date, primarily due to a general lack of visible exposures. Correlation of reflectors within radargrams acquired by the Shallow Radar (SHARAD) (Seu et al., Planet. Space Sci., 2004) onboard Mars Reconnaissance Orbiter makes a detailed stratigraphic reconstruction of the NPLD possible. An extensive set of radargrams is available over Planum Boreum and individual reflectors can be traced over hundreds of kilometers (Seu et al., JGR, 2007a; Putzig et al., Icarus, 2009; Holt et al., Nature, 2010) with a theoretical vertical resolution of ~9 m in water ice (Seu et al., JGR, 2007a). In this study, we present a highly-detailed stratigraphic reconstruction of the first ~500 m of the NPLD at a scale down to the single reflector. A set of 8 horizons was tracked across 700+ radargrams, and thicknesses were calculated for each stratigraphic interval assuming a bulk composition of water ice. Along with the quantitative analysis of derived isopach maps, this study is based on the qualitative comparison of "radar facies" in different locations of Planum Boreum with techniques borrowed from traditional sequence stratigraphy. In general, the NPLD is characterized by uniform layering. However, important layer extent and thickness variations are observed within the lowermost sequence. Limited

  8. Thermal structure of pumpellyite-actinolite facies regions in the Sanbagawa belt, Shikoku, SW Japan

    Sakaguchi, M.


    On the basis of the mineral assemblages of pelitic rocks, the Sanbagawa belt in Shikoku, SW Japan, has been divided, from low- to high-grade parts, into the chlorite, garnet, albite-biotite and oligoclase-biotite zones (Higashino, 1990). Also, the mineral assemblage of pumpellyite + actinolite + epidote + chlorite or epidote + actinolite + hematite + chlorite, which defines the pumpellyite-actinolite (PA) facies (e.g., Banno, 1998), is widely recognized in metabasites in the chlorite zone (e.g. Banno & Sakai, 1989). However, the detailed study on the PA facies regions has been done only in the Omoiji-Nagasawa area (Nakajima et al., 1977) and Asemigawa-Shirataki area (Nakajima, 1982) in central Shikoku, and thus, it is still hard to solve the regional thermal structure of the PA facies region. This study is aimed to reveal the thermal structure of the PA facies region of the Sanbagawa belt in Shikoku by analyzing the mineral assemblages and mineral chemistries of metabasites from the nine newly studied areas. The studied areas studied belong to the chlorite zone in the Oboke and Besshi units; the Oboke unit structurally underlay the Besshi unit. The mineral assemblages include pumpellyite + epidote + actinolite, epidote + actinolite _ hematite and epidote + Na-amphibole + actinolite + hematite. The metabasites from some areas involve Na-pyroxene-bearing assemblages, but the analyses of the Schreinemakers bundle of Tagiri et al. (1992) show that these assemblages do not define the Na-pyroxene-chlorite subfacies. As the low-grade metamorphic rocks do not have the hematite + pumpellyite paragenesis, its metamorphic temperature is estimated to be higher than the discontinuous reaction temperature of pumpellyite + hematite + quartz = epidote + actinolite + H2O, as shown by Nakajima et al. (1977). It is difficult to detect the difference in temperature in the PA facies regions by analyzing mineral assemblages. To detect the difference in temperature, and then to reveal

  9. Analysis of hydrogeochemical facies in groundwater of upper part of Cross River Basin, southeastern Nigeria

    Stephen, Ukpai N.; Celestine, Okogbue O.; Solomon, Onwuka O.


    Upper Cross River Hydrogeological Basin lies within latitudes 60 021N to 60 241N and longitudes 80 001E to 80 161E, and is generally underlain by shales of Asu River group of Albian age. The area has Histories of intensive mineralization which influenced groundwater system, resulting to occurrence of different water types. This study determines the various water types via evaluation of major ion concentration from representative water samples collected across the area. Twenty (20) water samples were analyzed using Spectrophotometer of HACH DR/2010 series, and results showed that groundwater in the area is generally hard and polluted with TDS in some places. Statistical inspection was performed on the results using aqua-chem, and it delineated five hydro-chemical facies, namely: Ca-Mg-Cl-S04, Ca-Mg-HCO3-Cl-SO4, Ca-Mg-HCO3, Na-K-HCO3 and Na-K-Cl-SO4; all lie between slight acidic and weak alkaline water. These chemical facies (water types) diffused from non-point sources in urban area and point source from south of Abakaliki town. The dispersion of the facies plumes is possibly controlled by advection process through structural weak zones such as fractures. Hydraulic heads determined from hand-dug wells indicate local potentiometric surfaces, hence, showed local groundwater flow system which is possibly controlled by the underlying low permeable aquicludes formed by shales. The protective capacity of the aquitards was somewhat reduced by the permeating fractures which exposed the aquifers to polluting effects of mineralized water-types.

  10. Carbon and oxygen isotope compositions of the carbonate facies in the Vindhyan Supergroup, central India

    S Banerjee; S K Bhattacharya; S Sarkar


    The Vindhyan sedimentary succession in central India spans a wide time bracket from the Paleopro- terozoic to the Neoproterozoic period.Chronostratigraphic significance of stable carbon and oxygen isotope ratios of the carbonate phase in Vindhyan sediments has been discussed in some recent studies.However,the subtle controls of facies variation,depositional setting and post-depositional diagenesis on stable isotope compositions are not yet clearly understood.The Vindhyan Super- group hosts four carbonate units,exhibiting a wide variability in depositional processes and paleogeography.A detailed facies-specific carbon and oxygen isotope study of the carbonate units was undertaken by us to investigate the effect of these processes and to identify the least altered isotope values.It is seen that both carbon and oxygen isotope compositions have been affected by early meteoric water diagenesis.The effect of diagenetic alteration is,however,more pronounced in case of oxygen isotopes than carbon isotopes.Stable isotope compositions remained insensitive to facies only when sediments accumulated in a shallow shelf setting without being exposed.Major alteration of original isotope ratios was observed in case of shallow marine carbonates,which became exposed to meteoric fluids during early diagenetic stage.Duration of exposure possibly determined the magnitude of alteration and shift from the original values.Moreover,dolomitization is found to be accompanied by appreciable alteration of isotope compositions in some of the carbonates.The present study suggests that variations in sediment depositional settings,in particular the possibility of subaerial exposure,need to be considered while extracting chronostratigraphic signi ficance from 13C data.

  11. Characterization of facies and permeability patterns in carbonate reservoirs based on outcrop analogs. Final report

    Kerans, C.; Lucia, F.J.; Senger, R.K.; Fogg, G.E.; Nance, H.S.; Hovorka, S.D.


    The primary objective of this research is to develop methods for better describing the three-dimensional geometry of carbonate reservoir flow units as related to conventional or enhanced recovery of oil. San Andres and Grayburg reservoirs were selected for study because of the 13 Bbbl of remaining mobile oil and 17 Bbbl of residual oil in these reservoirs. The key data base is provided by detailed characterization of geologic facies and rock permeability in reservior-scale outcrops of the Permian San Andres Formation in the Guadalupe Mountains of New Mexico. Emphasis is placed on developing an outcrop analog for San Andres strata that can be used as (1) a guide to interpreting the regional and local geologic framework of the subsurface reservoirs (2) a data source illustrating the scales and patterns of variability of rock-fabric facies and petrophysical properties, particularly in lateral dimension, and on scales that cannot be studied during subsurface reservoir characterization. The research approach taken to achieve these objectives utilizes the integration of geologic description, geostatistical techniques, and reservoir flow simulation experiments. Results from this research show that the spatial distribution of facies relative to the waterflood direction can significantly affect how the reservoir produces. Bypassing of unswept oil occurs due to cross flow of injected water from high permeability zones into lower permeability zones were high permeability zones terminate. An area of unswept oil develops because of the slower advance of the water-injection front in the lower permeability zones. When the injection pattern is reversed, the cross-flow effect changes due to the different arrangements of rock-fabric flow units relative to the flow of injected water, and the sweep efficiency is significantly different. Flow across low-permeability mudstones occurs showing that these layers do not necessarily represent flow barriers.

  12. Fluid heterogeneity during granulite facies metamorphism in the Adirondacks: stable isotope evidence

    Valley, J.W.; O'Neil, J.R.


    The preservation of premetamorphic, whole-rock oxygen isotope ratios in Adirondack metasediments shows that neither these rocks nor adjacent anorthosites and gneisses have been penetrated by large amounts of externally derived, hot CO2-H2O fluids during granulite facies metamorphism. This conclusion is supported by calculations of the effect of fluid volatilization and exchange and is also independently supported by petrologic and phase equilibria considerations. The data suggest that these rocks were not an open system during metamorphism; that fluid/rock ratios were in many instances between 0.0 and 0.1; that externally derived fluids, as well as fluids derived by metamorphic volatilization, rose along localized channels and were not pervasive; and thus that no single generalization can be applied to metamorphic fluid conditions in the Adirondacks. Analyses of 3 to 4 coexisting minerals from Adirondack marbles show that isotopic equilibrium was attained at the peak of granulite and upper amphibolite facies metamorphism. Thus the isotopic compositions of metamorphic fluids can be inferred from analyses of carbonates and fluid budgets can be constructed. Carbonates from the granulite facies are on average, isotopically similar to those from lower grade or unmetamorphosed limestones of the same age showing that no large isotopic shifts accompanied high grade metamorphism. Equilibrium calculations indicate that small decreases in ??18O, averaging 1 permil, result from volatilization reactions for Adirondack rock compositions. Additional small differences between amphibolite and granulite facies marbles are due to systematic lithologie differences. The range of Adirondack carbonate ??18O values (12.3 to 27.2) can be explained by the highly variable isotopic compositions of unmetamorphosed limestones in conjunction with minor 18O and 13C depletions caused by metamorphic volatilization suggesting that many (and possibly most) marbles have closely preserved their

  13. Submarine-fan facies associations of the Eocene Butano Sandstone, Santa Cruz mountains, California

    Nilsen, Tor H.


    The Eocene Butano Sandstone was deposited as a submarine fan in a relatively small, partly restricted basin in a borderland setting. It is possibly as thick as 3000 m and was derived from erosion of nearly Mesozoic granitic and older metamorphic rocks located to the south. Deposition was at lower bathyal to abyssal water depths. The original fan may have been 120-to 160-km long and 80-km wide. Outcrops of submarine-canyon, innerfan, middle-fan, and outer-fan facies associations indicate that the depositional model of Mutti and Ricci Lucchi can be used to describe the Butano Sandstone.

  14. New interpretations of the facies of the Rhenish brown coal of West Germany

    Hagemann, H.W.; Wolf, M.


    New ideas concerning the understanding of the facies of the Rhenish brown coal of West Germany are discussed. These new interpretations are based on a significantly larger number of samples and refined procedures for analysis within the field of paleobotany, palynology, coal petrology and organic geochemistry than were available to P.W. Thomson and M. Teichmuller. The light and dark bands in the coal are mainly the result of different degrees of plant decomposition. The influence of the peat-forming plant communities plays a subordinate role in the petrographical composition of these particular strata of the Rhenish brown coal. 28 refs.

  15. Coralgal facies of the Upper Eocene-Lower Oligocene limestones in Letca-Rastoci area

    Ioana Prica


    Full Text Available In this paper are described the coralgal facies identified in the Upper Eocene-Lower Oligocene limestone succession (Cozla Formation outcropping in two quarries at Letca and Rastoci (Sălaj district, Romania. In the studied profiles the coral and algae limestones are interlayered with bioclastic limestones with foraminifera. On the top of relatively deep water deposits, coral and algae crusts and dendritic corals coated by algae were deposited. The environment registered a gradual deepening, the deposits being completely immersed, while bioclastic limestones with foraminifera were recurrently formed. This cycle is repeated, the whole succession being caracterized by several such “parasequences”.

  16. Mineralogy and geochemistry of the main glauconite bed in the Middle Eocene of Texas: paleoenvironmental implications for the verdine facies.

    Sherie C Harding

    Full Text Available The Main Glauconite Bed (MGB is a pelleted greensand located at Stone City Bluff on the south bank of the Brazos River in Burleson County, Texas. It was deposited during the Middle Eocene regional transgression on the Texas Gulf Coastal Plain. Stratigraphically it lies in the upper Stone City Member, Crockett Formation, Claiborne Group. Its mineralogy and geochemistry were examined in detail, and verdine facies minerals, predominantly odinite, were identified. Few glauconitic minerals were found in the green pelleted sediments of the MGB. Without detailed mineralogical work, glaucony facies minerals and verdine facies minerals are easily mistaken for one another. Their distinction has value in assessing paleoenvironments. In this study, several analytical techniques were employed to assess the mineralogy. X-ray diffraction of oriented and un-oriented clay samples indicated a clay mixture dominated by 7 and 14Å diffraction peaks. Unit cell calculations from XRD data for MGB pellets match the odinite-1M data base. Electron microprobe analyses (EMPA from the average of 31 data points from clay pellets accompanied with Mössbauer analyses were used to calculate the structural formula which is that of odinite: Fe(3+ 0.89 Mg0.45 Al0.67 Fe(2+ 0.30 Ti0.01 Mn0.01 Σ = 2.33 (Si1.77 Al0.23 O5.00 (OH4.00. QEMSCAN (Quantitative Evaluation of Minerals by Scanning Electron Microscopy data provided mineral maps of quantitative proportions of the constituent clays. The verdine facies is a clay mineral facies associated with shallow marine shelf and lagoonal environments at tropical latitudes with iron influx from nearby runoff. Its depositional environment is well documented in modern nearshore locations. Recognition of verdine facies clays as the dominant constituent of the MGB clay pellets, rather than glaucony facies clays, allows for a more precise assessment of paleoenvironmental conditions.

  17. Mineralogy and geochemistry of the main glauconite bed in the Middle Eocene of Texas: paleoenvironmental implications for the verdine facies.

    Harding, Sherie C; Nash, Barbara P; Petersen, Erich U; Ekdale, A A; Bradbury, Christopher D; Dyar, M Darby


    The Main Glauconite Bed (MGB) is a pelleted greensand located at Stone City Bluff on the south bank of the Brazos River in Burleson County, Texas. It was deposited during the Middle Eocene regional transgression on the Texas Gulf Coastal Plain. Stratigraphically it lies in the upper Stone City Member, Crockett Formation, Claiborne Group. Its mineralogy and geochemistry were examined in detail, and verdine facies minerals, predominantly odinite, were identified. Few glauconitic minerals were found in the green pelleted sediments of the MGB. Without detailed mineralogical work, glaucony facies minerals and verdine facies minerals are easily mistaken for one another. Their distinction has value in assessing paleoenvironments. In this study, several analytical techniques were employed to assess the mineralogy. X-ray diffraction of oriented and un-oriented clay samples indicated a clay mixture dominated by 7 and 14Å diffraction peaks. Unit cell calculations from XRD data for MGB pellets match the odinite-1M data base. Electron microprobe analyses (EMPA) from the average of 31 data points from clay pellets accompanied with Mössbauer analyses were used to calculate the structural formula which is that of odinite: Fe(3+) 0.89 Mg0.45 Al0.67 Fe(2+) 0.30 Ti0.01 Mn0.01) Σ = 2.33 (Si1.77 Al0.23) O5.00 (OH)4.00. QEMSCAN (Quantitative Evaluation of Minerals by Scanning Electron Microscopy) data provided mineral maps of quantitative proportions of the constituent clays. The verdine facies is a clay mineral facies associated with shallow marine shelf and lagoonal environments at tropical latitudes with iron influx from nearby runoff. Its depositional environment is well documented in modern nearshore locations. Recognition of verdine facies clays as the dominant constituent of the MGB clay pellets, rather than glaucony facies clays, allows for a more precise assessment of paleoenvironmental conditions.

  18. Mineralogy and Geochemistry of the Main Glauconite Bed in the Middle Eocene of Texas: Paleoenvironmental Implications for the Verdine Facies

    Harding, Sherie C.; Nash, Barbara P.; Petersen, Erich U.; Ekdale, A. A.; Bradbury, Christopher D.; Dyar, M. Darby


    The Main Glauconite Bed (MGB) is a pelleted greensand located at Stone City Bluff on the south bank of the Brazos River in Burleson County, Texas. It was deposited during the Middle Eocene regional transgression on the Texas Gulf Coastal Plain. Stratigraphically it lies in the upper Stone City Member, Crockett Formation, Claiborne Group. Its mineralogy and geochemistry were examined in detail, and verdine facies minerals, predominantly odinite, were identified. Few glauconitic minerals were found in the green pelleted sediments of the MGB. Without detailed mineralogical work, glaucony facies minerals and verdine facies minerals are easily mistaken for one another. Their distinction has value in assessing paleoenvironments. In this study, several analytical techniques were employed to assess the mineralogy. X-ray diffraction of oriented and un-oriented clay samples indicated a clay mixture dominated by 7 and 14Å diffraction peaks. Unit cell calculations from XRD data for MGB pellets match the odinite-1M data base. Electron microprobe analyses (EMPA) from the average of 31 data points from clay pellets accompanied with Mössbauer analyses were used to calculate the structural formula which is that of odinite: Fe3+0.89 Mg0.45 Al0.67 Fe2+0.30 Ti0.01 Mn0.01) Σ = 2.33 (Si1.77 Al0.23) O5.00 (OH)4.00. QEMSCAN (Quantitative Evaluation of Minerals by Scanning Electron Microscopy) data provided mineral maps of quantitative proportions of the constituent clays. The verdine facies is a clay mineral facies associated with shallow marine shelf and lagoonal environments at tropical latitudes with iron influx from nearby runoff. Its depositional environment is well documented in modern nearshore locations. Recognition of verdine facies clays as the dominant constituent of the MGB clay pellets, rather than glaucony facies clays, allows for a more precise assessment of paleoenvironmental conditions. PMID:24503875

  19. Geochemical multielement signatures of glacial and interglacial facies of the Okhotsk Sea deepwater sediments during the past 350 kyr: A response to global climate changes at the orbital and millennial scales

    Chebykin, Eugene P.; Gorbarenko, Sergey A.; Stepanova, Ol'ga G.; Panov, Vsevolod S.; Goldberg, Evgeny L.


    The previously dated deepwater sediment core MR06-04 PC-7R (length 1723 cm; 350 kyr) recovered from the central Okhotsk Sea (OS) was analyzed for biogenic compounds and for 63 chemical elements (using the inductively coupled plasma-mass spectrometry method) with a high resolution (1 cm; ~200 years). A one box model with two main members" and mathematical methods (based on multielemental composition of sediments) for the calculation of weight fractions (at each time slice) of two main types of geochemical facies that dominate during considerably diverse climatic periods (glacial maxima and interglacial optima) were proposed and tested. This model can be applied to other analogous natural systems whose sedimentation is driven by two main types of geochemical facies. The application of the developed model to the studied core revealed that variations of weight fractions of the typical interglacial and glacial geochemical facies in the sediments along the core depth (named as warm and cold "covariators," respectively) change synchronously with global and regional climate variability. Profiles of warm and inversed cold covariators coincide tightly, and their values increase during warm marine isotope stages and substages and decrease during cold ones over the last 350 kyr. Millennial scale changes in covariators had occurred simultaneously with abrupt variability in the OS productivity and sediment lithology and with millennial global climate variability. Some discrepancies in the warm and inversed cold covariators calculated using specific mathematical treatments revealed the episodic influence of volcanogenic matter presented in the core by visible tephra layers and cryptotephras.

  20. Estudio sedimentológico del Keuper inferior, a partir del análisis de facies, en el sector central de la Cordillera Bética. Algunas consideraciones paleogeográficas

    López Chicano, M.


    Full Text Available The lower Keuper of the central sector of Betic Cordillera shows a predominance of clays with variegated colours. They have intercalations of thin layers of sandstones (fine grain, gypsum and carbonates. Through sedimentological and stratigraphic analysis we can conclude that these materials are from a systems tract fluviocoastal further more it allows us to distinguish sorne different facies types which characterize the following subenvironments. They are set in a framework of mud flat, found on a vast tidal coastal lutitic plain. Terrigenous sediments (fine sands from the mainland are deposited on the lutitic plain by ephemeral streams. In this coastal environment there are subenvironments of salt marsh, salt pans, sabkha, coastal lagoons, etc. The distribution in time and space of these facies was mainly controlled by the climate and the frequent incursions of the sea over the coastal plain, facilited by the flat geographical nature of coastline.En el Keuper inferior del sector central de la Cordillera Bética hay un predominio de materiales arcillosos, de colores abigarrados, con niveles intercalados de areniscas de grano fino, yesos y carbonatos. A partir del análisis estratigráfico y sedimentológico se han interpretado estos materiales como pertenecientes a un cortejo fluviocostero. Este análisis ha permitido, previamente, diferenciar diversas asociaciones de facies que caracterizan varios ambientes sedimentarios. Esencialmente, se enmarcan en un mud flat, dentro de una extensa llanura costera parcialmente afectada por mareas. A ésta llegan sedimentos detríticos continentales (arenas finas mediante corrientes fluviales efímeras. Dentro de este mismo medio costero aparecen ambientes de marisma, salt pans, sabkha, laguna, etc. La evolución en el tiempo y en el espacio de estas facies está controlada principalmente por el clima y por las frecuentes ingresiones del mar sobre la llanura costera, las cuales están facilitadas por la

  1. Facies Architecture And Sequence Stratigraphy of Jurassic Tidal Successions in the Lajas Formation, Neuquen Basin, Argentina; an Outcrop Analogue For the Tilje Formation, Offshore Mid-Norway

    McIlroy, D.; Flint, S.


    A common element of sequence stratigraphic models for ancient shallow marine systems is the switch from wave-dominated shoreface deposition during highstand to tidal/estuarine deposition within incised valleys which provide the necessary amplification of tidal currents, during lowstand/early base level rise. Thus, tide-dominated sedimentation is restricted to specific base level positions, which has important implications for reservoir geometry and quality. The Lajas Formation is studied as an analogue to the Jurassic Tilje Formation. The similar age, tectonic setting, sedimentology and aggradational nature of the tidal succession make the Lajas an ideal analogue with which to study facies architecture and test sequence stratigraphic models. This is especially so, since field data can be tied to geophysical data associated with producing oil fields. The lower Jurassic Lajas Formation of the Neuquen basin comprises 500 m of well-exposed tide-dominated sediments deposited as two low frequency unconformity-bounded sequences which are tide-dominated throughout.

  2. Primary and redeposited facies from a large-magnitude, rhyolitic, phreatomagmatic eruption: Cana Creek Tuff, Late Carboniferous, Australia

    McPhie, J.


    The Cana Creek Tuff is one of four rhyolitic ignimbrite members of the Late Carboniferous Currabubula Formation, a volcanogenic conglomeratic braidplain sequence exposed along the western margin of the New England Orogen in northeastern New South Wales. The source is not exposed but was probably located tens of kilometres to the west of existing outcrops. The medial to distal parts of the tuff average about 70 m in thickness, are widespread (minimum present area ˜ 1400 km 2), and comprise a primary pyroclastic facies (ignimbrite, ash-fall tuff) and a redeposited volcaniclastic facies (sandstone, conglomerate). Both facies are composed of differing proportions of crystal fragments (quartz, plagioclase, K-feldspar), pumiceous clasts (pumice, shards, fine ash), and accidental lithics. The eruption responsible for this unit was explosive and of large magnitude (dense rock equivalent volume about 100 km 3). That it was also phreatomagmatic in character is proposed on the basis of: the intimate association of primary and redeposited facies; the presence of accretionary lapilli both in ignimbrite and in ash-fall tuff; the fine grain size of juvenile pyroclasts; the low grade of the ignimbrite; and the close similarity in facies, composition and magnitude to the deposits from the 20,000y. B.P. phreatomagmatic eruption at Taupo, New Zealand (the Wairakei and parts of the Hinuera Formations). The eruption began and ended from a vent with excess water available, possibly submersed in a caldera lake, and generated volcaniclastic sheet floods and debris flows. The emplacement of the primary pyroclastic facies is correlated with an intervening stage when the water:magma mass ratio was lower. The deposits from a large-magnitude, phreatomagmatic eruption are predicted to show systematic lateral variations in facies. Primary pyroclastic facies predominate near the source although the preserved stratigraphy is an incomplete record because of widespread contemporaneous erosion

  3. Determinación de carbono orgánico en materias primas cerámicas en presencia de siderita, FeCO3

    Gazulla, M. F.


    Full Text Available Not availableLa materia orgánica es una de las impurezas presentes en las materias primas utilizadas en la fabricación de pavimentos y revestimientos cerámicos. Durante el proceso de cocción, el carbono orgánico (Corgánico puede producir la aparición de un núcleo negro conocido como “corazón negro”, que puede causar defectos en el producto final. Las materias primas cerámicas contienen Corgánico a nivel de mg·kg-1 (procedente de la materia orgánica y carbono inorgánico (Cinorgánico a nivel de porcentaje (procedente de siderita (FeCO3, calcita (CaCO3 y dolomita (CaMg(CO32, principalmente. La presencia de siderita puede interferir en la determinación de Corgánico puesto que su temperatura de descomposición difiere muy poco de la temperatura de determinación del Corgánico, no ocurriendo lo mismo con la calcita y la dolomita, cuyas temperaturas de descomposición son superiores. Existen diversos métodos para la determinación de Corgánico en muestras sólidas, aunque no se han encontrado estudios cuantitativos sobre dicha determinación en presencia de siderita. En este trabajo se han desarrollado dos métodos para determinar Corgánico en materias primas y composiciones cerámicas mediante análisis elemental, en presencia de siderita, que pueden ser utilizados en el control de la aparición de corazón negro en baldosas cerámicas. La metodología desarrollada presenta bajos límites de cuantificación e incertidumbres, siendo un método rápido y preciso.

  4. Sedimentary Facies Models on Carbonatite in the Upper Shuaiba Member of Lower Cretaceous in Daleel Field, Oman

    Wang Feng; Jiang Zaixing; Zhou Liqing; Zhao Guoliang; Wang Lin; Zheng Ning; Xiang Shu'an


    The Upper Shuaiba Member (USH) is the main force pay bed in the Daleel field in northern Oman; 5 layers including A, B, C, D, and E were divided in profile, and layer D and layer E are the main beds. With the development of exploration in the Daieel oil field, studying the sedimentary systems about their inner composition and the collocation in dimension, and setting up the sedimentary models in the USH are becoming more and more necessary and important to meet the further exploration requirement. Based on the data of geology, seism, and paleo-biology, according to the analysis method on carbonatite depositional system, the litho-facies assemblage and sedimentary environment in the USH were studied. Intershoal low-lying sub-facies (where the water depth is 10-50 m) and shallow shoal sub-facies (where the water depth is not more than 10 m) were extinguished in the layer D, and storm deposit was found in layer E1, in which intershoal low-lying sub-facies also developed. The feature of the sedimentary sub-facies and the sedimentary condition were analyzed, and the sedimentary model was set up in the article: the carbonatite intershoal low-lying developed under the background of open land in shallow sea, where storm events usually occurred in the Lower Cretaceous in the area.

  5. Trace element signature and U-Pb geochronology of eclogite-facies zircon, Bergen Arcs, Caledonides of W Norway

    Bingen, Bernard; Austrheim, Håkon; Whitehouse, Martin J.; Davis, William J.

    Secondary-ion mass spectrometry (SIMS) U-Pb and trace element data are reported for zircon to address the controversial geochronology of eclogite-facies metamorphism in the Lindås nappe, Bergen Arcs, Caledonides of W Norway. Caledonian eclogite-facies overprint in the nappe was controlled by fracturing and introduction of fluid in the Proterozoic-Sveconorwegian-granulite-facies meta-anorthosite-norite protolith. Zircon grains in one massive eclogite display a core-rim structure. Sveconorwegian cores have trace element signatures identical with those of zircon in the granulite protolith, i.e. 0.31<=Th/U<=0.89, heavy rare earth element (HREE) enrichment, and negative Eu anomaly. Weakly-zoned to euhedral oscillatory-zoned Caledonian rims are characterized by Th/U<=0.13, low LREE content (minimum normalized abundance for Pr or Nd), variable enrichment in HREE, and no Eu anomaly. A decrease of REE towards the outermost rim, especially HREE, is documented. This signature reflects co-precipitation of zircon with garnet and clinozoisite in a feldspar-absent assemblage, and consequently links zircon to the eclogite-facies overprint. The rims provide a mean 206Pb/238U crystallization age of 423+/-4 Ma. This age reflects eclogite-forming reactions and fluid-rock interaction. This age indicates that eclogite-facies overprint in the Lindås nappe took place at the onset of the Scandian (Silurian) collision between Laurentia and Baltica.

  6. Multiscale approach to (micro)porosity quantification in continental spring carbonate facies: Case study from the Cakmak quarry (Denizli, Turkey)

    De Boever, Eva; Foubert, Anneleen; Oligschlaeger, Dirk; Claes, Steven; Soete, Jeroen; Bertier, Pieter; Özkul, Mehmet; Virgone, Aurélien; Swennen, Rudy


    Carbonate spring deposits gained renewed interest as potential contributors to subsurface reservoirs and as continental archives of environmental changes. In contrast to their fabrics, petrophysical characteristics - and especially the importance of microporosity (quarry (Denizli, Turkey): the extended Pond, the dipping crystalline Proximal Slope Facies and the draping Apron and Channel Facies deposits formed by encrustation of biological substrate. Integrating mercury injection capillary pressure, bulk and diffusion Nuclear Magnetic Resonance (NMR), NMR profiling and Brunauer-Emmett-Teller (BET) measurements with microscopy and micro-computer tomography (µ-CT), shows that NMR T2 distributions systematically display a single group of micro-sized pore bodies, making up between 6 and 33% of the pore space (average NMR T2 cut-off value: 62 ms). Micropore bodies are systematically located within cloudy crystal cores of granular and dendritic crystal textures in all facies. The investigated properties therefore do not reveal differences in micropore size or shape with respect to more or less biology-associated facies. The pore network of the travertine facies is distinctive in terms of (i) the percentage of microporosity, (ii) the connectivity of micropores with meso- to macropores, and (ii) the degree of heterogeneity at micro- and macroscale. Results show that an approach involving different NMR experiments provided the most complete view on the 3-D pore network especially when microporosity and connectivity are of interest.

  7. El concepto de «facies» aplicado al Paleolítico Superior



    Full Text Available La existencia comprobada de distintas «faciès» dentro del Musteriense, ampliamente estudiada por F. Bordes, ha sido, como se sabe, objeto de discusión en lo que se refiere a su interpretación y a las causas determinantes de sus diferencias. El tema puede ser enfocado desde dos puntos de vista bien distintos. Para Bordes (1959, 1972 et alibi las diferencias entre las cuatro o cinco faciès del Musteriense, que aparecen interestratificadas en varios yacimientos, se deberían a la existencia de distintos grupos humanos con sus peculiares tradiciones culturales, que en un régimen de nomadismo moderado habrían visitado alternativamente los yacimientos, estableciéndose temporalmente en ellos. Para la llamada «Escuela americana», con Freeman (1966, 1973 et alibi y Binford (1966 y 1972 principalmente, tales diferencias se deberían más bien a un condicionamiento de los mismos grupos al medio ambiente, de acuerdo con actividades específicas distintas y frecuentemente de carácter estacional.

  8. Archaeal populations in two distinct sedimentary facies of the subsurface of the Dead Sea.

    Thomas, C; Ionescu, D; Ariztegui, D


    Archaeal metabolism was studied in aragonitic and gypsum facies of the Dead Sea subsurface using high-throughput DNA sequencing. We show that the communities are well adapted to the peculiar environment of the Dead Sea subsurface. They harbor the necessary genes to deal with osmotic pressure using high- and low-salt-in strategies, and to cope with unusually high concentrations of heavy metals. Methanogenesis was identified for the first time in the Dead Sea and appears to be an important metabolism in the aragonite sediment. Fermentation of residual organic matter, probably performed by some members of the Halobacteria class is common to both types of sediments. The latter group represents more than 95% of the taxonomically identifiable Archaea in the metagenome of the gypsum sediment. The potential for sulfur reduction has also been revealed and is associated in the sediment with EPS degradation and Fe-S mineralization as revealed by SEM imaging. Overall, we show that distinct communities of Archaea are associated with the two different facies of the Dead Sea, and are adapted to the harsh chemistry of its subsurface, in different ways.

  9. Global dominance of coralline red-algal facies: A response to Miocene oceanographic events

    Halfar, Jochen; Mutti, Maria


    Rhodoliths (free-living coralline red algae) can thrive under a wide range of temperatures, reduced light, and increased nutrient levels, and often form a distinct so-called rhodalgal lithofacies that is an important component of Cenozoic shallow-water carbonates. Global distributions illustrate that from the late-early to early-late Miocene (Burdigalian early Tortonian), rhodalgal facies reached peak abundances and commonly replaced coral-reef environments, accompanied by a decline in other carbonate-producing phototrophs. We argue that the dominance of red algae over coral reefs was triggered in the Burdigalian by enhanced trophic resources associated with a global increase in productivity, as evidenced by a long-term shift toward higher carbon isotope values. Rhodalgal lithofacies expanded further in the middle Miocene when strengthened thermal gradients associated with the establishment of the East Antarctic Ice Sheet led to enhanced upwelling while climate change generated increased weathering rates, introducing land-derived nutrients into the oceans. Globally cooler temperatures following a climatic optimum in the early-middle Miocene contributed to sustain the dominance of red algae and prevented the recovery of coral reefs. The global shift in nearshore shallow-water carbonate producers to groups tolerant of higher levels of trophic resources provides further evidence for increased nutrient levels during that time interval and shows the sensitivity of shallow-water carbonate facies as indicators of past oceanographic conditions.

  10. Permian Mengkarang coal facies and environment, based on organic petrology study

    Nana Suwarna


    Full Text Available Permian Mengkarang Coal Measures is situated in the middle part of Sumatera Island. Some fresh outcrop samples of the Permian Mengkarang coals have been analyzed both macroscopically and microscopically, to asses their depositional environment. On the basis of organic-petrological analysis, the coal seams show variation in the predominance of some macerals, indicating successions of environmental changes. The dominant maceral group is vitrinite, present in very low to very high values; whilst the minor one is inertinite showing low amount. Environmental information derived from the organic facies study shows that the coals were deposited in wet zone of mire, ranges from wet limnic-telmatic zone to telmatic wet forest swamp under rapid burial condition, due to rapid basin subsidence. The organic facies concept is thus applicable in basin studies context and has potential to become an additional tool for interpretation of depositional environment.    

  11. Application of seismic facies and attributes analysis on the identification of Permian igneous rock

    Xu Yongzhong; Yang Haijun; Liu Yongfu; Wang Shuangshuang; Yang Peng; Zhao Jixiang


    Seismic facies and attributes analysis techniques are introduced.The geological characteristics of some oil fields in western China are used in conjunction with drilling results and logging data to identify the lithology,intrusion periods,and distribution range of the Permian igneous rocks in this area.The lithologic classification,the vertical and horizontal distribution,and the intrusion periods of igneous rock were deduced through this study.Combining seismic facies and attributes analysis based on optimization can describe the igneous rock in detail.This is an efficient way to identify lithology and intrusion periods.Using geological data and GR-DT logging cross-plots the Permian igneous rock from TP to TT was divided into three periods.The lithology of the first period is tuff and clasolite with a thickness ranging from 18 to 80 ms.The second is basalt with a thickness ranging from 0 to 20 ms.The third is tuff and clasolite and dacite whose thickness ranges from 60 to 80 ms.These results can help understand the clasolite trap with low amplitude and the lithologic trap of the Carboniferous and Silurian.They can also guide further oil and/or gas exploration.

  12. Facies recognition using a smoothing process through Fast Independent Component Analysis and Discrete Cosine Transform

    Sanchetta, Alexandre Cruz; Leite, Emilson Pereira; Honório, Bruno César Zanardo


    We propose a preprocessing methodology for well-log geophysical data based on Fast Independent Component Analysis (FastICA) and Discrete Cosine Transform (DCT), in order to improve the success rate of the K-NN automatic classifier. The K-NN have been commonly applied to facies recognition in well-log geophysical data for hydrocarbon reservoir modeling and characterization. The preprocess was made in two different levels. In the first level, a FastICA based dimenstion reduction was applied, maintaining much of the information, and its results were classified; In second level, FastICA and DCT were applied in smoothing level, where the data points are modified, so individual points have their distance reduced, keeping just the primordial information. The results were compared to identify the best classification cases. We have applied the proposed methodology to well-log data from a petroleum field of Campos Basin, Brazil. Sonic, gamma-ray, density, neutron porosity and deep induction logs were preprocessed with FastICA and DCT, and the product was classified with K-NN. The success rates in recognition were calculated by appling the method to log intervals where core data were available. The results were compared to those of automatic recognition of the original well-log data set with and without the removal of high frequency noise. We conclude that the application of the proposed methodology significantly improves the success rate of facies recognition by K-NN.

  13. Plagioclase deformation in upper-greenschist facies meta-pegmatite mylonites from the Austroalpine Matsch Unit (Eastern Alps, Italy)

    Eberlei, Tobias; Habler, Gerlinde; Abart, Rainer; Grasemann, Bernhard


    Feldspars are common rock forming minerals as they are stable over a wide range of bulk rock compositions and metamorphic conditions within the Earth's crust. The deformation mechanisms of feldspar play an important role in rheological models for the crust and therefore have received considerable attention in studies on natural rocks and in experimental studies. The interaction of frictional and viscous deformation mechanisms and the onset of crystal plastic deformation in feldspars occur over a broad range of pressures and temperatures. In this work, we present new microstructural, textural and mineral chemical data of plagioclase from Permian metapegmatites within the Austroalpine Matsch Unit in Southern Tyrol (Italy). These crystalline basement rocks were deformed and metamorphosed at conditions close to the greenschist/amphibolites facies transition at 480±26°C during the Cretaceous (Habler et al., 2009). The investigated samples have been collected from meter-scale shear zones which typically occur at boundaries of lithological subunits. The southern tectonic boundary of this unit is commonly referred to as the "Vinschgau Shear Zone" (Schmid & Haas, 1989). We applied the Electron Backscatter Diffraction method to investigate the grain- and subgrain-boundaries and the nature of effective deformation mechanisms in plagioclase. Large albite porphyroclasts in the mylonitic Permian metapegmatites show grain internal traces of dissolution surfaces and the formation of new, strain-free grains with straight grain boundary segments and partly 120° grain boundary triple junctions in dilatant sites. The aggregates of new grains neither have a lattice preferred orientation nor a crystallographic orientation relation with the adjacent clast, and are characterized by the lack of grain internal deformation, suggesting that these are new precipitates rather than clast-fragments or recrystallized subgrains. Furthermore, the porphyroclasts show cracks and kinks, associated

  14. Interpretation of the relations between massive, pillowed and brecciated facies in an archean submarine andesite volcano — amulet andesite, rouyn-noranda, Canada

    Cousineau, Pierre; Dimroth, Erich


    The Amulet andesite formation in the Archean terrain of Rouyn-Noranda, P.Q., consists of 19 flows, distinguished by variations in phenocryst content and vesicularity and by the presence of concentric contraction fractures. Detailed mapping of flows revealed the presence of three main facies: (1) massive facies; (2) pillowed facies; and (3) foreset-bedded (brecciated) facies. The massive facies consists of > 50% massive lava overlain by pillow lava and/or pillow breccia. The pillowed facies consists of > 50% pillows. In some flows, the pillowed facies contains a thin sheet of massive lava at the base of the flow (facies 2a). Generally, massive lava fills braided channels 10-50 m wide (facies 2b). Facies 2c consists of pillows and large, irregular, megapillows. Determination of the flow direction shows that facies 1 is proximal, facies 2 distal. The foreset-bedded facies 3 consists of alternating thin (1-2 m) lobes of massive lava, pillow lava and broken-pillow breccia. It makes up flows 16-19 at the top of the sequence. Flow M, a unit entirely composed of massive lava, is ponded against flows 9 and 10. We interpret the growth of the Amulet andesite volcano in the light of new work on ocean-floor basalt and on the 1969-1973 Mauna Ulu eruption. The feeding fissure was located in the area of massive facies. At the beginning of eruptions lava spread laterally as a sheet-flood flow (massive base of facies 2a) but rapidly became channelized. The pillow lava and in particular the facies 2b, 2c and 3 are considered as the subaqueous equivalents of tube-fed pahoehoe. Flow M probably represents a lava lake. Shallowing-upward of the sequence during the built-up of the volcano is indicated by increasing vesicularity of the flows and by an upward increase of the proportion of broken pillow breccia. This increase is gradual from flow 1 to flow 15 but abrupt from flow 15 to 16-19.

  15. Utilización de una nueva materia prima borácica para la formulación de esmaltes

    Gómez-Tena, M. P.


    contenido en B2O3 entre un 10-11 % en peso. Es en gran parte amorfo, siendo el cuarzo la fase cristalina presente de forma mayoritaria. Características tales, como presentar una baja solubilidad y formar fácilmente fase vítrea, hace que sea posible utilizar el nuevo borato, como materia prima en composiciones de esmalte. Su aptitud para la formulación de esmaltes, ha sido el resultado de varios años de investigación en colaboración con el Instituto de Tecnología Cerámica. En este trabajo se ha estudiado la viabilidad de fabricar esmaltes cerámicos haciendo uso de una nueva materia prima borácica sintética, la cual permite aportar boro a la composición de los esmaltes sin necesidad de hacerlo en forma fritada. Se ha podido obtener vidriados con similares características técnicas y estéticas que los obtenidos a partir de esmaltes de uso industrial que contienen fritas típicas en su composición, por lo que resulta posible formular esmaltes mediante el empleo de la nueva materia prima de boro sintética. De los resultados se deriva, que la utilización de esta nueva materia prima (E-4972 es especialmente adecuada para la obtención de vidriados de bajo brillo a elevada temperatura.


    Figueiredo, Izabel Cristina; Maciel,Bruno Ferreira; MARQUES, Marcos Omir


    A qualidade da cana-de-açúcar como matéria-prima para obtenção de álcool é o principal fator a ser levado em conta para o melhor desempenho da fermentação alcoólica. Assim, nos últimos anos a maioria das empresas tem demonstrado a grande importância dos fatores intrínsecos e extrínsecos que afetam a qualidade da cana-de-açúcar. Fatores extrínsecos são aqueles que estão relacionados com materiais estranhos ao colmo (terra, pedra, restos de cultura, plantas invasoras) ou compostos que são produ...

