Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy
- Autores
- Ben Mansour, Walid; Wiens, Douglas A.; Mark, Hannah F.; Russo, Raymond M.; Richter, Andreas Jorg; Marderwald, Eric Rodolfo; Barrientos, Sergio
- Año de publicación
- 2022
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Geological processes in Southern Patagonia are affected by the Patagonian slab window, formed by the subduction of the Chile Ridge and subsequent northward migration of the Chile Triple Junction. Using shear wave splitting analysis, we observe strong splitting of up to 2.5 s with an E-W fast direction just south of the triple junction and the edge of the subducting Nazca slab. This region of strong anisotropy is coincident with low uppermost mantle shear velocities and an absence of mantle lithosphere, indicating that the mantle flow occurs in a warm, low-viscosity, 200–300 km wide shallow mantle channel just to the south of the Nazca slab. The region of flow corresponds to a volcanic gap caused by depleted mantle compositions and absence of slab-derived water. In most of Patagonia to the south of this channel, splitting fast directions trend NE-SW consistent with large-scale asthenospheric flow.
Fil: Ben Mansour, Walid. Washington University in St. Louis; Estados Unidos
Fil: Wiens, Douglas A.. Washington University in St. Louis; Estados Unidos
Fil: Mark, Hannah F.. Washington University in St. Louis; Estados Unidos
Fil: Russo, Raymond M.. University of Florida; Estados Unidos
Fil: Richter, Andreas Jorg. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina
Fil: Marderwald, Eric Rodolfo. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Barrientos, Sergio. Universidad de Chile; Chile - Materia
-
SHEAR-WAVE SPLITTING
MANTLE FLOW
PATAGONIAN SLAB WINDOW - 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:11336/223548
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Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal AnisotropyBen Mansour, WalidWiens, Douglas A.Mark, Hannah F.Russo, Raymond M.Richter, Andreas JorgMarderwald, Eric RodolfoBarrientos, SergioSHEAR-WAVE SPLITTINGMANTLE FLOWPATAGONIAN SLAB WINDOWhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Geological processes in Southern Patagonia are affected by the Patagonian slab window, formed by the subduction of the Chile Ridge and subsequent northward migration of the Chile Triple Junction. Using shear wave splitting analysis, we observe strong splitting of up to 2.5 s with an E-W fast direction just south of the triple junction and the edge of the subducting Nazca slab. This region of strong anisotropy is coincident with low uppermost mantle shear velocities and an absence of mantle lithosphere, indicating that the mantle flow occurs in a warm, low-viscosity, 200–300 km wide shallow mantle channel just to the south of the Nazca slab. The region of flow corresponds to a volcanic gap caused by depleted mantle compositions and absence of slab-derived water. In most of Patagonia to the south of this channel, splitting fast directions trend NE-SW consistent with large-scale asthenospheric flow.Fil: Ben Mansour, Walid. Washington University in St. Louis; Estados UnidosFil: Wiens, Douglas A.. Washington University in St. Louis; Estados UnidosFil: Mark, Hannah F.. Washington University in St. Louis; Estados UnidosFil: Russo, Raymond M.. University of Florida; Estados UnidosFil: Richter, Andreas Jorg. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; ArgentinaFil: Marderwald, Eric Rodolfo. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Barrientos, Sergio. Universidad de Chile; ChileAmerican Geophysical Union2022-09info: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/11336/223548Ben Mansour, Walid; Wiens, Douglas A.; Mark, Hannah F.; Russo, Raymond M.; Richter, Andreas Jorg; et al.; Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy; American Geophysical Union; Geophysical Research Letters; 49; 18; 9-2022; 1-100094-8276CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1029/2022GL099871info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:53:56Zoai:ri.conicet.gov.ar:11336/223548instacron: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 09:53:57.077CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy |
title |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy |
spellingShingle |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy Ben Mansour, Walid SHEAR-WAVE SPLITTING MANTLE FLOW PATAGONIAN SLAB WINDOW |
