The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab
- Autores
- Kay, S. Mahlburg; Ardolino, A. A.; Gorring, M. L.; Ramos, Victor Alberto
- Año de publicación
- 2007
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Oligo-Miocene Somuncura province is the largest (∼55 000 km2) back-arc mafic volcanic field in Patagonia, and one of Earth's largest with no clear link to a hotspot or major extension. Major and trace element and Sr-Nd-Pb isotopic data suggest involvement of a plume-like component in the mantle magma source mixed with hydrous, but not high field strength element (HFSE)-depleted components, from a disintegrating subducting plate. Magmatism is attributed to mantle upwelling related to disturbances during plate reorganization, possibly at a time when the South America plate was nearly stationary over the underlying mantle. Melting was enhanced by hydration of the mantle during Paleogene subduction. Crustal contamination was minimal in a refractory crust that had been extensively melted in the Jurassic. Eruption began with low-volume intraplate alkaline mafic flows with depleted Nd-Sr isotopic signatures. These were followed by voluminous ∼29-25 Ma tholeiitic mafic flows with flat light and steep heavy rare earth element (REE) patterns, intraplate-like La/Ta ratios, arc-like Ba/La ratios and enriched Sr-Nd isotopic signatures. Their source can be explained by mixing EM1-Tristan da Cunha-like and depleted mantle components with subduction-related components. Post-plateau ∼24-17 Ma alkaline flows with steep REE patterns, high incompatible element abundances, and depleted Sr-Nd isotopic signatures mark the ebbing of the mantle upwelling.
Fil: Kay, S. Mahlburg. Cornell University; Estados Unidos
Fil: Ardolino, A. A.. Dirección Nacional de Mineria y Geología; Argentina
Fil: Gorring, M. L.. Montclair State University; Estados Unidos
Fil: Ramos, Victor Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina - Materia
-
LARGE IGNEOUS PROVINCE (LIP)
PATAGONIA
PLUME-LIKE UPWELLING
SLAB INTERACTION
SOMUNCURA PLATEAU - 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:11336/92751
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The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slabKay, S. MahlburgArdolino, A. A.Gorring, M. L.Ramos, Victor AlbertoLARGE IGNEOUS PROVINCE (LIP)PATAGONIAPLUME-LIKE UPWELLINGSLAB INTERACTIONSOMUNCURA PLATEAUhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Oligo-Miocene Somuncura province is the largest (∼55 000 km2) back-arc mafic volcanic field in Patagonia, and one of Earth's largest with no clear link to a hotspot or major extension. Major and trace element and Sr-Nd-Pb isotopic data suggest involvement of a plume-like component in the mantle magma source mixed with hydrous, but not high field strength element (HFSE)-depleted components, from a disintegrating subducting plate. Magmatism is attributed to mantle upwelling related to disturbances during plate reorganization, possibly at a time when the South America plate was nearly stationary over the underlying mantle. Melting was enhanced by hydration of the mantle during Paleogene subduction. Crustal contamination was minimal in a refractory crust that had been extensively melted in the Jurassic. Eruption began with low-volume intraplate alkaline mafic flows with depleted Nd-Sr isotopic signatures. These were followed by voluminous ∼29-25 Ma tholeiitic mafic flows with flat light and steep heavy rare earth element (REE) patterns, intraplate-like La/Ta ratios, arc-like Ba/La ratios and enriched Sr-Nd isotopic signatures. Their source can be explained by mixing EM1-Tristan da Cunha-like and depleted mantle components with subduction-related components. Post-plateau ∼24-17 Ma alkaline flows with steep REE patterns, high incompatible element abundances, and depleted Sr-Nd isotopic signatures mark the ebbing of the mantle upwelling.Fil: Kay, S. Mahlburg. Cornell University; Estados UnidosFil: Ardolino, A. A.. Dirección Nacional de Mineria y Geología; ArgentinaFil: Gorring, M. L.. Montclair State University; Estados UnidosFil: Ramos, Victor Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; ArgentinaOxford University Press2007-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/92751Kay, S. Mahlburg; Ardolino, A. A.; Gorring, M. L.; Ramos, Victor Alberto; The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab; Oxford University Press; Journal Of Petrology; 48; 1; 12-2007; 43-770022-3530CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1093/petrology/egl053info:eu-repo/semantics/altIdentifier/url/https://academic.oup.com/petrology/article/48/1/43/1489017info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:13:42Zoai:ri.conicet.gov.ar:11336/92751instacron: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:34982025-09-29 10:13:42.361CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab |
title |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab |
spellingShingle |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab Kay, S. Mahlburg LARGE IGNEOUS PROVINCE (LIP) PATAGONIA PLUME-LIKE UPWELLING SLAB INTERACTION SOMUNCURA PLATEAU |
title_short |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab |
title_full |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab |
title_fullStr |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab |
title_full_unstemmed |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab |
title_sort |
The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab |
dc.creator.none.fl_str_mv |
Kay, S. Mahlburg Ardolino, A. A. Gorring, M. L. Ramos, Victor Alberto |
author |
Kay, S. Mahlburg |
author_facet |
Kay, S. Mahlburg Ardolino, A. A. Gorring, M. L. Ramos, Victor Alberto |
author_role |
author |
author2 |
Ardolino, A. A. Gorring, M. L. Ramos, Victor Alberto |
author2_role |
author author author |
dc.subject.none.fl_str_mv |
LARGE IGNEOUS PROVINCE (LIP) PATAGONIA PLUME-LIKE UPWELLING SLAB INTERACTION SOMUNCURA PLATEAU |
topic |
LARGE IGNEOUS PROVINCE (LIP) PATAGONIA PLUME-LIKE UPWELLING SLAB INTERACTION SOMUNCURA PLATEAU |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Oligo-Miocene Somuncura province is the largest (∼55 000 km2) back-arc mafic volcanic field in Patagonia, and one of Earth's largest with no clear link to a hotspot or major extension. Major and trace element and Sr-Nd-Pb isotopic data suggest involvement of a plume-like component in the mantle magma source mixed with hydrous, but not high field strength element (HFSE)-depleted components, from a disintegrating subducting plate. Magmatism is attributed to mantle upwelling related to disturbances during plate reorganization, possibly at a time when the South America plate was nearly stationary over the underlying mantle. Melting was enhanced by hydration of the mantle during Paleogene subduction. Crustal contamination was minimal in a refractory crust that had been extensively melted in the Jurassic. Eruption began with low-volume intraplate alkaline mafic flows with depleted Nd-Sr isotopic signatures. These were followed by voluminous ∼29-25 Ma tholeiitic mafic flows with flat light and steep heavy rare earth element (REE) patterns, intraplate-like La/Ta ratios, arc-like Ba/La ratios and enriched Sr-Nd isotopic signatures. Their source can be explained by mixing EM1-Tristan da Cunha-like and depleted mantle components with subduction-related components. Post-plateau ∼24-17 Ma alkaline flows with steep REE patterns, high incompatible element abundances, and depleted Sr-Nd isotopic signatures mark the ebbing of the mantle upwelling. Fil: Kay, S. Mahlburg. Cornell University; Estados Unidos Fil: Ardolino, A. A.. Dirección Nacional de Mineria y Geología; Argentina Fil: Gorring, M. L.. Montclair State University; Estados Unidos Fil: Ramos, Victor Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina |
description |
The Oligo-Miocene Somuncura province is the largest (∼55 000 km2) back-arc mafic volcanic field in Patagonia, and one of Earth's largest with no clear link to a hotspot or major extension. Major and trace element and Sr-Nd-Pb isotopic data suggest involvement of a plume-like component in the mantle magma source mixed with hydrous, but not high field strength element (HFSE)-depleted components, from a disintegrating subducting plate. Magmatism is attributed to mantle upwelling related to disturbances during plate reorganization, possibly at a time when the South America plate was nearly stationary over the underlying mantle. Melting was enhanced by hydration of the mantle during Paleogene subduction. Crustal contamination was minimal in a refractory crust that had been extensively melted in the Jurassic. Eruption began with low-volume intraplate alkaline mafic flows with depleted Nd-Sr isotopic signatures. These were followed by voluminous ∼29-25 Ma tholeiitic mafic flows with flat light and steep heavy rare earth element (REE) patterns, intraplate-like La/Ta ratios, arc-like Ba/La ratios and enriched Sr-Nd isotopic signatures. Their source can be explained by mixing EM1-Tristan da Cunha-like and depleted mantle components with subduction-related components. Post-plateau ∼24-17 Ma alkaline flows with steep REE patterns, high incompatible element abundances, and depleted Sr-Nd isotopic signatures mark the ebbing of the mantle upwelling. |
publishDate |
2007 |
dc.date.none.fl_str_mv |
2007-12 |
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/11336/92751 Kay, S. Mahlburg; Ardolino, A. A.; Gorring, M. L.; Ramos, Victor Alberto; The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab; Oxford University Press; Journal Of Petrology; 48; 1; 12-2007; 43-77 0022-3530 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/92751 |
identifier_str_mv |
Kay, S. Mahlburg; Ardolino, A. A.; Gorring, M. L.; Ramos, Victor Alberto; The somuncura large igneous province in Patagonia: Interaction of a transient mantle thermal anomaly with a subducting slab; Oxford University Press; Journal Of Petrology; 48; 1; 12-2007; 43-77 0022-3530 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1093/petrology/egl053 info:eu-repo/semantics/altIdentifier/url/https://academic.oup.com/petrology/article/48/1/43/1489017 |
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 |
dc.publisher.none.fl_str_mv |
Oxford University Press |
publisher.none.fl_str_mv |
Oxford University Press |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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13.070432 |