  17. Disseminação de práticas lean em armazéns de matérias-primas utilizando kaizen

    Casarin, Nadiesca


    Dissertação (mestrado) - Universidade Federal de Santa Catarina, Centro Tecnológico. Programa de Pós-Graduação em Engenharia de Produção Essa dissertação tem como tema central a aplicação de uma das abordagens industriais mais estudadas e utilizadas nos últimos anos: a produção lean. O objetivo é desenvolver um método para a disseminação de práticas enxutas na logística interna, mais especificamente, em armazéns de matérias-primas. A aplicação dessas práticas, oriundas do Sistema Toyota de...

  18. Sawadalepis prima n. g., n. sp. (Cestoda: Cyclophyllidea) from the Schreiber's bent-winged bat Miniopterus schreibersii Kuhl (Chiroptera: Vespertilionidae) from China.

    Makarikova, Tatiana A; Makarikov, Arseny A


    Sawadalepis n. g. is erected for Sawadalepis prima n. sp. in Schreiber's bent-winged bat Miniopterus schreibersii Kuhl (Chiroptera: Vespertilionidae) from southern China. Diagnostic features of the currently monotypic genus include attributes of the osmoregulatory system and female genital organs. The dorsal osmoregulatory canals are shifted bilaterally towards the margins of proglottides in relation to the ventral canals. The genital pores are unilateral and sinistral. Among female attributes, the copulatory part of the vagina is covered externally by a dense layer of intensely stained cells; the conductive part of the vagina is clearly distinguishable from the seminal receptacle; the uterus has ventral and dorsal diverticula, extending bilaterally beyond the longitudinal osmoregulatory canals; and the eggs are spherical with thick outer coat.

  19. La suspensión de la cobertura por la mora en el pago de la prima en el contrato de seguros

    Núñez del Prado S., Alonso


    A partir de la discusión que sobre el tema se tuvo en la comisión creada por el Ministerio de Justicia, para la elaboración de un Proyecto de Ley del Contrato de Seguros en el Perú, en este artículo, se comenta, evalúa y critica la regla, que contemplan algunas legislaciones, incluida la peruana, de ‘suspensión automática de cobertura por mora en el pago de la prima en el contrato de seguros’. El autor, luego de una breve introducción, en que nos ambienta sobre el tema, comenta con detalle la...

  20. Active metasomatism in the Cerro Prieto geothermal system, Baja California, Mexico: a telescoped low pressure/temperature metamorphic facies series

    Schiffman, P.; Elders, W.A.; Williams, A.E.; McDowell, S.D.; Bird, D.K.


    In the Cerro Prieto geothermal field, carbonate-cemented, quartzofeldspathic sediments of the Colorado River delta are being actively metasomatized into calc-silicate metamorphic rocks by reaction with alkali chloride brines between 200/sup 0/ and 370/sup 0/C, low fluid and lithostatic pressures, and low oxygen fugacities. Petrologic investigations of drill cores and cutting from over 50 wells in this field identified a prograde series of calc-silicate mineral zones which include as index minerals: wairakite, epidote, prehnite, and clinopyroxene. Associated divariant mineral assemblages are indicative of a very low pressure/temperature metamorphic facies series which encompasses the clay-carbonate, zeolite, greenschist, and amphibolite facies. This hydrothermal metamorphic facies series, which is becoming increasingly recognized in other active geothermal systems, is characterized by temperature-telescoped dehydration and decarbonation mineral equilibria. Its equivalent should now be sought in fossil hydrothermal systems.

  1. DNA hypermethylation and decreased mRNA expression of MAL, PRIMA1, PTGDR and SFRP1 in colorectal adenoma and cancer.

    Kalmár, Alexandra; Péterfia, Bálint; Hollósi, Péter; Galamb, Orsolya; Spisák, Sándor; Wichmann, Barnabás; Bodor, András; Tóth, Kinga; Patai, Árpád V; Valcz, Gábor; Nagy, Zsófia Brigitta; Kubák, Vivien; Tulassay, Zsolt; Kovalszky, Ilona; Molnár, Béla


    Colorectal cancer (CRC) development is accompanied by changes in expression for several genes; but the details of the underlying regulatory procesess remain unknown. Our aims were to assess the role of epigenetic processes in tumour formation and to identify characteristic DNA methylation and miRNA alterations in the colorectal adenoma-carcinoma sequence. Whole genome expression profiling was performed on colonic biopsy samples (49 healthy normal, 49 colorectal adenoma (AD), 49 CRC); on laser capture microdissected (LCM) epithelial and stromal cells from 6 CRC-normal adjacent tissue (NAT) samples pairs, and on demethylated human CRC cell lines using HGU133 Plus 2.0 microarrays (Affymetrix). Methylation status of genes with gradually altering expression along the AD-CRC sequence was further analysed on 10-10 macrodissected and 5-5 LCM samples from healthy colon, from adenoma and from CRC biopsy samples using bisulfite-sequencing PCR (BS-PCR) followed by pyrosequencing. In silico miRNA prediction for the selected genes was performed with miRWALK algorithm, miRNA expression was analysed on 3 CRC-NAT sample pairs and 3 adenoma tissue samples using the Human Panel I + II (Exiqon). SFRP1 immunohistochemistry experiments were performed. A set of transcripts (18 genes including MAL, SFRP1, SULT1A1, PRIMA1, PTGDR) showed decreasing expression (p methylation changes do not appear to play role (e.g. BCL2, MAL, PTGS2). Demethylation treatment could upregulate gene expression of genes that were found to be hypermethylated in human CRC tissue samples. Decreasing protein levels of SFRP1 was also observed along the adenoma-carcinoma sequence. Hypermethylation of the selected markers (MAL, PRIMA1, PTGDR and SFRP1) can result in reduced gene expression and may contribute to the formation of colorectal cancer.

  2. Lacustrine sedimentation and facies model for the last 45,000 yr in Chalco basin. Central Mexico

    Ortega, B.; Lozano, S.; Caballero, M.; Herrera, D.


    Chalco basin in central Mexico (19° 15' N, 98° 58' W, 2200 m asl) is one of the most detailed lake sediment sequence analyzed in Mexico for paleoclimatic and paleoenvironmental studies. In this former lake, five drill cores up to 27 m depth were recovered in 1987-1989 by the UNAM team, and three cores covering most of the former sequence were obtained in 2008 and 2011. The upper 27 m of the Chalco lacustrine sequence contains the record of the last 45 kyr climate history in the northern American tropics. The active tectonic and volcanic setting of Chalco Lake in the Trans-Mexican Volcanic Belt, provides an opportunity to evaluate environmental (volcanic + tectonic vs. climatic) controls on lacustrine sedimentation. The establishment of a detailed time scale by 14C in pollen extracts provides an accurate chronological control. The stratigraphical and sedimentological analyses presented here provided the recognition of depositional environments and the architecture of the upper lacustrine succession. Sedimentary facies were defined on the basis of sedimentological descriptions, microscopic observation and compositional analyses. According to compositional criteria, facies were identified and groped into two main categories according to compositional criteria: 1) detrital and volcaniclastic, and 2) biogenic facies. The clastic facies includes massive to laminated, silty and clayey sediments composed of clay minerals, feldspars, amphiboles with minor amounts of quartz, opaque minerals and calcite. Diatoms are the most common biological remains in all the clastic facies. Most of the volcaniclastic deposits correspond to fall-out deposits, some of them of well documented eruptions of the nearby large stratovolcanoes Popocatepetl and Nevado de Toluca, which in turn serve as stratigraphical markers. The biogenic facies are massive to finely laminated diatom ooze and ostracod ooze layers. The sedimentary architecture of the lacustrine succession has been controlled by

  3. Palynostratigraphy and sedimentary facies of Middle Miocene fluvial deposits of the Amazonas Basin, Brazil

    Dino, Rodolfo; Soares, Emílio Alberto Amaral; Antonioli, Luzia; Riccomini, Claudio; Nogueira, Afonso César Rodrigues


    Palynostratigraphic and sedimentary facies analyses were made on sedimentary deposits from the left bank of the Solimões River, southwest of Manaus, State of Amazonas, Brazil. These provided the age-dating and subdivision of a post-Cretaceous stratigraphic succession in the Amazonas Basin. The Novo Remanso Formation is subdivided into upper and lower units, and delineated by discontinuous surfaces at its top and bottom. The formation consists primarily of sandstones and minor mudstones and conglomerates, reflecting fluvial channel, point bar and floodplain facies of a fluvial meandering paleosystem. Fairly well-preserved palynoflora was recovered from four palynologically productive samples collected in a local irregular concentration of gray clay deposits, rich in organic material and fossilized wood, at the top of the Novo Remanso Formation upper unit. The palynoflora is dominated by terrestrial spores and pollen grains, and is characterized by abundant angiosperm pollen grains ( Tricolpites, Grimsdalea, Perisyncolporites, Tricolporites and Malvacearumpollis). Trilete spores are almost as abundant as the angiosperm pollen, and are represented mainly by the genera Deltoidospora, Verrutriletes, and Hamulatisporis. Gymnosperm pollen is scarce. The presence of the index species Grimsdalea magnaclavata Germeraad et al. (1968) indicates that these deposits belong to the Middle Miocene homonymous palynozone (Lorente, 1986; Hoorn, 1993; Jaramillo et al., 2011). Sedimentological characteristics (poorly sorted, angular to sub-angular, fine to very-coarse quartz sands facies) are typical of the Novo Remanso Formation upper part. These are associated with a paleoflow to the NE-E and SE-E, and with an entirely lowland-derived palinofloristic content with no Andean ferns and gymnosperms representatives. All together, this suggests a cratonic origin for this Middle Miocene fluvial paleosystem, which was probably born in the Purus Arch eastern flank and areas surrounding the

  4. Geomorphological facies reconstruction of Late Quaternary alluvia by the application of fluvial architecture concepts

    Houben, Peter


    This paper investigates the methodical implications, the benefits, and the constraints of applying the fluvial architecture concept to Late Quaternary shallow-subsurface alluvial deposits. The focus is upon a typical small- to mesoscale valley floor of the temperate zone. The studied reach is part of the river Wetter catchment (517 km 2) in central Germany. A large number of studies on Late Quaternary terrestrial paleoenvironmental change of the temperate zone refer to such small- to mesoscale catchments, which are mostly occupied by mixed- to suspended-load rivers. As in many cases mostly coring-based evidence is available, the observation and measurement is limited to lithology and lithofacies boundaries; facies geometry must be inferred. Moreover, in those environments differences in lithofacies are obscured by a significantly reduced range of grain size distributions. An example of an ancient channel belt of Late Glacial to Holocene age serves to delineate the methodical practice and utility of the fluvial architecture approach. Field evidence is obtained from detailed cross-sectional surveys and comprises descriptions of lithofacies, structural, pedogenetical, biotic features, Munsell color, and total organic carbon magnetic volume susceptibility. Cross-sectional lithofacies information is represented by spatially attributed, scaled borehole logs. The example also accentuates the need for applying additional stratigraphical methods such as physical age determination, macrofossil analysis, and tephrological stratigraphy. These methods form the basis to discern stacked channel facies and derive a diachrony of channel forms. Thus, the adapted architecture approach provides a significant surplus of information on channel dimensions, ages, and channel-floodplain interconnectedness. Distinct fluvial landforms such as channels, levees, abandoned channels, swamps, and floodplain flats can be highlighted. A number of methodical constraints are discussed in detail, e

  5. Salt facies and budgets as environmental indicators in the Dead Sea

    Kiro, Yael; Goldstein, Steven L.; Stein, Mordechai; Garcia-Veigas, Javier; Levy, Elan J.; Lazar, Boaz


    Deep drilling in the Dead Sea reveals thick sections of halite that precipitated during the last three interglacials, when lake levels were low. Pore water and halite fluid inclusions show an increase in Mg concentration and a decrease in Na/Cl ratio during precipitation of halite, both during the last interglacial and the beginning of the Holocene. A mass balance based on the thickness of the halite layers and the changes in the chemical composition of the brine has been developed in order to calculate the change in the lake levels. Results indicate a drastic decrease in fresh water input, with the average discharge at 30% and 50% of the modern over thousands of years during the last interglacial and early Holocene, respectively. However, packages of detritus alternating with the halite indicate wetter episodes over intervals of centuries to a few millennia with conditions similar to the present-day, as well as more severe conditions with ~10% of the modern discharge over periods of decades to a few centuries. The different facies of halite in the core are well preserved. The lake level calculation based on the salt budget shows that although the lake level decreased drastically, the lake was always >100 m depth, and the absence of significant halite dissolution supports this conclusion. Thus, the halite reflects deep-water facies. There are two main halite crystal types. Small cumulate crystals that are formed on the lake surface, which alternate with bottom-growth crystals with relatively scarce fluid inclusion bands. The frequency of the crystal alternation varies between seasonal and multi-year changes and reflects the hydrological and limnological regime. The small cumulate crystals require that the lake surface was supersaturated with respect to halite, indicating high evaporation and possibly a thermally stratified water column. The bottom-growth crystals are formed only when it is not disturbed by the "rain" of cumulate crystals, with a lower degree of

  6. Submarine-fan facies associations of the Upper Cretaceous and Paleocene Gottero Sandstone, Ligurian Apennines, Italy

    Nilsen, Tor H.; Abbate, Ernesto


    The Upper Cretaceous and Paleocene Gottero Sandstone was deposited as a small deep-sea fan on ophiolitic crust in a trench-slope basin. It was thrust northeastward as an allochthonous sheet in Early and Middle Cenozoic time. The Gottero, as thick as 1500 m, was probably derived from erosion of Hercynian granites and associated metamorphic rocks in northern Corsica. Outcrops of inner-fan channel, middle-fan channel and interchannel, outer-fan lobe, fan-fringe, and basin-plain facies associations indicate that the depositional model of Mutti and Ricci Lucchi for mixed-sediment deep-sea fans can be used. The original fan had a radius of 30 to 50 km.

  7. Permian sequence stratigraphy of slope facies in southern Guizhou and chronostratigraphic correlation

    史晓颖; 梅仕龙; 孙岩


    The Permian in slope facies area of southern Guizhou consists of 16 third order sequences, which can be grouped as four sequence sets and further into two mesosequences. Most of them are delineated by conformable or submarine erosion surfaces, and well controlled by conodont and fusulinid zones. Four important sea-level falls are recognized in the area, which occur respectively at the basal Sweetognathodus white! zone, lower S.aff. hanzhongensis zone, middle Jinogondolella xuanhanensis zone and the basal Clarkina y/n/zone. Among the recognized transgression events, three are regarded as the most significant. They occur respectively at the basal Neogondolella exculptus zone, basal Jinogondolella nankingensis zone and the lower Clarkina postbitteri zone, and are all accompanied by faunal turnovers. The key surfaces in sequences can be used to fine-tune the boundaries of bio-chronozones, stages and series.

  8. A note on upscaling retardation factor in hierarchical porous media with multimodal reactive mineral facies

    Soltanian, Mohamad Reza; Huang, Chaocheng; Dai, Zhenxue; Deng, Hailin


    We present a model for upscaling the time-dependent effective retardation factor in hierarchical porous media with multimodal reactive mineral facies. The model extends the approach by Deng et al. (2013) in which they expanded a Lagrangian-based stochastic theory presented by Rajaram (1997) in order to describe the scaling effect of retardation factor. They used a first-order linear approximation in deriving their model to make the derivation tractable. Importantly, the linear approximation is known to be valid only to variances of 0.2. In this article we show that the model can be derived with a higher-order approximation, which allows for representing variances from 0.2 to 1.0. We present the derivation, and use the resulting model to recalculate the time-dependent effective retardation for the scenario examined by Deng et al. (2013).

  9. Bayesian inversion of seismic attributes for geological facies using a Hidden Markov Model

    Nawaz, Muhammad Atif; Curtis, Andrew


    Markov chain Monte-Carlo (McMC) sampling generates correlated random samples such that their distribution would converge to the true distribution only as the number of samples tends to infinity. In practice, McMC is found to be slow to converge, convergence is not guaranteed to be achieved in finite time, and detection of convergence requires the use of subjective criteria. Although McMC has been used for decades as the algorithm of choice for inference in complex probability distributions, there is a need to seek alternative approaches, particularly in high dimensional problems. Walker & Curtis (2014) developed a method for Bayesian inversion of 2-D spatial data using an exact sampling alternative to McMC which always draws independent samples of the target distribution. Their method thus obviates the need for convergence and removes the concomitant bias exhibited by finite sample sets. Their algorithm is nevertheless computationally intensive and requires large memory. We propose a more efficient method for Bayesian inversion of categorical variables, such as geological facies that requires no sampling at all. The method is based on a 2-D Hidden Markov Model (2D-HMM) over a grid of cells where observations represent localized data constraining each cell. The data in our example application are seismic attributes such as P- and S-wave impedances and rock density; our categorical variables are the hidden states and represent the geological rock types in each cell-facies of distinct subsets of lithology and fluid combinations such as shale, brine-sand and gas-sand. The observations at each location are assumed to be generated from a random function of the hidden state (facies) at that location, and to be distributed according to a certain probability distribution that is independent of hidden states at other locations - an assumption referred to as `localized likelihoods'. The hidden state (facies) at a location cannot be determined solely by the observation at that

  10. Strain localization in shear zones during exhumation: a graphical approach to facies interpretation

    Cardello, Giovanni Luca; Augier, Romain; Laurent, Valentin; Roche, Vincent; Jolivet, Laurent


    Strain localization is a fundamental process determining plate tectonics. It is expressed in the ductile field by shear zones where strain concentrates. Despite their worldwide distribution in most metamorphic units, their detailed characterization and processes comprehension are far to be fully addressed. In this work, a graphic approach to tectono-metamorphic facies identification is applied to the Delfini Shear Zone in Syros (Cyclades, Greece), which is mostly characterized by metabasites displaying different degree of retrogression from fresh eclogite to prasinite. Several exhumation mechanisms brought them from the depths of the subduction zone to the surface, from syn-orogenic exhumation to post-orogenic backarc extension. Boudinage, grain-size reduction and metamorphic reactions determinate strain localization across well-deformed volumes of rocks organized in a hierarchic frame of smaller individual shear zones (10-25 meters thick). The most representative of them can be subdivided in 5 tectono-metamorphic (Tm) facies, TmA to E. TmA records HP witnesses and older folding stages preserved within large boudins as large as 1-2 m across. TmB is characterized by much smaller and progressively more asymmetric boudins and sigmoids. TmC is defined by well-transposed sub- to plane-parallel blueschist textures crossed by chlorite-shear bands bounding the newly formed boudins. When strain increases (facies TmD-E), the texture is progressively retrograded to LP-HT greenschist-facies conditions. Those observations allowed us to establish a sequence of stages of strain localization. The first stage (1) is determined by quite symmetric folding and boudinage. In a second stage (2), grain-size reduction is associated with dense shear bands formation along previously formed glaucophane and quartz-rich veins. With progressively more localized strain, mode-I veins may arrange as tension gashes that gradually evolve to blueschist shear bands. This process determinates the

  11. Facies volcánicas del depósito de avalancha de detritos del volcán Tata Sabaya, Andes Centrales Volcanic facies of the debris avalanche deposit of Tata Sabaya Volcano, Central Andes

    Benigno Godoy


    Full Text Available Las avalanchas de detritos, asociadas a colapsos parciales de edificios volcánicos, son fenómenos comunes en la evolución de un volcán. Este tipo de flujos son por inestabilidades, que pueden deberse a factores tales como la existencia de zonas afectadas por alteración hidrotermal, cambios climáticos, terremotos, intrusión de magmas en zonas superficiales (criptodomos y/o diques y/o movimiento de fallas bajo el edificio volcánico o cercanas a él. El producto final de estos flujos -denominado depósito de avalancha de detritos (DAD- presenta morfologías típicas de cerrillos y drenajes cerrados. En los Andes Centrales se han reconocido, al menos, 14 centros volcánicos con depósitos de avalancha asociados, entre los que está el volcán Tata Sabaya (Bolivia. El colapso que ha dado origen a este depósito podría haberse generado por una combinación de actividad sísmica y magmática en el volcán. El depósito asociado al colapso parcial de este volcán se distribuye sobre la parte baja del flanco sur del volcán y sobre la parte noroccidental de la cuenca del salar de Coipasa. Cubre una superficie de más de 230 km² y tiene un volumen estimado de 6±1 km³. Sobre la base de las composiciones litológicas, se ha establecido que el depósito está constituido por 6 tipos distintos de cerrillos, los cuales son: lávicos, piroclásticos, sedimentarios mixtos, brecha piroclástica y andesítico-basálticos. Considerando el tipo predominante de cerrillos y su distribución espacial dentro del depósito, se ha definido 6 facies diferentes (Facies de Bloques Toreva, Facies de Cerrillos Volcánicos, Facies Central, Facies de Cerrillos Sedimentarios, Facies Mixta y Facies de Cerrillos de Brecha Piroclástica. Tomando en cuenta la distribución espacial de estas facies, se propone la estructura del paleovolcán previa a su colapso parcial.Debris avalanches associated with partial sector collapse of volcanic edifices are common phenomena in the

  12. 3D modeling of stratigraphic units and simulation of seismic facies in the Lion gulf margin; Modelisation 3D des unites stratigraphiques et simulation des facies sismiques dans la marge du golfe du Lion

    Chihi, H.


    This work aims at providing a contribution to the studies carried out on reservoir characterization by use of seismic data. The study mainly consisted in the use of geostatistical methods in order to model the geometry of stratigraphic units of the Golfe du Lion margin and to simulate the seismic facies from high resolution seismic data. We propose, for the geometric modelling, a methodology based on the estimation of the surfaces and calculation afterwards of the thicknesses, if the modelling of the depth is possible. On the other hand the method consists in estimating the thickness variable directly and in deducing the boundary surfaces afterwards. In order to simulate the distribution of seismic facies within the units of the western domain, we used the truncated Gaussian method. The used approach gave a satisfactory results, when the seismic facies present slightly dipping reflectors with respect to the reference level. Otherwise the method reaches its limits because of the problems of definition of a reference level which allows to follow the clino-forms. In spite of these difficulties, this simulation allows us to estimate the distribution of seismic facies within the units and then to deduce their probable extension. (author) 150 refs.

  13. Beaulieu-Boycott-Innes syndrome: an intellectual disability syndrome with characteristic facies.

    Casey, Jillian; Jenkinson, Allan; Magee, Alex; Ennis, Sean; Monavari, Ahmad; Green, Andrew; Lynch, Sally A; Crushell, Ellen; Hughes, Joanne


    We report a female child from an Irish Traveller family presenting with severe intellectual disability, dysmorphic features, renal anomalies, dental caries and cyclical vomiting. Current health issues include global developmental delay, mild concentric left ventricular hypertrophy, dental malocclusion and caries and a single duplex left kidney. The proband and her mother also have multiple epiphyseal dysplasia. Whole-exome sequencing was performed to identify the underlying genetic cause. DNA from the proband was enriched with the Agilent Sure Select v5 Exon array and sequenced on an Illumina HiSeq. Rare homozygous variants were prioritized. Whole-exome sequencing identified three linked homozygous missense variants in THOC6 (c.298T>A, p.Trp100Arg; c.700G>C, p.Val234Leu; c.824G>A, p.Gly275Asp) as the likely cause of this child's intellectual disability syndrome, resulting in a molecular diagnosis of Beaulieu-Boycott-Innes syndrome (BBIS). This is the first report of BBIS in Europe. BBIS has been reported previously in two Hutterite families and one Saudi family. A review of all patients to date shows a relatively homogenous phenotype. Core clinical features include low birth weight with subsequent growth failure, short stature, intellectual disability with language delay, characteristic facies, renal anomalies and dental malocclusion with caries. Some patients also have cardiac defects. All patients show characteristic dysmorphic facial features including a tall forehead with high anterior hairline and deep-set eyes with upslanting palpebral fissures. The coexistence of intellectual disability together with these characteristic facies should provide a diagnostic clue for BBIS during patient evaluation.




    Full Text Available A combined multidisciplinary approach has been applied to calculate minimum values of the stratigraphic completeness and, secondarily, sedimentation rates in 9.2 m thick Rosso Ammonitico facies from central Apennines (Italy and 11 m thick deposits of the same facies in Southern Spain. Middle - Upper Toarcian expanded sedimentation in Valdorbia section (Umbria-Marche Apennines and extremely condensed Oxfordian-Tithonian sedimentation at Puerto Escaño section (External Subbetic have been investigated using combined taphonomic, ichnologic and sedimentologic data and analyses. At Valdorbia, infaunal tiering is largely preserved and 27 horizons of infaunal-tiering truncation and casting reveal strong erosional activity forced by tempestite/turbidite events. Therefore, microstratigraphic gaps could be evaluated without biostratigraphic control. In this expanded section, 13 horizons of firm- and hardgrounds have been recorded showing simple or gradational tiering. Conversely, in the condensed Puerto Escaño section, taphonomic analysis reveals 25 horizons of bioclasts truncation (mainly in ammonites, and 56 horizons of firm-hardgrounds intensively bioturbated. In Valdorbia rather than in Puerto Escaño section, the evaluation of flattening in burrows and spherical bioclasts reveal a measurable mechanical compaction and dissolution. In addition, Rosso Ammonitico at Valdorbia section favoured the calculation of decompaction coefficients (nd for each lithology easier than in Puerto Escaño section. In condensed and essentially hiatal Rosso Ammonitico, mottled deposits due to intense bioturbation dominate and tiering cannot be recognizable. This fact is accentuated by usual overprinting of elementary depositional events, which in turn hampered the accurate calculation of missing deposits. Therefore, in condensed Rosso Ammonitico the latter was only available in terms of minimal missing-record trough the analysis of truncated bioclasts. 

  15. Latest development in seismic texture analysis for subsurface structure, facies, and reservoir characterization: A review

    Gao, Dengliang


    In exploration geology and geophysics, seismic texture is still a developing concept that has not been sufficiently known, although quite a number of different algorithms have been published in the literature. This paper provides a review of the seismic texture concepts and methodologies, focusing on latest developments in seismic amplitude texture analysis, with particular reference to the gray level co-occurrence matrix (GLCM) and the texture model regression (TMR) methods. The GLCM method evaluates spatial arrangements of amplitude samples within an analysis window using a matrix (a two-dimensional histogram) of amplitude co-occurrence. The matrix is then transformed into a suite of texture attributes, such as homogeneity, contrast, and randomness, which provide the basis for seismic facies classification. The TMR method uses a texture model as reference to discriminate among seismic features based on a linear, least-squares regression analysis between the model and the data within an analysis window. By implementing customized texture model schemes, the TMR algorithm has the flexibility to characterize subsurface geology for different purposes. A texture model with a constant phase is effective at enhancing the visibility of seismic structural fabrics, a texture model with a variable phase is helpful for visualizing seismic facies, and a texture model with variable amplitude, frequency, and size is instrumental in calibrating seismic to reservoir properties. Preliminary test case studies in the very recent past have indicated that the latest developments in seismic texture analysis have added to the existing amplitude interpretation theories and methodologies. These and future developments in seismic texture theory and methodologies will hopefully lead to a better understanding of the geologic implications of the seismic texture concept and to an improved geologic interpretation of reflection seismic amplitude

  16. The crater-facies kimberlite system of Tokapal, Bastar District, Chhattisgarh, India

    Mainkar, Datta; Lehmann, Bernd; Haggerty, Stephen E.


    Discovery of diamondiferous kimberlites in the Mainpur Kimberlite Field, Raipur District, Chhattisgarh in central India, encouraged investigation of similar bodies in other parts of the Bastar craton. The earlier known Tokapal ultramafic intrusive body, located beyond the 19-km milestone in Tokapal village along the Jagdalpur-Geedam road, was reinterpreted as crater-facies kimberlite. Its stratigraphic position in the Meso-Neoproterozoic intracratonic sedimentary Indravati basin makes it one of the oldest preserved crater-facies kimberlite systems. Ground and limited subsurface data (dug-, tube-wells and exploratory boreholes) have outlined an extensive surface area (>550 ha) of the kimberlite. The morphological and surface color features of this body on enhanced satellite images suggest that there is a central feeder surrounded by a collar and wide pyroclastic apron. Exploration drilling indicates that the central zone probably corresponds to a vent overlain by resedimented volcaniclastic (epiclastic) rocks that are surrounded by a 2-km-wide spread of pyroclastic rocks (lapilli tuff, tuff/ash beds and volcaniclastic breccia). Drill-holes also reveal that kimberlitic lapilli tuffs and tuffs are sandwiched between the Kanger and Jagdalpur Formations and also form sills within the sedimentary sequence of the Indravati basin. The lapilli tuffs are commonly well stratified and display slumping. Base surges and lava flows occur in the southern part of the Tokapal system. The geochemistry and petrology of the rock correspond to average Group I kimberlite with a moderate degree of contamination. However, the exposed rock is intensely weathered and altered with strong leaching of mobile elements (Ba, Rb, Sr). Layers of vesicular fine-grained glassy material represent kimberlitic lava flows. Tuffs containing juvenile lapilli with pseudomorphed olivine macrocrysts are set in a talc-serpentine-carbonate matrix with locally abundant spinel and sphene. Garnet has not been

  17. Modeling 3-D permeability distribution in alluvial fans using facies architecture and geophysical acquisitions

    Zhu, Lin; Gong, Huili; Dai, Zhenxue; Guo, Gaoxuan; Teatini, Pietro


    Alluvial fans are highly heterogeneous in hydraulic properties due to complex depositional processes, which make it difficult to characterize the spatial distribution of the hydraulic conductivity (K). An original methodology is developed to identify the spatial statistical parameters (mean, variance, correlation range) of the hydraulic conductivity in a three-dimensional (3-D) setting by using geological and geophysical data. More specifically, a large number of inexpensive vertical electric soundings are integrated with a facies model developed from borehole lithologic data to simulate the log10(K) continuous distributions in multiple-zone heterogeneous alluvial megafans. The Chaobai River alluvial fan in the Beijing Plain, China, is used as an example to test the proposed approach. Due to the non-stationary property of the K distribution in the alluvial fan, a multiple-zone parameterization approach is applied to analyze the conductivity statistical properties of different hydrofacies in the various zones. The composite variance in each zone is computed to describe the evolution of the conductivity along the flow direction. Consistently with the scales of the sedimentary transport energy, the results show that conductivity variances of fine sand, medium-coarse sand, and gravel decrease from the upper (zone 1) to the lower (zone 3) portion along the flow direction. In zone 1, sediments were moved by higher-energy flooding, which induces poor sorting and larger conductivity variances. The composite variance confirms this feature with statistically different facies from zone 1 to zone 3. The results of this study provide insights to improve our understanding on conductivity heterogeneity and a method for characterizing the spatial distribution of K in alluvial fans.

  18. Experimental Investigation on Dilation Mechanisms of Land-Facies Karamay Oil Sand Reservoirs under Water Injection

    Lin, Botao; Jin, Yan; Pang, Huiwen; Cerato, Amy B.


    The success of steam-assisted gravity drainage (SAGD) is strongly dependent on the formation of a homogeneous and highly permeable zone in the land-facies Karamay oil sand reservoirs. To accomplish this, hydraulic fracturing is applied through controlled water injection to a pair of horizontal wells to create a dilation zone between the dual wells. The mechanical response of the reservoirs during this injection process, however, has remained unclear for the land-facies oil sand that has a loosely packed structure. This research conducted triaxial, permeability and scanning electron microscopy (SEM) tests on the field-collected oil sand samples. The tests evaluated the influences of the field temperature, confining stress and injection pressure on the dilation mechanisms as shear dilation and tensile parting during injection. To account for petrophysical heterogeneity, five reservoir rocks including regular oil sand, mud-rich oil sand, bitumen-rich oil sand, mudstone and sandstone were investigated. It was found that the permeability evolution in the oil sand samples subjected to shear dilation closely followed the porosity and microcrack evolutions in the shear bands. In contrast, the mudstone and sandstone samples developed distinct shear planes, which formed preferred permeation paths. Tensile parting expanded the pore space and increased the permeability of all the samples in various degrees. Based on this analysis, it is concluded that the range of injection propagation in the pay zone determines the overall quality of hydraulic fracturing, while the injection pressure must be carefully controlled. A region in a reservoir has little dilation upon injection if it remains unsaturated. Moreover, a cooling of the injected water can strengthen the dilation potential of a reservoir. Finally, it is suggested that the numerical modeling of water injection in the Karamay oil sand reservoirs must take into account the volumetric plastic strain in hydrostatic loading.

  19. Three-dimensional facies architecture of the Salem Limestone (middle Mississippian), Eastern Margin of Illinois basin

    Nadeem, A.; Keith, B.D.; Thompson, T.A. [Indiana Univ., Bloomington, IN (United States)


    Mapping of sedimentary surfaces in the Middle Mississippian Salem Limestone exposed on sawed quarry walls in south-central Indiana has revealed a hierarchy of depositional units representative of the extremely dynamic hydrographic regime of the upper shoreface zone. The depositional units on the scale of microform and mesoform are represented by the microfacies and the facies respectively. Based on their hierarchy, genetically related depositional units and associated bounding surfaces were grouped together to construct four architectural packages (APs) of the scale of mesoforms. AP-I is dominantly an echinoderm- and bryozoan-rich grainstone and consists of bedforms ranging from small ripples bounded by first-order surfaces to two- and three- dimensional megaripples bounded by the second-order surfaces. It formed as part of a giant ramp (asymmetric wavefield) within the intrashoal channel setting. AP-II, also a skeletal grainstone, is a complex of giant sandwaves that moved into the area under the infulence of a storm and partly filled the basal channel form of AP-I. Large avalanche foresets with tangential toesets prevail. AP-III is a dark-gray spatially discontinuous skeletal grainstone to packstone that laterally grades into a skeletal packstone to wackestone. It locally developed overhangs, rips-ups, and hardground on its upper surface. AP-IV is a skeletal and oolitic grainstone formed of tabular two-dimensional megaripples (planar cross-beds) and three-dimensional oscillatory megaripples (trough cross-beds). These architectural packages based on the bedform architecture and micro-and mesoscale compositional changes can be used to characterize micro-, meso, and macroscale heterogeneities. Models of facies architecture from this and similar outcrop studies can be applied to the subsurface Salem reservoirs in the Illinois Basin using cores.

  20. Radar backscattering from snow facies of the Greenland ice sheet: Results from the AIRSAR 1991 campaign

    Rignot, Eric; Jezek, K.; Vanzyl, J. J.; Drinkwater, Mark R.; Lou, Y. L.


    In June 1991, the NASA/JPL airborne SAR (AIRSAR) acquired C- (lambda = 5.6cm), L- (lambda = 24cm), and P- (lambda = 68m) band polarimetric SAR data over the Greenland ice sheet. These data are processed using version 3.55 of the AIRSAR processor which provides radiometrically and polarimetrically calibrated images. The internal calibration of the AIRSAR data is cross-checked using the radar response from corner reflectors deployed prior to flight in one of the scenes. In addition, a quantitative assessment of the noise power level at various frequencies and polarizations is made in all the scenes. Synoptic SAR data corresponding to a swath width of about 12 by 50 km in length (compared to the standard 12 x 12 km size of high-resolution scenes) are also processed and calibrated to study transitions in radar backscatter as a function of snow facies at selected frequencies and polarizations. The snow facies on the Greenland ice sheet are traditionally categorized based on differences in melting regime during the summer months. The interior of Greenland corresponds to the dry snow zone where terrain elevation is the highest and no snow melt occurs. The lowest elevation boundary of the dry snow zone is known traditionally as the dry snow line. Beneath it is the percolation zone where melting occurs in the summer and water percolates through the snow freezing at depth to form massive ice lenses and ice pipes. At the downslope margin of this zone is the wet snow line. Below it, the wet snow zone corresponds to the lowest elevations where snow remains at the end of the summer. Ablation produces enough meltwater to create areas of snow saturated with water, together with ponds and lakes. The lowest altitude zone of ablation sees enough summer melt to remove all traces of seasonal snow accumulation, such that the surface comprises bare glacier ice.

  1. The undefended accused in a minefield

    in nature.2 According to Steytler3 the key element of an adversarial trial is ... accused may elect to close his case without leading any evidence and face the risk of a conviction, due to the fact that there was a prima facie case ... The concept of ..... This section was introduced into the criminal trial process following upon.

  2. 8 CFR 1245.3 - Adjustment of status under section 13 of the Act of September 11, 1957, as amended.


    ... whose status may be adjusted under section 13, any alien who is prima facie eligible for adjustment of...)(15)(G)(ii) of the Immigration and Nationality Act who performed diplomatic or semi-diplomatic duties... duties were of a custodial, clerical, or menial nature, and members of their immediate families, are...

  3. Cl-rich minerals in Archean granulite facies ironstones from the Beartooth Mountains, Montana, USA: Implications for fluids involved in granulite metamorphism

    Henry, D. J.


    The implications of Cl-rich minerals in granulite facies rocks are discussed. Results from ironstones of the Beartooth Mountains, Montana are discussed. It is suggested that CO2-brine immiscibility might be applicable to granulite facies conditions, and if so, then aqueous brines might be preferentially adsorbed onto mineral surfaces relative to CO2.

  4. Sedimentary Micro-facies and Macro Heterogeneity of Reservoir Beds in the Third Member of the Qingshankou Formation, Qian'an Area,Songliao Basin


    An analysis of drill cores and well logs shows that the main micro-facies of the third member sand bodies of the Qingshankou Formation in Qian'an are subaqueous distributary channel facies,sheet sand facies and subaqueous fan facies (olistostrome). Maps showing the distribution of these micro-facies together with inter-channel bay and prodelta mocro-facies are presented for different time-slices (lower, middle and upper parts of the Qingshankou Formation). These maps reveal the instability and change of sediment transport in the Baokang sedimentary system during the depositional period. Sediment transport was from the west in the early stage, from the south in the middle stage and from the northwest in the late stage. Values of thickness, porosity and permeability of the sand bodies in the third member of the Qingshankou Formation show that they have low to medium porosity and low permeability, and are characterized by serious reservoir heterogeneity. The joints between micro-facies and subaqueous fan micro-facies are characterized by the highest heterogeneity,the sheet sand and distal sand bar subfacies come next, and the heterogeneity of the subaqueous distributary channel sand bodies is relatively weak.

  5. Facies analysis and paleoenvironmental interpretation of Piacenzian carbonate deposits from the Guitar Formation of Car Nicobar Island, India

    Amit K. Ghosh


    Full Text Available Facies characterization of Piacenzian (late Pliocene carbonate sediments of the Guitar Formation in Car Nicobar Island, India and the subsequent integration of paleoecological data have been applied to interpret the paleoenvironment of the coralline algal-reef deposits. Thin-section analysis reveals that Amphiroa, Corallina and Jania are the dominant geniculate corallines, while Lithothamnion, Mesophyllum, Phymatolithon, Lithophyllum, Spongites and Lithoporella are the major non-geniculate corallines contributing to the sedimentary facies. Numerous small and larger benthic foraminifera also dominate the biogenic assemblages. Corals, barnacle shells, echinoid spines, fragments of bryozoans, mollusks and ostracodes are the subordinate constituents. Grainstones dominate the studied facies while packstones and boundstones (with wackestone elements are the sub-lithofacies showing a fair representation. Six carbonate facies presenting a complete reef complex have been distinguished that were deposited in shallow intertidal, back-reef shelf/lagoon, reef and deeper fore-reef shelf settings. Evidences of coralline algal and benthic foraminiferal assemblages, taphonomic signatures of abrasion and fragmentation, grain size, angularity and encrustation indicate a shallow to relatively deeper bathymetric horizon of approximately 10–60 m that corresponds to a regime of high to moderate hydrodynamic conditions.

  6. Facies analysis of the Late Cretaceous deposits from Corni Quarry (north-eastern border of Gilău Mountains

    Emanoil Săsăran


    Full Text Available The Late Cretaceous deposits outcropping along the northeastern border of Gilău Mountains form a NW-SE-oriented crest. The crest is delimited westwards by the crystalline formations of Baia de Arieş Nappe. Within these deposits, two distinctive sedimentary complexes could be separated: a The Gosau-type facies formation, that can be correlated to the “Lower Gosau Subgroup” (Wagreich & Faupl, 1994, represented by alluvial/fluvial fans and shallow marine deposits; b The flysch-type formation, that is similar with the “Upper Gosau Subgroup” (Wagreich & Faupl, 1994 and includes deep sea deposits (hemipelagites/turbidites.The syndepositional and postdepositional tectonics controlled the sedimentation and facies distribution; the shallow carbonate deposits are embedded in distal shelf marine ones. Isolated blocks of various sizes represent the rudist-bearing limestones (from m2 up to hundreds of m2. The present study focuses on the identification of facies and depositional environments of the limestones outcropping along Pleşcuţa valley, in Corni Quarry (SW from Finişel village. Based on sedimentological features and faunal associations, the following facies associations have been identified: 1 Marls and limestone with terrigenous clasts; 2 Build-ups with tubular/massive corals and rudists; 3 pillarstone-type bioaccumulations with branching/platy corals; 4 bioclastic rudstone/grainstone; 5 bioclastic floatstone/ packstone. All these facies associations indicate a coastal environment developed along a shelf margin influenced by both the terrigenous supply, and the relative sea level variations.

  7. Preservation of Blueschist Facies Minerals Along a Shear Zone By Fast Flowing CO2-Bearing Fluids - a Field Study from the Cycladic Blueschist Unit on Syros, Greece

    Kleine, B. I.; Skelton, A.; Huet, B.; Pitcairn, I.


    Our study was undertaken at Fabrika Beach on the southeastern shore of Syros which belongs to the Greek Cycladic archipelago in the Aegean Sea. The island is situated within the Attic-Cycladic metamorphic core complex belt and is now located in the back-arc of the active Hellenic subduction zone. At Fabrika Beach, blueschist facies minerals are observed in haloes fringing a shear zone within greenschist facies rocks. The approximately vertical shear zone cuts a near horizontal layer of greenschist facies rocks. The blue haloes are ca. 1 m wide, and are seen on both sides of the shear zone. The haloes consist of a carbonated blueschist facies mineral assemblage. Based on petrological, geochemical and thermodynamic evidence we show that these haloes were preserved at greenschist facies conditions in response to fast flowing CO2-bearing fluid. Furthermore, we use a simple mass balance to calculate the fluid flux within the shear zone which would be required to cause the observed preservation of blueschist facies minerals. We constructed a simplified P-T vs. XCO2 pseudosection using PerPlex 6.6.6 to confirm that preservation of carbonated blueschist can occur at greenschist facies conditions in the presence of CO2-bearing fluid. The flux of CO2-bearing fluid along the shear zone was rapid with respect to the fluid flux in the surrounding rocks. Mass balance calculations reveal that the fluid flux within the shear zone was at least 100 - 2000 times larger than the fluid flux within the surrounding rocks. Mineral textures show greenschist facies minerals partially replacing blueschist minerals in the haloes supporting our interpretation that blueschist facies minerals were preserved during greenschist facies retrogression.

