931 resultados para MERA, JUAN LEÓN, 1832-1894
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Parte 1 - Atos do Poder Legislativo
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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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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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Juan Manuel Abascal Palazón, Antonio Caballos Rufino, Santiago Castellanos Garcia y Juan Santos Yanguas (eds.)
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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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Homenaje a Georges Laplace, realizado en Vitoria-Gasteiz el 13,14 y 15 de noviembre de 2012. Edición a cargo de Aitor Calvo, Aitor Sánchez, Maite García-Rojas y Mónica Alonso-Eguíluz.
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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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Esta dissertação tem como objetivo compreender e analisar o jacobinismo brasileiro tendo como foco os anos de 1894 até 1897. Pretende-se perceber como esse grupo conseguiu construir um projeto de personalização do poder em torno do Marechal Floriano Peixoto em momentos críticos da história República brasileira: durante a Revolta da Armada de 1894; no momento de transição do governo militar para o governo civil de Prudente de Moraes em 1894/95; e na ocasião da morte do Marechal Floriano Peixoto em 1895. Para tanto, o estudo propõe uma reflexão sobre a utilização do discurso jornalístico como instrumento na fabricação da imagem dos revoltosos da Marinha como restauradores monarquistas e de Floriano como herói da República, buscando assim, perceber igualmente a dinâmica de sua elaboração e as suas repercussões na sociedade brasileira. Chegaremos a conclusão que as forças jacobinas enfraqueceram no momento do atentado a Prudente de Morais em 1897, mas seus discursos ainda tiveram eco na primeira metade do século XX na República brasileira.
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[EN]Nowadays the use of web applications is a routine not only for companies but also for anyone interested in them. Thus, this market has risen hugely since the introduction of The Internet in our daily lives. Everyone has experienced the moment when you have to choose an access service and you do not know which one to select. At that moment, it is when this web application comes into action. It provides a useful interface in order to choose between access services as well as an analysis tool for the different access technologies in the market. Written in Java language, this web application is as simple as it can be, offering a complete interface that meets the needs of everyone, from the people at home to the largest company.
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El Pasado 21 de mayo del 2014 la Asamblea de la Liga de Fútbol Profesional aprobó el reglamento de Control Económico de los Clubes y Sociedades Anónimas Deportivas. Tres meses después la LFP publico que el Getafe no podía inscribir al jugador Pedro León Sánchez-Gil por incumplimiento de los reglamentos ya citados. La presente revisión bibliográfica tiene como objetivos clarificar las diferentes normativas que se presentan por parte la de LFP y RFEF. Además de exponer los diferentes procedimientos que se han seguido por parte de Pedro Sánchez León, Getafe, AFE, CSD, LFP y RFEF en relación a la prohibición de la participación del nombrado jugador en la Liga.
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Qens/wins 2014 - 11th International Conference on Quasielastic Neutron Scattering and 6th International Workshop on Inelastic Neutron Spectrometers / editado por:Frick, B; Koza, MM; Boehm, M; Mutka, H
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1 carta (manuscrita) ; 225x330 mm