Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes
International audience The South Chile ridge (SCR) intersects the Patagonian trench around 46° 09’S, forming the triple junction among the Antarctic, Nazca, and South America plates. Subduction of the SCR since ~18 Ma produced the opening of a slab window beneath Patagonia and a noticeable magmatic...
Published in: | Terra Nova |
---|---|
Main Authors: | , , , , , , |
Other Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2021
|
Subjects: | |
Online Access: | https://hal-insu.archives-ouvertes.fr/insu-03141233 https://hal-insu.archives-ouvertes.fr/insu-03141233/document https://hal-insu.archives-ouvertes.fr/insu-03141233/file/ter.12521.pdf https://doi.org/10.1111/ter.12521 |
id |
ftuniveiffel:oai:HAL:insu-03141233v1 |
---|---|
record_format |
openpolar |
spelling |
ftuniveiffel:oai:HAL:insu-03141233v1 2023-05-15T14:04:10+02:00 Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes Suárez, Rodrigo Sue, Christian Ghiglione, Matías Guillaume, Benjamin Ramos, Miguel Martinod, Joseph Barberón, Vanesa Instituto de Estudios Andinos “Don Pablo Groeber” (INDEAN) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Facultad de Ciencias Exactas y Naturales Buenos Aires (FCEyN) Universidad de Buenos Aires Buenos Aires (UBA)-Universidad de Buenos Aires Buenos Aires (UBA) Institut des Sciences de la Terre (ISTerre) Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Gustave Eiffel-Université Grenoble Alpes (UGA) Géosciences Rennes (GR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS) Argentinian-French ECOS-SUD A15U02 2021-08 https://hal-insu.archives-ouvertes.fr/insu-03141233 https://hal-insu.archives-ouvertes.fr/insu-03141233/document https://hal-insu.archives-ouvertes.fr/insu-03141233/file/ter.12521.pdf https://doi.org/10.1111/ter.12521 en eng HAL CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1111/ter.12521 insu-03141233 https://hal-insu.archives-ouvertes.fr/insu-03141233 https://hal-insu.archives-ouvertes.fr/insu-03141233/document https://hal-insu.archives-ouvertes.fr/insu-03141233/file/ter.12521.pdf doi:10.1111/ter.12521 info:eu-repo/semantics/OpenAccess ISSN: 0954-4879 EISSN: 1365-3121 Terra Nova https://hal-insu.archives-ouvertes.fr/insu-03141233 Terra Nova, 2021, 33 (4), pp.364-374. ⟨10.1111/ter.12521⟩ [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics info:eu-repo/semantics/article Journal articles 2021 ftuniveiffel https://doi.org/10.1111/ter.12521 2023-03-25T21:53:12Z International audience The South Chile ridge (SCR) intersects the Patagonian trench around 46° 09’S, forming the triple junction among the Antarctic, Nazca, and South America plates. Subduction of the SCR since ~18 Ma produced the opening of a slab window beneath Patagonia and a noticeable magmatic gap in the cordillera, profuse volcanism, and topographic uplift in the retroarc. To study seismicity distribution and present‐day stress resulting from this particular framework, we analyze databases of seismic events and earthquake focal mechanisms. Our study finds that clusters of intraplate crustal seismic events are disrupted by a ~450‐470 km seismicity gap above the slab window. Calculated stress tensors depict a strike‐slip tectonic regime north of the triple junction, and ~W‐E compression to the south of the seismic gap. We propose that the seismotectonic behavior of the upper plate is disturbed at the first order by the trench‐ridge intersection, leading to a heterogeneous stress field. Article in Journal/Newspaper Antarc* Antarctic HAL Univ-Eiffel (Université Gustave Eiffel) Antarctic Patagonia The Antarctic Terra Nova 33 4 364 374 |
institution |
Open Polar |
collection |
HAL Univ-Eiffel (Université Gustave Eiffel) |
op_collection_id |
ftuniveiffel |
language |
English |
topic |
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics |
spellingShingle |
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics Suárez, Rodrigo Sue, Christian Ghiglione, Matías Guillaume, Benjamin Ramos, Miguel Martinod, Joseph Barberón, Vanesa Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes |
topic_facet |
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics |
description |
International audience The South Chile ridge (SCR) intersects the Patagonian trench around 46° 09’S, forming the triple junction among the Antarctic, Nazca, and South America plates. Subduction of the SCR since ~18 Ma produced the opening of a slab window beneath Patagonia and a noticeable magmatic gap in the cordillera, profuse volcanism, and topographic uplift in the retroarc. To study seismicity distribution and present‐day stress resulting from this particular framework, we analyze databases of seismic events and earthquake focal mechanisms. Our study finds that clusters of intraplate crustal seismic events are disrupted by a ~450‐470 km seismicity gap above the slab window. Calculated stress tensors depict a strike‐slip tectonic regime north of the triple junction, and ~W‐E compression to the south of the seismic gap. We propose that the seismotectonic behavior of the upper plate is disturbed at the first order by the trench‐ridge intersection, leading to a heterogeneous stress field. |
author2 |
Instituto de Estudios Andinos “Don Pablo Groeber” (INDEAN) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Facultad de Ciencias Exactas y Naturales Buenos Aires (FCEyN) Universidad de Buenos Aires Buenos Aires (UBA)-Universidad de Buenos Aires Buenos Aires (UBA) Institut des Sciences de la Terre (ISTerre) Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Gustave Eiffel-Université Grenoble Alpes (UGA) Géosciences Rennes (GR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR) Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS) Argentinian-French ECOS-SUD A15U02 |
format |
Article in Journal/Newspaper |
author |
Suárez, Rodrigo Sue, Christian Ghiglione, Matías Guillaume, Benjamin Ramos, Miguel Martinod, Joseph Barberón, Vanesa |
author_facet |
Suárez, Rodrigo Sue, Christian Ghiglione, Matías Guillaume, Benjamin Ramos, Miguel Martinod, Joseph Barberón, Vanesa |
author_sort |
Suárez, Rodrigo |
title |
Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes |
title_short |
Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes |
title_full |
Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes |
title_fullStr |
Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes |
title_full_unstemmed |
Seismotectonic implications of the south chile ridge subduction beneath the patagonian andes |
title_sort |
seismotectonic implications of the south chile ridge subduction beneath the patagonian andes |
publisher |
HAL CCSD |
publishDate |
2021 |
url |
https://hal-insu.archives-ouvertes.fr/insu-03141233 https://hal-insu.archives-ouvertes.fr/insu-03141233/document https://hal-insu.archives-ouvertes.fr/insu-03141233/file/ter.12521.pdf https://doi.org/10.1111/ter.12521 |
geographic |
Antarctic Patagonia The Antarctic |
geographic_facet |
Antarctic Patagonia The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
ISSN: 0954-4879 EISSN: 1365-3121 Terra Nova https://hal-insu.archives-ouvertes.fr/insu-03141233 Terra Nova, 2021, 33 (4), pp.364-374. ⟨10.1111/ter.12521⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1111/ter.12521 insu-03141233 https://hal-insu.archives-ouvertes.fr/insu-03141233 https://hal-insu.archives-ouvertes.fr/insu-03141233/document https://hal-insu.archives-ouvertes.fr/insu-03141233/file/ter.12521.pdf doi:10.1111/ter.12521 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1111/ter.12521 |
container_title |
Terra Nova |
container_volume |
33 |
container_issue |
4 |
container_start_page |
364 |
op_container_end_page |
374 |
_version_ |
1766275187251085312 |