  8. Facies y ambientes del grupo Salta (cretácico-paleógeno en Tumbaya, Quebrada de Humahuaca, provincia de Jujuy Facies and environments of the Salta Group (Cretaceous-Paleogene in Tumbaya, Quebrada de Humahuaca, JujuyProvince

    María Cristina Sánchez


    Full Text Available Los depósitos rojos del Grupo Salta (Cretácico-Paleógeno que afloran en la quebrada de Tumbaya, margen derecha de la quebrada de Humahuaca (provincia de Jujuy, se caracterizan por presentar facies distintas a las típicas de otros lugares de la cuenca. Son facies proximales de ambiente general árido a semiárido cuya acumulación avanzó sobre el extremo N-NO del alto constituido por la dorsal Salto-Jujeña. La relación de base y de techo del depósito es de discordancia erosiva con el Grupo Mesón (Cámbrico y angular con acumulaciones cuaternarias de bajada respectivamente. En el afloramiento están representadas las principales unidades del Grupo Salta tanto del synrift como del postrift. El reconocimiento y estudio de las facies permitió identificar y caracterizar de base a techo los Subgrupos Pirgua, Balbuena y Santa Bárbara, y las distintas formaciones de cada subgrupo. En el Subgrupo Pirgua (arenas eólicas no es posible diferenciar sus tres unidades formacionales, por lo tanto se lo menciona como Formación Pirgua. En el Subgrupo Balbuena se reconocen las Formaciones Lecho, que consta de facies fluviales de tipo mantos de crecida, y Yacoraite que muestra condiciones ambientales transicionales, continentales y marino litoral-sublitoral carbonático influenciado por mareas y tormentas. El Subgrupo Santa Bárbara está presente con sus Formaciones Mealla, Maíz Gordo y Lumbrera que representan una sucesión fluvial granodecreciente con desarrollo de paleosuelos múltiples; se reconocen mantos de crecida asociadas a planicies fangosas.The red deposits of Salta Group (Cretaceous-Paleogene which outcrops in the quebrada de Tumbaya, right margin of Quebrada de Humahuaca (province of Jujuy, they are characterized by facies that differs from the typical ones in their places of the Salta Group basin. They are proximal facies, characterized by arid and semi-arid conditions whose accumulation advanced on the N-NW side of the Salto-Jujuy high

  9. Propriedades micromeríticas e análise físico-química de matérias-primas de alopurinol

    Vanessa Vidaletti Lago


    Full Text Available O controle de qualidade de matérias-primas é imprescindível, pois visa assegurar a qualidade do produto acabado. O objetivo do trabalho foi avaliar a qualidade físico-química e farmacotécnica de matérias-primas de alopurinol, fármaco utilizado para a prevenção e o tratamento de crises de gota, amplamente prescrito e produzido por indústrias e farmácias magistrais. As amostras (A, B, C e D de alopurinol oriundas de diferentes fornecedores foram submetidas a ensaios farmacopeicos (características organolépticas; solubilidade; ensaios de identificação: teste de precipitação e varredura no UV; ensaios de pureza: limpidez de solução, perda por dessecação, cinzas sulfatadas; doseamento, análise térmica (DSC, TG, análise granulométrica e determinação das propriedades de fluxo (ângulo de repouso, densidade bruta e de compactação, fator de Hausner, índice de compressibilidade e compactabilidade. As amostras foram aprovadas em todos os ensaios farmacopeicos. Nas curvas de DSC, o ponto de fusão foi de cerca de 380 °C para todas as amostras e, após a fusão houve a degradação, confirmada pelas curvas TG, com uma perda de massa de aproximadamente 100 %. A partir da distribuição granulométrica as amostras A e B foram classificadas como pós finos e as C e D como finíssimos. Os valores de ângulo de repouso caracterizaram as amostras A, B, C e D como de fluxo fraco e, o fator de Hausner e índice de compressibilidade caracterizaram as amostras como amostras de fluxo bastante deficiente. Os ensaios demonstraram-se úteis para avaliar a qualidade das amostras. A adição de adjuvantes apropriados durante o preparo das formulações de alopurinol é essencial para melhoramento do fluxo.

  10. Wagnerite-MA5BC From Granulite-Facies Paragneiss, Larsemann Hills, Prydz Bay, East Antarctica

    Ren, L.; Grew, E. S.; Xiong, M.; Ma, Z.


    Wagnerite-Ma5bc, which is one of three new polytypes of (Mg,Fe)_2(PO_4)(F,OH) (Chopin, Armbruster &Leyx, this conference), occurs in paragneiss associated with banded cordierite-prismatine gneiss. It forms anhedral to euhedral grains mostly 0.5-2 mm across, some with a tabular habit. Textures are consistent with a primary assemblage wagnerite-Ma5bc + plagioclase + apatite + magnetite + ilmenite-hematite that crystallized under granulite-facies conditions (750 - ˜860^oC, 6-7 kbar). Also present are biotite, quartz, K-feldspar, monazite, xenotime, corundum, hercynite, sulfide. Electron microprobe analyses give P_2O_5 41.39, SiO_2 0.06, TiO_2 0.88, FeO 4.16, MnO 0.09, MgO 44.54, CaO 0.09, F 6.87, H_2O (calculated for OH + F = 1) 2.04, O=F -2.89, total 97.22 wt%, corresponding to (Mg1.88Fe0.10Ti0.02)(P0.99O_4)(F0.61OH0.39). Space group is Ia. Lattice parameters a = 9.645(2)Å, b = 31.659(6) Å , c = 11.914(2) Å, â=108.26 (3)^o, V= 3455(1) Å^3 for Z=40, Dcalc = 3.18(1) g/cm^3. The crystal structure has been solved by direct methods and refined to R_1=0.0413 for the independent 4521 reflections [I>2σ(I)] using MoKα radiation. The primary difference among the wagnerite polytypes is ordering of the (F,OH) positions. F can occupy one of two positions resulting in two distinct configurations along the a direction. In magniotriplite the sequence of configurations in the b direction is disordered, whereas in wagnerite-Ma2bc the sequence is ordered 121212... and in wagnerite-Ma5bc, 12112... Magniotriplite and the wagnerite polytypes do not overlap in composition: minerals richer in Fe and Mn (average ionic radius >= 0.76 Å) crystallize as the disordered minerals in the triplite group, whereas highly magnesian minerals (average ionic radius = 86% of the Mg end member) crystallize as the ordered wagnerite polytypes. Magniotriplite formed at moderate temperatures (e.g., amphibolite-facies), whereas wagnerite-Ma2bc is found in rocks formed under a wide range of P

  11. Facies, Stratigraphic and Depositional Model of the Sediments in the Abrolhos Archipelago (Bahia, BRAZIL)

    Matte, R. R.; Zambonato, E. E.


    Located in the Mucuri Basin on the continental shelf of southern Bahia state, northeast Brazil, about 70 km from the city of Caravelas,the Abrolhos archipelago is made up of five islands; Santa Barbara, Redonda, Siriba, Guarita and Sueste. The exhumed sediments in the Abrolhos archipelago are a rare record of the turbidite systems which fill the Brazilian Atlantic Basin, and are probably an unprecedented example of a plataform turbidite system (Dr. Mutti, personal communication). Despite the limited area, the outcrops display a wide facies variation produced by different depositional processes, and also allow for the observation of the layer geometries. Associated with such sedimentary rocks, the Abrolhos Volcanic Complex belongs stratigraphically to the Abrolhos Formation. These igneous rocks were dated by the Ar / Ar method, with ages ranging from 60 to 40 My, placing such Volcanic Complex between the Paleocene and Eocene. The sedimentary section is best exposed in the Santa Barbara and Redonda islands and altogether it is 70 m thick. The measured vertical sections show a good stratigraphic correlation between the rocks of the western portion of the first island and those of Redonda Island. However, there is no correlation between the eastern and western portions of Santa Barbara Island, since they are very likely interrupted by the igneous intrusion and possibly by faulting. The sedimentary stack consists of deposits with alternated regressive and transgressive episodes interpreted as high frequency sequences. The coarse facies, sandstones and conglomerates, with abrupt or erosive bases record regressive phases. On the other hand, finer sandstones and siltstones facies, which are partly bioturbated, correspond to phases of a little sediment supply. In the central and eastern portions of Santa Barbara Island, there is a trend of progradational stacking, while both in the western portion of Santa Barbara and in Redonda islands an agradational trend is observed

  12. Understanding chemical and facies variability in the Murray Formation, Gale crater, from ChemCam data

    Rivera-Hernandez, Frances; Mangold, Nicolas; Sumner, Dawn Y.; Nachon, Marion; Wiens, Roger C.; Maurice, Sylvestre; Forni, Olivier; Frydenvang, Jens; Newsom, Horton; Dehouck, Erwin; Payre, Valerie


    The primary goal of the Mars Science Laboratory (MSL) mission is to determine if habitable environments existed on Mars [1]. To evaluate the potential for habitability, reconstructing the transport and depositional history of the sedimentary rocks at Gale Crater relies on the accurate interpretation of changes in depositional facies. This study uses ChemCam data to identify and characterize chemical variations that may be due to grain size and possibly facies changes within the Murray formation, a fluvio-lacustrine unit in Gale Crater dominated by interbedded mudstones and fine-grained sandstones [1]. These analyses compliment current efforts by APXS and ChemCam in reconstructing a chemostratigraphic record for the Curiosity rover traverse [e.g.,2,3]. Textural analyses from images taken by the Mars Hand Lens Imager (MAHLI), and the ChemCam Remote Micro Imager (RMI), and ChemCam chemical data were used to exclude targets with resolvable diagenetic features. Remaining targets were analyzed for chemical heterogeneity using the Gini Index (G), where G=0 indicates no point-to-point chemical variation and G=1 for a completely heterogeneous target [4]. Sandstones with grains larger than the laser beam diameter ( 0.3-0.5 mm; medium sand) typically have G>0.25 [4]. Hence, heterogeneity in composition among closely spaced points on a single target may reflect variations in mineralogy among individual sand grains or concentrations of grains. In contrast, homogeneous rocks may have homogeneous grain compositions or only contain grains smaller than sand. Thus, even when the presence of sand grains cannot be demonstrated from images, their presence can be inferred using the Gini Index. Preliminary analyses from sols 1400-1500 suggest that the abundances of FeOT, SiO2, Al2O3, and TiO2 do not vary significantly in individual rock targets (G0.1). Most variations between targets are likely associated with resolvable diagenetic features [e.g.,5,6]. However, Murray bedrock targets

  13. Toward a Facies Model for AMS Fabrics in Deposits from Pyroclastic Currents

    Ort, M. H.; Newkirk, T.; Vilas, J. F.; Vazquez, J. A.


    Studies of the anisotropy of magnetic susceptibility (AMS) in deposits from pyroclastic density currents have been made for 30 years. Early studies sought to find vent locations, but later studies have also used AMS to interpret flow and depositional processes. These studies show that AMS fabrics reflect shear directions at the base of the depositional regime and thoughtful interpretations of the directions, coupled with good observations of the deposits, can lead to a better understanding of depositional and flow processes in the currents. Here, we compare the AMS fabrics and deposit characteristics of deposits of dense and dilute pyroclastic density currents in order to develop an AMS facies model for such deposits. Deposits from individual phreatomagmatic density currents produced in the NE Hopi Buttes volcanic field, NE Arizona, can be traced from the maar edge laterally for 1.5 km or more. This allows the depositional facies to be described and sampled for AMS. The most proximal facies, consisting of tuff breccias, is characterized by a disorganized AMS fabric, marked by some grouping of the AMS axes but a very weak foliation. By about 350 m from the maar rim and extending out over a kilometer, a well lineated and foliated fabric develops in the stratified to sand-wave-bearing lapilli-tuffs, reflecting the shear within the well-developed current. At distances over a km from the vent, where the deposits are plane-parallel tuffs, a girdled fabric develops, with overlapping K1 and K2 axes. This likely reflects weak shearing within the slowing flow. At Caviahue caldera, Neuquen, Argentina, lateral sampling of ignimbrites from within the caldera and on a SE transect to ~25 km from the caldera rim, reveals systematic changes in the AMS fabric, with less obvious changes in the sedimentary characteristics. Intracaldera ignimbrites are rheomorphic and very densely welded, and their AMS fabrics are very strongly foliated but with a weak lineation. Moving out from the

  14. Structural and alteration controls on gold mineralization the of the amphibolite facies Detour Lake Deposit, Canada

    Dubosq, Renelle; Schneider, David


    The 15M oz Detour Lake deposit is a Neoarchean orogenic gold ore body located in the northern most region of the Abitibi district within the Superior Province. The mine is an open pit design in the high strain zone of the Sunday Lake Deformation Zone (SLDZ). The ductile-brittle SLDZ parallels the broadly E-W Abitibi greenstone belt and the deposit is situated in a dilation zone between volcanoclastic rocks of the Caopatina Assemblage and Lower Detour Lake Formation, consisting of ultramafic talc-chlorite-sericite schist. The Upper Detour Lake Formation consists of pillowed and massive flows and hyloclastic units crosscut by minor felsic to intermediate dykes. All of the formations are sub-vertical, north-dipping units with stretching lineations indicating dip-slip motion. The Detour deposit differs from other classic ore deposits in the dominantly greenschist facies Abitibi Subprovince by possessing an amphibolite facies metamorphic assemblage of actinolite-biotite-plagioclase-almandine. Consequently, the typical indicator minerals used to identify alteration and mineralization, such as secondary biotite, may not be useful. Petrological and geochemical analyses have revealed at least four populations of biotite: 1) large euhedral crystals located within quartz-carbonate veins, 2) small, euhedral zoned crystals present as alteration haloes, 3) very small, anhedral to subhedral indistinct crystal present in mafic volcanic host rock, and 4) large euhedral crystals defining the main metamorphic foliation in the metasediments. Extensive examination of mineral assemblages, alteration products, and vein structure in rock core across barren and mineralized zones has documented over a dozen vein types which can be grouped into two main categories: 1) sulfidized quartz-carbonate veins associated with biotite alteration and 2) late carbonate veins. Gold grades do not prove to be dependent on vein type but rather on the host rock composition: the highest ore grades are present

  15. The Randeck Maar: Facies development and habitat differentiation of a Miocene lacustrine system

    Rasser, Michael W.; Kern, Andrea K.


    The Randeck Maar in S Germany is a well-known fossil lagerstätte (Early/Middle Miocene, MN5) with exceptionally preserved fossils. Although it is a locally restricted succession of lake sediments with a diameter of only 1200 m and less than 60 m of preserved sediments, it appears to comprise a complex structure with a high scientific potential on a global scale, because the lake sediments and their fossils can provide evidence for the impact of the Mid-Miocene Climatic Optimum (MMCO) on the environment and its organisms as well as the ecological interactions between animals and/or plants during that interval. No other European locality provides such a rich insight into an ecosystem that existed during the MMCO. Excavations of Staatliches Museum für Naturkunde Stuttgart provided new insights into the facies types of this maar lake. They showed that a high variety of facies types existed beside the traditional separation into a basal tuffitic development, followed by calcareous and bituminous ('dysodil') laminates, and terminal massive freshwater limestones. Palaeoenvironmental reconstructions are based on the mentioned excavations and re-evaluations of collection material. They show that the Randeck Maar was a typical maar lake with a rich flora and fauna. Based on all plant remains, the IPR vegetational analysis points towards subhumid sclerophyllous forests, suggesting seasonal drought. 380 taxa in all are known thus far, which are dominated by plants (168) and insects (79). The taxonomic re-evaluation combined with palaeoecological considerations allows for the reconstruction of a palaeoenvironmental model. In brief, three main sections can be differentiated for the habitats of the Randeck Maar lake system: (1) Deep- and open-water lake habitats with local and short-termed mass occurrences of insect larvae, amphibians, and/or gastropods, while fish are particularly scarce. The interpretation of the water chemistry is problematic because palaeoenvironmental

  16. Cenomanian-Turonian facies succession in the Guerrero-Morelos Basin, Southern Mexico

    Aguilera-Franco, Noemí; Hernández Romano, Ulises


    The Cenomanian-Turonian succession of southern Mexico is characterized by an abrupt change from shallow marine to pelagic facies. The drowning of the platform coincides with the widely documented Cenomanian-Turonian Oceanic Anoxic Event (CTOAE). A proper understanding of the drowning event and the effects of the OAE requires, as an essential first step, the construction of a detailed stratigraphic framework. This has been achieved and utilizes sedimentological data as well as a combination of benthic and planktonic biostratigraphic schemes. Deposition of the Cenomanian-Turonian sedimentary rocks of the Guerrero-Morelos basin was controlled by tectonic and oceanographic factors resulting in depositional environments ranging from a semi-restricted shelf, ramp, pelagic and prodelta deposits. Facies analysis indicates that shallow marine limestones of the Morelos Formation (lower-upper Cenomanian) were deposited in intertidal-shallow supratidal and subtidal environments in a semi-restricted shelf. Peloidal-bioclastic packstone-wackestones with minor grainstones are the predominant texture of these rocks. Abundant large benthic foraminifers, calcareous algae (dasycladacean) and mollusks (gastropods and rudists) characterize the fossil assemblage. The Cuautla Formation (uppermost Cenomanian-Turonian) represents sedimentation on a low-energy, wave-dominated, carbonate ramp. The inner ramp accumulated bioclastic banks and shoals composed of peloidal-benthic foraminifer-grainstone, calcareous red and green algae, rudists and minor solitary corals. The middle ramp is represented by nodular packstones with a diverse assemblage of echinoderms, green and red algae, bryozoan, rudists, solitary corals, roveacrinids, calcisphaerulids, and non-keeled planktonic foraminifers. The outer ramp is dominated by argillaceous wackestone-packstone characterized by calcisphaerulids, roveacrinids, and non-keeled planktonic foraminifers. An increase in terrigenous-clastic material towards the

  17. Timing of the granulite facies metamorphism in the Sanggan area, North China craton: zircon U-Pb geochronology

    GUO; Jinghui


    Serre, southern Calabria (Italy), Contrib. Mineral. Petrol., 1980, 73: 23-38.[28]Kroner, A., Stern, R. J., Dawoud, A. S. et al., The Pan-African continental margin in northeastern Africa: evidence from a geochronological study of granulites at Saboloka, Sudan, Earth Planet Sci. Lett., 1987, 85:91-104.[29]Mezger, K., Geochronology in granulites, in Granulites and Crustal Evolution (eds. D. Vielzeuf, Ph. Vidal), Dordrecht: Kluwer Academic Publishers 1990, 451-470.[30]Kroner, A., Jaeckel, P., Williams, I. S., Pb-loss patterns in zircons from a high-grade metamorphic terrain as revealed by different dating methods: U-Pb and Pb-Pb ages for igneous and metamorphic zircons from northern Sri Lanka, Precambrian Research, 1994, 66: 151-181.[31]Pupin, J. P., Zircon and granite petrology, Contrib. Mineral. Petrol., 1980, 73: 207-220.[32]Vavra, G., On the kinematics of zircon growth and its petrogenetic significance: a cathodoluminescence study, Contrib. Mineral. Petrol., 1990, 106: 90-99.[33]Ganguly, J., Tirone, M., Hervig, R. L., Diffusion kinetics of Samarium and Neodymium in garnet, and a method for determining cooling rates of rocks, Science, 1998, 281: 805-807.[34]Hensen, B. J., Zhou, B., Retention of isotopic memory in garnets partially broken down during an overprinting granulite-facies metamorphism: implications for the Sm-Nd closure temperature, Geology, 1995, 23(3): 225-228.[35]Guo, J. H., Wang, S. S., Sang, H. Q. et al., 40Ar39Ar age spectra of garnet porphyroblast: Implications for metamorphic age of high-pressure granulite in the North China craton, Acta Petrologia Sinica (in Chinese with English abstract), 2001,17(3): 436-442.[36]Whitehouse, M. J., Granulite facies Nd-isotopic homogenization of the Lewisian complex of northwest Scotland, Nature,1988, 331: 705-707.[37]Wang, S. S., Hu, S. L., Zhai, M. G. et al., An application of the 40Ar-39Ar dating technique to the formation time of Qingyuan granite-greenstone terrain in NE

  18. Determinación espectrofotométrica de un producto activo zeolítico en materia prima y tabletas vaginales

    Mercedes Machuá Veitía


    Full Text Available El empleo de productos activos zeolíticos como fármacos de acción específica requiere el desarrollo de técnicas analíticas para el control de la calidad de las formas terminadas. Se desarrolló y validó un método espectrofotométrico de análisis para una zeolita activada con cinc (PAZ-ZZ a partir de la reacción con zincón. Se evaluó la linealidad, precisión, exactitud y especificidad del método propuesto. La técnica se aplicó posteriormente al análisis de materia prima PAZ-ZZ y tabletas vaginales que contienen este principio activo; los resultados se compararon con los obtenidos para espectroscopia de absorción atómica.The use of active zeolitic products as drugs of specific action requires the development of analytical techniques to control the quality of the finished product. A spectrophotometric method of analysis was validated for a zinc?activated zeolite (PAZ-ZZ, starting from the reaction with zincum. The lineality, precision, exactitude and specificity of the proposed method were evaluated. This technique was later applied to the analysis of PAZ-ZZ raw material and vaginal tablets containing this active principle. The results were compared with those obtained for atomic absortion spectroscopy.

  19. Formas de abastecimiento de materias primas en el sistema textil artesanal y estrategias de reproducción social entre artesanas de la estepa patagónica

    María Roberta Capretti


    Full Text Available Con foco en la producción textil artesanal en Patagonia, y desde una descripción etnográfica, se abordarán las vías de aprovisionamiento de materias primas (vellones de lana para el hilado manual de la fibra, desde un grupo de artesanas, asociadas al Mercado de la Estepa, en la zona rural de la Provincia de Río Negro, Argentina. Pese a que el territorio patagónico se caracteriza por contar con una gran cantidad de ovinos, y ser Argentina una de las principales regiones laneras del mundo, la orientación del mercado de fibras hacia la exportación limita el acceso a insumos en la producción textil artesanal. En este contexto, quienes se dedican a esta tarea, como complemento de sus ingresos familiares, deben implementar diversas estrategias de reproducción, individuales y colectivas, mediadas y tensionadas por diversas reciprocidades, con el objeto de asegurarse el acceso a ciertos recursos. Específicamente, se analizarán las limitaciones alrededor de la conservación de ovinos criollos y del acceso a su fibra, tomando el caso de la oveja localmente denominada Linca.

  20. Composición quimicomineralógica de las materias primas y ahorro de energía en la industria del cemento

    Soria Santamaría, Francisco


    Full Text Available In the field of energy saving, mainly thermic, in the cement industry, not only should we consider the possibilities in the technological process or the finished product, but also the influence of the chemical-mineral composition of the raw materials. The distinct parameters which fall into the reactivity of the crudes are analyzed, such as the size of the grain (fineness, chemical and mineral composition of the principal components. There follows an exposition of the importance of the minority components as smelting and mineralizers, finally emphasizing the interest and practical behaviour of some of them.

    En el campo del ahorro de energía, principalmente térmica, en la industria cementera, no sólo deben contemplarse las posibilidades en cuanto al proceso tecnológico o el producto acabado, sino también la influencia de la composición quimicomineralógica de las materias primas. Se analizan los distintos parámetros que inciden en la reactividad de los crudos, tales como tamaño de grano (finura, composición química y mineralogía de los componentes principales. A continuación se hace una exposición de la importancia de los componentes minoritarios como fundentes y mineralizadores, destacando finalmente el interés y comportamiento práctico de alguno de ellos.

  1. Comparison of drier- to wetter-interval estuarine roof facies in the Eastern and Western Interior coal basins, USA

    Archer, A.W.; Feldman, H.R.; Kvale, E.P.; Lanier, Wendy E.


    Many of the Carboniferous coals in the eastern interior of the US are associated with siliciclastic roof facies that were deposited within a fluvio-estuarine transition. These facies include a variety of rhythmites, some of which exhibit tidal cycles. Drier-interval coals (Westphalian B-C, Stephanian) tend to be more laterally restricted and more commonly are associated with paleovalleys. Conversely, wetter-interval coals (Westphalian D) are very widespread and are not restricted to paleovalleys. Throughout the Lake Carboniferous, wet paleoclimates associated with these coals lead to valley incision during sea-level lowstand when large tropical rivers downcut older sediments deposited during previous sea-level highstands. During subsequent rise of sea level, these fluvial valleys were flooded and converted to estuaries where tidal ranges and sedimentation rates were significantly amplified. Based on modern analogs and interpretation of many examples of Carboniferous tidal rhythmites, the localized depositional rates in these settings are exceptionally high. The estuaries became sediment sinks, trapping sediment that is pumped in from both fluvial and marine sources. As a result, sedimentation readily keeps pace with rising baselevel. Extensive intertidal flats and shallow subtidal flats are created and prograde over the valley-confined mires. Thick tidal cycles and upright trees (some with attached foliage) record rapid burial of mires. This model is supported with examples of roof facies from the Westphalian B-C of the Eastern Interior Basin, and the Stephanian of the Western Interior Basin. In these areas facies within each cycle range from well-developed, extensive paleosols and coals, to widespread marine shales or limestones. Variations in both sea level and climate resulted in a complex history of valley fill during which coals could be developed at any time (except during widespread flooding). Minable, low-sulfur and low-ash coals occur, but the coals are

  2. Facies control on seismites in an alluvial-aeolian system: The Pliocene dunefield of the Teruel half-graben basin (eastern Spain)

    Liesa, Carlos L.; Rodríguez-López, Juan Pedro; Ezquerro, Lope; Alfaro, Pedro; Rodríguez-Pascua, Miguel Ángel; Lafuente, Paloma; Arlegui, Luis; Simón, José L.


    The recognition of seismically induced soft-sediment deformation structures (SSDS) in sedimentary successions characterized by different facies, and hence by different rheology, is challenging. This is the case for high porosity and high permeability aeolian facies interbedded with muddy wet interdune deposits and alluvial conglomerates and sandstones. Several types of SSDS have been studied in two exposures of the Upper Pliocene (2.9-2.6 Ma) sediments of a fault-bounded intracontinental aeolian dune field in the Teruel Basin (Iberian Chain, eastern Spain). Among SSDS, load and fluid-escape structures, apart from several animal tracks, have been recognized. Those structures show an irregular distribution through the studied stratigraphic sections, being scarce in homogenous aeolian sands and frequent in water-related facies. A detailed study of the distribution and geometry of SSDS and their relationships with respect to the stratigraphic architecture and facies has allowed a critical discrimination of trigger mechanisms, i.e. biological or physical overloading vs. earthquakes. The seismically induced structures are concentrated into seven deformed beds, showing an uneven lateral distribution and geometry closely controlled by the hosting sedimentary facies and their rheology. These seismites resulted from liquefaction during moderate earthquakes (estimated magnitude from 5.0 to 6.8). The most probable seismogenic source was the Sierra del Pobo normal fault zone, located 2 km to the East. Results show how an appropriate recognition of sedimentary facies is crucial to understand the lateral variability of seismites in sedimentary environments characterized by sharp facies changes.

  3. Combination Features of Depositional Sub-facies of Debris-flowon the Jiangjiagou Valley,Yunnan Province%东川蒋家沟泥石流沉积亚相组合特征

    崔之久; 冯金良


    在自然界中,泥石流形成环境、发育规律、空间分布等特征的演化和分异,导致了不同时期、不同区域、不同沉积过程和不同沉积地貌部位泥石流沉积亚相组合的变异。该文拟在作者所建泥石流沉积模式基础上,以蒋家沟为例进一步讨论泥石流亚相的组合及变异规律。此外,初步探讨了夷平面解体后,泥石流沉积在地貌回春不同阶段的发育规律。%In the nature, due to the debris-flow developing under different environment and depositing various landform, it led to combination variation of depositional sub-facies on the different period, various regions and different depositional landform. On the basis of depositional model of debris-flow built by author, the combination and variation of depositional sub-facies of debris-flow on the Jiangjiagou valley,Yunnan Province,was discussed. The main features of debris-flow of Jiangjiagou are as follows: (1)the erosion layer(C) very developed;(2)the layer(B) of surface mud didn't run in succession;(3)the thickness of debris layer(A) is thin;(4)the layer(D) of floor mud developed weakly. The main combination of sub-facies is C-A-C and B-A-C.

  4. Carbonate platform facies development of the Turonian Wata Formation in central and eastern Sinai, Egypt

    Khalifa, M. A.; Farouk, S.; Hassan, A. M.


    The Wata carbonate platform in central and eastern Sinai show a clear pattern of evolutionary development during sedimentation. Three facies are recognized in the carbonate platform. Inner-platform in the south, inter-platform basin in the middle, and outer-platform in the northwest. Such classification was probably performed by the effect of Syrian Arc System that culminated during Turonian in Sinai. Inner-platform includes fining-upward cycles, each begins with packstone, followed by wackestone and capped by lime-mudstone or claystone or molluscan bioclastic wackestone at the base capped by sandy oolitic packstone or dolostone. The dominant faunal associations are molluscs, and echinoids. Inter-platform basin occurs north of inner-platform and extends northwest-southeast direction and comprises fining-upward cycles, each of which begins with bioclastic ostracodal packstone, calcisphere packstone, bioclastic packstone, capped by wackestone and lime-mudstone The faunal association includes, sponge spines, ostracodes, molluscan debris and calcispheres. They were deposited in shoal marine and barrier. The outer-platform occurs at Gebel Giddi and extended northwestwards. The lithofacies are entirely represented by calcisphere wackestone/packstone, with a reduced thickness of 20 m.

  5. Geology and paleontology of the reef facies of the Pirabas Formation (Early Miocene

    Vladimir de Araújo Távora


    Full Text Available This work concerns with the detailed geological and paleontological study of the reef facies of the Pirabas Formation, that outcrop at the Maçarico beach, of Salinópolis district, Pará State, as a small, isolated and lenticular sedimentary bodie developed in the inner platform inner ramp of the Pirabas Sea. The biotic constituents are diverse and composed by three groups of coralline algae, sponges, corals, bryozoans, echinoids, foraminifera, ostracodes and molluscs. Three stages of the ecologic sucession were recognized in this patch reef: stabilization, colonization and diversification. Thin micritic crusts, recognized at top of the beds in diversification stage suggest the degradation of the environmental conditions favorable to reef accretion probably due to continentalization of the depositional site. The petrographic investigation reveals only one, homogeneous depositional microfacies, named biomicrite, without compositional and textural changes. The marine cementation is represented by microcrystalline agglomerates and micritic cement, locally neomorphosed to biosparite and detrital carbonatic components of the unconsolidated biogenic debris, resulted from the disintegration of the aragonite from the algalic remains accumulated as micritic mud. In the construction of the reef framework the red macroalgae were fundamental to the lithification and building of the framework, and very important to the protection and cementation of the others constituents.

  6. Single well multidisciplinary facies reconstruction (De Lute-6 Upper Carboniferous, Netherlands)

    Van Der Zwan, C.J. (Nederlandse Aardolie Maatschappij B.V., Assen (Netherlands)); Van De Laar, J.G.M.; Pagnier, H.J.M.; Van Amerom, H.W.J. (Geological Survey of the Netherlands, Heerlen (Netherlands))


    De Lutte-6 is a key well situated in onshore Netherlands. A cored lithological sequence from the Upper Carboniferous has been investigated by means of palynology, palynofacies, paleobotany, and sedimentology. Paleobotanical data suggest a late Westphalian C to late Westphalian D Age. Palynological assemblages have a late Westphalian D-Stephanian character. This discrepancy suggests that the local paleobotanical remains allow for a more precise age determination, whereas the palynological data provide information about the regional facies development. Palynofacies analyses combined with palynoflora data indicate a gradual transition from a waterlogged flood plain characterized by a diverse lycopod/cordait palynoflora, to well-drained flood plain with an impoverished cordait/conifer palynoflora. The sedimentological data, combined with the palynological and the paleobotanical data, suggest that the flood plains alternate with swamp and lake deposits. The transition from a waterlogged flood plain to a well-drained flood plain coincides with transition from intervals characterized by seat-earth soils (indicating humid conditions) to intervals characterized by immature calcie soils (witnessing semihumid to semi-arid conditions).

  7. Towards the definition of AMS facies in the deposits of pyroclastic density currents

    Ort, M.H.; Newkirk, T.T.; Vilas, J.F.; Vazquez, J.A.; Ort, M.H.; Porreca, Massimiliano; Geissman, J.W.


    Anisotropy of magnetic susceptibility (AMS) provides a statistically robust technique to characterize the fabrics of deposits of pyroclastic density currents (PDCs). AMS fabrics in two types of pyroclastic deposits (small-volume phreatomagmatic currents in the Hopi Buttes volcanic field, Arizona, USA, and large-volume caldera-forming currents, Caviahue Caldera, Neuquén, Argentina) show similar patterns. Near the vent and in areas of high topographical roughness, AMS depositional fabrics are poorly grouped, with weak lineations and foliations. In a densely welded proximal ignimbrite, this fabric is overprinted by a foliation formed as the rock compacted and deformed. Medial deposits have moderate–strong AMS lineations and foliations. The most distal deposits have strong foliations but weak lineations. Based on these facies and existing models for pyroclastic density currents, deposition in the medial areas occurs from the strongly sheared, high-particle-concentration base of a density-stratified current. In proximal areas and where topography mixes this denser base upwards into the current, deposition occurs rapidly from a current with little uniformity to the shear, in which particles fall and collide in a chaotic fashion. Distal deposits are emplaced by a slowing or stalled current so that the dominant particle motion is vertical, leading to weak lineation and strong foliation.


    Albert C. Reynolds; Dean S. Oliver; Yannong Dong; Ning Liu; Guohua Gao; Fengjun Zhang; Ruijian Li


    Knowledge of the distribution of permeability and porosity in a reservoir is necessary for the prediction of future oil production, estimation of the location of bypassed oil, and optimization of reservoir management. The volume of data that can potentially provide information on reservoir architecture and fluid distributions has increased enormously in the past decade. The techniques developed in this research will make it easier to use all the available data in an integrated fashion. While it is relatively easy to generate plausible reservoir models that honor static data such as core, log, and seismic data, it is far more difficult to generate plausible reservoir models that honor dynamic data such as transient pressures, saturations, and flow rates. As a result, the uncertainty in reservoir properties is higher than it could be and reservoir management can not be optimized. In this project, we have developed computationally efficient automatic history matching techniques for generating geologically plausible reservoir models which honor both static and dynamic data. Specifically, we have developed methods for adjusting porosity and permeability fields to match both production and time-lapse seismic data and have also developed a procedure to adjust the locations of boundaries between facies to match production data. In all cases, the history matched rock property fields are consistent with a prior model based on static data and geologic information. Our work also indicates that it is possible to adjust relative permeability curves when history matching production data.

  9. Application of Musical Information Retrieval (MIR Techniques to Seismic Facies Classification. Examples in Hydrocarbon Exploration

    Paolo Dell’Aversana


    Full Text Available In this paper, we introduce a novel approach for automatic pattern recognition and classification of geophysical data based on digital music technology. We import and apply in the geophysical domain the same approaches commonly used for Musical Information Retrieval (MIR. After accurate conversion from geophysical formats (example: SEG-Y to musical formats (example: Musical Instrument Digital Interface, or briefly MIDI, we extract musical features from the converted data. These can be single-valued attributes, such as pitch and sound intensity, or multi-valued attributes, such as pitch histograms, melodic, harmonic and rhythmic paths. Using a real data set, we show that these musical features can be diagnostic for seismic facies classification in a complex exploration area. They can be complementary with respect to “conventional” seismic attributes. Using a supervised machine learning approach based on the k-Nearest Neighbors algorithm and on Automatic Neural Networks, we classify three gas-bearing channels. The good performance of our classification approach is confirmed by borehole data available in the same area.

  10. Biostratigraphy, facies analysis of Upper Cretaceous-Lower Paleocene strata in south Zagros basin (southwestern Iran)

    Afghah, Massih


    In this study, two stratigraphic sections of the Tarbur Formation named Kuh-e Gadvan and Kuh-e Tir were selected. The thicknesses of the whole sediments of the sections studied are about 1100 m of which 400 thin sections were studied. Two biozones are determined in Kuh-e Gadvan and three biozones are described in Kuh-e Tir section. According to established biozones, the age of Tarbur Formation of Kuh-e Gadvan section is assigned to Campanian-Maastrichtian and Tarbur Formation age determination shows relation to Maastrichtian-Lower Paleocene in Kuh-e Tir section. Seven major lithofacies are distinguished along two studied stratigraphic columns which are foraminifer-bioclast wackestone, algal-foraminifer- intraclast wackestone, rudist biclast wackestone, bioclast packstone, bioclast-intraclast grainstone, coral and rudist boundstone. According to the recognized lithofacies, paleoenvironment of the Tarbur formation consists of lagoon, open margin of the reef landward, margin of the reef, flat reef, and seaward margin of the reef. Comparison of studied sections allows that geologic setting had been controlled biostratigraphy and facies change.

  11. Elastic properties of granulite facies rocks of Mahabalipuram, Tamil Nadu, India

    M V M S Rao; K J Prasanna Lakshmi; L P Sarma; K B Chary


    Compressional and shear wave velocities and attenuation measurements have been carried out in some of the borehole samples of acidic, basic and intermediate granulites of Mahabalipuram, Tamil Nadu, India. The results have been obtained at ambient conditions using ‘time-of-flight’ pulse transmission technique at 1.0MHz frequency. The results show linear relationships between velocity and density, and velocity and attenuation properties of the rocks. The acidic granulites show lower velocities and higher attenuation than the intermediate and basic granulites. The average values of the Poisson’s ratio of acidic, intermediate and basic granulites have been found to be 0.210, 0.241 and 0.279 respectively. The variations in velocities and attenuation in these low porosity crystalline rocks are found to be strongly influenced by their mineral composition. The laboratory velocity data (extrapolated to high pressure) of the present study and the published field velocity data from deep seismic sounding studies indicate that these granulite facies rocks may belong to mid-crustal depths only.

  12. Recent Advances in Characterizing Depositional Facies and Pore Network Modeling in Context of Carbon Capture Storage: An Example from the Cambrian Mt. Simon Sandstone in the Illinois Basin

    Freiburg, J. T.; Nathan, W.; Best, J.; Reesink, A.; Ritzi, R. W., Jr.; Pendleton, J.; Dominic, D. F.; Tudek, J.; Kohanpur, A. H.


    In order to understand subsurface flow dynamics, including CO2 plume migration and capillary trapping, a diverse set of geologic properties within the reservoir, from the pore scale to the basin scale, must be understood and quantified. The uncertainty about site-specific geology stems from the inherent variation in rock types, depositional environments, and diagenesis. In collaboration with geocellular and multiphase modeling, detailed characterization of the Lower Mt. Simon Sandstone (LMSS), a reservoir utilized for carbon capture storage, is supporting data-driven conceptual models to better understand reservoir heterogeneity and its relationship to reservoir properties. This includes characterization of sedimentary facies and pore scale modeling of the reservoir The Cambrian-age Lower Mt. Simon Sandstone (LMSS) is a reservoir utilized for two-different carbon capture storage projects in the Illinois Basin, USA. The LMSS is interpreted to have formed in a braided river environment comprising a hierarchy of stratification, with larger scale depositional facies comprising assemblages of smaller scale facies. The proportions, geometries, length scales, and petrophysical attributes of the depositional facies, and of the textural facies they comprise, are being quantified. Based on examination of core and analog outcrop in adjacent areas, the LMSS is comprised of five dominant depositional facies, the most abundant facies being planar to trough cross-bedded sandstones produced by subaqueous sand dunes. This facies has the best reservoir conditions with porosity up to 27% and permeability up to 470 mD. Three-dimensional pore network modeling via micro computed tomography of this facies shows well-connected and unobstructed pore throats and pore space. This presentation will outline the depositional heterogeneity of the LMSS, its relationship to diagenetic fabrics, and its influence on fluid movement within the reservoir.

  13. Aplicación de una medida de riesgo coherente para el cálculo de la prima de riesgo en un seguro de rentas = Application of a coherent risk measure in the price calculation of an income insurance (annuities)

    Montserrat Hernández Solís; Emma Berenguer Cárceles


    ... último aplicado por primera vez en el campo delos seguros de vida. Utilizando las leyes de Gompertz y Makeham primero calculamos la prima a nivel general y en una segunda parte, se aplica el principio de...

  14. Application of a coherent risk measure in the price calculation of an income insurance (annuities) = Aplicación de una medida de riesgo coherente para el cálculo de la prima de riesgo en un seguro de rentas

    Montserrat Hernández Solís; Emma Berenguer Cárceles


    ... último aplicado por primera vez en el campo delos seguros de vida. Utilizando las leyes de Gompertz y Makeham primero calculamos la prima a nivel general y en una segunda parte, se aplica el principio de...

  15. Asignación de primas en el seguro del automóvil utilizando el Análisis en ComponentesPrincipales Funcionales = Premium allocation in the car insurance by using Functional Principal Component Analysis.

    Herranz Peinado, C. Patricia


    Full Text Available El estudio de las primas de riesgo en el seguro del automóvil es de suma importancia, debido a la gran competitividad existente en el mercado asegurador. En este artículo se pretende proponer un sistema de bonificación-penalización de las primas de riesgo utilizando el Análisis Funcional en Componentes Principales. En concreto, se realiza un estudio empírico con los datos reales de una compañía aseguradora con cobertura nacional. Aplicando el sistema propuesto de bonificación-penalización a los perfiles de comportamiento de los asegurados, se obtienen las primas de riesgo para cada uno de los perfiles considerados y tramos de edad. = The study of the premium risk in the car insurance is really important because the insurance market is very competitive. In this article we show a bonus-malus method of risk premiums. To do this, we use the Functional Principal Component Analysis. More precisely, we explain an empirical study with the real data of an insurance company. By applying the bonus-malus method that we have given, we are able to obtain the premium risk for different profiles and age ranges.

  16. The sediment composition and predictive mapping of facies on the Propeller Mound—A cold-water coral mound (Porcupine Seabight, NE Atlantic)

    Heindel, Katrin; Titschack, Jürgen; Dorschel, Boris; Huvenne, Veerle A. I.; Freiwald, André


    Here we provide a detailed qualitative and quantitative insight on recent sediment composition and facies distribution of a cold-water coral (CWC) mound using the example of the Propeller Mound on the Irish continental margin (Hovland Mound Province, Porcupine Seabight). Five facies types on Propeller Mound are defined: (1) living coral framework, (2) coral rubble, (3) dropstone, (4) hardground, representing the on-mound facies, and (5) hemipelagic sediment facies, which describes the off-mound area. This facies definition is based on already published video-data recorded by Remotely Operated Vehicle (ROV), photo-data of gravity cores, box cores, and dredges from sediment surfaces as well as on the composition of the sediment fraction coarser than 125 μm, which has been analyzed on five selected box cores. Sediment compositions of the living coral framework and coral rubble facies are rather similar. Both sediment types are mainly produced by corals (34 and 35 wt%, respectively), planktonic foraminifers (22 and 29 wt%, respectively), benthic foraminifers (both 7 wt%), and molluscs (21 and 10 wt%, respectively), whereas the living coral framework characteristically features additional brachiopods (6 wt%). Hardgrounds are well-lithified coral rudstones rich in coral fragments (>30 surf%), foraminifers, echinoderms, and bivalves. The dropstone facies and the hemipelagic sediment typically carry high amounts of lithoclasts (36 and 53 wt%, respectively) and planktonic foraminifers (35 and 32 wt%, respectively); however, their faunal diversity is low compared with the coral-dominated facies (12 and <2 wt% coral fragments, 7 and 6 wt% benthic foraminifers, and 4 and 0 wt% balanids). Using the maximum likelihood algorithm within ArcGIS 9.2, spatial prediction maps of the previously described mound facies are calculated over Propeller Mound and are based on mound morphology parameters, ground-truthed with the sedimentary and faunal information from box cores, photographs

  17. Calcareous nannofossils and sedimentary facies in the Upper Cretaceous Bozeş Formation (Southern Apuseni Mountains, Romania

    Ramona Balc


    Full Text Available The lithology, sedimentology and biostratigraphy of the Bozes Formation, which crop out in the SE Metaliferi Mountains (Apuseni Mts. have been investigated in order to establish the age of the deposits and the depositional environment. The sedimentary structures and facies are interpreted as indicating a deep-water depositional environment, representing part of a submarine fan lobe. Three facies assemblages have been identified and described. Calcareous nannofossils were used to determine the age of the investigated deposits. The presence of Lucianorhabdus cayeuxii and Calculites obscurus indicates the CC17 biozone, while UC13 Zone is pointed out by the continuous occurrence of Arkhangelskiella cymbiformis and the absence of Broinsonia parca parca. Thus, the age of the studied deposits is Late Santonian -?Early Campanian.

  18. Turbidite Facies Study of Halang Formation on Pangkalan River, Karang Duren - Dermaji Village, Banyumas District, Central Java - Indonesia

    Rizal, Yan; Lagona, Raymond; Dwijo Santoso, Wahyu


    The Halang formation had been exposed continuously in Pangkalan river, Banyumas Basin. Detailed stratigraphic studies by which using measuring section method was performed on Halang formation which found along Pangkalan river. The facies of Halang formation based on sedimentological study can be divided into five facies association, namely with: proximal channel, distal levee, frontal splay 1, crevasse splay, and frontal splay 2. The thickness of distal levees deposit indicates that Halang formation is confirmed as mud rich system turbidities. Fasies association of Halang formation is controlled by several factors. Changes in sediment supply are that one of factor which created a change in fasies association. Sediment supply has changes caused by sea level changes which are resulting of global climatic changes or tectonic factor. Moreover, volcanism process during Late Miocene leads the sediment supply changes.

  19. Sedimentary facies interpretation of Gamma Ray (GR log as basic well logs in Central and Lower Indus Basin of Pakistan

    Adeel Nazeer


    Full Text Available Rocks and most type of soils emit Gamma Ray (GR in varying amount. The emitting elements of primary gamma radiations include potassium 40, uranium, and thorium which are associated with rocks forming minerals in variable amount. GR log is used to predict the varying lithology in borehole by measuring the spontaneous emission of GR radiation from rocks. Role of GR logs in the identification of subsurface facies is the main focused research theme of this manuscript including with objective of brief introduction of GR log and its applications in the identification of facies in the field of Petroleum Geosciences by analyzing the examples of GR log(s from wells, Lower Indus Basin, Pakistan.

  20. Timing of the granulite facies metamorphism in the Sanggan area, North China craton: zircon U-Pb geochronology


    Zircon U-Pb ages are reported for three samples of intrusive rocks in Khondalite series in the Sanggan area, North China craton. The age of meta-granite is dated as 2005±9 Ma, implying that the sedimentary sequences in Khondalites series formed before 2.0Ga. The age of 1921 ±1Ma for the meta-diorite constrain the age of granulite facies metamorphism younger than this date. The age of 1892±10 Ma for garnet granite is obtained, but the granite crystallization age seems a little younger than the date considering the morphology of zircons. On the basis of these dates and of a concise review of previous age data, it is inferred that the Khondalite series was subjected to granulite facies metamorphism at about 1.87Ga together with tonalitic granulites and HP basic granulites in the Sanggan area.

  1. Non-seagrass meadow sedimentary facies of the Pontinian Islands, Tyrrhenian Sea: A modern example of mixed carbonate siliciclastic sedimentation

    Brandano, Marco; Civitelli, Giacomo


    The soft bottom of the Mediterranean continental shelf is characterized by a heterozoan skeletal assemblage ( sensu [James, N.P., 1997. The cool-water carbonate depositional realm. In: James, N.P., Clarke, J. (Eds), Cool-water Carbonates. Spec. Publ. Soc. Sediment. Geol., vol. 56, pp.1-20.]). Although the contemporary presence of terrigenous and skeletal carbonate sediments has been well established [Tortora, P., 1996. Depositional and erosional coastal processes during the last postglacial sea-level rise: an example from the Central Tyrrhenian continental shelf (Italy). J. Sed. Res. 66, 391-405.; Fornós, J.J., Ahr, W.M., 1997. Temperate carbonates on a modern, low-energy, isolated ramp: the Balearic Platform, Spain. Journal of Sedimentary Research , 67, 364-373.; Fornós, J.J., Ahr, W.M., 2006. Present-day temperate carbonate sedimentation on the Balearic Platform, western Mediterranean: compositional and textural variation along a low-energy isolated ramp. In: Pedley, H.M., Carannante, G. (Eds.) 2006, Cool-water Carbonates: Depositional Systems and Palaeoenvironmental Controls. Geological Society, London, Special Publications, 255, pp. 121-135], the interactions between carbonate and terrigenous-siliciclastic sedimentation has not been documented well enough. A total of 33 surface sediment samples from the Pontinian shelf (Tyrrhenian Sea, central Mediterranean) have been analysed. Sampling stations range from 15 to 250 mwd (meter water depth) and are located along five transects (PonzaW, PonzaNW, Ponza NE, Ponza E, Zannone), plus four samples collected around Palmarola Island. Sectors colonized by seagrass meadows have not been sampled. A total of 6 sedimentary facies (F) and 10 microfacies (mf) have been recognized by using component analyses, grain size percentage, sorting, carbonate content and authigenic mineralization rate. These facies and microfacies represent the Pontian Islands shelf sedimentation, in the interval between the upper infralittoral and the

  2. Facies analysis and sequence stratigraphy of the Asmari Formation in the northern area of Dezful Embayment, south-west Iran

    Fateme Zabihi Zoeram


    Full Text Available This paper concerns the sequence stratigraphy of the Oligocene (Rupelian–Chattian–Early Miocene (Burdigalian Asmari Formation based on microfacies analysis of the sediments in the Ghale Nar Oilfield, central area of Zagros fold-thrust belt. Fourteen facies types typical for upward shallowing trend from open marine (MF 1–3, to shoal (MF 4-5, semi-restricted and restricted lagoon (MF 6–12 and finally to near-shore lagoon (MF 13-14 depositional environments were identified. Based on the environmental interpretations, we reconstructed a homoclinal ramp mainly represented by its inner and middle sectors. Facies types MF 4–14 are characterized by the occurrence of large and small porcelaneous benthic foraminifera representing a shallow-water setting of an inner ramp influenced by wave and tide processes. MF1 (Pabdeh Formation, and 2 -3 with planktonic, large and small hyaline benthic foraminifera represent between FWWB and SWB. Four third-order depositional sequences were recognized. In this study, in order to better correlate the identified sequences with pre-defined sequences of the Asmari Formation in the Dezful Embayment and the Izeh zone that are chronologically well-defined, we use their number instead of their name. Sequence 2 mainly consists of an open marine environment in the base, followed by semi-restricted to restricted lagoonal facies. Sequences 36 are characterized by semi-restricted to restricted lagoonal facies. Moreover, the regional relative sea-level change curves correlate well with the global sea-level change curves.

  3. Multiscale heterogeneity characterization of tidal channel, tidal delta and foreshore facies, Almond Formation outcrops, Rock Springs uplift, Wyoming

    Schatzinger, R.A.; Tomutsa, L. [BDM Petroleum Technologies, Bartlesville, OK (United States)


    In order to accurately predict fluid flow within a reservoir, variability in the rock properties at all scales relevant to the specific depositional environment needs to be taken into account. The present work describes rock variability at scales from hundreds of meters (facies level) to millimeters (laminae) based on outcrop studies of the Almond Formation. Tidal channel, tidal delta and foreshore facies were sampled on the eastern flank of the Rock Springs uplift, southeast of Rock Springs, Wyoming. The Almond Fm. was deposited as part of a mesotidal Upper Cretaceous transgressive systems tract within the greater Green River Basin. Bedding style, lithology, lateral extent of beds of bedsets, bed thickness, amount and distribution of depositional clay matrix, bioturbation and grain sorting provide controls on sandstone properties that may vary more than an order of magnitude within and between depositional facies in outcrops of the Almond Formation. These features can be mapped on the scale of an outcrop. The products of diagenesis such as the relative timing of carbonate cement, scale of cemented zones, continuity of cemented zones, selectively leached framework grains, lateral variability of compaction of sedimentary rock fragments, and the resultant pore structure play an equally important, although less predictable role in determining rock property heterogeneity. A knowledge of the spatial distribution of the products of diagenesis such as calcite cement or compaction is critical to modeling variation even within a single facies in the Almond Fin. because diagenesis can enhance or reduce primary (depositional) rock property heterogeneity. Application of outcrop heterogeneity models to the subsurface is greatly hindered by differences in diagenesis between the two settings. The measurements upon which this study is based were performed both on drilled outcrop plugs and on blocks.

  4. Preliminary Facies Reconstruction of a Late Pleistocene Cypress Forest Discovered on the Northern Gulf of Mexico Continental Shelf

    Gonzalez Rodriguez, S. M.; Bentley, S. J.; DeLong, K. L.; Xu, K.; Caporaso, A.; Obelcz, J. B.; Harley, G. L.; Reese, C. A.; Truong, J. T.


    We are investigating the origin and preservation of an ancient bald cypress forest (Taxodium distichum) discovered on the continental shelf seafloor, offshore of Gulf Shores, Alabama, USA, in 20 m water depth. The forest was likely buried in the late Pleistocene, possibly exhumed by Hurricane Ivan in 2004, and is now exposed as stumps in life position with little evidence of decay before recent marine exposure. Radiocarbon analyses show that the forest age is near (and in some cases beyond) the limits of 14C dating, at least 41-45 ky BP. In August 2015 and July 2016, submersible vibracores (up to 5 m in length) were collected. Ongoing core analyses include: organic content (loss on ignition), granulometry, and core logging using a Geotek Multi Sensor Core Logger to generate imagery, bulk density, and x-ray fluorescence data. To bolster 14C analyses, cores collected in 2016 are presently being dated using optically stimulated luminescence. Local stratigraphy consists of a surface facies of Holocene transgressive sands, underlain by possible estuarine sediments of interbedded sand and mud (potentially Holocene or Pleistocene), overlying a swamp or delta plain facies (likely Pleistocene) containing woody debris and mud. Deeper woody facies are thought to include the soil horizons of the ancient cypress forest. Cores collected in 2016 revealed a Pleistocene paleosol beneath Holocene sands in a nearby trough. Elevation differences between swamp and paleosol horizons will be evaluated from bathymetric and subbottom data, to help characterize the preserved ancient landscape. Initial interpretation based on close proximity of Pleistocene swamp and oxidized paleosol sediments, and regional geomorphic gradients suggest that this relatively diverse assemblage of facies developed up to tens of km from the glacial-age coastline, and relatively rapid burial prevented erosion by coastal processes during the Holocene transgression thus preserving the tree stumps and wood debris.

  5. Sedimentology, petrology, and gas potential of the Brallier Formation: upper Devonian turbidite facies of the Central and Southern Appalachians

    Lundegard, P.D.; Samuels, N.D.; Pryor, W.A.


    The Upper Devonian Brallier Formation of the central and southern Appalachian basin is a regressive sequence of siltstone turbidites interbedded with mudstones, claystones, and shales. It reaches 1000 meters in thickness and overlies basinal mudrocks and underlies deltaic sandstones and mudrocks. Facies and paleocurrent analyses indicate differences between the depositional system of the Brallier Formation and those of modern submarine fans and ancient Alpine flysch-type sequences. The Brallier system is of finer grain size and lower flow intensity. In addition, the stratigraphic transition from turbidites to deltaic sediments is gradual and differs in its facies succession from the deposits of the proximal parts of modern submarine fans. Such features as massive and pebbly sandstones, conglomerates, debris flows, and massive slump structures are absent from this transition. Paleocurrents are uniformly to the west at right angles to basin isopach, which is atypical of ancient turbidite systems. This suggests that turbidity currents had multiple point sources. The petrography and paleocurrents of the Brallier Formation indicate an eastern source of sedimentary and low-grade metasedimentary rocks with modern relief and rainfall. The depositional system of the Brallier Formation is interpreted as a series of small ephemeral turbidite lobes of low flow intensity which coalesced in time to produce a laterally extensive wedge. The lobes were fed by deltas rather than submarine canyons or upper fan channel systems. This study shows that the present-day turbidite facies model, based mainly on modern submarine fans and ancient Alpine flysch-type sequences, does not adequately describe prodeltaic turbidite systems such as the Brallier Formation. Thickly bedded siltstone bundles are common features of the Brallier Formation and are probably its best gas reservoir facies, especially when fracture porosity is well developed.

  6. Assessing automated image analysis of sand grain shape to identify sedimentary facies, Gran Dolina archaeological site (Burgos, Spain)

    Campaña, I.; Benito-Calvo, A.; Pérez-González, A.; Bermúdez de Castro, J. M.; Carbonell, E.


    Gran Dolina is a cave (Sierra de Atapuerca, Spain) infilled by a 25 m thick sedimentary record, divided into 12 lithostratigraphic units that have been separated into 19 sedimentary facies containing Early and Middle Pleistocene hominin remains. In this paper, an automated image analysis method has been used to study the shape of the sedimentary particles. Since particle shape is interpreted as the result of sedimentary transport and sediment source, this study can provide valuable data about the sedimentological mechanism of sequence formation. The shape of the sand fraction in 73 samples from Gran Dolina site and Sierra de Atapuerca was analyzed using the Malvern Morphologi G3, an advanced particle characterization tool. In this first complete test, we used this method to the published sequence of Gran Dolina, defined previously through field work observations and geochemical and textural analysis. The results indicate that this image analysis method allows differentiation of the sedimentary facies, providing objective tools to identify weathered layers and measure the textural maturity of the sediments. Channel facies have the highest values of circularity and convexity, showing the highest textural maturity of particles. On the other hand, terra rossa and debris flow samples show similar values, with the lowest particle maturity.

  7. Long-lived high-temperature granulite-facies metamorphism in the Eastern Himalayan orogen, south Tibet

    Zhang, Zeming; Xiang, Hua; Dong, Xin; Ding, Huixia; He, Zhenyu


    The Namche Barwa Complex exposed in the Eastern Himalayan Syntaxis, south Tibet, underwent high-pressure (HP) and high-temperature (HT) granulite-facies metamorphism and associated anatexis. The HP pelitic granulites contain garnet, kyanite, sillimanite, cordierite, biotite, quartz, plagioclase, K-feldspar, spinel, ilmenite and graphite. These minerals show composite reaction texture and varying chemical compositions and form four successive mineral assemblages. Phase equilibrium modeling constrains the P-T conditions of 10-12 kbar and 550-700 °C for the prograde stage, 13-16 kbar and 840-880 °C for the peak-metamorphic stage, and 5-6 kbar and 830-870 °C for the late retrograde stage, indicating that the HP granulites recorded a clockwise P-T path involving the early heating burial and anatexis through dehydration melting of both muscovite and biotite, and the late isothermal decompression and gradual melt crystallization under HT granulite-facies conditions. The zircon U-Pb dating reveals that the HT granulite-facies metamorphism probably initiated at ca. 40 Ma, and lasted to ca. 8 Ma. Therefore, the present study provides robust evidence for a long-lived HT metamorphism and associated anatexis in the deeply buried Indian continent and important constraints on the leucogranite generation and tectonic evolution of the Himalayan orogen.




    Full Text Available The Late Jurassic-Early Cretaceous Apulia platform margin and the transition to adjacent basinal deposits (inner platform to basin are well exposed in the Gargano Promontory. Detailed field work has allowed to recognize eight main facies associations which reflect various depositional environments, and which document a differentiated zonation, from the inner platform to the basin. A shallow lagoon existed in the internal part of the Gargano Promontory with a transition to tidal flat areas (F1. Oolitic shoals (F2 bordered this internal peritidal area passing seaward to a reef-flat with abundant corals (F3. A reef-front, associated with a coral rubble zone, has been found in some areas (F4. In the external margin zone, massive wackestones with Ellipsactinia occur (F5 and pass gradually to a rudstone facies on the proximal slope (F6. The base-of-slope facies association consists of pelagic sediments interbedded with gravity-displaced deposits (F7 and F8. The depositional profile of the Apulia Platform is typical of the Tethyan Jurassic-Early Cretaceous platforms, with slope declivities in the order of 25°-28°. The remarkable progradation of the platform in the northern tract of the Gargano (Lesina and Varano lakes area and its substantial stability east- and southwards (Mattinata area suggest a possible windward position of the margin in this latter portion and, in contrast, a leeward position of the northern portion.   

  9. Trace element geochemistry and tectonic characterization of the granulite facies rocks from Southwest Obudu Plateau, southeastern Nigeria

    Ekere E. Ukwang; Barth N. Ekwueme


    The trace elements characteristics of the migmatitic gneisses (biotite-garnet- and hornblende-biotite), granulite facies rocks (charnockitic gneisses) and meta-peridotite in the area of Southwest Obudu Plateau indicate that the area exhibits a high degree of geochemical variability. Compatible trace elements (Ni and Cr) are comparatively high in the granulite facies rocks and meta-peridotite. Ni ranges from 28×10-6 to 266×10-6 whilst Cr ranges from 62×10-6 to 481×10-6 for the granulite facies rocks (charnockitic gneisses), and for the meta-peridotite Ni varies between 2045×10-6 and 2060×10-6. Incompatible trace elements show a higher variability in these rocks. The rocks in the area of Southwest Obudu Plateau generally are characterized by the high concentrations of Ba, Ce, Sr, Rb, Ga, Ni, Cr, Co, Zr, Pr and moderate concentrations of Cu, Sm and Th. The available data show that the charnockitic gneisses are of lower crustal origin. The enrichment of the meta-peridotite in compatible trace elements suggests the primitive mantle would be the source region, with slight contamination during ascent. These diverse origins collaborate the tectonic setting of the area as shown by discrimination diagrams. The diverse tectonic settings range from arc to collisional. Alkaline to sub-alkaline magmatism in the area was probably contemporaneous with the tectonic events that occurred in the area during the Proterozoic.

  10. La canonica di Santa Maria del Fiore e i suoi abitanti nella prima metà del XV secolo

    Gabriella Battista


    Full Text Available The essay analyzes the residence of the canons of the Cathedral of Florence in the period covered by The Years of the Cupola with attention both to its architectonic and social-political-cultural aspects in order to define the architectural natural and function of the complex and identify its residents and the circumstances of their common life. Through the systematic study of the documentation regarding the definition and management of the close it is possible to reconstruct the steps in the creation of a new dignified and comfortable cloistered space for the metropolitan clergy: a building complex that was appropriately detached from the new church, which had to remain magnificently free around its entire circumference. This new residence for canons, chaplains and other ecclesiastical collaborators, designed to accommodate the values of residency, common life and discipline, was realized in the tight urban fabric of the medieval city at great cost for the purchase of private real estate which was gradually incorporated into the project according to the predetermined ‘design’. It was defined along lines that remained unchanged until the 19th century following a policy of adapting structures previously destined to civil habitation and enclosing them in a cloistered environment sheltered from urban circulation with a single monumental entrance towards the church and its portal ‘of the Canons’. In order to understand the duties incumbent upon the canons and chaplains it was necessary to examine the synodal constitutions of previous periods. These documents offered a view of the common life in the canonry according to the dictates of the constitutions that regulated discipline: from the assignment of dwellings on the basis of seniority to the designation of places for the sharing of meals and, finally, the necessity of providing small personal spaces for meditation and study. The resident canons belonged to the highest rank of society

  11. Upscaling retardation factor in hierarchical porous media with multimodal reactive mineral facies.

    Deng, Hailin; Dai, Zhenxue; Wolfsberg, Andrew V; Ye, Ming; Stauffer, Philip H; Lu, Zhiming; Kwicklis, Edward


    Aquifer heterogeneity controls spatial and temporal variability of reactive transport parameters and has significant impacts on subsurface modeling of flow, transport, and remediation. Upscaling (or homogenization) is a process to replace a heterogeneous domain with a homogeneous one such that both reproduce the same response. To make reliable and accurate predictions of reactive transport for contaminant in chemically and physically heterogeneous porous media, subsurface reactive transport modeling needs upscaled parameters such as effective retardation factor to perform field-scale simulations. This paper develops a conceptual model of multimodal reactive mineral facies for upscaling reactive transport parameters of hierarchical heterogeneous porous media. Based on the conceptual model, covariance of hydraulic conductivity, sorption coefficient, flow velocity, retardation factor, and cross-covariance between flow velocity and retardation factor are derived from geostatistical characterizations of a three-dimensional unbounded aquifer system. Subsequently, using a Lagrangian approach the scale-dependent analytical expressions are derived to describe the scaling effect of effective retardation factors in temporal and spatial domains. When time and space scales become sufficiently large, the effective retardation factors approximate their composite arithmetic mean. Correlation between the hydraulic conductivity and the sorption coefficient can significantly affect the values of the effective retardation factor in temporal and spatial domains. When the temporal and spatial scales are relatively small, scaling effect of the effective retardation factors is relatively large. This study provides a practical methodology to develop effective transport parameters for field-scale modeling at which remediation and risk assessment is actually conducted. It does not only bridge the gap between bench-scale measurements to field-scale modeling, but also provide new insights into

  12. Multiscale characterization of pyritized plant tissues in blueschist facies metamorphic rocks

    Bernard, Sylvain; Benzerara, Karim; Beyssac, Olivier; Brown, Gordon E., Jr.


    Pyritized plant tissues with well-preserved morphology were studied in rocks from Vanoise (western Alps, France) that experienced high-pressure, low-temperature metamorphic conditions in the blueschist facies during the Alpine orogeny. Organic and inorganic phases composing these fossils were characterized down to the nanometer scale by Raman microspectroscopy, scanning transmission X-ray microscopy and transmission electron microscopy. The graphitic but disordered organic matter composing these fossils is chemically and structurally homogeneous and mostly contains aromatic functional groups. Its original chemistry remains undefined likely because it was significantly transformed by diagenetic processes and/or thermal degradation during metamorphism. Various mineral phases are closely associated with this organic matter, including sulphides such as pyrite and pyrrhotite, carbonates such as ankerite and calcite, and iron oxides. A tentative time sequence of formation of these diverse mineral phases relative to organic matter decay is proposed. The absence of traces of organic matter sulphurization, the pervasive pyritization of the vascular tissues and the presence of ankerite suggest that the depositional/diagenetic environment of these metasediments was likely rich in reactive iron. Fe-sulphides and ankerite likely precipitated early and might have promoted the preservation of the fossilized biological soft tissues by providing mechanical resistance to compaction during diagenesis and subsequent metamorphism. In contrast, iron oxides which form rims of 100-nm in thickness at the interface between organic matter and Fe-sulphides may result from metamorphic processes. This study illustrates that it may be possible in some instances to deconvolve metamorphic from diagenetic imprints and opens new avenues to better constrain processes that may allow the preservation of organic fossils during diagenesis and metamorphism.

  13. Chemical modifications accompanying blueschist facies metamorphism of Franciscan conglomerates, Diablo Range, California

    Moore, Diane E.; Liou, J.G.; King, B.-S.


    As part of an investigation of blueschist-facies mineral parageneses in pebbles and matrix of some Franciscan metaconglomerates of the Diablo Range, California, textural and major-element chemical analyses were conducted on a number of igneous pebbles that comprise a range of rock types from granite and dacite to gabbro and basalt. Compositions of the igneous pebbles differ significantly from common igneous rocks, particularly with respect to Ca, K, Na, Si and H2O. The SiO2 and H2O contents are characteristically high and the K2O contents low. The CaO and Na2O contents may be relatively enriched or reduced in different pebbles. The igneous pebbles show little evidence of alteration prior to their incorporation into the Franciscan conglomerates, and the chemical modifications are considered to have been produced during metamorphism of the conglomerates to (lawsonite + albite + aragonite ?? jadeite)-bearing assemblages. The observed variations in the pebbles are shown to be functions of: (1) bulk chemistry; (2) the igneous mineral assemblage; (3) the stable metamorphic mineral assemblage; and (4) the composition of pore fluids in the conglomerates. The relative proportions of Mg and Fe in most of the pebbles apparently have been unaffected by the metamorphism, and these parameters, along with other textural and chemical factors, were used to determine the petrogenetic affinities of the igneous pebbles. The plutonic and most of the volcanic pebbles correspond to calc-alkaline rock series, whereas a few volcanic pebbles show apparent Fe-enrichment characteristic of tholeiitic rocks. A continental margin arc-batholith complex would be the best source for these igneous detrital assemblages. Conglomerates in local areas differ in igneous lithologies from conglomerates in other areas and probably differ somewhat in age, perhaps reflecting varying degrees of unroofing of such a complex during deposition of Franciscan sediments. ?? 1981.

  14. Disjunctive Grade Variation from Greenschist to Granulite Facies, Siyom Valley, Eastern Arunachal Pradesh, India

    Clarke, G. L.; Bhowmik, S. K.; Aitchison, J. C.; Ireland, T. R.


    The Siyom Valley section in eastern Arunachal Pradesh exposes an inverted metamorphic succession (Nandini & Thakur, 2011), metapelitic assemblages increasing in grade northwards from chlorite, through biotite, garnet-staurolite and kyanite-bearing schist to kyanite-sillimanite migmatite. Grade changes are mostly controlled by shallowly north, and northwest-dipping fault structures. Two textural stages of garnet growth can be identified in the ilmenite-bearing amphibolite facies rocks, staurolite having formed late in, or after, deformation responsible for the main penetrative foliation (S2). Kyanite and rutile inclusions in garnet indicate that their growth in migmatite preceded that of matrix sillimanite, ilmenite and cordierite, though unrecrystallized kyanite is also common in the feldspathic matrix. Preliminary data indicate the pronounced tectonic thinning of metasedimentary protoliths during exhumation, and the probability of a pronounced step in grade in the middle part of the river section. Similarities with sections in the Sikkim (Dasgupta et al., 2004) and western Arunachal Pradesh (Goswami et al., 2009) Himalaya reflect the lateral continuity of the south-vergent thrusts that controlled the exhumation of the high-grade rocks, with debate concerning the location and significance of the Main Central Thrust zone begging protolith and metamorphic age data. Dasgupta, S.,Ganguly, J. & Neogi, S., 2004. Inverted metamorphic sequence in the Sikkim Himalayas: crystallization history, P-T gradient and implications. Journal of Metamorphic Geology, 22, 395-412. Goswami, S., Bhowmik, S.K. & Dasgupta, S., 2009. Petrology of a non-classical Barrovian inverted metamorphic sequence from the western Arunachal Himalaya, India. Journal of Asian Earth Sciences, 36, 390-406. Nandini, P. & Thakur, S.S., 2011. Metamorphic evolution of the Lesser Himalayan Crystalline Sequence, Siyom Valley, NE Himalaya, India. Journal of Asian Earth Sciences, 40, 1089-1100

  15. Jurassic evaporite facies of the Afghan-Tajik and Amu Darya basins in northern Afghanistan and adjacent areas (evapfacafg.shp)

    U.S. Geological Survey, Department of the Interior — This shapefile contains polygons that describe the spatial extent of Jurassic age evaporite facies (Gaurdak formation) in the Afghan-Tajik and Amu Darya basins.

  16. Facies interpretations and lateral variability based on correlation of conventional core in the Logan canyon and Mississauga formations of the Scotian Basin

    Piper, D.J.W. [Geological Survey of Canada (Canada); Gould, K.M.; Pe-Piper, G. [Saint Mary' s University (Canada)], email:


    In the Lower Cretaceous of the Scotian Basin in Canada, sediment facies have been interpreted mostly using vertical successions of rock. However, other studies show that the lateral extent and variability of sediment facies must be understood to assess reservoir extent and connectivity. The aim of this paper is to present the investigation of two areas of the Scotian Basin. In each area, a regional correlation was performed using gamma ray well logs and the lithology, sedimentary and biogenic structures were determined for 67 different cores. It was found that the determination of facies and vertical successions was useful for comparing and correlating across multiple wells. In addition it was shown that gamma logs are effective for regional correlation but can only correlate major changes. This paper demonstrated that gamma logs are useful for performing facies interpretations and determining lateral variability.

  17. Thickness of Jurassic evaporite facies in the Afghan-Tajik and Amu Darya basins of northern Afghanistan and adjacent areas (evapisoafg.shp)

    U.S. Geological Survey, Department of the Interior — This shapefile contains polylines (isopachs) that describe the thickness of Jurassic age evaporite facies (Gaurdak formation) in the Afghan-Tajik and Amu Darya basins

  18. GMX_FAC: usSEABED facies data for the entire U.S. Gulf of Mexico and Caribbean (Puerto Rico and U.S. Virgin Islands)

    U.S. Geological Survey, Department of the Interior — The facies data layer (_FAC.txt) is a point coverage of known sediment samplings, inspections, and probings from the usSEABED data collection and integrated using...

  19. Sediments of the Dry Tortugas, south Florida, USA: Facies distribution on a ramp-like isolated carbonate platform

    Gischler, Eberhard; Isaack, Anja; Hudson, J. Harold


    Four sedimentary facies may be delineated based on quantitative analysis of texture and composition of modern surface sediments on the Dry Tortugas carbonate platform. These include (1) mollusk-Halimeda wackestone, (2) mollusk packstone-to-grainstone, (3) coralgal-Halimeda grainstone, and (4) coralgal grainstone. Even though the Tortugas platform is characterized by an open circulation due to deep, broad marginal channels and a lack of a continuous surface-breaking marginal reef, facies are not distributed at random and show bathymetrical zonation. Also, facies appear to cover wide belts rather than forming a mosaic. Mollusk-Halimeda wackestone occurs in protected platform interior areas ca. 10-18 m deep. Mollusk packstone-to-grainstone occurs in more open platform interior settings adjacent to channels and in deeper outer reef areas of 14-25 m water depth. Coralgal-Halimeda grainstone is found on shallow marginal shoals (1-11 m deep), and coralgal grainstone on the somewhat deeper (3-16 m), seaward edges of these shoals. However, there is bathymetrical overlap of facies in intermediate depths of ca. 5-17 m. This limitation has implications for the interpretation of the fossil record, because changes in water depth are commonly thought to be reflected in facies changes, e.g., in sequence stratigraphy. Comparison with previous sediment studies of the 1930s, 1960s, and 1970s in the area exhibit a decrease in coral fragments and increases in coralline algal and mollusk shell fragments. These observations might be a result of environmental changes such as coral decline and die-outs during temperature events, disease, and the increase in macroalgae (due to the ecological extinction of the echinoid Diadema). The results suggest that more long-term studies are needed that further explore the influence of environmental change on reef sediment composition. Dry Tortugas surface sediments consist of lower portions of Halimeda plates and mollusk shell fragments and higher

  20. Validación del sistema ultramicroelisa en la certificación de placenta humana como materia prima farmacéutica y cosmética

    Maydelin Trujillo Alfonso

    Full Text Available Introducción: el Laboratorio de Control Viral de la Planta Derivados de la Placenta realiza la certificación de la placenta humana como materia prima farmacéutica y cosmética mediante el sistema ultramicroanalítico. Objetivo: validar el sistema ultramicroelisa de determinación de antígeno de superficie del virus de la hepatitis B, anticuerpos contra el virus de la hepatitis C y virus de inmunodeficiencia humana tipo 1 y 2 en muestras de suero de cordón umbilical. Métodos: se realizó la calificación de la operación y la validación del desempeño analítico de los sistemas UMELISA HBsAg Plus, UMELISA HCV y UMELISA HIV 1+2 Recombinant empleandocomo sistemas de referencia el Hepanostika HBsAg Uni-FormII, Hepanostika HCV Ultra y Vironostika HIV-Uni-Form II Ag/Ab. Resultados: la calificación de la operación para las tres técnicas analíticas resultó satisfactoria. Los parámetros de especificidad diagnóstica y analítica fueron de 100 %, así como la concordancia con las técnicas de referencia. El coeficiente de variación fue menor del 10 % durante el estudio de precisión interensayo, menor que el 20 % intraensayo y se demostró la robustez de las técnicas para pequeños cambios en la temperatura de incubación. Conclusiones: los sistemas ultramicroelisa utilizados como método de control de la calidad de la placenta humana resultaron específicos, precisos y robustos en las condiciones ensayadas, por lo que pueden emplearse de manera segura y confiable.

  1. Procedimiento para la gestión de los impactos ambientales negativos asociados a la recuperación de materias primas en Cienfuegos, Cuba.

    David Javier Castro Rodríguez


    Full Text Available El reciclaje constituye una actividad priorizada en Cuba. El objetivo fue implementar un procedimiento para la gestión de los impactos ambientales negativos asociados a los procesos operativos de la Empresa de Recuperación de Materias Primas de Cienfuegos. El procedimiento se construyó utilizando la propuesta del Instituto Andaluz de Tecnología para la gestión por procesos y los ocho pasos en la solución de problemas. Se combinaron herramientas de gestión bajo el principio de convergencia metodológica. Los impactos ambientales fueron evaluados mediante el software GAIA versión 1.0, utilizando los criterios propuestos por la Guía Metodológica de Evaluación de Impacto Ambiental de Conesa. Se identificaron 97 impactos ambientales negativos, entre severos y moderados integraron el 80.41 % de ellos. El factor ambiental más impactado fue el físico-químico con el 50.52 %. El subproceso no metálico resultó el más impactante, con el 50 % de los impactos severos negativos totales y el 34 % de los moderados. Se identificaron las principales causas asociadas y se diseñó un plan de intervención de 35 medidas con base en los principios de Producción Más Limpia. Los resultados contribuyen a lograr la gestión de los impactos ambientales negativos de la entidad y a la sostenibilidad del reciclaje.

  2. Apprendere dagli studenti prima di entrare in classe. La comunicazione tra studenti delle superiori e insegnanti in formazione iniziale con l'email

    Alison Cook-Sather


    Full Text Available Questo articolo presenta uno studio svolto nell’ambito di un progetto di ricerca in cui, nell’arco di un intero semestre accademica, è prevista la comunicazione sistematica per email fra studenti universitari e studenti della scuola superiore. I primi frequentano dei corsi di laurea tenuti da due college nel nordest degli Stati Uniti per poter ottenere l’abilitazione come docenti, mentre i secondi studiano presso delle scuole superiori di secondo livello situate nello stesso territorio. Dallo studio emerge che lo scambio di comunicazione fra i due gruppi, che avviene prima che gli studenti universitari comincino le prime esperienze pratiche in classe, genera una serie di risultati interessanti. Secondo entrambi i gruppi, le comunicazioni: (1 favoriscono le creazione di legami più personalizzati rispetto a quelli che generalmente si formano nei vincoli organizzativi e nei limiti dei ruoli tipici dei corsi universitari; 2 determinano, in modo più o meno positivo, le modalità di comunicazione proprie dei partecipanti; (3 favoriscono l’analisi critica e la riflessione; (4 offrono ai partecipanti la possibilità di capire meglio il punto di vista degli altri; e (5 costituiscono una traccia persistente delle interazioni. Gli scambi di email creano una specie di spazio liminale - una zona spazio-tempo intermedio in cui sia i futuri insegnanti che gli studenti svolgono ruoli diversi da quelli abituali - consentendo ai partecipanti al progetto di provare nuovi modi di essere, sviluppare nuovi modi di interagire e sperimentare dei ruoli diversi nell’ottica di capire meglio la loro idea personale di identità professionale.

  3. Geomorphology, facies architecture, and high-resolution, non-marine sequence stratigraphy in avulsion deposits, Cumberland Marshes, Saskatchewan

    Farrell, K. M.


    This paper demonstrates field relationships between landforms, facies, and high-resolution sequences in avulsion deposits. It defines the building blocks of a prograding avulsion sequence from a high-resolution sequence stratigraphy perspective, proposes concepts in non-marine sequence stratigraphy and flood basin evolution, and defines the continental equivalent to a parasequence. The geomorphic features investigated include a distributary channel and its levee, the Stage I crevasse splay of Smith et al. (Sedimentology, vol. 36 (1989) 1), and the local backswamp. Levees and splays have been poorly studied in the past, and three-dimensional (3D) studies are rare. In this study, stratigraphy is defined from the finest scale upward and facies are mapped in 3D. Genetically related successions are identified by defining a hierarchy of bounding surfaces. The genesis, architecture, geometry, and connectivity of facies are explored in 3D. The approach used here reveals that avulsion deposits are comparable in process, landform, facies, bounding surfaces, and scale to interdistributary bayfill, i.e. delta lobe deposits. Even a simple Stage I splay is a complex landform, composed of several geomorphic components, several facies and many depositional events. As in bayfill, an alluvial ridge forms as the feeder crevasse and its levees advance basinward through their own distributary mouth bar deposits to form a Stage I splay. This produces a shoestring-shaped concentration of disconnected sandbodies that is flanked by wings of heterolithic strata, that join beneath the terminal mouth bar. The proposed results challenge current paradigms. Defining a crevasse splay as a discrete sandbody potentially ignores 70% of the landform's volume. An individual sandbody is likely only a small part of a crevasse splay complex. The thickest sandbody is a terminal, channel associated feature, not a sheet that thins in the direction of propagation. The three stage model of splay evolution

  4. Facies distribution, depositional environment, and petrophysical features of the Sharawra Formation, Old Qusaiba Village, Central Saudi Arabia

    Abbas, Muhammad Asif; Kaminski, Michael; Umran Dogan, A.


    moderate-scale transgressive episodes, while the thin shale interbeds in the middle and upper part of the Sharawra Formation represent small-scale transgressions. Overall, the Sharawra Formation contains a series of repetitive transgressive and regressive events and has been interpreted as a pro-deltaic deposit in previous studies. In the present study, the lowermost sandstone thickly bedded facies lie within the transition zone environment. The siltstone facies and the horizontally stratified facies show a middle shore face environment. The middle shore face environment is present locally. The bioturbation in the uppermost facies is indicative of the upper shore face environment. The porosity values do not vary much, as the average porosity for the sandstone facies is about 15%, for the siltstones it ranges about 7%. The permeability is variable throughout the formation, the values range from 50 to 300 md. Although sandstone has a good porosity and permeability, the siltstone facies exhibit poor petrophysical characteristics. In terms of reservoir characterization, the mineralogical mature, moderately well sorted top most sandstone facies, with appreciable porosity and permeability can be considered as a potential reservoir rock. This study has provided a base for future quantitative studies in this important formation in the area.

  5. Natural gas; Gas Natural

    Lopes, Carlos A.; Moraes, Claudia C.D. [Eletricidade de Sao Paulo S.A. (ELETROPAULO), Sao Paulo, SP (Brazil); Fonseca, Carlos H.F. [Centrais Eletricas de Santa Catarina S.A., Florianopolis, SC (Brazil); Silva, Clecio Fabricio da; Alves, Ricardo P. [Companhia Paranaense de Energia (COPEL), Curitiba, PR (Brazil); Sposito, Edivaldo Soares; Hulle, Lutero [Espirito Santo Centrais Eletricas S.A. (ESCELSA), Vitoria, ES (Brazil); S. Martins, Icaro da [Centrais Eletricas do Norte do Brasil S.A. (ELETRONORTE), Belem, PA (Brazil); Vilhena, Joao Luiz S. de [Companhia Energetica de Minas Gerais (CEMIG), Belo Horizonte, MG (Brazil); Fagundes, Zaluar Aquino [Companhia Estadual de Energia Eletrica do Estado do Rio Grande do Sul, Porto Alegre, RS (Brazil)


    An increase in the consumption of natural gas in Brazil is an expected fact in what concerns energetic planning. This work presents the existing situation in what concerns natural gas utilization in the main world economies, as well as an analysis of the participation of this fuel among the energy final consumption per sources. The Brazilian consumption of natural gas is also analysed as well as the international agreement between Brazil and Bolivia for natural gas commercialization. Some legal, institutional and political aspects related to natural gas commercialization are also discussed. Finally, several benefits to be brought by the utilization of natural gas are presented 10 refs., 3 tabs.

  6. Facies analysis of a Toarcian-Bajocian shallow marine/coastal succession (Bardas Blancas Formation) in northern Neuquén Basin, Mendoza province, Argentina

    Bressan, Graciela S.; Kietzmann, Diego A.; Palma, Ricardo M.


    Strata of the Bardas Blancas Formation (lower Toarcian-lower Bajocian) are exposed in northern Neuquén Basin. Five sections have been studied in this work. Shoreface/delta front to offshore deposits predominate in four of the sections studied exhibiting a high abundance of hummocky cross-stratified, horizontally bedded and massive sandstones, as well as massive and laminated mudstones. Shell beds and trace fossils of the mixed Skolithos-Cruziana ichnofacies appear in sandstone beds, being related with storm event deposition. Gravel deposits are frequent in only one of these sections, with planar cross-stratified, normal graded and massive orthoconglomerates characterizing fan deltas interstratified with shoreface facies. A fifth outcrop exhibiting planar cross-stratified orthoconglomerates, pebbly sandstones with low-angle stratification and laminated mudstones have been interpreted as fluvial channel deposits and overbank facies. The analysis of the vertical distribution of facies and the recognition of stratigraphic surfaces in two sections in Río Potimalal area let recognized four transgressive-regressive sequences. Forced regressive events are recognized in the regressive intervals. Comparison of vertical distribution of facies also shows differences in thickness in the lower interval among the sections studied. This would be related to variations in accommodation space by previous half-graben structures. The succession shows a retrogradational arrangement of facies related with a widespread transgressive period. Lateral variation of facies let recognize the deepening of the basin through the southwest.

