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

Autores
Koukharsky, Magdalena Maria L.; Kleiman, L.; Etcheverría, M.; Quenardelle, Sonia Monica; Bercowski, Felisa
Año de publicación
2009
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
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.
Fil: Koukharsky, Magdalena Maria L.. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Kleiman, L.. Comisión Nacional de Energía Atómica; Argentina
Fil: Etcheverría, M.. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina
Fil: Quenardelle, Sonia Monica. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Bercowski, Felisa. No especifica;
Materia
Argentine Precordillera
Carbonífero Superior
Precordillera Argentina
Retroarc Volcanism
Subaerial And Submarine Volcanism
Upper Carboniferous
Volcanismo de Retroarco
Volcanismo Subaéreo y Submarino
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/76632
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/76632
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of ArgentinaKoukharsky, Magdalena Maria L.Kleiman, L.Etcheverría, M.Quenardelle, Sonia MonicaBercowski, FelisaArgentine PrecordilleraCarbonífero SuperiorPrecordillera ArgentinaRetroarc VolcanismSubaerial And Submarine VolcanismUpper CarboniferousVolcanismo de RetroarcoVolcanismo Subaéreo y Submarinohttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1During 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.Fil: Koukharsky, Magdalena Maria L.. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Kleiman, L.. Comisión Nacional de Energía Atómica; ArgentinaFil: Etcheverría, M.. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; ArgentinaFil: Quenardelle, Sonia Monica. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Bercowski, Felisa. No especifica;Pergamon-Elsevier Science Ltd2009-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/76632Koukharsky, Magdalena Maria L.; Kleiman, L.; Etcheverría, M.; Quenardelle, Sonia Monica; Bercowski, Felisa; Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 27; 4; 4-2009; 299-3080895-9811CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2009.02.002info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981109000157info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-17T10:49:30Zoai:ri.conicet.gov.ar:11336/76632instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-17 10:49:31.039CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
title Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
spellingShingle Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
Koukharsky, Magdalena Maria L.
Argentine Precordillera
Carbonífero Superior
Precordillera Argentina
Retroarc Volcanism
Subaerial And Submarine Volcanism
Upper Carboniferous
Volcanismo de Retroarco
Volcanismo Subaéreo y Submarino
title_short Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
title_full Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
title_fullStr Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
title_full_unstemmed Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
title_sort Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina
dc.creator.none.fl_str_mv Koukharsky, Magdalena Maria L.
Kleiman, L.
Etcheverría, M.
Quenardelle, Sonia Monica
Bercowski, Felisa
author Koukharsky, Magdalena Maria L.
author_facet Koukharsky, Magdalena Maria L.
Kleiman, L.
Etcheverría, M.
Quenardelle, Sonia Monica
Bercowski, Felisa
author_role author
author2 Kleiman, L.
Etcheverría, M.
Quenardelle, Sonia Monica
Bercowski, Felisa
author2_role author
author
author
author
dc.subject.none.fl_str_mv Argentine Precordillera
Carbonífero Superior
Precordillera Argentina
Retroarc Volcanism
Subaerial And Submarine Volcanism
Upper Carboniferous
Volcanismo de Retroarco
Volcanismo Subaéreo y Submarino
topic Argentine Precordillera
Carbonífero Superior
Precordillera Argentina
Retroarc Volcanism
Subaerial And Submarine Volcanism
Upper Carboniferous
Volcanismo de Retroarco
Volcanismo Subaéreo y Submarino
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv 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.
Fil: Koukharsky, Magdalena Maria L.. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Kleiman, L.. Comisión Nacional de Energía Atómica; Argentina
Fil: Etcheverría, M.. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina
Fil: Quenardelle, Sonia Monica. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Bercowski, Felisa. No especifica;
description 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.
publishDate 2009
dc.date.none.fl_str_mv 2009-04
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/76632
Koukharsky, Magdalena Maria L.; Kleiman, L.; Etcheverría, M.; Quenardelle, Sonia Monica; Bercowski, Felisa; Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 27; 4; 4-2009; 299-308
0895-9811
CONICET Digital
CONICET
url http://hdl.handle.net/11336/76632
identifier_str_mv Koukharsky, Magdalena Maria L.; Kleiman, L.; Etcheverría, M.; Quenardelle, Sonia Monica; Bercowski, Felisa; Upper Carboniferous retroarc volcanism with submarine and subaerial facies at the western Gondwana margin of Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 27; 4; 4-2009; 299-308
0895-9811
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2009.02.002
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981109000157
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.001348

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