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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/76632
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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 Técnicas2025-09-03T09:48:17Zoai: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:34982025-09-03 09:48:17.618CONICET 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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1842268915803095040 |
score |
13.13397 |