  7. Facies analysis and sequence stratigraphy review of Ponta Grossa formation, Parana Basin - emphasis on the Tibagi Member sandstones; Analise de facies e revisao da estratigrafia de sequencias da Formacao Ponta Grossa, Bacia do Parana - enfase nos arenitos do Membro Tibagi

    Candido, Ary Gustavo [PETROBRAS, Campos dos Goytacases, RJ (Brazil). Unidade de Negocio Exploracao e Producao da Bacia de Campos. Gerencia de Avaliacao de Blocos e Interpretacao Geologica e Geofisica]. E-mail:; Rostirolla, Sidnei Pires


    Lithostratigraphic studies of Ponta Grossa Formation (Devonian - Parana Basin) suggest the recognition of three members, denominated: Jaguariaiva Member, Tibagi Member and Sao Domingos Member. This work studies the formation as a whole, but predominantly the Tibagi Member, the most controversial, regarding its stratigraphic genesis. Differing from the other members, that are predominantly pelitic, the Tibagi Member has a sandy composition with the facies; distal storm, proximal storm, deltaic outlet bars and littoral drift currents. The disposition of these facies, formed in marine transitional environment, reveals deposition with a pro gradational array, beginning in shallow platformal environment, with strong storm influence, and covered by deltaic outlet bar deposits. Finally, the coastal drift currents process prevailed. Based on the facies analysis and the comparison between gamma-ray profiles of outcrops and geophysical profiles of wells, the formation was divided in two depositional sequences. In the upper sequence, where it is suggested that Tibagi Member sandstones represent deposits formed in a tract similar to a shelf edge systems tract. This system tract was used (elaborated for passive margin basins, and not for ramp type basins, as the Parana Basin), to have the possibility of obtaining good explanations to understand the deltaic progradation associated with the deposition of that interval, clarifying issues referring to the relative sea level behavior, to the sedimentary contribution, and to the stratigraphic pile up. Finally, comparisons were made with existing stratigraphic models, with the aim to establish a discussion on this important subject in order to promote new debate on the Ponta Grossa Formation stratigraphic sequences. (author)

  8. Petrogenesis of the crater-facies Tokapal kimberlite pipe, Indrāvati Basin, Central India

    N.V. Chalapathi Rao; B. Lehmann; B.K. Panwar; Alok Kumar; D. Mainkar


    New geochemical data of the crater-facies Tokapal kimberlite system sandwiched between the lower and upper stratigraphic horizons of the Mesoproterozoic Indrāvati Basin are presented. The kimberlite has been subjected to extensive and pervasive low-temperature alteration. Spinel is the only primary phase identifiable, while olivine macrocrysts and juvenile lapilli are largely pseudomorphed (talc-serpentine-carbonate alteration). However, with the exception of the alkalies, major element oxides display systematic fractionation trends; likewise, HFSE patterns are well correlated and allow petrogenetic interpretation. Various crustal contamination indices such as (SiO2 þ Al2O3 þ Na2O)/(MgO þ K2O) and Si/Mg are close to those of uncontaminated kimberlites. Similar La/Yb (79e109) of the Tokapal samples with those from the kimberlites of Wajrakarur (73e145) and Narayanpet (72e156), Eastern Dharwar craton, southern India implies a similarity in their genesis. In the discriminant plots involving HFSE the Tokapal samples display strong affinities to Group II kimberlites from southern Africa and central India as well as to‘transitional kimberlites’ from the Eastern Dharwar craton, southern India, and those from the Prieska and Kuruman provinces of southern Africa. There is a striking similarity in the depleted-mantle (TDM) Nd model ages of the Tokapal kimberlite system, Bastar craton, the kimberlites from NKF and WKF, Eastern Dharwar craton, and the Majhgawan diatreme, Bundelkhand craton, with the emplacement age of some of the lamproites from within and around the Palaeo-Mesoproterozoic Cuddapah basin, southern India. These similar ages imply a major tectonomagmatic event, possibly related to the break-up of the supercontinent of Columbia, at 1.3e1.5 Ga across the three cratons. The ‘transitional’ geochemical features displayed by many of the Mesoproterozoic potassic-ultrapotassic rocks, across these Indian cratons are inferred to be memories of the

  9. Middle Miocene coralline algal facies from the NW Transylvanian Basin (Romania)

    Chelaru, Ramona; Bucur, Ioan I.; Sǎsǎran, Emanoil; Bǎlc, Ramona; Tǎmas, Tudor


    s\\varan E., Bucur I.I., Bǎlc R., Tǎmas T. & Beldean C. (2011). Carbonate facies with rhodoliths from Vǎlenii Șomcutei (NW Transylvanian Basin). In: Bucur I.I. & Sǎs\\varan E. (eds) - 10th International Symposium on Fossil Algae, Cluj-Napoca, Abstract Book, p. 16. [2] Szakács A., Pécskay Z., Silye L., Balogh K., Vlad D. & Fülöp A. (2012). On the age of the Def Tuff, Transylvanian Basin (Romania). Geologica Carpathica, vol. 63(2), p. 139-148.

  10. Petrogenesis of the crater-facies Tokapal kimberlite pipe, Indrāvati Basin, Central India

    N.V. Chalapathi Rao


    Full Text Available New geochemical data of the crater-facies Tokapal kimberlite system sandwiched between the lower and upper stratigraphic horizons of the Mesoproterozoic Indrāvati Basin are presented. The kimberlite has been subjected to extensive and pervasive low-temperature alteration. Spinel is the only primary phase identifiable, while olivine macrocrysts and juvenile lapilli are largely pseudomorphed (talc-serpentine-carbonate alteration. However, with the exception of the alkalies, major element oxides display systematic fractionation trends; likewise, HFSE patterns are well correlated and allow petrogenetic interpretation. Various crustal contamination indices such as (SiO2 + Al2O3 + Na2O/(MgO + K2O and Si/Mg are close to those of uncontaminated kimberlites. Similar La/Yb (79–109 of the Tokapal samples with those from the kimberlites of Wajrakarur (73–145 and Narayanpet (72–156, Eastern Dharwar craton, southern India implies a similarity in their genesis. In the discriminant plots involving HFSE the Tokapal samples display strong affinities to Group II kimberlites from southern Africa and central India as well as to ‘transitional kimberlites’ from the Eastern Dharwar craton, southern India, and those from the Prieska and Kuruman provinces of southern Africa. There is a striking similarity in the depleted-mantle (TDM Nd model ages of the Tokapal kimberlite system, Bastar craton, the kimberlites from NKF and WKF, Eastern Dharwar craton, and the Majhgawan diatreme, Bundelkhand craton, with the emplacement age of some of the lamproites from within and around the Palaeo-Mesoproterozoic Cuddapah basin, southern India. These similar ages imply a major tectonomagmatic event, possibly related to the break-up of the supercontinent of Columbia, at 1.3–1.5 Ga across the three cratons. The ‘transitional’ geochemical features displayed by many of the Mesoproterozoic potassic-ultrapotassic rocks, across these Indian cratons are inferred to be

  11. Brittle–viscous deformation of vein quartz under fluid-rich low greenschist facies conditions

    H. J. Kjøll


    Full Text Available A coarse grained, statically crystallized quartz vein, embedded in a phyllonitic matrix, was studied by EBSD and optical microscopy to gain insights into the processes of strain localization in quartz deformed under low-grade conditions, broadly coincident with the frictional–viscous transition. The vein is from a high strain zone at the front of the Porsa Imbricate Stack in the Paleoproterozoic Repparfjord Tectonic Window in northern Norway. The vein was deformed under lower greenschist facies conditions during deformation along a large out-of-sequence phyllonitic thrust of Caledonian age. The host phyllonite formed at the expense of metabasalt wherein feldspar broke down to form interconnected layers of fine, synkinematic phyllosilicates. In the mechanically weak framework of the phyllonite, the studied quartz vein acted as a relatively rigid body deforming mainly by coaxial strain. Viscous deformation was initially accommodated by basal ⟨a⟩ slip of quartz during the development of a mesoscopic pervasive extensional crenulation cleavage. Under the prevailing boundary conditions, however, dislocation glide-accommodated deformation of quartz resulted inefficient and led to dislocation tangling and strain hardening of the vein. In response to hardening, to the progressive increase of fluid pressure and the increasing competence contrast between the vein and the weak foliated host phyllonite, quartz crystals began to deform frictionally along specific, optimally oriented lattice planes, creating microgouges along microfractures. These were, however, rapidly sealed by nucleation of new grains as transiently over pressured fluids penetrated the deforming system. The new nucleated grains grew initially by solution-precipitation and later by grain boundary migration. Due to the random initial orientation of the vein crystals, strain was accommodated differently in the individual crystals, leading to the development of remarkably different

  12. Insights on Coral Adaptation from Polyp and Colony Morphology, Skeletal Density Banding and Carbonate Depositional Facies

    Oehlert, A. M.; Hill, C. A.; Piggot, A. M.; Fouke, B. W.


    densities were measured in vertical cross-sections of each whole corallum using standard X-ray techniques utilizing a calibrated step wedge to portray banding and overall density. The combination of the stereoscope and X-ray analyses across spatial and temporal gradients provide insight into how coral reef carbonate depositional facies are affected by changes in key environmental parameters, such as increased pollution, or changing photosynthetic activity with depth or sea surface temperature fluctuations.

  13. Late Neogene sedimentary facies and sequences in the Pannonian Basin, Hungary

    Juhasz, E.; Phillips, L.; Muller, P.; Ricketts, B.; Toth-Makk, A.; Lantos, M.; Kovacs, L.O.


    This paper is part of the special publication No.156, The Mediterranean basins: Tertiary extension within the Alpine Orogen. (eds B.Durand, L. Jolivet, F.Horvath and M.Seranne). Detailed sedimentological, facies and numerical cycle analysis, combined with magnetostratigraphy, have been made in a number of boreholes in the Pannonian Basin, in order to study the causes of relative water-level changes and the history of the basin subsidence. Subsidence and infilling of the Pannonian Basin, which was an isolated lake at that time occurred mainly during the Late Miocene and Pliocene. The subsidence history was remarkably different in the individual sub-basins: early thermal subsidence was interrupted in the southern part of the basin, while high sedimentation rate and continuous subsidence was detected in the northeastern sub-basin. Three regional unconformities were detected in the Late Neogene Pannonian Basin fill, which represent 0.5 and 7.5 Ma time spans corresponding to single and composite unconformities. Consequently two main sequences build up the Late Neogene Pannonian Basin fill: a Late Miocene and a Pliocene one. Within the Late Miocene sequence there are smaller sedimentary cycles most probably corresponding to climatically driven relative lake-level changes in the Milankovitch frequency band. Considering the periods, the estimated values for precession and eccentricity in this study (19 and 370 ka) are close to the usually cited ones. In the case of obliquity the calculated period (71 ka) slightly deviates from the generally accepted number. Based on the relative amplitudes of oscillations, precession (sixth order) and obliquity (fifth order) cycles had the most significant impact on the sedimentation. Eccentricity caused cycles (fourth order) are poorly detectable in the sediments. The longer term (third order) cycles had very slight influence on the sedimentation pattern. Progradation, recorded in the Late Miocene sequence, correlates poorly in time

  14. La prima cosa da fare

    Franco Zagari


    Full Text Available The first thing to do to improve our cities quality, is to work on the propriety of public spaces, involving the communities interested in the choices and management of these places. Among many kinds of land government, the landscape approach is perhaps underestimated, but it has great capacity to redistribute quality and centrality throughout the city.

  15. Materias primas vs materia gris

    Fabio Aldemar Gómez Sierra


    Full Text Available Los alimentos y los combustibles, en la última década, sobre pasaron el límite de la demanda; la causa no es sólo la evolución demográfica, ni el cambio climático, también es el efecto de las emergentes y poderosas economías asiáticas, especialmente la China, que está aumentando la exigencia energética y consume más y mejores alimentos; 500 millones de ciudadanos chinos están en capacidad de requerirlos y de viajar por el mundo como turistas.

  16. Early Cretaceous Shallow-Water Platform Carbonates of the Bolkar Mountains, Central Taurides - South Turkey: Facies Analysis and Depositional Environments

    Solak, Cemile; Taslı, Kemal; Koç, Hayati


    The study area comprises southern non-metamorphic part of the Bolkar Mountains which are situated in southern Turkey, eastern part of the Central Taurides. The studied five outcrops form geologically parts of the tectonostratigraphic units called as allochthonous Aladag Unit and autochthonous Geyikdagi Unit. The aim of this study is to describe microfacies and depositional environments of the Bolkar Mountains Early Cretaceous shallow- water platform carbonates. The Lower Cretaceous is represented by continuous thick- bedded to massive dolomite sequence ranging from 100 to 150 meters thick, which only contains locally laminated limestone intercalations in the Yüğlük section and thick to very thick-bedded uniform limestones ranging from approximately 50 to 120 meters, consist of mainly laminated- fenestral mudstone, peloidal-intraclastic grainstone-packstone, bioclastic packstone- wackestone, benthic foraminiferal-intraclastic grainstone-packstone, ostracod-fenestral wackestone-mudstone, dasycladacean algal packstone-wackestone and ooidal grainstone microfacies. Based on a combination sedimantological data, facies/microfacies and micropaleontological (predominantly dasycladacean algae and diverse benthic foraminifera) analysis, it is concluded that Early Cretaceous platform carbonates of the Bolkar Mountains reflect a tidally affected tidal-flat and restricted lagoon settings. During the Berriasian- Valanginian unfavourable facies for benthic foraminifera and dolomitization were predominate. In the Hauterivian-early Aptian, the effect of dolomitization largely disappeared and inner platform conditions still prevailed showing alternations of peritidal and lagoon facies, going from peritidal plains (representing various sub-environments including supratidal, intertidal area, tidal-intertidal ponds and ooid bars) dominated by ostracod and miliolids, to dasycladacean algae-rich restricted lagoons-subtidal. These environments show a transition in the vertical and

  17. Paleotopographic controls on facies development in various types of braid-delta depositional systems in lacustrine basins in China

    Dong Feng


    Full Text Available Braid-delta depositional systems are widely developed in most continental basins in China. Research indicates that, for different types of braid delta, the facies sequence and association, which are critical to the prediction of the distribution of reservoirs, differ greatly. This study illustrates the differences in braid-delta depositional systems in terms of sedimentary characteristics, associated systems and reservoir distributions using three typical paleodeltas in western China: the Zhenbei delta of the upper Triassic Yanchang Formation in the Ordos Basin, the Yuanba delta of the upper Triassic Xujiahe Formation in the Sichuan Basin and the Jimsar delta of the upper Permian Wutonggou Formation in the Junggar Basin. A stratigraphic framework was established using seismic data, logs and cores by choosing stable mud sections as regional correlation markers and, topographies of these deltas were reconstructed based on the decompaction and paleobathymetric corrections. Based on both the paleotopography of these deltas and the differences of their sedimentary facies, these braided deltas can be classified into two systems: steep-gradient braid-delta-turbidite system and low-gradient braid-delta-lacustrine system. Moreover, the low-gradient braid-delta-lacustrine system can be further divided into interfingered and sharp contact sub-types according to the contact relation between the delta sands and lacustrine muds. This study shows that the paleotopography of basin margins strongly controls the accommodation as braid deltas prograde into lacustrine basins and, influences the location of the shoreline in response to changes in the lake level. Furthermore, paleotopography plays a significant role in facies and reservoir distribution which is important for petroleum exploration and development.

  18. Annual variation of topography and surface sedimentary facies of 2014~2015 years in the Gochang coast, southwestern Korea

    Ryang, Woo Hun; Kang, Sol Ip


    The Gochang coast is characterized by macro-tide, open-coast, linear shoreline, and sand substrates. It is located on the southwestern coast of Korea along the eastern part of the Yellow Sea, comprising the Donghori, Gwangseungri, and Myengsasipri areas from the north to south. This study has investigated annual variation of topography, accumulation rates, surface sediment texture, and sedimentary facies during 2014~2015. In the intertidal area, topographic elevation and surface sediments were measured and sampled at 63 sites during the 7 seasons from winter (Feb.) in 2014 to summer (Aug.) in 2015. Surface sediments of the subtidal area were sampled at 110 and 119 sites with 500 m interval for the two seasons of winter and summer in 2015, respectively. In the Gochang coast of 2014~2015 years, surface sedimentary facies represent a fining trend from shoreline to offshore. Area distribution of sedimentary facies also becomes finer from the north to south. Annual accumulation rates of the Gochang intertidal area represent av. -0.081m/yr from winter to winter, av. -0.018m/yr from spring to spring, av. -0.019m/yr from summer to summer during 2014~2015, respectively. It was indicative of an erosion-dominated environment. Keywords: macro-tide, open-coast, surface sediment, accumulation rate, Gochang coast Acknowledgements: This study was supported by the research grant from the Korean Ministry of Oceans and Fisheries (PJT200538). This presentation is an interim result of the coastal research program in the study area.

  19. Facies architecture and high-resolution sequence stratigraphy of an Upper Cretaceous platform margin succession, southern central Pyrenees, Spain

    Pomar, Luis; Gili, Eulalia; Obrador, Antonio; Ward, William C.


    Excellent exposures of Upper Cretaceous (Santonian) carbonate platforms on the northern flank of Sant Corneli anticline (southern central Pyrenees) provide detailed information of facies architecture in both depositional strike and dip directions. Basic accretional units are differentiated by facies contrast across mappable surfaces. These surfaces do not show clear evidence of subaerial erosion and are correlated basinward with bedding planes across which there are subtle changes in skeletal composition. Two types of basic accretional units have been identified based on bedding patterns, internal facies architecture and skeletal composition: (1) Rudist buildups consist of a rudist and coral belt at the platform margin, passing landward into a slender-hippuritid lithosome, locally overlain by a bioclastic blanket that passes basinward, into bioclastic "apron-like" clinobeds and into fine-grained packstone/wackestone. (2) Calcarenite wedges consist of yellow-brown, benthic-foraminifer-rich grainstones to grain-dominated packstones, with scattered rudist shells and small coral colonies, passing basinward into mud-dominated packstones to wackestones, with variable siliciclastic content (quartz sand to silt and clay). Rudist buildups and calcarenite wedges alternate, although not rhythmically. These changes in platform skeletal composition reflect changes in the dominant type of carbonate-producing biota independently of the changes in accommodation. Both types of basic accretional units: rudist buildups and calcarenite wedges, form simple sequences and parasequences according to internal lithofacies arrangement and inferred sea-level cyclicity (cycles or paracycles). High-frequency sea-level cyclicity fits in the Milankovitch frequency band. Long-term changes in accommodation governing aggradation, progradation and backstepping of basic sequences and parasequences reflect tectonic influence rather than long-term changes in eustatic sea level.

  20. First sign of Clethrionomys glareolus in the Po valley plain / Prima segnalazione in Pianura Padana di Clethrionomys glareolus

    Luis Nieder


    Full Text Available Abstract The presence of Clethrionomys glareolus (Schreber, 1790 populations is reported in the Po valley, formerly considered outside the distribution area of the species. An initial series of captures was made in the high-water area of the Po near S. Nazzaro (Monticelli d'Ongina - PC following with research was extended along the river's banks in Emilia both upstream and downstream. The search for this species was carried out by analysing food pellets relating to Strix aluco, Tyto alba e Athene noctua, thought to be among the most common predators of these intensive herbaceous and arboreal agricultural biocoenosis. The information we gathered was integrated with other Authors' unpublished and bibliographical data. The presence of C. glareolus was noted in habitats quite different from the expected ones. Many of the problems raised by the presence of this species in "islands" along the main body of the Po river and its tributaries, and by its presumed absence from particulary suitable environments such as the Carrega woods, the Ticino park and Mesola wood must still be resolved. Riassunto Viene segnalata la presenza di popolazioni di Clethrionomys glareolus (Schreber 1790 nella pianura Padana precedentemente considerata al di fuori dell'areale della specie. A partire da una prima serie di catture nell'area golenale del Po presso S. Nazzaro (Monticelli d'Ongina - PC, si è successivamente proceduto ad allargare l'area di ricerca lungo l'argine emiliano del Po, sia a monte sia a valle. La ricerca di questa specie è avvenuta tramite l'analisi di boli alimentari relativi a Strix aluco, Tyto alba e Athene noctua, ritenuti tra i più comuni predatori di queste biocenosi agricole intensive erbacee ed arboree. I dati da noi raccolti sono stati integrati con quelli bibliografici e inediti di altri Autori. È stata riscontrata la presenza


    Teguh Agung Samudra


    Full Text Available Corporate Social Responsibility (CSR is an idea that corporate social responsibility was born to answer the problem posed in the midst of society. CSR is expected to help the development process by increasing the role of the company for the welfare of the community, especially communities around the company. The purpose of this study is to get the concept CSR program of PT. Kalimantan Prima Persada (PT KPP in accordance with the needs of the community, social public opinion regarding the company's existence and analyze the relationship between CSR programs to increase revenue and public education. The research was carried out by simple random sampling with the number of respondents 60 families (family head. Respondents are the beneficiaries of CSR in 3 (three villages, namely Binderang, Bitahan Baru and Bitahan. Analysis of the data with the three stages, namely to determine the public perception was measured using a Likert scale (Allen and Seaman, 2007 and categorized into three major groups, namely good, average, and bad. Analyzed for levels of perception using calculating Value Perception (NP, the classification category is based on the total score obtained by the respondents for each aspect presented on the questionnaire. For data analysis the factors that influence the perception of the community in the role of CSR PT. KPP using multiple regression analysis (Multiple Linear Regression Analysis processed through the SPSS program (Statistical Program for Social Science. The results showed that the concept of CSR Program PT. KPP has had planning documents and strategies in the CSR Program SOP system so that programs that have been implemented with the aim to empower people and can fit the needs of the community. As many as 15% of respondents admitted that the existence of a company's CSR program is quite good and affect the existence of the company, while the respondents who perception bad as many as 10%. Income and household education in the

  2. Determinação do teor de princípios ativos em matérias-primas vegetais Determination of active principles in vegetable raw materials

    Maria Teresa F. Bara


    Full Text Available Castanha-da-índia (Aesculus hippocastanum L., hipérico (Hypericum perforatum L., guaraná (Paullinia cupana H.B.K. e ginkgo (Ginkgo biloba L. fazem parte de formulações de medicamentos fitoterápicos muito comercializados no Brasil. Neste trabalho foi avaliada a qualidade de amostras de pós e extratos destas plantas. Para a determinação do teor de princípios ativos foram aplicados métodos farmacopéicos ou citados na literatura científica e os resultados demonstraram serem adequados para a análise destes produtos farmacêuticos. Verificou-se que 60% das amostras analisadas de guaraná e ginkgo estavam em desacordo com as especificações farmacopéicas ou as declaradas pelos laudos dos fabricantes, em relação ao teor de princípios ativos. Além disso, 100% e 20%, respectivamente, das amostras de hipérico e de castanha-da-índia apresentaram teores abaixo das especificações. Os dados obtidos mostraram ser de grande importância e necessidade a implementação de técnicas quantitativas no controle de qualidade físico-químico de matérias-primas vegetais.Pharmaceutical preparations containing Aesculus hippocastanum L., Hypericum perforatum L., Paullinia cupana H.B.K. and Ginkgo biloba L. have large market. In this work the quality of the powder or extracts of these plants were evaluated. Pharmacopoeia methods or those cited on cientific literature for quantification of active substances were employed and the data showed them to be adequate for these analyses. The analytical results demonstrated that 60% of the samples of P. cupana and G. biloba, and 100% and 20%, respectively of samples of H. perforatum and A. hippocastanum were not in agreement with the specifications. This analysis showed to be valuable for herbal medicines quality control.

  3. Evaluación de distintas materias primas para la producción de almácigo de tomate

    Fernando Richmond


    Full Text Available Se evaluaron mezclas de materias primas naturales en diferentes proporciones y en el siguiente orden: fibra de coco (Cocos nucifera, aserrín de melina (Gmelina arborea y abono orgánico Coope Victoria, para utilizarlos como sustrato en la etapa de almácigo de tomate híbrido FBM-17. Se hicieron mezclas entre sí de fibra de coco y aserrín de melina en diferentes proporciones (30%, 40% y 50% de cada material, para un total de 9 tratamientos; el abono orgánico se agregó para completar el 100%. Se evaluó la variable porcentaje de germinación 7 días después de la siembra (dds y porcentaje de plantas trasplantables a 27 dds en cada parcela útil. Además, en 10 plántulas escogidas al azar dentro de cada parcela útil (a 27 dds se evaluó: altura de plántula, grosor del tallo, peso seco de raíz y parte aérea, relación raíz/parte aérea y calidad de adobe. Del total de tratamientos, los mayores valores para las variables evaluadas se obtuvieron en los 3 tratamientos donde la proporción de aserrín de melina fue 30%, junto con el tratamiento de 40% de fibra de coco + 40% de aserrín de melina + 20% de abono orgánico Coope Victoria; entre ellos el sustrato con tendencia a dar mejores resultados en todas las variables fue la mezcla 30-30-40. Los valores inferiores para las variables evaluadas se obtuvieron en el tratamiento donde no se incluyó en la mezcla abono orgánico (50-50-0, excepto para las variables porcentaje de germinación y relación raíz/parte aérea. La inclusión de abono orgánico en la mezcla del sustrato favoreció la obtención de valores satisfactorios.

  4. Floristic composition and structure of a peat swamp forest in the conservation area of the PT National Sago Prima, Selat Panjang, Riau, Indonesia

    Yusi Rosalina


    Full Text Available We studied the floristic composition and structure of the logged-over peat swamp forest in the  PT National Sago Prima of PT Sampoerna Agro Tbk. group for future management of the conservation area that has been  set aside by the company.  In January - February 2012, 25 quadrats of 20 m × 20 m were laid out systematically along a transect,  thus covering a sampled area of 1-ha.  The results showed that the study site was a regenerating and developing secondary  peat swamp forests having high plant species richness. The total number of species recorded was 73 species of 38 families, consisting of 49 species (30 families of trees (DBH≥ 10 cm , 42     species (24 families of saplings (H > 1.5 m and DBH < 10 cm and 41 species (27 families of seedlings and undergrowth. Tree density was 550 individuals/ha and total tree basal area was 18.32 m2. The Shannon-Wiener’s Diversity Index for trees was high  (3.05  Two tree species with the highest Importance Values (IV were Pandanus atrocarpus (IV = 45.86 % and Blumeodendron subrotundifolium (22.46%. The tree families with the highest IV were Pandanaceae (45.86, Myrtaceae (40.37 and Dipterocarpaceae (39.20.  Forest structure dominated by trees with a diameter below 20 cm amounting to 408 trees/ha (74.05%. D and E strata with height of less than 20 m, and density of 431 trees/ha (78.36%. Jaccard Similarity index among species, showed strong association between Pandanus atrocarpus and Blumeodendron subrotundifolium and based on this association combined with high IVs, the two parameters of species characterized the forest, hence the forest  could be designated as the Pandanus atrocarpus–Blumeodendron   subrotundifolium association. Primary forest species with high economic values were still present in the forest. Eleven species can be included in the IUCN Red List, of which Shorea rugosa is in the category of Critically Endangered,  Shorea teysmanniana Endangered and

  5. Regional variation in the Amitsoq gneisses related to crustal levels during late Archean granulite facies metamorphism: Southern west Greenland

    Nutman, A. P.; Bridgwater, D.; Mcgregor, V. R.


    The dominant lithology at Kangimut sangmissoq is described as nebulitic tonalitic gneiss containing highly distended plagioclase phyric amphibolites. The gneiss amphibolite complex was intruded by Nuk gneiss between 3.05 and 2.90 Ga and later (2.6 to 2.7 Ga) by post granulite facies granitoid sheets. The amphibolites are though to be Ameralik dikes and the older gray gneiss are then Amitsoq by definition. The problem arises when the isotopic data are considered, none of which indicate rocks older that about 3.0 Ga.

  6. Visual Mapping of Sedimentary Facies Can Yield Accurate And Geomorphically Meaningful Results at Morphological Unit to River Segment Scales

    Pasternack, G. B.; Wyrick, J. R.; Jackson, J. R.


    Long practiced in fisheries, visual substrate mapping of coarse-bedded rivers is eschewed by geomorphologists for inaccuracy and limited sizing data. Geomorphologists perform time-consuming measurements of surficial grains, with the few locations precluding spatially explicit mapping and analysis of sediment facies. Remote sensing works for bare land, but not vegetated or subaqueous sediments. As visual systems apply the log2 Wentworth scale made for sieving, they suffer from human inability to readily discern those classes. We hypothesized that size classes centered on the PDF of the anticipated sediment size distribution would enable field crews to accurately (i) identify presence/absence of each class in a facies patch and (ii) estimate the relative amount of each class to within 10%. We first tested 6 people using 14 measured samples with different mixtures. Next, we carried out facies mapping for ~ 37 km of the lower Yuba River in California. Finally, we tested the resulting data to see if it produced statistically significant hydraulic-sedimentary-geomorphic results. Presence/absence performance error was 0-4% for four people, 13% for one person, and 33% for one person. The last person was excluded from further effort. For the abundance estimation performance error was 1% for one person, 7-12% for three people, and 33% for one person. This last person was further trained and re-tested. We found that the samples easiest to visually quantify were unimodal and bimodal, while those most difficult had nearly equal amounts of each size. This confirms psychological studies showing that humans have a more difficult time quantifying abundances of subgroups when confronted with well-mixed groups. In the Yuba, mean grain size decreased downstream, as is typical for an alluvial river. When averaged by reach, mean grain size and bed slope were correlated with an r2 of 0.95. At the morphological unit (MU) scale, eight in-channel bed MU types had an r2 of 0.90 between mean

  7. Petrological and zircon evidence for the Early Cretaceous granulite-facies metamorphism in the Dabie orogen, China

    Gao, Xiao-Ying; Zhang, Qiang-Qiang; Zheng, Yong-Fei; Chen, Yi-Xiang


    An integrated study of petrology, mineralogy, geochemistry, and geochronology was carried out for contemporaneous mafic granulite and diorite from the Dabie orogen. The results provide evidence for granulite-facies reworking of the ultrahigh-pressure (UHP) metamorphic rock in the collisional orogen. Most zircons from the granulite are new growth, and their U-Pb ages are clearly categorized into two groups at 122-127 Ma and 188 ± 2 Ma. Although these two groups of zircons show similarly steep HREE patterns and variably negative Eu anomalies, the younger group has much higher U, Th and REE contents and Th/U ratios, much lower εHf(t) values than the older group. This suggests their growth is associated with different types of dehydration reactions. The older zircon domains contain mineral inclusions of garnet + clinopyroxene ± quartz, indicating their growth through metamorphic reactions at high pressures. In contrast, the young zircon domains only contain a few quartz inclusions and the garnet-clinopyroxene-plagioclase-quartz barometry yields pressures of 4.9 to 12.5 kb. In addition, the clinopyroxene-garnet Fe-Mg exchange thermometry gives temperatures of 738-951 °C. Therefore, the young zircon domains would have grown through peritectic reaction at low to medium pressures. The younger granulite-facies metamorphic age is in agreement not only with the adjacent diorite at 125 ± 1 Ma in this study but also the voluminous emplacement of coeval mafic and felsic magmas in the Dabie orogen. Mineral separates from both mafic granulite and its adjacent diorite show uniformly lower δ18O values than normal mantle, similar to those for UHP eclogite-facies metaigneous rocks in the Dabie orogen. In combination with major-trace elements and zircon Lu-Hf isotope compositions, it is inferred that the protolith of mafic granulites shares with the source rock of diorites, both being a kind of mafic metasomatites at the slab-mantle interface in the continental subduction channel

  8. Las almas indisciplinadas: comentario crítico y estilístico de Plut., De facie 945B

    Luisa Lesage Gárriga


    Full Text Available El mito escatológico que aparece al final del tratado de Plutarco De facie in orbe lunae todavía a día de hoy presenta problemas textuales y de interpretación que deben ser estudiados. Con este análisis del texto, que parte de estudios de crítica textual y crítica literaria y estilística, intento arrojar algo de luz sobre un pasaje que versa sobre el destino de las almas licenciosas.

  9. Los cazadores recolectores pampeanos y sus rocas : La obtención de materias primas líticas vista desde las canteras arqueológicas del centro de Tandilia

    Colombo, Mariano


    Las investigaciones arqueológicas realizadas en el marco de esta tesis, estuvieron orientadas a comprender las actividades y procesos vinculados con la extracción de rocas por parte de los grupos cazadores y recolectores pampeanos durante épocas pasadas. Para ello los focos de análisis más específicos fueron los sitios de obtención de materias primas líticas (canteras y talleres), en especial aquellos en que se explotaron unas de las rocas más ampliamente utilizadas en el contexto regional pa...

  10. Metodología para el cálculo de la prima ajustada por riesgo que debe aportar una institución del sistema cooperativo, por concepto de seguro de depósitos

    Rosero Zurita, Josseth Marcela


    El objetivo de la presente tesis es establecer una metodología apropiada que logre determinar el valor de la prima ajustada por riesgo que debe aportar una IFI, la cual deberá tener la connotación de estar fijada entre 0 y 3,5 por mil anual. Rango definido por la Ley de Creación de la Red de Seguridad Financiera. Para desarrollar la metodología se ha considerado pertinente dividir el estudio en cuatro capítulos: El primero tiene como propósito revisar los hechos históricos de mayor releva...

  11. Análisis para el uso eficiente de recursos y revisión de políticas en una bodega de materias primas, para la reducción de los niveles de inventarío

    Yong Cruz, Carlos; Sarzosa C., Rodrigo


    La presente tesis de grado pretende realizar un análisis de los distintos procesos de la administración de inventarios que se desarrollan en las bodegas de materia prima, material de empaque y de exportación de producto terminado. Este estudio va a ser realizado en las instalaciones de una empresa líder del mercado en las divisiones de cuidado personal y del hogar. La empresa ha identificado que las actuales políticas y niveles de inventario generan un alto valor en la inversión del d...

  12. Nódulos opalinos en facies marginales del salar Olaroz (Puna Argentina

    Alonso, R.


    Full Text Available This article reports the results of a petrological and geochemical study of silica nodules from Quaternary alluvial fallS of the Olaroz Salar. The nodules are mainly constituted by C-T opal, d. (101 spacing to 4,11 A, implying a high-disorder; this is commonly observed in opa! rocks formed in near surface environments, without burial and heating. The chemical composition of the nodules is anomalous when compared with other typical silica-rocks formed in arid continental closed basin, without any eruptive environments (for instance the Cuenca del Tajo in Spain. The siliceous nodules do not have the characteristics of the silcretes and are not associated to the evaporitic facies of the salar. Their genesis is probably related to contamination of groundwater of the alluvial fan with high-silica thermal water. The C-T opal would thus precipitate by either displacing tbe terrigenous host-rock or replacing previous ulexite nodules.Se realiza un estudio petrológico y geoquímico de los nódulos silíceos que se encuentran incluidos en sedimentos terrígenos cuaternarios de la Cuenca de Olaroz (La Puna, Argentina. Estos nódulos se localizan en abanicos aluviales que aparecen encajados, debido a los cambios en el nivel de base que se produce desde el Pleistoceno a la actualidad, durante la evolución de los cuerpos lacustres a salares. Un estudio mediante DRX revela que son rocas constituidas por ópalo C-T, con un espaciado (101 a 4,11 A, que implica un grado de desorden alto, típico de las rocas silíceas formadas en superficie y que no han sufrido enterramiento ni influencia térmica. Su composición química es anómala si se compara con rocas silíceas continentales formadas en ambiente endorreico y fuera de un marco volcánico (Mioceno de la Cuenca del Tajo. No poseyendo características de silcretas y no estando asociadas a la sedimentación evaporítica de los salares, se considera la influencia de aguas termales. La contaminación local y en

  13. Brittle-viscous deformation of vein quartz under fluid-rich low greenschist facies conditions

    Jørgen Kjøll, Hans; Viola, Giulio; Menegon, Luca; Sørensen, Bjørn


    A coarse grained, statically crystallized quartz vein with a random CPO, embedded in a phyllonitic matrix, was studied by optical microscopy, SEM imaging and EBSD to gain insights into the processes of strain localization in quartz deformed under low greenschist facies conditions at the frictional-viscous transition. The vein is located in a high strain zone at the front of an imbricate stack of Caledonian age along the northwesternmost edge of the Repparfjord Tectonic Window in northern Norway. The vein was deformed within the Nussirjavrri Fault Zone (NFZ), an out-of-sequence thrust with a phyllonitic core characterized by a ramp-flat-ramp geometry, NNW plunging stretching lineations and top-to-the SSE thrusting kinematics. Deformation conditions are typical of the frictional-viscous transition. The phyllonitic core formed at the expense of metabasalt wherein feldspar broke down to form interconnected layers of fine, synkinematic phyllosilicates. In the mechanically weak framework of the phyllonite, the studied quartz vein acted as a relatively rigid body deforming mainly by coaxial strain. Viscous deformation, related to the development of a mesoscopic pervasive extensional crenulation cleavage, was accommodated within the vein initially by basal slip of suitably oriented quartz crystals, which produced e.g. undulose extinction, extinction bands and bulging grain boundaries. In the case of misoriented quartz crystals, however, glide-accommodated dislocation creep resulted soon inefficient and led to localized dislocation tangling and strain hardening. In response to 1) hardening, 2) progressive increase of fluid pressure within the actively deforming vein and 3) increasing competence contrast between the vein and the surrounding weak, foliated phyllonitic fault core, quartz crystals began to deform frictionally along specific lattice planes oriented optimally with respect to the imposed stress field. Microfaulting generated small volumes of gouge along

  14. Large Early Permian eruptive complexes in northern Saxony, Germany: Volcanic facies analysis and geochemical characterization

    Hübner, Marcel; Breitkreuz, Christoph; Repstock, Alexander; Heuer, Franziska


    In the course of formation of extensional basins during the Early Permian a widespread volcanic activity led to the deposition of volcanic and volcanosedimentary units in Saxony (Walter 2006, Hoffmann et al. 2013). Situated east of Leipzig, the North Saxonian Volcanic Complex (NSVC) hosts two large caldera complexes, the Rochlitz and Wurzen Volcanic Systems, with diameters of 90 and 52 km, respectively. Volume estimates (> 1000 km3) qualify these as supereruptions according to Mason et al. (2004). In addition to the large caldera systems, the NSVC hosts several small pyroclastic flow deposits ranging from crystal-poor (e.g. Cannewitz and vitrophyric Ebersbach ignimbrites) to crystal-rich units (Wermsdorf and Dornreichenbach ignimbrites). Additionally rhyolitic lava and subvolcanic units are present. The Chemnitz basin (Schneider et al. 2012), located to the south of the NSVC, harbours caldera-outflow facies deposits of the Rochlitz eruption (Fischer 1991), i.e. the partially vitrophyric Planitz ignimbrite. The Rochlitz and Wurzen caldera-fill ignimbrites exhibit relatively high crystal contents with maxima up to 52 and 58 vol.-%, for corresponding 66 and 68 wt.-% SiO2. This is comparable with the 'monotonous intermediates' (Hildreth 1981) in the Cenozoic western USA investigated by Huber et al. (2012). In contrast, the Planitz ignimbrite in the Chemnitz basin reveals predominantly crystal-poor pyroclastics ( 70 analyses), and mineral geochemistry to reconstruct the eruption history and magma genesis of this large Late Paleozoic magmatic complex in Central Europe. Volcanic textures and geochemical trends indicate magma mingling and mixing to have been important during the formation of the Wurzen caldera system. Geothermometric and -barometric calculations based on composition of pyroxene and feldspar suggest deeply seated crustal magma chambers for the NSVC and the Planitz ignimbrite. Fischer, F. (1991): Das Rotliegende des ostthüringisch-westsächsischen Raumes

  15. Classification et clé de détermination des faciès d'écoulements en rivières de montagne



    Full Text Available La diversité hydromorphodynamique de 294 faciès d'écoulement appartenant à 15 rivières des Pyrénées a été analysée. A partir d'une Analyse Factorielle des Correspondances Multiples et d'une classification hiérarchique sur les coordonnées des individus, 6 groupes principaux puis 18 sous-groupes de faciès d'écoulement ont pu être différenciés. Une clé de détermination des faciès d'écoulement pour rivière de montagne est proposée. Cinq niveaux de discrimination successifs, quantitatifs ou qualitatifs, permettent d'identifier sur le terrain les 18 sous-groupes de faciès d'écoulement. La validité écologique de cette classification de faciès a été testée sur les biomasses et densités de truites ainsi que sur les densités de frayères. L'appartenance aux 18 sous-groupes explique de 45,6 % de la variabilité des biomasses totales à 18,8 % (p<0.05 de la variabilité des biomasses d'alevins (p<0.05.

  16. Protolith age of Santa Maria Chico granulites dated on zircons from an associated amphibolite-facies granodiorite in southernmost Brazil.

    Hartmann, Léo A; Liu, Dunyi; Wang, Yenbin; Massonne, Hans-Joachim; Santos, João O S


    U-Pb dating of zircon was undertaken with the Beijing SHRIMP II (sensitive high resolution ion microprobe) on anamphibolite facies granodiorite and an almandine-albite granulite from the Santa Maria Chico Granulitic Complex, southern Brazilian Shield. This work was also done to unravel protolith ages which are often hidden in the array of partly reset data. The obtained metamorphic ages of the granodiorite gneiss and the granulite are 2035 +/- 9 Ma and 2006 +/- 3 Ma, respectively. These data are within the range of metamorphic ages determined in previous studies (2022 +/- 18 Ma and 2031 +/- 40 Ma). However, protolith ages for the granodiorite (2366 +/- 8 Ma) and the granulite (2489 +/- 6 Ma) were obtained which are outside the previously recognized range (> 2510-2555 Ma). The magmatic protolith age of the granodiorite refers to a previously little known magmatic event in the shield. Further investigations may demonstrate that amphibolite facies zircon crystals are useful as a window into geological events in associated granulites, because zircon ages are blurred in the studied granulites.

