Seismotectonic implications of the South Chile ridge subduction beneath the Patagonian Andes

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, p...

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Published in:Terra Nova
Main Authors: Suárez, Rodrigo Javier, Sue, Christian, Ghiglione, Matias, Guillaume, Benjamin, Ramos, Miguel Esteban, Martinod, Joseph, Barberon, Vanesa
Format: Article in Journal/Newspaper
Language:English
Published: Wiley Blackwell Publishing, Inc
Subjects:
Online Access:http://hdl.handle.net/11336/136256
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author Suárez, Rodrigo Javier
Sue, Christian
Ghiglione, Matias
Guillaume, Benjamin
Ramos, Miguel Esteban
Martinod, Joseph
Barberon, Vanesa
author_facet Suárez, Rodrigo Javier
Sue, