996 resultados para Córdoba, Juan
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This series will include all those people who, by means of their contributions, great and small, played a part in the consolidation of ichthyology in Argentina. The general plan of this work consists of individual factsheets containing a list of works by each author, along with reference bibliography and, whenever possible, personal pictures and additional material. The datasheets will be published primarily in chronological order, although this is subject to change by the availability of materials for successive editions. This work represents another approach for the recovery and revalorization of those who set the foundations of Argentine ichthyology while in diverse historical circumstances. I expect this to be the beginning of a major work that achieves the description of such a significant part of the history of natural sciences in Argentina.
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1 carta (mecanografiada) ; 210x274 mm. Ubicación: Caja 1 - Carpeta 19
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Detailed oxygen, hydrogen and carbon isotope studies have been carried out on igneous and metamorphic rocks of the Stony Mountain complex, Colorado, and the Isle of Skye, Scotland, in order to better understand the problems of hydrothermal meteoric water-rock interaction.
The Tertiary Stony Mountain stock (~1.3 km in diameter), is composed of an outer diorite, a main mass of biotite gabbro, and an inner diorite. The entire complex and most of the surrounding country rocks have experienced various degrees of 18O depletion (up to 10 per mil) due to interaction with heated meteoric waters. The inner diorite apparently formed from a low-18O magma with δ18O ≃ +2.5, but most of the isotopic effects are a result of exchange between H2O and solidified igneous rocks. The low-18O inner diorite magma was probably produced by massive assimilation and/or melting of hydrothermally altered country rocks. The δ18O values of the rocks generally increase with increasing grain size, except that quartz typically has δ18O = +6 to +8, and is more resistant to hydrothermal exchange than any other mineral studied. Based on atom % oxygen, the outer diorites, gabbros, and volcanic rocks exhibit integrated water/rock ratios of 0.3 ± 0.2, 0.15 ± 0.1, and 0.2 ± 0.1, respectively. Locally, water/rock ratios attain values greater than 1.0. Hydrogen isotopic analyses of sericites, chlorites, biotites, and amphiboles range from -117 to -150. δD in biotites varies inversely with Fe/Fe+Mg, as predicted by Suzuoki and Epstein (1974), and positively with elevation, over a range of 600 m. The calculated δD of the mid-to-late-Tertiary meteoric waters is about -100. Carbonate δ13C values average -5.5 (PDB), within the generally accepted range for deep-seated carbon.
Almost all the rocks within 4 km of the central Tertiary intrusive complex of Skye are depleted in 18O. Whole-rock δ18O values of basalts (-7. 1 to +8.4), Mesozoic shales (-0.6 to + 12.4), and Precambrian sandstones (-6.2 to + 10.8) systematically decrease inward towards the center of the complex. The Cuillin gabbro may have formed from a 18O-depleted magma (depleted by about 2 per mil); δ18O of plagioclase (-7.1 to + 2.5) and pyroxene (-0.5 to + 3.2) decrease outward toward the margins of the pluton. The Red Hills epigranite plutons have δ18O quartz (-2.7 to + 7.6) and feldspar (-6.7 to + 6.0) that suggest about 3/4 of the exchange took place at subsolidus temperatures; profound disequilibrium quartz-feldspar fractionations (up to 12) are characteristic. The early epigranites were intruded as low-18O melts (depletions of up to 3 per mil) with δ18O of the primary, igneous quartz decreasing progressively with time. The Southern Porphyritic Epigranite was apparently intruded as a low-18O magma with δ18O ≃ -2.6. A good correlation exists between grain size and δ18O for the unique, high-18O Beinn an Dubhaich granite which intrudes limestone having a δ18O range of +0.5 to +20.8, and δ13C of -4.9 to -1.0. The δD values of sericites (-104 to -107), and amphiboles, chlorites, and biotites (-105 to -128) from the igneous rocks , indicate that Eocene surface waters at Skye had δD ≃ -90. The average water/rock ratio for the Skye hydrothermal system is approximately one; at least 2000 km3 of heated meteoric waters were cycled through these rocks.
Thus these detailed isotopic studies of two widely separated areas indicate that (1) 18O-depleted magmas are commonly produced in volcanic terranes invaded by epizonal intrusions; (2) most of the 18O-depletion in such areas are a result of subsolidus exchange (particularly of feldspars); however correlation of δ18O with grain size is generally preserved only for systems that have undergone relatively minor meteoric hydrothermal exchange; (3) feldspar and calcite are the minerals mos t susceptible to oxygen isotopic exchange, whereas quartz is very resistant to oxygen isotope exchange; biotite, magnetite, and pyroxene have intermediate susceptibilities; and (4) basaltic country rocks are much more permeable to the hydrothermal convective system than shale, sandstone, or the crystalline basement complex.
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Investigación realizada dentro del Programa de Formación y Perfeccionamiento de Personal Investigador del Gobierno Vasco (2010-2013).
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Tesis doctoral originalmente defendida en la Universidad de Deusto el 29-09-2000
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[ES] Para más información sobre este trabajo, puede consultarse el registro: "Documentación geométrica de los restos del Teatro Romano de Córdoba", http://hdl.handle.net/10810/9167
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1 carta (manuscrita) ; 225x330 mm
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[ES] El análisis directo de los ajuares lítico y óseo que se conservan del yacimiento de San juan, nos induce a plantear una hipótesis principal, según la cual la ocupación prehistórica del depósito debió producirse fundamentalmente durante el Aziliense, aunque no puede descartarse un origen anterior, en las últimas fases del Magdaleniense.