  17. Facies, dissolution seams and stable isotope compositions of the Rohtas Limestone (Vindhyan Supergroup) in the Son valley area, central India

    S Banerjee; S K Bhattacharya; S Sarkar


    The early Mesoproterozoic Rohtas Limestone in the Son valley area of central India represents an overall shallowing-upward carbonate succession. Detailed facies analysis of the limestone reveals outer- to inner-shelf deposition in an open marine setting. Wave-ripples, hummocky cross strat- ifications and edgewise conglomerates argue against a deep marine depositional model for the Rohtas Limestone proposed earlier. Stable isotope analysis of the limestone shows that 13C and 18O values are compatible with the early Mesoproterozoic open seawater composition. The ribbon limestone facies in the Rohtas Limestone is characterized by micritic beds, each decoupled in a lower band enriched and an upper band depleted in dissolution seams. Band-wise isotopic analysis reveals systematic short-term variations. Comparative enrichment of the heavier isotopes in the upper bands is attributed to early cementation from sea water and water derived from the lower band undergoing dissolution because of lowering of pH at depth. The short-term positive shifts in isotopic compositions in almost every upward gradational transition from a seamed band to a non-seamed band support the contention that dissolution seams here are of early diagenetic origin, although their formation was accentuated under overburden pressure.

  18. Sedimentary facies and hydrocarbon accumulation in the Third member of Shahejie Formation in Beijing-Tianjin Depression

    Jin, X.; Zhang, Z.


    The exploration practice in the Beijing-Tianjin area shows that the key point of improving seismic interpretation level in a complex district lies in the high accuracy of seismic work, extraction of available seismic information and the use of the comprehensive interpretation method basing on both structure interpretation and seismic stratigraphy. This paper presents the geological interpretation results of analyzing the Third member of Shahejie Formation in Beijing-Tianjin Depression by using the method stated above. It describes the seismic facies, sedimentary facies as well as the generation, accumulation and distribution of hydrocarbons, and points out that the lower part of the member is a subaqueous fan and point bar deposit, while the middle part is a fan-delta deposit. According to the thermo-evolution-profile and TTI estimated, it is assumed that the lower part of the member is source rock with sandstone development and is also a very good reservoir rock because of having two sets of source rock reservoir and seal rock. Having structures such as Jiuzhou anticline and its down dip and Liuquan fault structure, it is favorable for hydrocarbon accumulation. 4 figures.

  19. Protolith age of Santa Maria Chico granulites dated on zircons from an associated amphibolite-facies granodiorite in southernmost Brazil

    Hartmann, Leo A. [Universidade Federal do Rio Grande do Sul (UFRGS), Porto Alegre, RS (Brazil). Inst. de Geociencias; Liu, Dunyi; Wang, Yenbin [Chinese Academy of Geological Sciences, Beijing (China); Massonne, Hans-Joachim [Universitaet Stuttgart (Germany). Inst. fuer Mineralogie und Kristallchemie; Santos, Joao O.S. [University of Western Australia, Perth, WA (Australia). Centre for Global Targeting


    U-Pb dating of zircon was undertaken with the Beijing SHRIMP II (sensitive high resolution ion microprobe) on an amphibolite facies granodiorite and an almandine-albite granulite from the Santa Maria Chico Granulitic Complex, southern Brazilian Shield. This work was also done to unravel protolith ages which are often hidden in the array of partly reset data. The obtained metamorphic ages of the granodiorite gneiss and the granulite are 2035 {+-} 9 Ma and 2006 {+-} 3 Ma, respectively. These data are within the range of metamorphic ages determined in previous studies (2022 {+-} 18 Ma and 2031 {+-} 40 Ma). However, protolith ages for the granodiorite (2366 {+-} 8 Ma) and the granulite (2489 {+-} 6 Ma) were obtained which are outside the previously recognized range (> 2510-2555 Ma). The magmatic protolith age of the granodiorite refers to a previously little known magmatic event in the shield. Further investigations may demonstrate that amphibolite facies zircon crystals are useful as a window into geological events in associated granulites, because zircon ages are blurred in the studied granulites. (author)

  20. The changing microstructural arrangement of graphite during deformation and hydrothermal alteration of amphibolite-facies mylonite, Alpine Fault, New Zealand.

    Kirilova, M.; Toy, V.; Timms, N.; Craw, D.; Little, T. A.; Halfpenny, A.; Beyssac, O.


    Graphitisation in a convergent plate boundary setting, such as the Alpine Fault, New Zealand, is associated both with fault weakening and orogenic gold mineralisation. Previously, these processes have been investigated in rocks that experienced mineralisation at maximum of greenschist-facies conditions. However, metals are most mobile at upper greenschist- to amphibolite-facies. We examine the microstructural record of mobilisation of graphite at these conditions due to dislocation and diffusion creep in the Alpine Fault zone and as a function of varying shear strain magnitude. We have mapped graphite distribution across a strain gradient in samples, recovered from Deep Fault Drilling Project (DFDP) boreholes, by using reflected light and scanning electron microscopy. Raman spectrometry was used to determine the degree of maturity of the carbonaceous material. In the schists and protomylonites, graphite occurs as very fine (1-5μm), dusty grains, dispersed as inclusions in the main mineral phases (quartz, anorthite, muscovite, biotite). Further into the mylonite zone, the modal proportion of graphite increases and it forms clusters and trains, aligned with the foliation. In the brittlely-deformed rocks (cataclasites and gouges on or near the fault principal slip zone) graphite is most abundant (Schleicher et al., in press. N.Z.J.Geol&Geophys). We thus infer hydrothermal enrichment caused graphite remobilization, re-deposition, and enrichment in structurally controlled microstructural sites. We will discuss implications of these microstructural and mineralogical changes for strain localisation and deformation-induced permeability.

  1. Sedimentary facies reconstruction and kinematic restoration of tight gas fields. Studies from the Upper Permian in Northwestern Germany

    Vackiner, Anna Alexandra [RWTH Aachen Univ. (Germany). Energy and Mineral Resources Group


    Outstanding Ph.D. thesis nominated for a Springer Theses Prize by the RWTH Aachen University, Germany. A multi-disciplinary study with application in the oil and gas industry. Approx. 60 color figures. The thesis of Anna Alexandra Vackiner focuses on the geometric architecture and tectonic evolution of the Permian series, combining seismic interpretation (3D block), field studies in an analogue basin (Panamint Valley in California), as well as 2D restoration of representative cross sections through time in order to illustrate the complex interaction between multiphase extension, inversion and salt diapirism. It will be of major interest for exploration geologists involved in tectonically complex areas. - Francois Roure, August 2012 This thesis improves the understanding and localization of the Upper Rotliegend II tight gas reservoir rock facies. It provides insights into the detailed Upper Rotliegend II palaeo-topography and local tectonically induced sediment thickness changes prior to a multi-phase tectonic overprinting. The research presented in this study further focuses on the tectonically induced synsedimentary facies distribution in transtensional continental settings on the basis of a comparison with a modern field analogue, which enables a detailed analysis of the reservoir rock's distribution and its properties. The study is rounded off with an analysis of the influence of the multiphase tectonic overprinting on the mature Upper Rotliegend II reservoir rocks.

  2. Preservation of large titanosaur sauropods in overbank fluvial facies: A case study in the Cretaceous of Argentina

    González Riga, Bernardo J.; Astini, Ricardo A.


    Patagonia exhibits a particularly abundant record of Cretaceous dinosaurs with worldwide relevance. Although paleontological studies are relatively numerous, few include taphonomic information about these faunas. This contribution provides the first detailed sedimentological and taphonomical analyses of a dinosaur bone quarry from northern Neuquén Basin. At Arroyo Seco (Mendoza Province, Argentina), a large parautochthonous/autochthonous accumulation of articulated and disarticulated bones that represent several sauropod individuals has been discovered. The fossil remains, assigned to Mendozasaurus neguyelap González Riga, correspond to a large (18-27-m long) sauropod titanosaur collected in the strata of the Río Neuquén Subgroup (late Turoronian-late Coniacian). A taphonomic viewpoint recognizes a two-fold division into biostratinomic and fossil-diagenetic processes. Biostratinomic processes include (1) subaerial biodegradation of sauropod carcasses on well-drained floodplains, (2) partial or total skeletal disarticulation, (3) reorientation of bones by sporadic overbank flows, and (4) subaerial weathering. Fossil-diagenetic processes include (1) plastic deformation of bones, (2) initial permineralization with hematite, (3) fracturing and brittle deformation due to lithostatic pressure; (4) secondary permineralization with calcite in vascular canals and fractures, and (5) postfossilization bone weathering. This type of bone concentration, also present in Rincón de los Sauces (northern Patagonia), suggests that overbank facies tended to accumulate large titanosaur bones. This taphonomic mode, referred to as "overbank bone assemblages", outlines the potential of crevasse splay facies as important sources of paleontological data in Cretaceous meandering fluvial systems.

  3. Sequence Stratigraphy and Sedimentary Facies in the Lower Member of the Permian Shanxi Formation, Northeastern Ordos Basin, China

    Wei Du; Zaixing Jiang; Ying Zhang; Jie Xu


    The Lower Permian Shanxi(山西) Formation is one of the main gas-bearing stratigraphic units in northeastern Ordos(鄂尔多斯) Basin,China.Based on an integrated investigation of well logs,cores,and outcrop,we delineated the sedimentary facies of the lower member of the Shanxi Formation and divided the succession into three third-order sequences from base to top as SQ1,SQ2,and SQ3.The lower region of Shanxi Formation was deposited in the following sedimentary facies or subfacies: subaqueous braided channel,subaqueous interdistributary,mouth bar,swamp and shelf in the Daniudi(大牛地)Gas Field and braided channel,and shelf and lake at Heidaigou(黑岱沟)outcrop.Braided-river deposits form the lowstand systems tract (LST) in each sequence.Braided channels mark the sequence boundaries at Heidaigou outcrop.A shelf and lake depositional environment with dark gray mudstone forms the transgressive systems tract (TST).The location where dark gray mudstone first appears above the braided channel marks the first flooding surface (FFS),and the end of that marks the maximum flooding surface (MFS).The highstand systems tract (HST) deposits are fine-grained sediments with an aggradational parasequence at Heidaigou outcrop and swamp coalbed in the Daniudi Gas Field.Mouth-bar sand bodies in braided delta front,which form the LST in each sequence,form excellent reservoirs in the Daniudi Gas Field.

  4. Sedimentary facies and gas accumulation model of Lower Shihezi Formation in Shenguhao area, northern Ordos basin, China

    Lin, Weibing; Chen, Lin; Lu, Yongchao; Zhao, Shuai


    The Lower Shihezi formation of lower Permian series in Shenguhao develops the highest gas abundance of upper Paleozoic in China, which has already commercially produced on a large scale. The structural location of Shenguhao belongs to the transition zone of Yimeng uplift and Yishan slope of northern Ordos basin, China. Based on the data of core, well logging and seismic, the sedimentary facies and gas accumulation model have been studied in this paper. Sedimentary facies analysis shows that the braided delta is the major facies type developed in this area during the period of Lower Shihezi formation. The braided delta can be further divided into two microfacies, distributary channel and flood plain. The distributary channel sandbody develops the characteristics of scour surface, trough cross beddings and normal grading sequences. Its seismic reflection structure is with the shape of flat top and concave bottom. Its gamma-ray logging curve is mainly in a box or bell shape. The flood plain is mainly composed of thick mudstones. Its seismic reflection structure is with the shape of parallel or sub-parallel sheet. Its gamma-ray logging curve is mainly in a linear tooth shape. On the whole, the distribution of sandbody is characterized by large thickness, wide area and good continuity. Based on the analysis of the sea level change and the restoration of the ancient landform in the period of Lower Shihezi formation, the sea level relative change and morphology of ancient landform have been considered as the main controlling factors for the development and distribution of sedimentary facies. The topography was with big topographic relief, and the sea level was relatively low in the early stage of Low Shihezi formation. The sandbody distributed chiefly along the landform depressions. The sandbody mainly developed in the pattern of multiple vertical superpositions with thick layer. In the later stage, landform gradually converted to be flat, and strata tended to be gentle

  5. Blueschist-facies high-Si phengites record the timing of greenschist-facies overprinting: a Rb-Sr and Ar-ar study of marbles from the Cyclades, Greece

    Bieling, D.; Bröcker, M.; Hacker, B.; Gans, P.


    In the Attic-Cycladic crystalline belt (Greece), white mica geochronology (Rb-Sr, K-Ar, Ar-Ar) has established time constraints for at least two metamorphic events: well-preserved high-pressure/low-temperature rocks yielded Eocene ages (c. 50-40 Ma); their greenschist-facies counterparts provided Oligocene-Miocene dates (c. 25-20 Ma). Previous studies indicated that the ages recorded by high-Si phengites may not correspond to the high-pressure stage but to the subsequent greenschist-facies overprint. This hypothesis is based on the observation that the range in Si-contents and the modal proportion of phengites with a specific Si-value are not significantly different between Eocene HP rocks and Oligocene-Miocene greenschists. The possibility that the barometric information and the geochronological record might be decoupled is of general importance for interpretation of phengite ages from polymetamorphic rocks. In order to look in more detail into this problem, we have studied marbles from Tinos and Sifnos. On both islands, HP rocks are best preserved in the upper parts of the metamorphic succession. Towards the base, the degree of greenschist overprinting increases. Phengite populations of blueschist- and greenschist facies rocks mostly show a considerable range in Si-values. However, in marbles which are either associated with HP or strongly retrogressed rocks, homogeneous high-Si phengite populations (>3.5 pfu) were recognized. On Tinos, Rb-Sr and Ar-Ar white mica dating of such samples yielded ages between 40 to 24 Ma. Of special interest are samples which yielded ages of c. 24 Ma. If the earlier metamorphic history is not taken into account, such datasets may suggest the erroneous conclusion of Miocene HP metamorphism. Recent studies [1] have reported large displacements (> 100km) for detachment faults in the Aegean. The critical parameter for such models is the age of HP metamorphism as deduced from white mica dating [1,2]. In the light of the complexities

  6. Anomalous Seismic Velocity Drop in Iron and Biotite Rich Amphibolite to Granulite Facies Transitional Rocks from Deccan Volcanic Covered 1993 Killari Earthquake Region, Maharashtra (India): a Case Study

    Pandey, O. P.; Tripathi, Priyanka; Vedanti, Nimisha; Srinivasa Sarma, D.


    65 Ma Deccan Volcanic Province of western India forms one of the largest flood basaltic eruptions on the surface of the earth. The nature of the concealed crust below this earthquake prone region, which is marked by several low velocity zones at different depths has hardly been understood. These low velocity zones have been invariably interpreted as fluid-filled zones, genetically connected to earthquake nucleation. While carrying out detailed geological and petrophysical studies on the Late Archean basement cores, obtained from a 617 m deep KLR-1 borehole, drilled in the epicentral zone of 1993 Killari earthquake region of the southern Deccan Volcanic Province, we came across several instances where we observed remarkable drop in measured P-wave velocity in a number of high density cores. We provide detailed petrographic and geological data on 11 such anomalous samples which belong to mid-crustal amphibolite to granulite facies transitional rocks. They are associated with a mean P-wave velocity of 6.02 km/s (range 5.82-6.22 km/s) conforming to granitic upper crust, but in contrast have a high mean density of 2.91 g/cm3 (range 2.75-3.08 g/cm3), which characterise mid to lower crust. This velocity drop, which is as much as 15 % in some cores, is primarily attributed to FeOT enrichment (up to about 23 wt%) during the course of mantle-fluid driven retrogressive metasomatic reactions, caused by exhumation of deep-seated mafic rocks. Presence of Iron content (mainly magnetite), widely seen as opaques in thin sections of the rocks, seems to have resulted into sharp increase in density, as well as mean atomic weight. Our study indicates that the measured V p is inversely related to FeOT content as well as mean atomic weight of the rock.

  7. Field-trip guide to subaqueous volcaniclastic facies in the Ancestral Cascades arc in southern Washington State—The Ohanapecosh Formation and Wildcat Creek beds

    Jutzeler, Martin; McPhie, Jocelyn


    Partly situated in the idyllic Mount Rainier National Park, this field trip visits exceptional examples of Oligocene subaqueous volcaniclastic successions in continental basins adjacent to the Ancestral Cascades arc. The >800-m-thick Ohanapecosh Formation (32–26 Ma) and the >300-m-thick Wildcat Creek (27 Ma) beds record similar sedimentation processes from various volcanic sources. Both show evidence of below-wave-base deposition, and voluminous accumulation of volcaniclastic facies from subaqueous density currents and suspension settling. Eruption-fed facies include deposits from pyroclastic flows that crossed the shoreline, from tephra fallout over water, and from probable Surtseyan eruptions, whereas re-sedimented facies comprise subaqueous density currents and debris flow deposits.

  8. Active metasomatism in the Cerro Prieto geothermal system, Baja California, Mexico: a telescoped low-pressure, low-temperature metamorphic facies series

    Schiffman, P.; Elders, W.A.; Williams, A.E.; McDowell, S.D.; Bird, D.K.


    In the Cerro Prieto geothermal field, carbonate-cemented, quartzofeldspathic sediments of the Colorado River delta are being actively metasomatized into calc-silicate metamorphic rocks by reaction with alkali chloride brines between 200 and 370 C, at low fluid and lithostatic pressures and low oxygen fugacities. Their petrologic investigations of drill cores and cuttings from more than 50 wells in this field identified a prograde series of zones that include as index minerals wairakite, epidote, prehnite, and clinopyroxene. Associated divariant mineral assemblages are indicate of a very low pressure, low-temperature metamorphic facies series spanning the clay-carbonate, zeolite, greenschist, and amphibolite facies. This hydrothermal facies series, which is now recognized in other active geothermal systems, is characterized by temperature-telescoped dehydration and decarbonation. Its equivalent can now be sought in fossil hydrothermal systems.

  9. Sequential development of platform to off-platform facies of the great American carbonate bank in the central Appalachians: chapter 15

    Brezinski, David K.; Taylor, John F.; Repetski, John E.


    In the central Appalachians, carbonate deposition of the great American carbonate bank began during the Early Cambrian with the creation of initial ramp facies of the Vintage Formation and lower members of the Tomstown Formation. Vertical stacking of bioturbated subtidal ramp deposits (Bolivar Heights Member) and dolomitized microbial boundtsone (Fort Duncan Member) preceded the initiation of platform sedimentation and creation of sand shoal facies (Benevola Member) that was followed by the development of peritidal cyclicity (Daragan Member). Initiation of peritidal deposition coincided with the development of a rimmed platform that would persist throughout much of the Cambrian and Early Odrovician. At the end of deposition of the Waynesboro Formation, the platform became subaerially exposed because of the Hawke Bay regression, bringing the Sauk I supersequence to and end. In the Conestoga Valley of eastern Pennsylvania, Early Cambrian ramp deposition was succeeded by deposition of platform-margin and periplatfrom facies of the Kinzers Formation.

  10. Active metasomatism in the Cerro Prieto geothermal system, Baja California, Mexico: A telescoped low-pressure, low-temperature metamorphic facies series

    Schiffman, P.; Elders, W. A.; Williams, A. E.; McDowell, S. D.; Bird, D. K.


    In the Cerro Prieto geothermal field, carbonate-cemented, quartzofeldspathic sediments of the Colorado River delta are being actively metasomatized into calc-silicate metamorphic rocks by reaction with alkali chloride brines between 200 and 370 °C, at low fluid and lithostatic pressures and low oxygen fugacities. Our petrologic investigations of drill cores and cuttings from more than 50 wells in this field identified a prograde series of zones that include as index minerals wairakite, epidote, prehnite, and clinopyroxene. Associated divariant mineral assemblages are indicative of a very low pressure, low-temperature metamorphic facies series spanning the clay-carbonate, zeolite, greenschist, and amphibolite facies. This hydro-thermal facies series, which is now recognized in other active geothermal systems, is characterized by temperature-telescoped dehydration and decarbonation. Its equivalent can now be sought in fossil hydrothermal systems.

  11. Bolívia, Brasil e o gás natural: um breve debate

    Hage,José Alexandre Altahyde


    O texto analisa as razões de se importar gás natural boliviano. O emprego do carburante importado foi admitido como uma das formas para neutralizar a crise de energia elétrica que o Brasil vem atravessando desde os anos 1990, cujo ápice se deu com o "apagão" de 2001. Além disso, o uso da matéria-prima traduz a ausência de políticas públicas coerentes para o setor energético. O Brasil aceitou, em grande parte, programas sugeridos pelas agências financeiras internacionais, que negavam o papel e...

  12. Facies transition and depositional architecture of the Late Eocene tide-dominated delta in northern coast of Birket Qarun, Fayum, Egypt

    Abdel-Fattah, Zaki A.


    Late Eocene successions in the Fayum Depression display notable facies transition from open-marine to brackish-marine realms. Stratigraphic and sedimentologic characteristics of the depositional facies are integrated with ichnological data for the recognition of four facies associations (FA1 to FA4). The transition from open-marine sandstones (FA1) to the brackish-marine deposits (FA2) heralds a transgressive - regressive dislocation. The shallowing- and coarsening-upward progradation from the basal prodelta mudstone-dominated facies (FA2a) to deltafront heterolithics (FA2b) and sandstone facies (FA2c) are overlain by finning-upward delta plain deposits which are expressed by the delta plain mudstone (FA2d) and erosive-based distributary channel fills (FA4). Prodelta/deltfront deposits of FA2 are arranged in thinning- and coarsening-upward parasequences which are stacked in a shallowing-upward progressive cycle. Shallow-marine fossiliferous sandstones (FA3) mark the basal part of each parasequence. Stratigraphic and depositional architectures reflect a tide-dominated delta rather than an estuarine and incised valley (IV) model. This can be evinced by the progressive facies architecture, absence of basal regional incision or a subaerial unconformity and the stratigraphic position above a maximum flooding surface (MFS), in addition to the presence of multiple tidally-influenced distributary channels. Stratigraphic and depositional characteristics of the suggested model resemble those of modern tide-dominated deltaic systems. Accordingly, this model contributes to our understanding of the depositional models for analogous brackish-marine environments, particularly tide-dominated deltas in the rock record.

  13. Effects of relative sea level changes on facies and diagenetic variability of a Pennsylvanian outcrop and near-surface reservoir analog, SE Kansas (Missourian, Drum Limestone)

    Gomez-Perez, I. [Univ. of Wisconsin, Madison, WI (United States); Fieldman, H.R.; Franseen, E.K. [Kansas Geological Survey, Lawrence, KS (United States)] [and others


    The Drum Limestone contains facies that are an analog to important petroleum reservoirs elsewhere in the Mid-continent. It consists predominantly of an oolitic shoal and algal buildup complex deposited and the seaward edge of a shale delta. This study integrates outcrop, core, well log, petrographic, and high-resolution reflection seismic data to understand the role of relative sea level fluctuations in the depositional and diagenetic history of the Drum reservoir facies. The Drum Limestone forms an E-W belt 30 km wide, is up to 21 m thick, and thins to less than one meter thick both up-dip and down-dip of the depositional shelf edge. The basal contact of the Drum Limestone is regionally erosive and interpreted to represent a relative sea level drop. The erosion surface is overlain by a basal oolite with lithoclasts. Two-thirds of the Drum oolite facies coexisted partially with algal-bryozoan buildups, in shallow-waters at the shelf edge. Ooids were likely transported by tidal and wave currents to paleotopographic lows forming basinward prograding (SSW direction) clinoforms. Landward, Drum facies grade to stromatolites, and basinward the oolite pinches out. An interpreted relative sea level fall at the end of this Drum depositional stage resulted in a sharp, regionally traceable surface with evidences of likely subaerial exposure in shelf positions, and represented basinward by an oolitic lithoclastic breccia capped by an incipient hardground. The surface is overlain by Drum trough-crossbedded (N-NE direction) bioclastic oolitic facies interbedded with shales, deposited during a relative sea level rise. This upper third of oolite deposition was influenced by siliciclastic input from the south that eventually overtook carbonate sedimentation. Facies and diagenetic changes documented for the Drum Limestone analog are providing important details on reservoir heterogeneities at a scale important for Mid-continent reservoirs.

  14. Mid-Eocene alluvial-lacustrine succession at Gebel El-Goza El-Hamra (Shabrawet area, NE Eastern Desert, Egypt): Facies analysis, sequence stratigraphy and paleoclimatic implications

    Wanas, H. A.; Sallam, E.; Zobaa, M. K.; Li, X.


    This study aims to provide the depositional facies, sequence stratigraphic and paleoclimatic characteristics of the Mid-Eocene (Bartonian) continental succession exposed at Gebel El-Goza El-Hamra (Shabrawet Area, NE Eastern Desert, Egypt). The studied succession consists of siliciclastic rocks followed upward by carbonate rocks. Detailed field observation and petrographic investigation indicate accumulation in floodplain-dominated alluvial and shallow lacustrine systems. The floodplain-dominated alluvial facies (45 m thick) is composed mainly of carbonate nodules-bearing, mottled mudrock with subordinate sandstone and conglomerate beds. The conglomerate and pebbly sandstone bodies interpreted as ephemeral braided channel deposits. The massive, laminated, planner cross-bedded, fine- to medium-grained sandstone bodies interlayered within mudstone reflect sheet flood deposits. The mudrocks associated with paleosols represent distal floodplain deposits. The shallow lacustrine facies (15 m thick) is made up of an alternation of marlstone, micritic limestone, dolostone and mudrock beds with charophytes and small gastropods. Both the alluvial and lacustrine facies show evidence of macro-and micro-pedogenic features. Pollen assemblages, stable δ18O and δ13C isotopes, and paleopedogenic features reflect prevalence of arid to semi-arid climatic conditions during the Bartonian. The sequence stratigraphic framework shows an overall fining-upward depositional sequence, consisting of Low- and High-accommodation Systems Tracts (LAST, HAST), and is bounded by two sequence boundaries (SB-1, SB-2). Conglomerate and pebbly sandstone deposits (braided channel and sheet flood deposits) of the lower part of the alluvial facies reflect a LAST. Mudrock and silty claystone facies (distal floodplain deposits) of the upper part of alluvial facies and its overlying lacustrine facies correspond to a HAST. The LAST, HAST and SB were formed during different accommodation-to-sediment supply (A

  15. Paleogeographic and litho-facies formation conditions of MidUpper Jurassic sediments in S-E Western Siberia (Tomsk Oblast)

    Shaminova, M.; Rychkova, I.; Sterzhanova, Ju


    This paper describes the criteria to identify Tumen (lower Bathonian) and Naunak (upper Bathonian-Callovian- Oxfordian) suites within S-E Western Siberia (Tomsk Oblast). The specific paleogeographic and litho-facies formation conditions of sediments and numerous vegetable remains and ichnofossils indicated the fact that this territory was the location of sedimentogenesis transition during Tumen and Naunak suite formation. Based on integrated survey oil-gas potential litho-facies groups were defined in Mid-Upper Jurassic sediments within S-E Western Siberia.

  16. Northernmost Known Outcrop in North America of Lower Cretaceous Porphyritic Ocoite Facies (Ocoa, Chile) at Western Mexico: the Talpa Ocoite

    Zárate-del Valle, P. F.; Demant, A.


    At Talpa de Allende region in Western Mexico is located the northernmost known outcrop of ocoite facies (andesite): the Talpa ocoite (TO). The ocoite facies consists of an calk-alkaline andesitic rock rich in K and characterized by the presence of megacrysts of plagioclase (An48-65). TO belongs to the so-called Guerrero Terrane composed of plutono-volcanic and volcano-sedimentary sequences of the Alisitos-Teloloapan arc that was accreted to the North American craton at the end of the early Cretaceous (Lapierre et al., 1992, Can. J. Earth Sci. 29. 2478--2489). Geodynamically TO belongs to lithological sequence number IV or "Tecoman" of Tardy et al. (1994, Tectonophysics 230, 49--73). TO in hand-sample shows typical megacrysts (>1 cm) of plagioclase and clinopyroxene in a dark green aphanitic matrix. This andesitic lava has a shoshonitic character as evidenced by chemical composition: SiO_2 TiO_2 Al_2O_3 Fe_2O_3 MnO MgO CaO Na_2O K_2O P_2O_5 LOI % Ba Sr (ppm) 55.64 0.73 16.61 8.39 0.13 3.59 6.40 3.55 2.85 0.36 1.84% 1093 880 Under microscope TO is characterized by a porphyritic texture made of large labradorite phenocrysts (up to 3 cm) and clinopyroxene with a matrix made of plagioclase microlites; TO has been affected by a low grade metamorphism process belonging to the prehnite-pumpellite facies as it happens in Chile (Levi, 1969, Contr. Mineral. and Petrol. 24-1, p. 30--49). Electron microprobe analysis shows that plagioclase (An55-57) is partly transformed into albite (An7-9); clinopyroxene shows a variation in composition from Wo33En41Fs17 to Wo40En44Fs24 and it is transformed towards the margin first into amphibole and then into biotite. TO outcrops located at East of Talpa river are affected by a deep rubefaction process. TO is not characterized by the presence of bitumen as it occurs in Northern Chile (Nova-Muñoz et al., 2001, EUG XI Meeting, OS09 Supo09 PO, 606); TO is related in time with albian-cenomanian volcanogenic massive sulphides of Western Mexico

  17. Generation of trondhjemite from partial melting of dacite under granulite facies conditions: an example from the New Jersey Highlands, USA

    Puffer, J.H.; Volkert, R.A.


    New field and geochemical data place the Losee Metamorphic Suite (a tonalite/trondhjemite complex) of northern New Jersey into the context of a major Proterozoic continental are represented by a discontinuous belt of northern Appalachian metadacite. Samples of Losee rock range from extremely leucocratic trondhjemite locally associated with amphibolite, to banded biotite, hornblende, pyroxene, and garnet-bearing tonalites. The major element and REE composition of the tonalite closely resembles dacite from continental are settings and model melts extracted from an eclogite residue by partial melting at 15 kbar. The REE composition of most Losee trondhjemite is enriched in REE, particularly HREE, compared with Losee tonalite, and is interpreted as the product of local anatectic melting of Losee tonalite (metadacite) that occurred in a granulite facies environment during the Grenville orogeny. ?? 1991.

  18. Geology of crystalline rocks of northern Fiordland: details of the granulite facies Western Fiordland Orthogneiss and associated rock units

    Bradshaw, J.Y.


    A c. 700 km2 area of northern Fiordland (South Island, New Zealand) is described in which Early Cretaceous high-pressure metamorphic rocks and virtually unmetamorphosed plutonic rocks occur. The dominant rocks are orthogneisses developed from synmetamorphic basic-intermediate intrusive complexes, the youngest and most widespread of which is the Early Cretaceous Western Fiordland Orthogneiss (WFO). The latter has undergone granulite facies metamorphism and occurs throughout much of western Fiordland. WFO was emplaced synkinematically in a subduction-related magmatic arc. A collisional event during or immediately following magma emplacement resulted in crustal thickening equivalent to onloading of a 20 km thick section over rocks already buried at mid-crustal depths. This event was responsible for peak load pressures of c. 12-13 kbar. The steeply dipping Surprise Creek Fault juxtaposes high-pressure metamorphic rocks of western and central Fiordland against virtually unmetamorphosed gabbroic rocks of the Early Cretaceous Darran Complex. -from Author

  19. Tectonic Facies and Mineralization in Tianjin%天津市大地构造相与成矿


      在板块构造理论指导下,对天津市大地构造相进行了系统的划分,全面地总结了天津成矿地质构造环境。各种矿床都是在大地构造演化过程中的特定大地构造相环境下形成的特殊地质体,成矿作用过程与大地构造演化密切相关。研究表明古弧盆相中的新太古代角闪斜长片麻岩中含铁矿残留透镜体;大陆裂谷相的长城纪含有比较重要的非金属矿产陶瓷土矿和含钾泥岩等;稳定型陆表海相沉积的中-新元古代水泥石灰岩矿、锰(硼)矿、砖瓦用页岩矿、铁矿等;印支晚期板内造山岩浆杂岩有岩浆矿床磷,岩浆期后热液矿床钨、金、重晶石等,接触交代(矽卡岩)矿床有钼、硫铁及铜矿等金属矿产;新生代地层为坳陷盆地相碎屑岩沉积,富含有丰富的油页岩、石油等矿产。本次工作的目的就是研究各级大地构造相单元与成矿构造体系及成矿类型的关系,建立大地构造相与成矿作用的时空及岩石构造组合关系。%Under the guidance about theory of plate tectonics,the division of tectonic facies were made in Tian-jin, and mineralization geologic structure environment was comprehensively summarized also. All kinds of depos-its formed in the special geological process of geotectonic evolution under the specific tectonic facies environ-ment, the mineralization and the geotectonic evolution are the close correlations. The research show that Neoar-chean hornblende plagioclase gneiss formed in paleo-arc basins in which there is residual lenticle iron ore. In Changchengian period continental rift tectofacies contains very important non-metallic minerals such as potassi-um and shale. Meso-Neoproterozoic the stable epicontinental marine environment contains shale, iron, manga-nese, boron, cement, limestone and other minerals. In the later period of Indosinian the plate mountain building environment has the igneous complex

  20. Metre-scale cyclicity in Middle Eocene platform carbonates in northern Egypt: Implications for facies development and sequence stratigraphy

    Tawfik, Mohamed; El-Sorogy, Abdelbaset; Moussa, Mahmoud


    The shallow-water carbonates of the Middle Eocene in northern Egypt represent a Tethyan reef-rimmed carbonate platform with bedded inner-platform facies. Based on extensive micro- and biofacies documentation, five lithofacies associations were defined and their respective depositional environments were interpreted. Investigated sections were subdivided into three third-order sequences, named S1, S2 and S3. Sequence S1 is interpreted to correspond to the Lutetian, S2 corresponds to the Late Lutetian and Early Bartonian, and S3 represents the Late Bartonian. Each of the three sequences was further subdivided into fourth-order cycle sets and fifth-order cycles. The complete hierarchy of cycles can be correlated along 190 km across the study area, and highlighting a general "layer-cake" stratigraphic architecture. The documentation of the studied outcrops may contribute to the better regional understanding of the Middle Eocene formations in northern Egypt and to Tethyan pericratonic carbonate models in general.


    Sudhanshu Kumar


    Full Text Available ABSTRACT: Potter's sequence is more appropriate terminology than potter facies, since not every individual with this syndrome has exactly the same set of symptoms and signs but they share a common chain of events triggered by differe nt causes, leading to the same endpoint of reduced or absent amniotic fluid. It has a charact eristic facial appearance associated with other abnormalities as Ophthalmic(Cataract, Cardiovascula r (Ventricular septal defect. Fallot's tetralogy, Patent ductus arteriosus, and muscu loskeletal (Clubbed feet, Sacral agenesis . Here we are presenting two cases of potter sequence due to polycystic kidney disease ( type-i in association with other congenital anomalies ( ab sence of left diaphragm ,pericardial effusion, pulmonary hypoplasia which is rare and incompatible to life

  2. Sedimentary facies and depositional environments related to Gondwana glaciation in Batovi and Suspiro regions, Rio Grande Do Sul, Brazil

    Tomazelli, Luiz José; Soliani, Enio


    Sedimentary facies were produced by Late Paleozoic Gondwana ice sheets in the Batovi and Suspiro regions, Rio Grande do Sul State, southern Brazil. The glaciogenic sediments, assigned to the Itararé Group of Paraná Basin, are the result of processes related to the subglacial, supraglacial and proglacial (ice-contact, glaciofluvial and glaciolacustrine) environments of the glacial depositional system. Several features developed by the action of glaciers were identified in the studied outcrops: striated and grooved pavements; striated, polished and faceted stones; finely laminated rhythmites bearing dropstones (varvites); erratic clasts and deposits exhibiting deformational structures such as folds, normal and reverse faults, and beds with abnormal dips. The available evidence suggests that the glacial episodes took place in a terrestrial (continental) context, far from direct marine influence.

  3. Multi-Temporal Investigation of Greenland Ice Sheet Snow Facies Using TanDEM-X Mission Data

    Rizzoli, Paola; Martone, Michele; Brautigam, Benjamin; Rott, Helmut; Moreira, Alberto


    This paper presents the first results of the developed approach for classifying Greenland ice sheet snow facies, based on the use of interferometric TanDEM-X SAR data. Large-scale mosaics of radar backscatter and volume decorrelation, derived from the interferometric coherence, are used as input data set for applying a classification algorithm based on the c-means fuzzy clustering. The unique data set provided by TanDEM-X is particularly suitable for this analysis due to the single-pass bistatic acquisition mode which does not suffer from temporal decorrelation. The obtained results have been verified with external snow melt data. Moreover, independent multi-temporal TanDEM-X backscatter data and interferometric time series have been analyzed as well.

  4. Geostatistical modeling of facies, bitumen grade and particle size distribution for the Joslyn oil sand open pit mine project

    Babak, Olena; Insalaco, Enzo; Mittler, Andreas [Total EandP Canada Ltd. (Canada)


    The Joslyn North Mine Project is currently in the pre-development stage; the aim of this study is to use different available data to draw a geological model of facies, bitumen grade, full particle size distribution (PSD) and ore/waste discrimination. The study was conducted with the database of around 800 wells, stochastic, indicator and Gaussian simulations were performed along with a sensitivity study. Results demonstrated the importance of some parameters for evaluating grade cases including variogram uncertainty, sampling limitations and errors in geostatistical workflow. In addition, modeling the full PSD dataset was shown to be useful. This study demonstrated how to use available database through an overall workflow to develop case scenarios for bitumen in place in ore and characterize the ore material.

  5. Reactive solute transport in physically and chemically heterogeneous porous media with multimodal reactive mineral facies: The Lagrangian approach

    Soltanian, Mohamad Reza; Dai, Zhenxue; Huang, Chaocheng


    Physical and chemical heterogeneities have a large impact on reactive transport in porous media. Examples of heterogeneous attributes affecting reactive mass transport are the hydraulic conductivity (K), and the equilibrium sorption distribution coefficient (Kd). This paper uses the Deng et al. (2013) conceptual model for multimodal reactive mineral facies and a Lagrangian-based stochastic theory in order to analyze the reactive solute dispersion in three-dimensional anisotropic heterogeneous porous media with hierarchical organization of reactive minerals. An example based on real field data is used to illustrate the time evolution trends of reactive solute dispersion. The results show that the correlation between the hydraulic conductivity and the equilibrium sorption distribution coefficient does have a significant effect on reactive solute dispersion. The anisotropy ratio does not have a significant effect on reactive solute dispersion. Furthermore, through a sensitivity analysis we investigate the impact...

  6. Stochastic Joint Simulation of Facies and Diagenesis: A Case Study on Early Diagenesis of the Madison Formation (Wyoming, USA Simulation stochastique couplée faciès et diagenèse. L’exemple de la diagenèse précoce dans la Formation Madison (Wyoming, USA

    Barbier M.


    Full Text Available The aim of this paper is to propose an integrated approach to reproduce both facies and diagenetic trends in a static reservoir model based on an outcrop case study. In Wyoming (USA, the Madison Formation (Mississippian is a thick (up to 350 m carbonate series, outcropping in several locations of the Bighorn foreland basin. Within these series, nine sedimentary facies have been identified. Based on their vertical stacking pattern, they are organized in small-scale facies sequences: 1 intertidal to supratidal facies sequence; 2 shallow subtidal to intertidal facies sequence; 3 deep subtidal facies sequence. These facies associations have been integrated in a synthetic depositional model, which corresponds to a carbonate ramp progressively evolving towards the most inner part of a platform. This enables to propose a sequence stratigraphy framework for the studied series, that represents at least six third-order sequences (some of them being locally eroded. The diagenetic study has been focused on the identification of the early diagenetic phases. Results from these analyses show the occurrence of several successive early diagenetic phases (micritization, marine calcite cementation, dolomitization, etc.. For modeling purposes, seven “diagenetic imprints” have been defined, each of them corresponding to a succession of diagenetic phases that can coexist in the same sedimentary facies. Moreover, as each sedimentary facies may be affected by several diagenetic imprints, a quantification of these imprints has been realized. A 3D gridded model designed for geostatistical modeling has been constructed in order to reproduce the facies organization of the three first third-order sequences (that are the best documented. The gridding is then based on the four sequence boundaries which have been recognized on every section. The relationships between sedimentary facies and diagenesis have been used to define lithofacies simulation rules. The simulations

  7. Sedimentology, eruptive mechanism and facies architecture of basaltic scoria cones from the Auckland Volcanic Field (New Zealand)

    Kereszturi, Gábor; Németh, Károly


    Scoria cones are a common type of basaltic to andesitic small-volume volcanoes (e.g. 10- 1-10- 5 km3) that results from gas-bubble driven explosive eruptive styles. Although they are small in volume, they can produce complex eruptions, involving multiple eruptive styles. Eight scoria cones from the Quaternary Auckland Volcanic Field in New Zealand were selected to define the eruptive style variability from their volcanic facies architecture. The reconstruction of their eruptive and pyroclastic transport mechanisms was established on the basis of study of their volcanic sedimentology, stratigraphy, and measurement of their pyroclast density, porosity, Scanning Electron Microscopy, 2D particle morphology analysis and Visible and Near Visible Infrared Spectroscopy. Collection of these data allowed defining three end-member types of scoria cones inferred to be constructed from lava-fountaining, transitional fountaining and Strombolian type, and explosive Strombolian type. Using the physical and field-based characteristics of scoriaceous samples a simple generalised facies model of basaltic scoria cones for the AVF is developed that can be extended to other scoria cones elsewhere. The typical AVF scoria cone has an initial phreatomagmatic phases that might reduce the volume of magma available for subsequent scoria cone forming eruptions. This inferred to have the main reason to have decreased cone volumes recognised from Auckland in comparison to other volcanic fields evolved dominantly in dry eruptive condition (e.g. no external water influence). It suggests that such subtle eruptive style variations through a scoria cone evolution need to be integrated into the hazard assessment of a potentially active volcanic field such as that in Auckland.

  8. Identification of Radar Facies and Linked Process-Based Palaeo-environmental Interpretations, Cooloola Sand Mass, Queensland, Australia

    Gontz, A. M.; McCallum, A. B.; Moss, P. T.; Shulmeister, J.


    During 2015 and 2014, nearly 60 km of high-resolution ground penetrating radar data were acquired on the Cooloola Sand Mass (CSM) in southeastern coastal Queensland. The CSM is part of the world's largest downdrift sand system. It contains three of the world's largest sand islands, several National Parks, a UNESCO World Heritage Site and covers 500 km of the eastern Australian coastline in northern New South Wales and southern Queensland. The large (>200 m) composite dunes of the CSM exhibit multiple activation phases, coastally eroding bluffs and dune development is not obvious from surficial exposures. This provides an ideal environment for ground penetrating radar. The dune sequences have been provisionally dated to the mid Quaternary through present and represent the potential for a large palaeo-environmental proxy dataset. GPR imagery was collected using a MALA GeoSciences Ground Explorer (GX) system with 160 and 450 MHz antennae from the numerous physiographic and ecological provinces as well as mapped surficial soil units at the CSM. These data were used to determine the subsurface architecture, identify radar facies and develop environmental interpretations. In the clean, aeolian quartz-rich sands, radar wave penetration exceeded 30 m (radar velocity = 0.07 m/ns) with the 160 MHz antenna. From the interpreted environmental units including palaeosol, dune slip face, dune stoss face, sand blow, beach, estuarine and fluvial, we are developing maps to relate the units and focus a detailed sampling regime that includes OSL, sediment geochemistry and sedimentology, The interpreted units, stratigraphic correlation and spatial distribution of the facies is the first step in a broader project to unravel the Quaternary environmental and climate records that are archived within the sediments of the CSM.

  9. Alluvial fan facies of the Yongchong Basin: Implications for tectonic and paleoclimatic changes during Late Cretaceous in SE China

    Chen, Liuqin; Steel, Ronald J.; Guo, Fusheng; Olariu, Cornel; Gong, Chenglin


    Late Cretaceous continental redbeds, the Guifeng Group of the Yongchong Basin in SE China have been investigated to conduct detailed fan facies description and interpretation. Tectonic activities determined the alluvial fan development along the basin margin, but the alluvial facies was linked with paleoclimate changes. The Guifeng Group is divided into the Hekou, Tangbian and Lianhe formations in ascending order. The Hekou conglomerates are typically polymict, moderately sorted with erosional bases, cut-and-fill features, normal grading and sieve deposits, representing dominant stream-flows on alluvial fans during the initial opening stage of the basin infill. The Tangbian Formation, however, is characterized by structureless fine-grained sediments with dispersed coarse clasts, and couplets of conglomerate and sandstone or siltstone and mudstone, recording a change to a playa and ephemeral lake environments with occasional stream flooding, thus indicating a basin expanding stage. The hallmark of the Lianhe Formation is disorganized, poorly sorted conglomerates lack of erosional bases, and a wide particle-size range from clay to boulders together reflect mud-rich debris-flows accumulating on fans, likely related to reactivation of faulting along the northwestern mountain fronts during a post-rift stage. The depositional system changes from stream-flows up through playa with ephemeral streams to debris-flows during the accumulation of the three formations are thus attributed to different source rocks and climatic conditions. Therefore, the fluvial-dominated fans of the Hekou Formation recorded a subhumid paleoclimate (Coniacian-Santonian Age). The dominant semiarid climate during the Campanian Age produced abundant fine-grained sediments in the playa and ephemeral lake environments of the Tangbian Formation. A climatic change towards more humidity during the late stage of the Guifeng Group (Maastrichtian Age) probably yielded high deposition rate of coarse clasts in

  10. Estimation of the tectonic slip-rate from Quaternary lacustrine facies within the intraplate Albacete province (SE of Spain)

    Rodriguez-Pascua, M. A.; Bischoff, J.; Garduno-Monroy, Victor H.; Pérez-López, R.; Giner-Robles, J.L.; Israde-Alcántara, I.; Calvo, J.P.; Williams, Ross W.


    The Quaternary lacustrine basin of Cordovilla (CB) represents one of the most active tectonic areas of the Prebetic Zone (Albacete, SE of Spain). The Quaternary sedimentary deposits of this basin are mainly endoreic lacustrine carbonate and alluvial deposits, developed in a semi-arid climate (Pleistocene-present). The basin is a NW-SE-elongated graben bounded by a major right-lateral oblique-fault, the Pozohondo Fault. This fault trends NW-SE, with an approximate trace of 55 km, and is composed of various segments which are identified by fault scarps. In order to establish the slip-rate of the most active segment of the Pozohondo Fault, called the Cordovilla segment, we carried out a detailed study of the affected Quaternary lacustrine deposits. We found that the lacustrine facies could be related to episodic moderate paleoearthquakes. The slip-rate is calculated to be 0.05 and 0.09 mm/yr, using radiometric dating for the vertical offsets of the lacustrine facies. A trenching study at the northern part of the Cordovilla segment revealed two events caused by paleoearthquakes, with the most recent expressed as an oblique-fault off-setting a poorly-developed soil. The magnitude of the last event was greater than 6, using various empirical relationships for the fault displacement and the surface-length rupture. We estimate episodic activity across the Cordovilla segment, to be characterized by moderate-sized paleoearthquakes (M6), which is in agreement with the tectonic context of an intraplate zone of the Iberian plate. ?? 2009 Elsevier B.V.

  11. Principal component analysis and hydrochemical facies characterization to evaluate groundwater quality in Varahi river basin, Karnataka state, India

    Ravikumar, P.; Somashekar, R. K.


    The present study envisages the importance of graphical representations like Piper trilinear diagram and Chadha's plot, respectively to determine variation in hydrochemical facies and understand the evolution of hydrochemical processes in the Varahi river basin. The analytical values obtained from the groundwater samples when plotted on Piper's and Chadha's plots revealed that the alkaline earth metals (Ca2+, Mg2+) are significantly dominant over the alkalis (Na+, K+), and the strong acidic anions (Cl-, SO4 2-) dominant over the weak acidic anions (CO3 2-, HCO3 -). Further, Piper trilinear diagram classified 93.48 % of the samples from the study area under Ca2+-Mg2+-Cl--SO4 2- type and only 6.52 % samples under Ca2+-Mg2+-HCO3 - type. Interestingly, Chadha's plot also demonstrated the dominance of reverse ion exchange water having permanent hardness (viz., Ca-Mg-Cl type) in majority of the samples over recharging water with temporary hardness (i.e., Ca-Mg-HCO3 type). Thus, evaluation of hydrochemical facies from both the plots highlighted the contribution from the reverse ion exchange processes in controlling geochemistry of groundwater in the study area. Further, PCA analysis yielded four principal components (PC1, PC2, PC3 and PC4) with higher eigen values of 1.0 or more, accounting for 65.55, 10.17, 6.88 and 6.52 % of the total variance, respectively. Consequently, majority of the physico-chemical parameters (87.5 %) loaded under PC1 and PC2 were having strong positive loading (>0.75) and these are mainly responsible for regulating the hydrochemistry of groundwater in the study area.

  12. Facies analysis and diagenetic features of the Aptian Dariyan Formation in Zagros Fold-Thrust Belt, SW Iran

    Haghighi, Arash Shaabanpour; Sahraeyan, Mohammad


    The Aptian Dariyan Formation (upper part of the Khami Group), is one of the important reservoir rocks in the Zagros Fold-Thrust Belt. The Zagros Fold-Thrust Belt is located on the boundary between the Arabian and Eurasian lithospheric plates and formed from collision between Eurasia and advancing Arabia during the Cenozoic. In these studied area, the Dariyan Formation with a thickness of 136 meters (Fahliyan section) and 100 meters (Kuh-e-Rahmat section), consists of carbonate rocks. Based on the facies analysis and sedimentological data, 16 microfacies were identified. The microfacies are attributed to five facies belts: tidal flat (lime mudstone, dolomitic mudstone and stromatolitic boundstone), lagoon (bioclastic packstone, orbitolinids bioclastic packstone and orbitolinids peloidal packstone), shoal (orbitolinids grainstone and peloidal grainstone), restricted (peloidal packstone, rudist floatstone/rudstone and orbitolinid wackestone), and open marine (orbitolinid floatstone, dasycladacean algae floatstone, bioclast pelagic foraminiferal wackestone/packstone, pelagic foraminiferal mudstone/wackestone, and calcispere packstone/wackestone). The depositional model relates to the carbonate ramp. The allochems of the Dariyan Formation are dominated by foraminifera, bioclasts and green algae. Peloids, and intraclasts are less abundant in this formation. Due to the great diversity and abundance of the foraminifera, this carbonate ramp is referred to as a "foraminifera-dominated carbonate ramp system". This carbonate system reflects a local regression in the Fahliyan section which can be related to the vertical movement of the Kazeroon Fault. The carbonates of Dariyan Formation have been affected by a variety of diagenetic processes such as compaction, dissolution, cementation, neomorphism, and dolomitization.

  13. Mebendazol: identificação das formas polimórficas em diferentes matérias-primas e medicamentos (referência e genéricos disponíveis no mercado nacional



    Full Text Available

    A presença de polimorfos diferentes em uma formulação pode comprometer a dissolução de um fármaco a partir de sua forma farmacêutica, uma vez que os polimorfos freqüentemente apresentam diferentes solubilidades. No entanto, as monografias farmacopéicas não apresentam, normalmente, ensaios para a identificação das possíveis formas polimórficas de um mesmo fármaco. O mebendazol possui três formas polimórficas diferentes, conhecidas como formas A, B e C, que apresentam diferentes propriedades físico-químicas e biofarmacêuticas. Estas formas apresentam, inclusive, diferentes comportamentos in vivo, sendo o polimorfo C o recomendado para formas farmacêuticas sólidas de uso oral. No presente trabalho utiliza-se a espectroscopia de infravermelho e o perfil de dissolução in vitro para caracterizar matérias-primas e comprimidos (referência e genéricos existentes no mercado brasileiro. O perfil de dissolução para três medicamentos que apresentavam as formas polimórficas A, B e C, foi obtido utilizando-se método da Farmacopéia Americana modificado, uma vez que o meio de dissolução farmacopéico não possibilita a distinção entre as formas polimórficas do mebendazol, devido à adição de lauril sulfato de sódio ao meio. Os resultados obtidos demonstram que as três formas polimórficas do mebendazol estão presentes nos medicamentos e duas delas em matérias-primas, sugerindo que um maior controle deveria ser utilizado para a seleção de matérias-primas que apresentam polimorfismo, assegurando, através de testes simples e rápidos, a qualidade de medicamentos genéricos. Palavras-chave: Mebendazol, polimorfismo, dissolução, biodisponibilidade, medicamento genérico.


    Sandro Antonio Malinowski


    Full Text Available Normal 0 21 false false false PT-BR X-NONE X-NONE MicrosoftInternetExplorer4 Resumo Este trabalho pretende propor um procedimento operacional objetivo para avaliar e qualificar os fornecedores de matéria-prima e insumos da Conquista Equipamentos para Montanhismo, segundo os critérios de avaliação da Norma ISO 9001:2000 item 7.4.1 – que trata do processo de aquisição. Os fornecedores de matéria-prima e insumos são avaliados segundo os seguintes critérios: entrega de pedidos, atendimento, qualidade dos produtos ou serviços apresentados e pelo interesse na resolução de problemas decorrentes do fornecimento. Nesse sentido, realizamos entre outubro e dezembro de 2003 uma pesquisa com cento e sete empresas que fornecem matéria-prima para a Conquista Montanhismo. Com a pesquisa pretendemos obter indicadores de desempenho que permitam à Conquista Montanhismo conhecer melhor seus fornecedores e conseqüentemente melhorar a qualidade de seus produtos.   Palavras-chave: organização, qualidade, fornecedores, clientes.   Abstract This work intends to consider an objective operational procedure to evaluate and to characterize the raw material suppliers and insumos of the Conquest Equipment, according to criteria of evaluation of Norm ISO 9001:2000 item 7.4.1 - that it deals with the acquisition process. The raw material suppliers and insumos are evaluated according to following criteria: delivery of order, attendance, presented product quality or services and interest in the resolution of decurrent problems of the supply. In this direction, we carry through between October and December of 2003 a research with one hundred and seven companies who supply raw material the Montanhismo Conquest. With the research we intend to get performance pointers that allow the Montanhismo Conquest to know its suppliers better and consequently to improve the quality of its products.   Key Words: organization, quality, suppliers, customers.

  15. A comparative study of representative 2D microstructures in Shaly and Sandy facies of Opalinus Clay (Mont Terri, Switzerland) inferred form BIB-SEM and MIP methods

    Houben, M.E.; Desbois, G.; Urai, J.L.


    A combination of Broad-Ion-Beam (BIB) polishing and Scanning Electron Microscopy (SEM) has been used to study qualitatively and quantitatively the microstructure of Opalinus Clay in 2D. High quality 2D cross-sections (ca. 1mm2), belonging to the Shaly and Sandy facies of Opalinus Clay, were investig

  16. Pore morphology and distribution in the Shaly facies of Opalinus Clay (Mont Terri, Switzerland): Insights from representative 2D BIB-SEM investigations on mm to nm scale

    Houben, M.E.; Desbois, G.; Urai, J.L.


    We used Broad-Ion-Beam polishing in combination with Scanning Electron Microscopy to study the microstructure and porosity in the Shaly facies of Opalinus Clay (northern Switzerland). With resolutions of a few nm, we studied areas of around 1 mm2, sufficiently large to be statistically representativ

  17. Tecnología y materias primas a la sombra de Don Segundo: Una cantera-taller en el valle de Piedra Parada

    Cristina Bellelli


    Full Text Available Se busca conocer cómo y en qué momentos la cantera-taller Don Segundo fue utilizada y cuál fue su papel en la definición de la base regional de recursos líticos del valle medio del río Chubut. Se actualiza la información referida a las distintas localizaciones y sitios de aprovisionamiento de la región, muchas de las cuales son de rocas de excelente calidad, muy accesibles y altamente disponibles. La única diferencia a favor de Don Segundo sería la gran concentración y densidad de rocas que se verifica en el sitio. Se definen las actividades de producción lítica a través de los análisis técnico-morfológicos de la evidencia arqueológica. En Don Segundo se dieron los primeros pasos de la secuencia de producción a través de la reducción de los bloques, extracción de formas base y preparación de bifaces. Estas tareas facilitaban el transporte a otras localizaciones donde se realizaron los pasos siguientes. Se analiza la representación de esta materia prima entre los conjuntos líticos de 28 sitios de la región para observar tendencias en su utilización a lo largo del tiempo y del espacio. Se concluye que su uso se verifica a lo largo de los 5000 años de ocupación de la región en todos los sitios ubicados a no más de 25 km en línea recta desde la fuente.The goal of this paper is to improve knowledge of the temporal span and uses of Don Segundo quarry, as well as the role it played in the regional lithic resource base. The quarry is located in a landscape of gentle hills, at 42º 36´ 30´´ south, and 70º 13´ 45´´ west, 2.5 km north in the middle Chubut valley, at 600 meters above sea level. It is a large lithic quarry (10,300 m² where a clastic sedimentary rock was available to the hunter-gatherers who inhabited the Piedra Parada area (Northwest of the Chubut province since AD 5000. The good properties of the rocks, the way in which it appears (outcrops, and the site's high visibility, are factors that would have

  18. Integrating bio-, chemo- and sequence stratigraphy of the Late Ordovician, Early Katian: A connection between onshore and offshore facies using carbon isotope analysis: Kentucky, Ohio, USA

    Young, Allison; Brett, Carlton; McLaughlin, Patrick


    A common problem in stratigraphic correlation is the difficulty of bridging shallow water shelf carbonates and down ramp shale-rich facies. This issue is well exemplified by the Upper Ordovician (lower Katian) Lexington Limestone of Kentucky, USA and adjacent dark shale facies in the deeper water Sebree Trough, an elongate, narrow bathymetric low abruptly north of the outcrop belt in the Ohio subsurface. Chronostratigraphic schemes for this interval have been proposed on the basis of conodont and graptolite biostratigraphy, mapping of event beds, and sequence stratigraphy through facies analysis. The relation of the siliciclastic rich offshore records of the "Point Pleasant-Utica" interval, well known to drillers because of its oil and gas potential, with the up-ramp shallow water carbonate dominated equivalents of the Lexington Formation is complicated by convoluted nomenclature, a major, abrupt change in facies, and disparity in the availability and completeness of records. Current genetic models of organic rich shale intervals, such as the Point Pleasant-Utica interval, are still lacking in detail, and will greatly benefit from detailed correlation with shallow water settings where more is understood about paleoclimatic conditions. In order to understand the development and evolution of this Late Ordovician Laurentian basin, it is important to understand the age relationships of depositional processes occurring at a range of depths, particularly in the less well studied epeiric sea setting of the "Point Pleasant-Utica" interval of Ohio and partial lateral equivalent, Lexington Formation of central Kentucky. The outcrop area of central Kentucky, exposed by the later uplift of the Cincinnati Arch, hosts numerous world-class exposures of the Lexington Formation, nearly all of which are representative of the highly fossiliferous, shallow-water marine platform carbonates. These successions display well differentiated depositional sequences, with sharp facies offsets

  19. Seleção de matérias-primas no desenvolvimento de formulações de massas cerâmicas Selection of raw materials in the development of ceramic bodies compositions

    L. Sánchez-Muñoz


    Full Text Available A partir de argilas de uso industrial, foram estudadas por ATD, ATG, MEV e DRX as alterações mineralógicas, microestruturais e dimensionais ocorridas com o incremento da temperatura. Com os dados de absorção de água e de retração linear foram obtidos diagramas de gresificação, propondo uma metodologia de seleção de matérias-primas para aplicação a novas massas cerâmicas.Starting from clays of industrial use, the mineralogical, microestrutural and dimensional alterations for increasing temperatures were studied by Differential Thermal Analysis, Thermogravimetric Analysis, Scanning Electron Microscopy and X-Ray Diffraction. Vitrification diagrams were obtained from water absorption and linear shrinkage data, a methodology of selection of raw materials for application to new ceramic bodies being proposed.

  20. Coal petrology of coal seams from the Leao-Butia Coalfield, Lower Permian of the Parana Basin, Brazil - Implications for coal facies interpretations

    Silva, M.B. [Laboratorio de Oceanografia Geologica, Departamento de Geociencias, Fundacao Universidade Federal do Rio Grande, FURG, Av. Italia km 08, Campus Carreiros, 96201-900, Rio Grande, RS (Brazil); Kalkreuth, W.; Holz, M. [Instituto de Geociencias, UFRGS, Av. Bento Goncalves, 9500 91501-970 Porto Alegre, RS (Brazil)


    In the Leao-Butia Coalfield, Rio Grande do Sul the coal seams occur in the Rio Bonito Formation, Guata Group, Tubarao Supergroup of the Parana Basin, Brazil and are of Permian (Artinskian-Kungurian) age. This study is the first detailed investigation on the coal petrographic characterization of the coal-bearing sequence in relation to the depositional settings of the precursor mires, both in terms of whole seam characterization and in-seam variations. The study is based on the analyses of nine coal seams (I2, CI, L4, L3, L2, L1, S3, S2, S1), which were selected from core of borehole D-193, Leao-Butia and represent the entire coal-bearing sequence. The interpretation of coal facies and depositional environment is based on lithotype, maceral and microlithotype analyses using different facies-critical petrographic indices, which were displayed in coal facies diagrams. The seams are characterized by the predominance of dull lithotypes (dull, banded dull). The dullness of the coal is attributed to relatively high mineral matter, inertinite and liptinite contents. The petrographic composition is dominated by vitrinite (28-70 vol.% mmf) and inertinite (> 30 vol.% mmf) groups. Liptinite contents range from 7 to 30 vol.% (mmf) and mineral matter from 4-30 vol.%. Microlithotypes associations are dominated by vitrite, duroclarite, carbominerite and inertite. It is suggested that the observed vertical variations in petrographic characteristics (lithotypes, microlithotypes, macerals, vitrinite reflectance) were controlled by groundwater level fluctuations in the ancient mires due to different accommodation/peat accumulation rates. Correlation of the borehole strata with the general sequence-stratigraphical setting suggests that the alluvial fan system and the coal-bearing mudstone succession are linked to a late transgressive systems tract of sequence 2. Based on average compositional values obtained from coal facies diagrams, a deposition in a limno-telmatic to limnic coal

  1. Comparisons of drier-interval to wetter-interval estuarine roof facies in the eastern and western interior coal basins, USA

    Archer, A.W.; Feldman, H.R.; Kvale, E.P.; Lanier, W.P. (Kansas State University, Manhattan, KS (United States). Dept. of Geology)


    Many of the Carboniferous coals in the eastern interior of the US are associated with siliciclastic roof facies that were deposited within a fluvio-estuarine transition. Drier-interval coals (Westphalian B-C, Stephanian) tend to be more laterally restricted and more commonly are associated with paleovalleys. Conversely, wetter-interval coals (Westphalian D) are very widespread and are not restricted to paleovalleys. Throughout the Late Carboniferous, wet paleoclimates associated with these coals lead to valley incision during sea-level lowstand when large tropical rivers downcut sediments deposited during previous sea-level highstands. During subsequent rise of sea level, these fluvial valleys were flooded and converted to estuaries. Based on modern analogs and interpretation of many examples of Carboniferous tidal rhythmites, the localized depositional rates in these settings are exceptionally high, with the estuaries becoming sediment sinks. As a result, sedimentation readily keeps pace with rising base-level. Extensive intertidal flats and shallow subtitle flats are created and prograde over the valley-confined mires. Thick tidal cycles and upright trees record rapid burial of mires. This model is supported with examples of roof facies from the Westphalian B-C of the Eastern Interior Basin, and the Stephanian of the Western Interior Basin. In these areas facies within each cycle range from well-developed, extensive paleosols and coals, to widespread marine shales or limestones. Minable, low-sulfur and low-ash coals occur, but the coals are relatively thin and discontinuous. Conversely, the Westphalian D coals are very widespread and significant peat accumulations were not confined to paleovalleys. Nonetheless, the lowest sulfur coals are related to rapid deposition of roof facies that occurred within the paleovalley whereas high-sulfur coals were formed in areas of lower sedimentation rate of roof facies that occurred beyond the confines of the paleovalley.

  2. Seismic modeling, rock physics, avo and seismic attribute analysis for illuminating sandstone facies of the Late Ordovic Ian Mamuniyat Reservoir, R-Field, Murzuq Basin-Libya

    Abushalah, Yousf Milad

    The Late Ordovician Mamuniyat Formation is the main hydrocarbon reservoir in the R-Field in Murzuq Basin, SW Libya. The Lower Mamuniyat, which is the only unit that was encountered in the study area, is composed of sandstone facies called Clean Mamuniyat and shaly sandstone facies called Dirty Mamuniyat. One major problem with the development of the R-Field is the difficulty of distinguishing the two units so this project was aimed to develop better methods for distinguishing between the two units of the Lower Mamuniyat. The other problem is to distinguish the transgressive shaly facies of the Bir Tlacsin, which has an impact on the hydrocarbon accumulation. Those issues manifested in limit of seismic resolution and interference that resulted from the converted shear mode waves. The dissertation was divided into three chapters. In the first chapter, seismic modeling using a deterministic and a Ricker wavelet were used to investigate the interference effects on the poststack seismic data and a bandpass filter was used to remove those effects. Instantaneous frequency, spectral-based colored inversion and rock physics were, then applied to determine the distributions of the sandstone facies of the Lower Mamuniyat Formation and to interpret the depositional setting of it. In the second chapter, spectral decomposition and inverted density were utilized to determine the distribution of the shaly facies of Bir Tlacsin, and its temporal thickness and to remap the top reservoir. In the last chapter, amplitude variation with offset (AVO) modeling, ray tracing, and spectral analysis were used to investigate the mode conversion and its effect on AVO signature, the amplitude of the near-mid and far offsets and frequency contents. Data enhancement then was performed using partial stacks and a bandpass filter.

  3. Sequence Stratigraphy and Sedimentary Facies of Lower Oligocene Yacheng Formation in Deepwater Area of Qiongdongnan Basin, Northern South China Sea:Implications for Coal-Bearing Source Rocks

    Jinfeng Ren; Hua Wang; Ming Sun; Huajun Gan; Guangzeng Song; Zhipeng Sun


    For unveiling coal-bearing source rocks in terrestrial-marine transitional sequences, the sequence stratigraphic framework and sedimentary facies of Lower Oligocene Yacheng Formation of Qiongdongnan Basin were investigated using seismic profiles, complemented by well bores and cores. Three third-order sequences are identified on the basis of unconformities on basin margins and cor-relative conformities in the basin center, namely SQYC3, SQYC2 and SQYC1 from bottom to top. Coal measure in Yacheng Formation of Qiongdongnan Basin were deposited within a range of facies asso-ciations from delta plain/tidal zone to neritic sea, and three types of favourable sedimentary facies as-sociations for coal measure were established within the sequence stratigraphic framework, including braided delta plain and alluvial fan, lagoon and tidal flat, and fan delta and coastal plain facies associa-tions. Results shown that, in the third-order sequences, coal accumulation in landward areas (such as delta plain) of the study area predominantly correlates with the early transgressive systems tract (TST) to middle highstand systems tract (HST), while in seaward areas (such as tidal flat-lagoon) it correlates with the early TST and middle HST. The most potential coal-bearing source rocks formed where the accommodation creation rate (Ra) and the peat-accumulation rate (Rp) could reach a state of balance, which varied among different sedimentary settings. Furthermore, intense tectonic subsidence and fre-quent alternative marine-continental changes of Yacheng Formation during the middle rift stage were the main reasons why the coal beds shown the characteristics of multi-beds, thin single-bed, and rapidly lateral changes. The proposed sedimentary facies associations may aid in predicting distribution of coal-bearing source rocks. This study also demonstrates that controlling factors analysis using sequence stratigraphy and sedimentology may serve as an effective approach for coal

  4. O estado da arte sobre o uso de resíduos como matérias-primas cerâmicas alternativas State of the art about the use of wastes as alternative to ceramic raw materials

    Romualdo R. Menezes


    Full Text Available Os resíduos industriais e urbanos vêm-se tornando um dos mais sérios problemas que a sociedade moderna enfrenta. Sua deposição de forma inadequada provoca a degradação do meio ambiente e a contaminação dos mananciais de água e do solo. Por outro lado, técnicos da indústria cerâmica se deparam com a escassez de reservas de matérias-primas de boa qualidade em locais economicamente viáveis de exploração. Assim, este trabalho objetiva apresentar uma visão geral da possibilidade de utilização dos resíduos industriais e urbanos como matérias-primas cerâmicas alternativas, enfocando a indústria cerâmica como uma fonte economicamente viável e ecologicamente correta para reciclagem de resíduos.The industrial and urban wastes have become one of the most serious problems faced by the modern society. These wastes cause environmental degradation, with pollution and contamination of water and soil. On the other hand, the ceramic industry faces scarcity of good quality raw materials in locations close to the industries. The aim of this work is to give an overview about the possibility to use industrial and urban wastes as alternative to ceramic raw materials, focusing the use in ceramic industry as an economical and environmentally safe alternative for recycling wastes.

  5. Estado da arte da aplicação do processo de hidroesterificação na produção de biodiesel a partir de matérias-primas de baixa qualidade

    Letícia Karen dos Santos


    Full Text Available O maior problema encontrado na produção de biodiesel pelos processos convencionais de transesterificação está na aquisição de matérias-primas, que devem ser de acidez e teor de umidade reduzidos, característica atendida pelos óleos vegetais refinados, o qual gera um custo elevado e inviabiliza o uso de diversas oleaginosas. O processo de hidroesterificação é a mais moderna alternativa na produção de biodiesel, pois permite o uso de qualquer matéria-prima graxa com teores elevados de acidez (ácidos graxos e umidade (água; esse processo envolve uma etapa de hidrólise seguida de esterificação. A hidrólise consiste em uma reação química entre a gordura (ou óleo com a água, gerando glicerina e ácidos graxos. Após a hidrólise, os ácidos graxos gerados são esterificados com metanol/etanol, obtendo-se o metil/etiléster com elevada pureza (biodiesel. Esse artigo traz um estudo da aplicação do processo de hidroesterificação para a produção de biodiesel utilizando óleos brutos, óleo de microalga, óleos residuais e gordura animal. Atuando em uma nova estratégia na cadeia produtiva do biodiesel, visando à solução de obstáculos técnicos, e consequentemente, contribuindo para o aumento do biodiesel na matriz energética e o desenvolvimento econômico e social deste mercado.

  6. Efectos metálicos “nobles” obtenidos mediante el desarrollo de tintas acuosas inkjet a través del empleo de materias primas cerámicas tradicionales

    S.L., Coloronda


    Full Text Available Coloronda, S.L. has tackled the technical viability of developing water-based inkjet inks (containing up to 5-μm particle sizes so as to obtain noble metallic effects by means of different raw materials traditionally used in the ceramic tile manufacturing process. In this context, several parameters and working conditions (i.e. heat treatment, temperature, particle size, chemical composition, etc. have been studied in order to examine their influence on the nucleation and crystallization mechanisms which are responsible for the physical-optical phenomena obtained on single-firing ceramic tiles.Coloronda, S.L. ha abordado la viabilidad técnica del desarrollo de tintas de inyección digital de naturaleza acuosa (con un tamaño de partícula inferior a 5 μm, con el objetivo de obtener efectos metálicos nobles a partir de materias primas tradicionalmente utilizadas por el sector cerámico. Para ello, se ha estudiado la influencia de las principales variables y condiciones de trabajo (tratamiento térmico, temperatura, distribución granulométrica, tamaño partícula, composición química, etc. sobre los mecanismos de nucleación y cristalización de las materias primas utilizadas, siendo éstos los responsables de los fenómenos ópticos producidos sobre baldosas cerámicas obtenidas por monococción.

  7. Explorando la intensidad de uso de las materias primas líticas en Pali Aike (provincia de Santa Cruz, Argentina Exploring the reduction intensity of lithic raw materials in Pali Aike (Santa Cruz province, Argentina

    Judith Charlin


    Full Text Available El objetivo general del presente trabajo es evaluar la intensidad de uso a la que estuvieron sujetas las materias primas líticas utilizadas en la manufactura de artefactos en Pali Aike (sector meridional de la provincia de Santa Cruz, Argentina. La muestra analizada comprende artefactos tallados de formatización unifacial y/o con rastros complementarios que fueron recuperados en diversas localidades del campo volcánico con ocupaciones asignadas al Holoceno tardío. Diversas variables son consideradas como indicadores de la intensidad de uso o grado de reducción de las rocas, tales como la longitud de los artefactos al momento del descarte, el grado de fragmentación de los mismos, el porcentaje de corteza que conservan, la cantidad de filos y/o puntas formatizados y/o con rastros complementarios por artefacto, el ángulo de desgaste y la reactivación de los filos y/o puntas. Los resultados obtenidos señalan la existencia de diferencias en la explotación y aprovechamiento de las materias primas líticas en algunas de estas variables, en tanto que otras no ofrecen un comportamiento diferencial o simplemente no resultan sensitivas a estos factores.The main goal of this paper is to evaluate the intensity of human utilization of lithic raw materials in Pali Aike (southern Santa Cruz Province, Argentina. The sample includes artifacts unifacially retouched and/or with macroscopic edge-wear damage from different Late Holocene localities within Pali Aike. The variables considered include the length of the artifacts, fragmentation, amount of retouched and/or wear damaged edges and/or points by artifact, percentage of cortex, and resharpening. The results show that some variables point to differences in the intensity of exploitation of different raw materials, while others are not sensitive to this variation.

  8. Rocas para moler: análisis de procedencia de materias primas líticas para artefactos de molienda (área Interserrana Bonaerense Rocks For Grinding: Lithic Raw Material Provenience Studies Of Grinding Technology, Interserrana Area Of Buenos Aires Province, Argentina

    Alejandra B. Matarrese


    Full Text Available Los artefactos de molienda representan frecuentemente grandes volúmenes de roca trasportados a los sitios arqueológicos del área Interserrana Bonaerense. En el contexto de los recientes estudios sistemáticos en relación a estos artefactos, en este trabajo se presentan los resultados de los análisis macroscópicos, de cortes delgados y de difracción de rayos X de una muestra de instrumentos confeccionados sobre materias primas sedimentarias y metamórficas. De manera complementaria, se consideran características de las formas-base y los pesos de parte de los artefactos estudiados. Los datos obtenidos se discuten respecto a la procedencia y estrategias de explotación de estos recursos líticos utilizados para los artefactos de molienda. Se identificó en los conjuntos estudiados el uso de rocas disponibles en afloramientos de los sistemas serranos pampeanos de Tandilia y Ventania e interserranos. El trasladado de estas materias primas líticas a los contextos bajo estudio implicaron diferentes esfuerzos de aprovisionamiento (locales, de media y de larga distancia. Las características petrográficas de las rocas seleccionadas para la producción de los artefactos de molienda se relacionan principalmente con una alta capacidad abrasiva. En algunos casos, se habrían aprovechado formas-base naturales aptas para ser usadas sin modificaciones previas. Estos datos comprenden un primer acercamiento a la gestión de recursos líticos para la manufactura y/o uso de artefactos de molienda por parte de grupos cazadores-recolectores prehispánicos pampeanos durante el Holoceno tardío.Grinding tools frequently comprise great volumes of rocks transported to the archaeological sites of the Interserrana area of Buenos Aires Province. The results from thin section and X-ray diffraction analyses of a sample of grinding artifacts manufactured from sedimentary and metamorphic raw material are presented in this paper in the context of recent systematic

  9. Aplicaciones de los minerales arcillosos de Cayo Guan, Cuba, como adsorbentes de metales pesados y materia prima cerámica

    Fonseca, D.


    Guan, municipio de Moa, hay junto a las importantes explotaciones industriales de lateritas, minerales arcillosos cuya caractarización química, mineralógica y evolución de fases con la temperatura han sido objeto de estudio por estos autores en un anterior trabajo; entre las características físicas, químicas y mineralógicas del yacimiento destacan los altos contenidos de óxidos de hierro y aluminio, bajas concentraciones de SiO2 y óxidos alcalinos, y la caolinita como mineral más abundante, además de hematita, gibsita y goethita en forma de geles. Se pretende en esta investigación estudiar sus propiedades tecnológicas para dilucidar la posible aplicabilidad a estos recursos minerales en la fabricación de ladrillos, baldosas de pasta roja, gres rústico y para la inmovilización de metales pesados en efluentes acuosos. El estudio por microscopía óptica de calefacción de los minerales arcillosos, indica que son unos materiales refractarios cuyo reblandecimiento aparece después de los 1500 ºC. El diagrama de trabajabilidad de las diferentes arcillas y el cálculo de la plasticidad por el método de la cuchara de Casagrande presentan dentro de la zona favorable para la extrusión sólo a una de las muestras. Los diagramas de gresificación informan que es a partir de 1400 ºC cuando se consigue una capacidad de absorción de agua < 0,6 %. El diseño de un programa ha posibilitado el cálculo de múltiples composiciones de un gres porcelánico preparado a partir de dichas arcillas, modificadas con materias primas de bajo coste que facilitan la formación de fase vítrea (feldespato potásico y casco de vidrio y/o incrementan el contenido de sílice (arena y diatomea utilizada como filtros en la industria cervecera. Se presentan los resultados de una de ellas (60 % de mineral arcilloso, 30 % de feldespato potásico y 10 % de diatomea que calcinada a 1250 ºC con una velocidad de calentamiento de 15 ºC/min dio lugar a una absorción de agua

  10. Radar facies and architecture of alluvial fans and related sediments in high-energy alpine environments, British Columbia

    Ekes, Csaba


    It is widely recognized that the dominant depositional processes on alluvial fans include rock falls, rock slides, rock avalanches, debris flows, sheetfloods and incised-channel floods. A fundamental question addressed in this thesis is: Can ground penetrating radar (GPR) differentiate between the sediments associated with these processes? Do these individual deposits have characteristic radar reflection signatures? The dissertation is divided into two parts. In part one, a calibration exercise conducted in southern British Columbia, it was demonstrated that GPR was able to obtain good penetration and resolution in rock fall, rock slide, fluvial and alluvial fan sediments, and that a characteristic radar reflection pattern (or radar facies) can be assigned to these deposits. Bedrock reflection pattern is characterised by a discontinuous radar signal and by stacked diffractions. The radar facies for rock slide and rock avalanche sediments, where boulders constitute the predominant clast size, is characterized by discontinuous, high amplitude, macro-scale, hyperbolic reflections that are different from diffractions generated by bedrock. Alluvial fans dominated by debris flow processes produce a chaotic and discontinuous radar pattern; diffractions in these patterns are attributed to boulders. Alluvial fans dominated by sheetflood processes are likely to produce surface-parallel, gently dipping, more or less continuous radar patterns. Large-scale meandering-river radar-patterns are characterized by high amplitude, continuous, dipping clinoforms. Braided-river radar facies, based on data collected on the Kicking Horse braidplain, are characterized by predominantly horizontally continuous reflections with few identifiable features. Based solely on GPR data, it was possible to distinguish between sediments of meandering and braided rivers. Analysis of over 95 km GPR data suggests that alluvial fan radar-reflection patterns are distinctly different from those observed in

  11. Syn-metamorphic interconnected porosity during blueschist facies reactive fluid fluxes at the slab-mantle interface

    Konrad-Schmolke, Matthias; Klitscher, Nicolai; Halama, Ralf; Wirth, Richard; Morales, Luiz


    At the slab-mantle interface in subdution zones fluids released from the downgoing plate infiltrate into a mechanical mixture of rocks with different chemical compositions, different hydration states and different rheological behaviour resulting in a highly reactive mélange within a steep temperature gradient. Fluid pathways, reaction mechanisms and reaction rates of such fluxes, however, are poorly known, although these parameters are thought to be crucial for several seismic phenomena, such as those commonly referred to as slow earthquakes (e.g., episodic tremor and slip (ETS)). We discovered syn-metamorphic fluid-pathways in the form of interconnected metamorphic porosity in eclogite and blueschist facies mélange rocks from the Franciscan Complex near Jenner, CA. The sampled rocks occur as rigid mafic blocks of different sizes (cm to decametre) in a weak chlorite-serpentine matrix interpreted to be an exhumed slab-mantle interface. Some of these mafic blocks record reactive fluid infiltration that transforms dry eclogite into hydrous blueschist with a sharp reaction front clearly preserved and visible from outcrop- down to µm-scale. We can show that a number of interconnected fluid pathways, such as interconnected metamorphic porosity between reacting omphacite and newly formed sodic amphibole enabled fluid infiltration and interface coupled solution-reprecipitation reactions at blueschist facies conditions. We investigated the different types of fluid pathways with TEM and visualized their interconnectivity with 3D focused ion beam (FIB) sections. The eclogitic parts of the samples preserve porous primary omphacite as a product of amphibole and epidote breakdown during subduction. This primary porosity in omphacite I results from a negative volume change in the solids during amphibole and epidote dehydration. The resulting pores appear as (fluid filled) elongated inclusions the orientations of which are controlled by the omphacite lattice. During

  12. Podstawy teoretyczne rozważań bioetycznych. Analiza postaw studentów wobec wybranych problemów medycznych

    Kopka, Jolanta


    Theoretical part of this article includes presentation of a few chosen ethical positions, which may variously imply moral decisions: natural law, utilitarianism, consequentalism, deontology and ethics of obligations prima facie. Empirical part presents results of questionnaire research made on 100 students of sociology and 170 students of medicine on the subject of their opinions on: abortion, euthanasia, transplants from the dead and embryos, cloning of cells and persons, gene...

  13. Protolith age of Santa Maria Chico granulites dated on zircons from an associated amphibolite-facies granodiorite in southernmost Brazil

    Léo A. Hartmann


    Full Text Available U-Pb dating of zircon was undertaken with the Beijing SHRIMP II (sensitive high resolution ion microprobe on anamphibolite facies granodiorite and an almandine-albite granulite from the Santa Maria Chico Granulitic Complex, southern Brazilian Shield. This work was also done to unravel protolith ages which are often hidden in the array of partly reset data. The obtained metamorphic ages of the granodiorite gneiss and the granulite are 2035 ± 9 Ma and 2006 ± 3 Ma, respectively. These data are within the range of metamorphic ages determined in previous studies (2022 ± 18 Ma and 2031 ± 40 Ma. However, protolith ages for the granodiorite (2366 ± 8 Ma and the granulite (2489 ± 6 Ma were obtained which are outside the previously recognized range (> 2510-2555 Ma. The magmatic protolith age of the granodiorite refers to a previously little known magmatic event in the shield. Further investigations may demonstrate that amphibolite facies zircon crystals are useful as a window into geological events in associated granulites, because zircon ages are blurred in the studied granulites.Um granodiorito de fácies anfibolito e um almandina-albita granulito do Complexo Granulítico Santa Maria Chico, porção sul do Escudo Brasileiro, foram datados pelo método U-Pb em zircão por Beijing SHRIMP II (sensitive high resolution ion microprobe. Esta investigação inclui a determinação das idades de protólitos que estão ocultas no conjunto de dados parcialmente re-equilibrados. As idades metamórficas obtidas no gnaisse granodiorítico e no granulito são 2035 ±9 Ma e 2006 ±3 Ma, respectivamente. Esses dados estão dentro da variação das idades metamórficas determinadas em estudos anteriores (2022 ±18 Ma e 2031 ±40 Ma. No entanto, as idades do protólito do granodiorito (2366 ±8 Ma e do granulito (2489 ±6 Ma estão fora da variação de idades ( > 2510-2555 Ma reconhecidas anteriormente. A idade magmática do protólito do granodiorito corresponde

  14. Late Jurassic blueschist facies pebbles from the Western Carpathian orogenic wedge and paleostructural implications for Western Tethys evolution

    Dal Piaz, Giorgio V.; Martin, Silvana; Villa, Igor M.; Gosso, Guido; Marschalko, Robert


    In spite of the absence of ophiolitic slices at the surface, some traces of the lost Tethys ocean are recorded along the Pieniny Klippen Belt (PKB), a narrow décollement thrust system sutured at the transpressive boundary between the Outer and Inner Carpathians. The enigmatic precollisional evolution of Western Carpathians can be deciphered from some late Albian to Campanian flysch conglomerates which display chrome spinel grains, ophiolitic detritus and pebbles of blueschist facies tholeiitic metabasalts yielding a 40Ar/39Ar plateau age of 155.4+/-0.6 Ma. Other detrital components are represented by extrabasinal pebbles of limestones, arc volcanics, and igneous to metamorphic basement rocks from southern sources. Our results suggest a markedly northward extension of the sublongitudinal Triassic Vardar (Meliata) Ocean and its subduction since the late Middle Jurassic, supposedly balanced westward by coeval spreading in the Ligurian-Piedmont basin of the Apennine-Western Alpine Tethys. A lateral kinematic connection between these diachronous and roughly parallel Tethys branches was provided on the north by a left-lateral east-west trending shear zone running from the Swiss-Austrian Penninic domain to the Northern Carpathians. This reconstruction replaces the classic model of two paired North Penninic and South Penninic oceanic basins and eastern homologues with the Briançonnais-Hochstegen and Czorstin microcontinents in between. The Late Jurassic-Early Cretaceous evolution of the Carpathian active margin was characterized by subduction metamorphism and accretion of a wide orogenic wedge; in this time, the shallowing to deeply subsiding basins inferred from facies analyses on the sedimentary units of the PKB were likely floored by individual sections of the growing wedge. Later, some exhuming blueschist ophiolitic units of the wedge were uplifted to the surface and functioned in the Albian-Campanian as an ``exotic ridge'' supplying clasts to the forearc basin

  15. Facies, stratal and stacking patterns of syn-rift sequences along present-day and fossil hyperextended rifted margins

    Ribes, Charlotte; Epin, Marie-Eva; Gillard, Morgane; Chenin, Pauline; Ghienne, Jean-Francois; Manatschal, Gianreto; Karner, Garry D.; Johnson, Christopher A.


