Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina

During Late Carboniferous times a continental magmatic arc developed at the western margin of Gondwana in South America, as several marine sedimentary basins were formed at the same time in the retroarc region. North of 33°S, at Cordón Agua del Jagüel, Precordillera of Mendoza, Argentina, a volcanic...

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Autor principal: Koukharsky, M.
Otros Autores: Kleiman, L., Etcheverría, M., Quenardelle, S., Bercowski, F.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 2009
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100 1 |a Koukharsky, M. 
245 1 0 |a Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina 
260 |c 2009 
270 1 0 |m Koukharsky, M.; Universidad de Buenos Aires, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Pabellón 2, (C1428EHA), Buenos Aires, Argentina; email: mkou@gl.fcen.uba.ar 
506 |2 openaire  |e Política editorial 
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520 3 |a During Late Carboniferous times a continental magmatic arc developed at the western margin of Gondwana in South America, as several marine sedimentary basins were formed at the same time in the retroarc region. North of 33°S, at Cordón Agua del Jagüel, Precordillera of Mendoza, Argentina, a volcanic sequence crops out which was emplaced in a submarine environment with some subaerial exposures, and it is intercalated in marine sediments of Agua del Jagüel Formation, which fills of one of these retroarc basins. This paper presents, for the first time, a facies analyses together with geochemical and isotopic data of this volcanic suite, suggesting its deposition in an ensialic retroarc marine basin. The volcanic succession comprises debris flows with either sedimentary or volcanic fragments, base surge, resedimented massive and laminated dacitic-andesitic hyaloclastite, pillow lava, basic hyaloclastite and dacitic-andesitic lavas and hyaloclastite facies. Its composition is bimodal, either basaltic or dacitic-andesitic. The geochemistry data indicate a subalkaline, low K calk-alkaline and metaluminous affinity. The geochemistry of the basalts points to an origin of the magmas from a depleted mantle source with some crustal contamination. Conversely, the geochemistry of the dacites-andesites shows an important participation of both crustal components and subduction related fluids. A different magmatic source for the basalts than for the dacites-andesites is also supported by Sr and Nd isotopic initial ratios and Nd model ages. The characteristics of this magmatic suite suggest its emplacement in an extensional setting probably associated with the presence of a steepened subduction zone at this latitude during Upper Carboniferous times. © 2009 Elsevier Ltd. All rights reserved.  |l eng 
593 |a Universidad de Buenos Aires, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Pabellón 2, (C1428EHA), Buenos Aires, Argentina 
593 |a Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Argentina 
593 |a U.A. de Geología, Comisión Nacional de Energía Atómica, Centro Atómico Ezeiza, Argentina 
593 |a Servicio Geológico Minero Argentino, Geología Regional, Julio A, Roca 651, (1322), Buenos Aires, Argentina 
593 |a Belgrano sn, Barreal (5405), Provincia de San Juan, Argentina 
690 1 0 |a ARGENTINE PRECORDILLERA 
690 1 0 |a CARBONIFERO SUPERIOR 
690 1 0 |a RETROARC VOLCANISM 
690 1 0 |a SUBAERIAL AND SUBMARINE VOLCANISM 
690 1 0 |a UPPER CARBONIFEROUS 
690 1 0 |a VOLCANISMO DE RETROARCO 
690 1 0 |a VOLCANISMO SUBAEREO Y SUBMARINO 
690 1 0 |a CARBONIFEROUS 
690 1 0 |a CONTINENTAL ARC 
690 1 0 |a CONTINENTAL MARGIN 
690 1 0 |a DEBRIS FLOW 
690 1 0 |a DEPOSITION 
690 1 0 |a EMPLACEMENT 
690 1 0 |a EXTENSIONAL TECTONICS 
690 1 0 |a FACIES ANALYSIS 
690 1 0 |a GONDWANA 
690 1 0 |a ISOTOPIC ANALYSIS 
690 1 0 |a MAGMA CHEMISTRY 
690 1 0 |a MANTLE SOURCE 
690 1 0 |a MARINE SEDIMENT 
690 1 0 |a SEDIMENTARY BASIN 
690 1 0 |a SUBDUCTION ZONE 
690 1 0 |a VOLCANISM 
651 4 |a PRECORDILLERA ARGENTINA 
651 4 |a ARGENTINA 
651 4 |a SOUTH AMERICA 
700 1 |a Kleiman, L. 
700 1 |a Etcheverría, M. 
700 1 |a Quenardelle, S. 
700 1 |a Bercowski, F. 
773 0 |d 2009  |g v. 27  |h pp. 299-308  |k n. 4  |p J. South Am. Earth Sci.  |x 08959811  |w (AR-BaUEN)CENRE-1080  |t Journal of South American Earth Sciences 
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856 4 0 |u https://hdl.handle.net/20.500.12110/paper_08959811_v27_n4_p299_Koukharsky  |y Handle 
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