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This series will include all those people who, by means of their contributions, great and small, played a part in the consolidation of ichthyology in Argentina. The general plan of this work consists of individual factsheets containing a list of works by each author, along with reference bibliography and, whenever possible, personal pictures and additional material. The datasheets will be published primarily in chronological order, although this is subject to change by the availability of materials for successive editions. This work represents another approach for the recovery and revalorization of those who set the foundations of Argentine ichthyology while in diverse historical circumstances. I expect this to be the beginning of a major work that achieves the description of such a significant part of the history of natural sciences in Argentina.
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Fecha: 31 de marzo de 1937 / Unidad de ínstalación: Carpeta Rectorado - D-1 / Nº de pág.: 2 (manuscritas)
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Esta serie tiene como finalidad dar a conocer las especies presentes en los diferentes estados provinciales. Tomando como base los trabajos de López et al., (2003); Reis et al., (2003); Liotta (2006) y Ferraris (2007) actualizamos el elenco ictiofaunístico de cada territorio provincial. No se realizan, con excepción del nombre vulgar y localidad tipo, comentarios y/o observaciones de las especies señaladas ya que estos se encuentran en la bibliografía adjunta. Se incluyen dos tablas que contienen información sobre especies introducidas y de aquellas de presencia dudosa o que requieran confirmación en el territorio provincial. Para éstas últimas se cita el trabajo que las menciona por vez primera. Consideramos que este modesto aporte contribuirá a precisar el conocimiento ictiofaunístico regional ya que además de la lista de especies, presentamos el marco biogeográfico e hídrico correspondiente. Por otra parte entendemos que la participación de autores involucrados en la región considerada, le da un verdadero sentido federal a esta contribución, además de reforzar vínculos en los protagonistas de nuestra especialidad. En este nuevo número presentamos la provincia de La Rioja que se encuentra enclavada en el centro-oeste de nuestro territorio, limitada por Catamarca, Córdoba, San Luis y San Juan. La familia Trichomycteridae es uno de los grupos más representativos del sistema hidrográfico de La Rioja adaptados a vivir en elevada altura y arroyos que ocasionalmente permanecen alimentados por el deshielo (López, et al., 2002). Esta familia es un ejemplo de gran adaptabilidad siendo capaz de vivir en ambientes de llanura como los de la Provincia de los Grandes Ríos (López et al., 2008) así como también en arroyos cordilleranos a más de 4000 m de elevación. A las 6 especies citadas por Liotta (2006: pág. 668) para la provincia de La Rioja debemos agregar 10, de las cuales 3 son endémicas y 4 son introducidas (Tabla I).
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This series will include all those people who, by means of their contributions, great and small, played a part in the consolidation of ichthyology in Argentina. The general plan of this work consists of individual factsheets containing a list of works by each author, along with reference bibliography and, whenever possible, personal pictures and additional material. The datasheets will be published primarily in chronological order, although this is subject to change by the availability of materials for successive editions. This work represents another approach for the recovery and revalorization of those who set the foundations of Argentine ichthyology while in diverse historical circumstances. I expect this to be the beginning of a major work that achieves the description of such a significant part of the history of natural sciences in Argentina.
Resumo:
Esta serie tiene como finalidad dar a conocer las especies presentes en los diferentes estados provinciales. Tomando como base los trabajos de López et al., (2003); Reis et al., (2003); Liotta (2006) y Ferraris (2007) hemos actualizado el elenco ictiofaunístico en cada territorio provincial, siguiendo la macrosistemática de Nelson (2006). No se realizan, con excepción del nombre vulgar y localidad tipo, comentarios ni observaciones sobre las especies señaladas ya que estos se encuentran en la bibliografía adjunta. Se incluyen dos tablas que contienen información sobre especies introducidas y de aquellas de presencia dudosa o que requieren confirmación en el territorio provincial. En este último caso se cita el trabajo que las menciona por primera vez. Consideramos que este modesto aporte contribuirá a precisar el conocimiento ictiofaunístico regional ya que además de la lista de especies, presentamos el marco biogeográfico e hídrico correspondiente. Por otra parte, entendemos que la participación de autores involucrados en la región considerada, le da un verdadero sentido federal a esta contribución, además de reforzar vínculos entre los protagonistas de nuestra especialidad. En este nuevo número, presentamos la provincia de San Juan que se encuentra enclavada en el centro-oeste de nuestro territorio, limitada por las provincias de La Rioja, Mendoza y San Luis. Se presenta por primera vez una lista exhaustiva de la ictiofauna de la provincia de San Juan basada en la revisión bibliográfica y de material de referencia de las colecciones Ictiológicas de la Universidad Nacional de San Juan y del Museo de La Plata. Se citan 21 especies, de las cuales 15 no habían sido mencionadas con anterioridad (Arratia et al., 1983; Murúa y Acosta, 1997; Liotta, 2006). Ocho especies han sido introducidas principalmente con fines deportivos. Se menciona la presencia de Percichthys chilensis, lo que constituiría el primer registro formal de esta especie ya que López-Arbarello (2004) la menciona para el Río Tunuyán (Mendoza), sin material de referencia.