    Research on the formation and evolution of deep-water rifted margins has undergone a major paradigm shift in recent years. An increasing number of studies of present-day and fossil rifted margins allows us to identify and characterize the architecture of hyperextended rifted margins. However, at present, little is known about the depositional environments, sedimentary facies and stacking and stratal patterns in syn-rift sequences within these domains. In this context, characterizing and understanding the spatial and temporal evolution of the stratal and stacking patterns is a new challenge. The syn-rift sequence at rifted margins is deposited during the initial stages of stretching to the onset of oceanic accretion and comprises pre-, syn- and post-kinematic deposits along the margin. A difficulty arises from the fact that the observed stratigraphic geometries and facies relationships result from the complex interplay between sediment supply and creation of accommodation, which in turn are controlled by regional synchronous events (i.e. crustal necking and onset of seafloor spreading) and diachronous events (i.e. migration of deformation during rifting, lags in sediment input to the distal margin). These parameters are poorly constrained in hyperextended rift systems. Indeed, the complex structural evolution of hyperextended systems include an evolution from initially distributed to localized extension (i.e. necking) and the development of poly-phase in-sequence and/or out of sequence extensional faulting associated with mantle exhumation and magmatic activity. This multiphase structural evolution can generate complex accommodation patterns over a highly structured top basement but can only be recognized if there is sufficient sediment input to record the events. In our presentation, we show preliminary results for fossil Alpine Tethys margins exposed in the Alps and seismic examples of the present-day deep water rifted margins offshore Australian-Antarctica, East

  16. New age data and geothermobarometric estimates from the Apuseni Mountains (Romania); evidence for Cretaceous amphibolite-facies metamorphism

    Reiser, Martin; Schuster, Ralf; Spikings, Richard; Tropper, Peter; Fügenschuh, Bernhard


    New Ar-Ar ms, Rb-Sr bt and Sm-Nd grt age data in combination with microprobe analyses and structural data from the Apuseni Mountains provide new constraints for the tectonic evolution of the Tisza and Dacia Mega-Units during the Late Jurassic-Late Cretaceous time interval, which is of special importance for the present day arrangement of tectonic units in the Alpine-Carpathian-Dinaridic region. Late Jurassic obduction of Transylvanian Ophiolites (155 Ma) partially reset Ar-Ar ms ages at the top of the Biharia Nappe System in the Dacia Mega-Unit. New Sm-Nd grt ages and P-T estimates yielded amphibolite-facies conditions of 500°C and about 0.8 GPa during the Early Cretaceous (125 Ma Sm-Nd age) for the Dacia Mega-Unit and during late Early Cretaceous times (104 Ma Sm-Nd age) for the Tisza Mega-Unit. This implies that not only the Dacia Mega-Unit, but also the Tisza Mega-Unit experienced a strong regional metamorphic overprint accompanying Alpine deformation. New 95 Ma Ar-Ar ms and 81 Ma Rb-Sr bt ages from the Bihor Nappe (Tisza Mega-Unit), in combination with fission track ages constrain rapid cooling of more than 20°C/Ma after the thermal maximum. The amplitude of cooling corresponds to data from the Dacia Mega-Unit, which started cooling 20 Ma earlier, but at a rate of only about 12°C/Ma. Kinematic indicators and stretching lineations show NE-directed, in-sequence nappe stacking for the Tisza and Dacia Mega-Units during "Austrian Phase" deformation (125-100 Ma). Following the Austrian Phase, the Dacia Mega-Unit was thrust over the Tisza Mega-Unit during the Turonian Phase (93-89 Ma). Constrained through NW-directed kinematic indicators and 94-80 Ma Rb-Sr bt ages, this tectonic phase is responsible for a pervasive retrograde greenschist-facies overprint and the geometry of the present-day nappe stack in the Apuseni Mountains.

  17. Sedimentología y petrología de los abanicos aluviales y facies adyacentes en el Neogeno de Paracuellos de Jarama (Madrid

    Alonso, M.


    Full Text Available Lateral and vertical variations of middle Miocene lithofacies (Lower and Intermediate Units of the Miocene of the Madrid Basin have been analyzed in the Paracuellos de Jarama area, near Madrid. A complete transition from medial to distal alluvial fan facies and palustrinelshaltow 1acustrine deposits can be observed. This sedimentary evolution is inferred from the detailed sedimentological. analysis carried out in each of the previously defined lithostratigraphic units: a1 Green shale and dolomite Unit, a2 Brown clays, arkosic and carbonate Unit; these two units are linked together into a Lower Group. b Coarse Arkosic Unit (Upper Group. Facies relationsbips within the Lower Group show a lateral change pattern between alluvial fan deposits, and palustrine deposits. Also the former ones gradually prograde over the palustrine deposits, as deduced from vertical evolution in the southernmost parts of the area. Upper Group represents a sudden progradation of the alluvial fan systems, that extensively overlie the distal facies observed in the Lower Group.
    Wide development of calcretes, sepiolite deposits, and nodular chert is an outstanding feature in the most distal parts of the alluvial fan bodies. They are studied in some detail provided the scarcity of well described examples of facies relationships in the kinds of deposits.

    Se estudia en este trabajo la variación lateral y vertical de las litofacies del Mioceno medio (Unidades Inferior e Intermedia en el área de Paracuellos de Jarama, próxima a Madrid, quedando representada en este área una transición completa entre depósitos de facies medias de abenícos aluviales y depósitos de ámbitos palustres. Estas conclusiones se extraen a partir del análisis sedimentológico realizado en cada una de las unidades previamente definidas: a Unidad de arcillas verdes y carbonatos y Unidad de arcillas pardas, arcillas y carbonatos en el Conjunto Inferior; b Unidad de

  18. Hydrogeochemical Facies of Hot Springs Water in Jebel Mara Mountain, Darfur, Western Sudan

    Sami H. Mohamed


    Full Text Available Hydrogeochemical assessment have been carried out to study the concentration ofNa+, K+, Mg2+, Ca2+, Cl-,SO42-, HCO3-, and other parameters like temperature, pH, electric conductivity (EC, total hardness(T.H and total dissolved solid (TDS in ten hot springs water samples of some parts of Jebel Mara Mountain, Western Sudan. The results of water analysis revealed the average values of pH,electrical conductivity, total dissolved solids and total hardness, 9.46, 428 µS/cm, 667.2 mg/l and 102 mg/l respectively. The pH, TDS and EC variations confirmed light-salty nature of groundwater. It is also apparent from the results that, average concentrations of sodium, potassium, calcium,magnesium, chloride, sulphate,and bicarbonate ions were 43.6, 16.4, 53.7, 44, 37.5, 26.2, 428.5 mg/l, respectively. Chloride ion concentration ranged from (30 to 46 mg/l, sulphate ion concentration ranged from (10 to 40mg/l and carbonate concentration measured ranged from (215 to 800 mg/l.The results were found to be above the recommended values given by W.H.O., 1984 and warranty further recommended studies for the best improvement and utilization of springs water.

  19. Coal facies evolution of the main minable coal-bed in the Heidaigou Mine, Jungar Coalfield, Inner Mongolia, northern China


    The No. 6 Coal-bed from the Heidaigou Mine, Jungar Coalfield, Inner Mongolia is a super-large Ga deposit. The dominant carrier of Ga is boehmite in coal. The study of coal facies may provide genetic enrichment information of Ga and its carrier (boehmite) in the Ga deposit. On the basis of study on coal petrology and mineralogy, it was found that the No. 6 Coal-bed from the Heidaigou Mine of Jungar was enriched in inertinites and the microlitho-types were dominated by clarodurite. The maceral morphological features and association indicate that the coal-bed was formed in a dry sedimentary environment or in a periodic dry sedimentary environment caused by the alternating variations of groundwater level. The optimum conditions for the enrichment of Ga and its particular carrier (boehmite) were dominated by four transitional conditions: (1) the upper delta plain which was the transitional zone between alluvial and lower delta plains, (2) the transitional zone between the dry and wet forest swamps, being slightly apt to the dry one, (3) the transitional tree density between the thick and loose ones, and (4) the low moor that was the transitional zone between two high moors during peat accumulation.

  20. Carbonate facies of the Upper Triassic Ojo Huelos Member, San Pedro Arroyo Formation (Chinle Group), southern New Mexico: Paleoclimatic implications

    Tanner, Lawrence H.; Lucas, Spencer G.


    The Upper Triassic (Adamanian LVF) Ojo Huelos Member of the San Pedro Arroyo Formation (Chinle Group) is a distinctive, carbonate-rich unit that occurs in the lower Chinle section of central New Mexico. The member consists mainly of micritic lime mudstones, ostracodal wackestones to grainstones, peloidal grainstones and distinctive pisolitic rudstones, interbedded with fine-grained siliciclastic mudstones. Most limestones exhibit some evidence of pedogenic brecciation and root penetration, and porous fabrics similar to those of modern limestone tufas occur locally. The interbedded mudstones are typically lenticular and commonly display a blocky ped fabric in which subequant peds are separated by sparry calcite veins. Fossils from the Ojo Huelos Member are freshwater (darwinulid) ostracodes, various freshwater fishes and aquatic/amphibious tetrapods-metoposaurs and phytosaurs. We interpret the carbonate facies as the deposits of carbonate lakes, ponds and wetlands that were partly spring-fed, whereas the interbedded and surrounding mudstones were alluvial in origin. The groundwater and overland hydrology of the region was likely controlled by the relative proximity to an upland recharge area in the Mogollon Highlands to the south, but sedimentary fabrics record strong overprinting by desiccation and pedogenic reworking. Consequently, we interpret the Ojo Huelos Member as recording a climate that varied from subhumid to semi-arid, which caused episodic falls in the hydrologic base-level. This resulted in landscape degradation, exemplified by significant pedogenic and erosional reworking of the carbonate sediments and fluvial incision.

  1. Sedimentary Facies Controls on the Upscaling of Petrophysical Properties from Core to Log Scales and Its Implications to Petroleum Exploration

    LiuKeyu; BrettTopham; LincolnPaterson; PeterEadington; PangXiongqi


    The clastic sedimentary realm comprises a number of genetically distinct depositional systems, which are dominated by distinct depositional processes. A variogram and a Levy-stable probability distribution-based geostatistical method have been applied to analyze petrophysical properties from well logs and cores from a variety of depositional environments in sedimentary basins from Australia to quantify the heterogeneity and upscaling range of different depositional systems. Two reservoir sequences with contrasting sedimentary facies, depositional processes and a diagenetic history are investigated for their petrographic, petrophysical and log characters and their scaling behaviour. The microscopic derived petrophysical parameters, including visual porosity, grain size, sorting and amount of matrix, core plug measured porosity and permeability and log-derived V-shale, porosity and permeability, have been found to be well correlated (]R]=0.72 to 0.91) across all the scales for the reservoir sequence deposited under a single predominant depositional process and a gradational change of the energy regime (Bilyara-1). In contrast, for the reservoir sequence (East Swan-2), which was deposited in heterogeneous processes and underwent diagenetic alteration, the crosscorrelation of the petrophysical properties derived from the three different scales is extremely poor (|R|=0.01-0.54). Logderived porosity and permeability for a thinly bedded reservoir sequence with an individual bed thinner than one metre can therefore be affected by the intrinsic averaging effects of the logging tools.

  2. Petrography of gypsum-bearing facies of the Codó Formation (Late Aptian, Northern Brazil

    Jackson D.S. Paz


    Full Text Available An original and detailed study focusing the petrography of evaporites from the Late Aptian deposits exposed in the eastern and southern São Luís-Grajaú Basin is presented herein, with the attempt of distinguishing between primary and secondary evaporites, and reconstructing their post-depositional evolution. Seven evaporites phases were recognized: 1. chevron gypsum; 2. nodular to lensoidal gypsum or anhydrite; 3. fibrous to acicular gypsum; 4. mosaic gypsum; 5. brecciated gypsum or gypsarenite; 6. pseudo-nodular anhydrite or gypsum; and 7. rosettes of gypsum. The three first phases of gypsum display petrographic characteristics that conform to a primary nature. The fibrous to acicular and mosaic gypsum were formed by replacement of primary gypsum, but their origin took place during the eodiagenesis, still under influence of the depositional setting. These gypsum morphologies are closely related to the laminated evaporites, serving to demonstrate that their formation was related to replacements that did not affect the primary sedimentary structures. The pseudo-nodular anhydrite or gypsum seems to have originated by mobilization of sulfate-rich fluids during burial, probably related to halokinesis. The rosettes of gypsum, which intercept all the other gypsum varieties, represent the latest phase of evaporite formation in the study area, resulting from either intrastratal waters or surface waters during weathering.Neste trabalho, é apresentado um estudo original e detalhado enfocando os aspectos petrográficos dos evaporitos de depósitos aptianos superiores expostos no sul e leste da Bacia de São Luís-Grajaú. O objetivo é o estabelecimento de critérios que permitam distinguir entre evaporitos primários e secundários, além da reconstrução de sua evolução pós-deposicional. Sete fases de evaporitos foram reconhecidas: 1. gipsita em chevron; 2. gipsita ou anidrita nodular a lenticular; 3. gipsita fibrosa a acicular; 4. gipsita em

  3. Fabrics, Facies And Flow Through A Large-Volume Ignimbrite: Pampa De Oxaya, Chile.

    Platzman, Ellen; Cooper, Frances


    Large volume pyroclastic currents form during some of the most destructive volcanic eruptions on the planet, yet because they are underrepresented in the geological record they remain poorly understood. The Miocene Oxaya ignimbrites, exposed along the western Andean slopes in northern Chile, form one of the largest ignimbrite provinces on earth. We use anisotropy of magnetic susceptibility (AMS) in conjunction with rock magnetic measurements to investigate flow behavior and depositional processes in one of the largest members of the Oxaya succession, the Cardones ignimbrite. Despite its prominence the location of the source caldera remains unknown and fundamental processes remain poorly constrained. During 2012 nearly 8km (7,773m) of core was recovered from the early Miocene ignimbrites in 11 holes at elevations ranging from 2336m to 3805m along the Andean escarpment east of Arica, Chile. The drill cores are remarkable in that they penetrate through the entirety of the ignimbrite sequence and into the basement below. Samples for this study were collected from a > 1 km long core drilled at an altitude 3692m. The core sampled 981 m of Cardones ignimbrite and 15 m of underlying sediments and volcaniclastics before penetrating 148 m of basement. Detailed measurements of the variation in bulk magnetic properties including natural remanent magnetization (NRM), susceptibility, ARM, and IRM, were used to monitor changes in concentration, composition and grainsize of the magnetic components though the ignimbrite. AMS in conjunction with detailed rock magnetic measurements were used to constrain flow processes. The data reveal a well-defined flow direction and systematic variations in flow processes with depth. Low field bulk magnetic susceptibility averages 3.2x10-3 SI. Rock magnetic studies and petrographic examination indicate that magnetite is likely to be the dominant magnetic phase although paramagnetic mineral phases also contribute to the magnetic fabric. The degree

  4. Equatorial Layered Deposits in Arabia Terra, Mars: Facies and Process Variability

    Pondrelli, M.; Rossi, A.; van Gasselt, S.; Le Deit, L.; Glamoclija, M.; Cavalazzi, B.; Franchi, F.; Fueten, F.; Hauber, E.; Zegers, T.


    evidence of sedimentary structures. Polyhydrated sulfates have been detected. At places, ELDs appear to be linked to and possibly sourced from tectonically controlled lineaments. Large cone-shaped mounds (100 to 500 m) are situated locally on top of ELDs. They consist of boulders embedded in a matrix, and about one-third of them display an orifice at their top. Outside of the craters, ELDs show large-scale cross stratification associated to duneforms, which suggests an aeolian origin possibly associated to playa deposits. We distinguish between fluid expulsion ELDs forming within the crater and aeolian ELDs outside and possibly inside the craters. Fluid expulsion ELDs would result from groundwater upwelling and following evaporitic precipitation, whereas aeolian ELDs would result from reworking and redeposition of the spring ELDs. References Allen and Oehler (2008), Astrobiology, 8, 1093-1112. Andrews-Hanna et al. (2007), Nature, 446, 163-166. Cavalazzi et al. (2007), Sed. Geol., 200, 73-88. Gendrin et al. (2005), Science, 307, 1587. Glamoclija et al. (2011), Geomicrob. J., 29, 733-751. Hoefen et al. (2003), Science, 302, 627-630. Panieri et al. (2010), Geobiology, 8, 101-111. Pondrelli et al. (2011), EPSL, 304, 511-519. Rossi et al. (2008), JGR, 113(8).

  5. Unraveling eclogite-facies fluid-rock interaction using thermodynamic modelling and whole-rock experiments: the in-situ eclogitization of metapelites from Val Savenca (Sesia Zone, Western Alps)

    Jentsch, Marie; Tropper, Peter


    A common feature of HP and UHP terranes is the subduction of crustal rocks to great depths. Previous investigations have shown that this process is triggered by fluids present during an eclogite-facies metamorphic overprint. An examples is exposed in the metapelites at Val Savenca in the Sesia-Lanzo Zone, Italy where Alpine eclogite-facies metamorphism and fluid flow led to partial transformation of Variscan amphibolite-eclogite facies metapelites (garnet + biotite + sillimanite + K-feldspar + plagioclase + quartz) to zoisite ± jadeite + kyanite + phengite + quartz. This transformation took place under P-T conditions of 1.7 - 2.1 GPa at 600°C and low a(H2O) of 0.3-0.6. The replacement of plagioclase by jadeite + zoisite + kyanite + quartz takes place also along former fractures. Biotite is replaced by the assemblage phengite + omphacite ± kyanite adjacent to former plagioclase, otherwise by phengite + rutile/titanite. Garnet and clinopyroxene show variable compositions depending in which micro-domain (plagioclase or biotite) they grew. The extreme development of microdomains can best be studied by thermodynamic pseudosection modelling of individual microdomains using stoichiometric mixtures of protolith minerals from this domain and the program DOMINO (De Capitani & Petrakakis, 2010). The aim of these calculations was: 1.) to reproduce the observed mineral assemblage and 2.) to provide constraints on the amount of fluid present in the transformation. The results so far indicate that the amount of fluid was very low, otherwise paragonite would have formed instead of jadeite and reproduction of the observed mineral assemblage has only been partly successful so far since biotite is still stable in the calculations. In addition to understand the role of fluids in the mineralogical and textural transformation piston-cylinder experiments with a fresh, natural orthogneiss granulite from the Moldanubic Unit in upper Austria with the assemblage garnet + biotite + K

  6. La llamada «Facies del País Vasco» del Magdaleniense inferior cantábrico. Apuntes estadísticos.

    Pilar Utrilla


    Full Text Available Se estudia la facies del Magdaleniense Inferior, llamada del País Vasco, comparándola, mediante un análisis factorial, al resto de los yacimientos cantábricos de esta época. Efectuados varios tipos de pruebas, los resultados vienen a ser similares con individualización de los yacimientos de facies Juyo por un lado, del grupo vasco dominado de Duruthy por otro, de los más tardíos en un tercero y, en ocasiones, los que hemos llamado de «concentración» de gentes, en un cuarto bloque. Aquí se enmarcan Castillo, Altamira, Tito Bustillo y, sorprendentemente, también Ermittia y en algún caso Aitzbitarte. El grupo vasco y el tardío presentan, por lo general, intercorrelaciones de factores bastante altas, llegando a fundirse a veces en un solo grupo.

  7. Experiments to constrain the garnet-talc join for metapelitic material at eclogite-facies conditions

    Chmielowski, Reia M.; Poli, Stefano; Fumagalli, Patrizia


    Increasing pressure due to the subduction of mica-dominated sediments results in a loss of biotite as garnet-talc becomes a stable assemblage. While this transition is observed in natural samples, it has not yet been well constrained experimentally. Previous experimental investigations into metapelitic compositions at the University of Milan (Poli and Schmidt 2002, Ferri et al., 2009) indicated that further work in the range of 600-700° C, 2-3 GPa was required to elucidate this tie-line transition. The assemblages leading to garnet-talc stability through tie-line flip reactions include biotite-chlorite, biotite-chloritoid, and biotite-kyanite. Furthermore the mutual stability of garnet-chlorite and chloritoid-biotite at relatively high pressure conditions below the garnet-talc field is reevaluated. Current investigations on two synthetic compositions (NM, NP) in the model metapelitic system CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O are carried out in a piston cylinder apparatus at pressures and temperatures up to 2.7 GPa and to 740°C. Experiments are buffered with graphite, and are generally run under fluid saturated conditions. Two capsules, one of each composition, are included within the pressure chamber for each experiment. The NM composition is representative of metapelites and the NP composition is representative of metagreywackes. Experiments are characterized by XRD, BSE images and EMPA. The following summary includes both current investigations and the above mentioned previous work, undertaken on the same chemical compositions. All assemblages also contain quartz, white mica, fluid ± zoisite or lawsonite. The assemblage garnet-chlorite-chloritoid ± staurolite is present at 500° C at pressures of 1.4 and 1.6 GPa. The assemblage biotite-staurolite-chlorite is present at 600° C, 1.2 GPa and at 625° C, 1.4 GPa. The assemblage biotite-chloritoid-chlorite is present at 600° C for pressures ≥ 1.3 GPa and ≤ 1.7 GPa. The assemblage garnet-chloritoid-biotite is

  8. Facies metamórficas y edades relativas de las rocas del extremo oriental del Brazo Huemul, provincia de Neuquén

    M.F. Gargiulo


    Full Text Available El estudio de las asociaciones minerales y facies metamórficas presentes en las rocas del extremo oriental del Brazo Huemul del lago Nahuel Huapi permitió establecer la sucesión temporal de aquellas unidades cuyos afloramientos son saltuarios, principalmente debido a la exuberante cubierta vegetal que caracteriza a este sector situado en el extremo sur de la provincia de Neuquén. En el área de estudio afloran rocas de composición principalmente tonalítica, que en este trabajo se correlaciona con el batolito patagónico Subcordillerano debido a que están atravesadas por dos tipos de diques básicos. Un grupo de estos diques está caracterizado por la asociación albita - clorita - epidoto - cummingtonita/grunerita - hornblenda, que indica condiciones de metamorfismo térmico transicional entre la facies de hornfels de albita - epidoto hacia la facies de hornfels de hornblenda, metamorfismo originado por la intrusión del Batolito Patagónico Cordillerano de edad cretácica. Motivo por lo cual estos diques han sido correlacionados con la Formación Montes de Oca. Los diques básicos correspondientes al otro tipo no están hornfelizados pero muestran asociaciones de metamorfismo de muy bajo grado en facies zeolita de alta temperatura (clorita + pumpellyita + laumontita + clorita/esmectita + óxidos de hierro y/o poseen alteración propilítica, por lo cual fueron asignados a la F. Ventana. La distinción entre estos dos tipos de diques permite poner en discusión la edad relativa del cuerpo tonalítico que los hospeda, proponiéndose en este trabajo una edad relativa jurásica inferior a media para el mismo.

  9. A Rare Glimpse of Paleoarchean Life: Geobiology of an Exceptionally Preserved Microbial Mat Facies from the 3.4 Ga Strelley Pool Formation, Western Australia.

    Duda, Jan-Peter; Van Kranendonk, Martin J; Thiel, Volker; Ionescu, Danny; Strauss, Harald; Schäfer, Nadine; Reitner, Joachim


    Paleoarchean rocks from the Pilbara Craton of Western Australia provide a variety of clues to the existence of early life on Earth, such as stromatolites, putative microfossils and geochemical signatures of microbial activity. However, some of these features have also been explained by non-biological processes. Further lines of evidence are therefore required to convincingly argue for the presence of microbial life. Here we describe a new type of microbial mat facies from the 3.4 Ga Strelley Pool Formation, which directly overlies well known stromatolitic carbonates from the same formation. This microbial mat facies consists of laminated, very fine-grained black cherts with discontinuous white quartz layers and lenses, and contains small domical stromatolites and wind-blown crescentic ripples. Light- and cathodoluminescence microscopy, Raman spectroscopy, and time of flight-secondary ion mass spectrometry (ToF-SIMS) reveal a spatial association of carbonates, organic material, and highly abundant framboidal pyrite within the black cherts. Nano secondary ion mass spectrometry (NanoSIMS) confirmed the presence of distinct spheroidal carbonate bodies up to several tens of μm that are surrounded by organic material and pyrite. These aggregates are interpreted as biogenic. Comparison with Phanerozoic analogues indicates that the facies represents microbial mats formed in a shallow marine environment. Carbonate precipitation and silicification by hydrothermal fluids occurred during sedimentation and earliest diagenesis. The deciphered environment, as well as the δ13C signature of bulk organic matter (-35.3‰), are in accord with the presence of photoautotrophs. At the same time, highly abundant framboidal pyrite exhibits a sulfur isotopic signature (δ34S = +3.05‰; Δ33S = 0.268‰; and Δ36S = -0.282‰) that is consistent with microbial sulfate reduction. Taken together, our results strongly support a microbial mat origin of the black chert facies, thus providing

  10. A Rare Glimpse of Paleoarchean Life: Geobiology of an Exceptionally Preserved Microbial Mat Facies from the 3.4 Ga Strelley Pool Formation, Western Australia.

    Jan-Peter Duda

    Full Text Available Paleoarchean rocks from the Pilbara Craton of Western Australia provide a variety of clues to the existence of early life on Earth, such as stromatolites, putative microfossils and geochemical signatures of microbial activity. However, some of these features have also been explained by non-biological processes. Further lines of evidence are therefore required to convincingly argue for the presence of microbial life. Here we describe a new type of microbial mat facies from the 3.4 Ga Strelley Pool Formation, which directly overlies well known stromatolitic carbonates from the same formation. This microbial mat facies consists of laminated, very fine-grained black cherts with discontinuous white quartz layers and lenses, and contains small domical stromatolites and wind-blown crescentic ripples. Light- and cathodoluminescence microscopy, Raman spectroscopy, and time of flight-secondary ion mass spectrometry (ToF-SIMS reveal a spatial association of carbonates, organic material, and highly abundant framboidal pyrite within the black cherts. Nano secondary ion mass spectrometry (NanoSIMS confirmed the presence of distinct spheroidal carbonate bodies up to several tens of μm that are surrounded by organic material and pyrite. These aggregates are interpreted as biogenic. Comparison with Phanerozoic analogues indicates that the facies represents microbial mats formed in a shallow marine environment. Carbonate precipitation and silicification by hydrothermal fluids occurred during sedimentation and earliest diagenesis. The deciphered environment, as well as the δ13C signature of bulk organic matter (-35.3‰, are in accord with the presence of photoautotrophs. At the same time, highly abundant framboidal pyrite exhibits a sulfur isotopic signature (δ34S = +3.05‰; Δ33S = 0.268‰; and Δ36S = -0.282‰ that is consistent with microbial sulfate reduction. Taken together, our results strongly support a microbial mat origin of the black chert facies

  11. Facies y ambientes del grupo Salta (cretácico-paleógeno en Tumbaya, Quebrada de Humahuaca, provincia de Jujuy

    María Cristina Sánchez


    Full Text Available Los depósitos rojos del Grupo Salta (Cretácico-Paleógeno que afloran en la quebrada de Tumbaya, margen derecha de la quebrada de Humahuaca (provincia de Jujuy, se caracterizan por presentar facies distintas a las típicas de otros lugares de la cuenca. Son facies proximales de ambiente general árido a semiárido cuya acumulación avanzó sobre el extremo N-NO del alto constituido por la dorsal Salto-Jujeña. La relación de base y de techo del depósito es de discordancia erosiva con el Grupo Mesón (Cámbrico y angular con acumulaciones cuaternarias de bajada respectivamente. En el afloramiento están representadas las principales unidades del Grupo Salta tanto del synrift como del postrift. El reconocimiento y estudio de las facies permitió identificar y caracterizar de base a techo los Subgrupos Pirgua, Balbuena y Santa Bárbara, y las distintas formaciones de cada subgrupo. En el Subgrupo Pirgua (arenas eólicas no es posible diferenciar sus tres unidades formacionales, por lo tanto se lo menciona como Formación Pirgua. En el Subgrupo Balbuena se reconocen las Formaciones Lecho, que consta de facies fluviales de tipo mantos de crecida, y Yacoraite que muestra condiciones ambientales transicionales, continentales y marino litoral-sublitoral carbonático influenciado por mareas y tormentas. El Subgrupo Santa Bárbara está presente con sus Formaciones Mealla, Maíz Gordo y Lumbrera que representan una sucesión fluvial granodecreciente con desarrollo de paleosuelos múltiples; se reconocen mantos de crecida asociadas a planicies fangosas.

  12. Las bioconstrucciones de corales y sus facies asociadas durante el Malm en la Cordillera Ibérica Central (provincia de Zaragoza

    Meléndez, A.


    Full Text Available The differents types of bioconstructions and associated facies in the Central Iberian Chain (Higueruelas Formation, Upper Kimmeridgian have been studied. Biohermes of different thickness (decimetric to metric and less lateral continuity are developped, highly colonized by corals, that are associated to oncolitic, bioclastic and oolitic of high energy facies, in marginal areas, near the litoral developpment. At the same time takes place an important set up of mud mounds, with a small coral colonisation, in protected arcas in a inner shelf, or in outer areas, where the action of the waves is not so effective. The environment protection is been generated in some places due to the appearance of oolitic barrier islands.Se estudian los diferentes tipos de bioconstrucciones de corales, y sus facies asociadas, presentes en el sector central de la rama aragonesa de la Cordillera Ibérica, en la Formación Higueruelas (Kimmeridgiense superior. Se desarrollan biohermos de potencias métricas a decimétricas y escasa continuidad lateral, intensamente colonizados por corales coloniales, que se encuentran asociados a facies oncolíticas, bioclásticas y oolíticas de alta energía en zonas marginales, próximas al desarrollo litoral. Al mismo tiempo tiene lugar una importante instalación de mud mounds, con escasa colonización de corales, en zonas protegidas dentro de la plataforma interna o en zonas más externas, donde la acción del oleaje no es efectiva. La protección del medio viene condicionada en algunos puntos por la aparición de islas barrera oolíticas.

  13. Rock formation characterization for carbon dioxide geosequestration: 3D seismic amplitude and coherency anomalies, and seismic petrophysical facies classification, Wellington and Anson-Bates Fields, Kansas, USA

    Ohl, Derek; Raef, Abdelmoneam


    Higher resolution rock formation characterization is of paramount priority, amid growing interest in injecting carbon dioxide, CO2, into subsurface rock formations of depeleting/depleted hydrocarbon reservoirs or saline aquifers in order to reduce emissions of greenhouse gases. In this paper, we present a case study for a Mississippian carbonate characterization integrating post-stack seismic attributes, well log porosities, and seismic petrophysical facies classification. We evaluated changes in petrophysical lithofacies and reveal structural facies-controls in the study area. Three cross-plot clusters in a plot of well log porosity and acoustic impedance corroborated a Neural Network petrophysical facies classification, which was based on training and validation utilizing three petrophysically-different wells and three volume seismic attributes, extracted from a time window including the wavelet of the reservoir-top reflection. Reworked lithofacies along small-throw faults has been revealed based on comparing coherency and seismic petrophysical facies. The main objective of this study is to put an emphasis on reservoir characterization that is both optimized for and subsequently benefiting from pilot tertiary CO2 carbon geosequestration in a depleting reservoir and also in the deeper saline aquifer of the Arbuckle Group, south central Kansas. The 3D seismic coherency attribute, we calculated from a window embracing the Mississippian top reflection event, indicated anomalous features that can be interpreted as a change in lithofacies or faulting effect. An Artificial Neural Network (ANN) lithofacies modeling has been used to better understand these subtle features, and also provide petrophysical classes, which will benefit flow-simulation modeling and/or time-lapse seismic monitoring feasibility analysis. This paper emphasizes the need of paying greater attention to small-scale features when embarking upon characterization of a reservoir or saline-aquifer for CO2

  14. Identification and Large-Scale Mapping of Riverbed Facies along the Hanford Reach of the Columbia River for Hyporheic Zone Studies

    Scheibe, T. D.; Hou, Z.; Murray, C. J.; Perkins, W. A.; Arntzen, E.; Richmond, M. C.; Mackley, R.; Johnson, T. C.


    The hyporheic zone (HZ) is the sediment layer underlying a river channel within which river water and groundwater may interact, and plays a significant role in controlling energy and nutrient fluxes and biogeochemical reactions in hydrologic systems. The area of this study is the HZ along the Hanford Reach of the Columbia River in southeastern Washington State, where daily and seasonal river stage changes, hydromorphology, and heterogeneous sediment texture drive groundwater-river water exchange and associated biogeochemical processes. The recent alluvial sediments immediately underlying the river are geologically distinct from the surrounding aquifer sediments, and serve as the primary locale of mixing and reaction. In order to effectively characterize the HZ, a novel approach was used to define and map recent alluvial (riverine) facies using river bathymetric attributes (e.g., slope, aspect, and local variability) and simulated hydrodynamic attributes (e.g., shear stress, flow velocity, river depth). The riverine facies were compared with riverbed substrate texture data for confirmation and quantification of textural relationships. Multiple flow regimes representing current (managed) and historical (unmanaged) flow hydrographs were considered to evaluate hydrodynamic controls on the current riverbed grain size distributions. Hydraulic properties were then mapped at reach and local scales by linking textural information to hydraulic property measurements from piezometers. The spatial distribution and thickness of riverine facies is being further constrained by integrating 3D time-lapse electrical resistivity tomography. The mapped distributions of riverine facies and the corresponding flow, transport and biogeochemical properties are supporting the parameterization of multiscale models of hyporheic exchange between groundwater and river water and associated biogeochemical transformations.

  15. Facies analysis of Hlodufell basaltic subglacial to emergent volcano, SW Iceland: insights into sub-ice growth mechanisms and meltwater drainage

    Skilling, I. P.


    Hlodufell is a subglacial to emergent basaltic volcano located 9km south of the Langjokull ice-cap in SW Iceland. This study is the first detailed facies analysis of this well-known volcano. The vertical facies architecture of the basal half of the volcano is typical of many basaltic subaqueous (including submarine) to emergent volcanoes, comprising basal pillow mounds overlain by Surtseyan eruption-fed subaqueously-deposited sediment gravity flows. However, facies in the upper part of the edifice demonstrate the influence of variable water levels more typical of englacial lakes. The Surtseyan sequence is overlain by two subaerial lava flow and cogenetic lava-fed delta sequences, separated by a second Surtseyan sequence. In addition, the uppermost lava flows are also draped by a thin veneer of Surtseyan tephra. Both lava-fed delta sequences are unusually dominated by subaerial lava breccias. This may be due to a number of factors that influence steep slope stability but the possibility of retreating ice walls should be considered. Detailed facies analysis also revealed evidence of the influence of ice on eruptive and depositional products throughout the history of the edifice. Some of the basal pillow mounds preserve metre-sized cavities with partial hyaloclastite fills, interpreted as meltout structures formed during sub-ice growth by ice-block stoping. Some mounds also have steep chill surfaces where pillows have been compressed against a rigid wall (now absent) interpreted as ice. The peripheral pillow mounds, particularly those to the immediate south of Hlodufell (Rani area) are draped by Surtseyan eruption-fed tephra deposited by erosive meltwater streamflows. The draping tephra was derived from both the first and second Surtseyan sequences. These observations illustrate that direct ice-contact and ice-block stoping was important during initial construction of the volcano and that meltwater drainage (particularly to the south) was important throughout its

  16. Petromagnetic Properties of Granulite-Facies Rocks from the Northern North China Craton:Implications for Magnetic and Evolution of the Continental Lower Crust

    Qingsheng Liu; Hongcai Wang; Jianping Zheng; Qingli Zeng; Qingsong Liu


    This paper studies magnetic properties and composition of granulite-facies rocks of both the Neogene and Archean continental lower crust in the Neogene xenolith-bearing Hannuoba(汉诺坝) alkaline basalt and the exposed lower crustal section in the Archean Huai'an(淮安) terrain (Wayaokou (瓦窑口)-Manjinggou(蔓菁沟) profile),the northern North China Craton.It provides a unique opportunity for a comparative study of magnetic properties and composition of both the Archean and Neogene continental lower crust.We measure magnetic parameters (susceptibility kand magnetic hysteresis parameters,such as saturation magnetization Js,saturation isothermal remanent magnetization Jrs,and intrinsic coercivity Hc) of eleven Hannuoba lower crustal xenoliths and nine terrain granulites from the Archean Huai'an terrain.Results indicate that the average values of k,Js and Jrs of Archean granulites are 4 122×10-6 Sl,523.1 A/m and 74.9 A/m,respectively,which are generally higher than those of granulite-facies xenoliths (1 657×10-6 SI,163.9 A/m and 41.9 A/m,respectively).These two types of granulites contain ilmenite,(titano) magnetite,minor hematite and some "magnetic silicates" (clinopyroxene,plagioclase and biotite).The Mg-rich ilmenite in granulite-facies xenolith is relatively higher than that in terrain granulites.We observe a more evolved character as higher magnetic as well as lower Sr/Nd,Cr/Nd,Ni/Nd,Co/Nd and V/Nd ratios in terrain granulites.These differences in magnetic characteristics reflect their different origins and evolutions.The high magnetization of granulites in the Huai'an terrain represents magnetic properties of the Archean continental lower crust,and low magnetization of granulite-facies xenoliths represents magnetic properties of the Cenozoic lower crusts in the northern North China Craton.

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  1. Caracterização de matérias-primas cerâmicas do Vale do Rio Caí Characterization of ceramic raw materials from the Caí River Valley, RS, Brazil

    J. E. Zorzi


    Full Text Available Este trabalho tem como objetivo a caracterização química e mineralógica de matérias-primas argilosas utilizadas pelas indústrias cerâmicas do Vale do Rio Caí, RS. Essa região, situada entre Porto Alegre e a Serra Gaúcha, é o maior centro produtor cerâmico para construção civil do estado do Rio Grande do Sul. Apesar da importância da indústria cerâmica para a economia local e do Estado, a grande maioria das argilas disponíveis para consumo nunca foi caracterizada satisfatoriamente e não existem dados técnicos e científicos que possam orientar tanto a correta exploração das jazidas quanto o desenvolvimento de produtos cerâmicos de maior valor agregado. Neste trabalho foram feitas análises por fluorescência e difração de raios X das principais argilas utilizadas pela indústria cerâmica da região. De acordo com o método de análise hierárquica de agrupamentos e tendo como base a composição química das amostras, foram identificados três grupos de matérias-primas: argilas residuais (ou primárias e dois grupos de argilas transportadas (ou secundárias. A diferenciação das matérias-primas em grupos se manifesta também na composição de fases das amostras, tal como determinada por difração de raios X e análise racional.This work aims to characterize the chemistry and mineralogy of clay raw materials used in the heavy clay industry of the Caí River Valley, in southern Brazil. This region lies between Porto Alegre and Serra Gaúcha and is regarded as the major production center of brick and tiles in the Rio Grande do Sul. Despite the importance of this activity for both the local and state economy, the vast majority of clay raw materials have never been satisfactorily characterized, so there is not adequate data to guide its correct exploitation or to allow the development of ceramic products of higher quality. In this work X-ray fluorescence and diffraction were applied to analyze the clays largely used by

  2. Zircon U-Pb Dating of Yushugou Terrain of High-Pressure Granulite Facies in Southern Tianshan Mountain and Its Geological SIgnificance


    The Yushugou terrain of high-pressure granulite facies in southern Tianshan Mountain is composed mainly of an ophiolite suite.Most selected zirocons are round or elliptical in shape,and some are of tetragonal prism with round edges.The granulometric analyses show that they are well sorted in sedimentation.ZrO2/HfO2 ratios in zircons range from 45 to 57.these characters,together with the petrologic and geochemical characters of plagioclase-garnet-orthopyroxenite bearing zircons,indicate that the protolith of plagioclase-garnet-orthopyroxenite may be derived mainly from volcanic base surge sedimentary debris in oceanic islands and from clays formed by seafloor weathering.Zircons are simply of pyroclastic debris.The ophiolite formation age of (440±18)Ma and the first-stage metamorphic age(amphibolite or granulite facies) of (364±5) Ma were obtained with a method of multiple grains in different groups and a method of concordia plot.These ages provide important information on the temporal and spatial occurrence of southern Paleoxoic Tianshan Ocean,The subduction rate of the oceanic crust and the formation mechanism of ophiolite of granulite facies.

  3. Formation history and protolith characteristics of granulite facies metamorphic rock in Central Cathaysia deduced from U-Pb and Lu-Hf isotopic studies of single zircon grains

    YU Jinhai; ZHOU Xinmin; Y. S. O'Reilly; ZHAO Lei; W. L. Griffin; WANG Rucheng; WANG Lijuan; CHEN Xiaomin


    The petrochemical as well as zircon U-Pb and Lu-Hf isotopic studies of granulite facies metamorphic rock from the Taoxi Group in eastern Nanling Range, Central Cathaysia indicate that its protolith is the sedimentary rock with low maturation index. The clastic materials are mostly from middle Neoproterozoic (~736 Ma) granitoid rocks with minor Neoarchaean and Paleoproterozoic rocks. The timing of this Neoproterozoic magmatism is in agreement with the second period of magmatism widespread surrounding the Yangtze Block. Hf isotopic data indicate that the Neoproterozoic granitoids resulted from the recycled Paleoproterozoic mantle-derived crustal materials. The sedimentary rock was deposited in Late Neoproterozoic Era, and carried into low crust in Early Paleozoic. The partial melting of the meta-sedimentary rock took place at about 480 Ma and subsequently granulite facies metamorphism occurred at ca. 443 Ma. The zircons forming during this time interval (Early Paleozoic) show large Hf isotope variations, and their -Hf(t) values increase from -13.2 to +2.36 with decreasing age, suggesting the injection of mantle-derived materials during partial melting and metamorphism processes in the Early Paleozoic. Calculation results show that this metamorphic rock, if evolved to Mesozoic, has similar isotopic composition to the nearby Mesozoic high Si peraluminous granites, implying that this kind of granulite facies metamorphic rock is probably the source material of some Mesozoic peraluminous granitoids in eastern Nanling Range.

  4. Projections of demand of natural gas in Mexico; Proyecciones de demanda de gas