title_short |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy |
title_full |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy |
title_fullStr |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy |
title_full_unstemmed |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy |
title_sort |
Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy |
dc.creator.none.fl_str_mv |
Ben Mansour, Walid Wiens, Douglas A. Mark, Hannah F. Russo, Raymond M. Richter, Andreas Jorg Marderwald, Eric Rodolfo Barrientos, Sergio |
author |
Ben Mansour, Walid |
author_facet |
Ben Mansour, Walid Wiens, Douglas A. Mark, Hannah F. Russo, Raymond M. Richter, Andreas Jorg Marderwald, Eric Rodolfo Barrientos, Sergio |
author_role |
author |
author2 |
Wiens, Douglas A. Mark, Hannah F. Russo, Raymond M. Richter, Andreas Jorg Marderwald, Eric Rodolfo Barrientos, Sergio |
author2_role |
author author author author author author |
dc.subject.none.fl_str_mv |
SHEAR-WAVE SPLITTING MANTLE FLOW PATAGONIAN SLAB WINDOW |
topic |
SHEAR-WAVE SPLITTING MANTLE FLOW PATAGONIAN SLAB WINDOW |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Geological processes in Southern Patagonia are affected by the Patagonian slab window, formed by the subduction of the Chile Ridge and subsequent northward migration of the Chile Triple Junction. Using shear wave splitting analysis, we observe strong splitting of up to 2.5 s with an E-W fast direction just south of the triple junction and the edge of the subducting Nazca slab. This region of strong anisotropy is coincident with low uppermost mantle shear velocities and an absence of mantle lithosphere, indicating that the mantle flow occurs in a warm, low-viscosity, 200–300 km wide shallow mantle channel just to the south of the Nazca slab. The region of flow corresponds to a volcanic gap caused by depleted mantle compositions and absence of slab-derived water. In most of Patagonia to the south of this channel, splitting fast directions trend NE-SW consistent with large-scale asthenospheric flow. Fil: Ben Mansour, Walid. Washington University in St. Louis; Estados Unidos Fil: Wiens, Douglas A.. Washington University in St. Louis; Estados Unidos Fil: Mark, Hannah F.. Washington University in St. Louis; Estados Unidos Fil: Russo, Raymond M.. University of Florida; Estados Unidos Fil: Richter, Andreas Jorg. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina Fil: Marderwald, Eric Rodolfo. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina Fil: Barrientos, Sergio. Universidad de Chile; Chile |
description |
Geological processes in Southern Patagonia are affected by the Patagonian slab window, formed by the subduction of the Chile Ridge and subsequent northward migration of the Chile Triple Junction. Using shear wave splitting analysis, we observe strong splitting of up to 2.5 s with an E-W fast direction just south of the triple junction and the edge of the subducting Nazca slab. This region of strong anisotropy is coincident with low uppermost mantle shear velocities and an absence of mantle lithosphere, indicating that the mantle flow occurs in a warm, low-viscosity, 200–300 km wide shallow mantle channel just to the south of the Nazca slab. The region of flow corresponds to a volcanic gap caused by depleted mantle compositions and absence of slab-derived water. In most of Patagonia to the south of this channel, splitting fast directions trend NE-SW consistent with large-scale asthenospheric flow. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022-09 |
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/11336/223548 Ben Mansour, Walid; Wiens, Douglas A.; Mark, Hannah F.; Russo, Raymond M.; Richter, Andreas Jorg; et al.; Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy; American Geophysical Union; Geophysical Research Letters; 49; 18; 9-2022; 1-10 0094-8276 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/223548 |
identifier_str_mv |
Ben Mansour, Walid; Wiens, Douglas A.; Mark, Hannah F.; Russo, Raymond M.; Richter, Andreas Jorg; et al.; Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy; American Geophysical Union; Geophysical Research Letters; 49; 18; 9-2022; 1-10 0094-8276 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2022GL099871 |
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 |
American Geophysical Union |
publisher.none.fl_str_mv |
American Geophysical Union |
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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13.070432 |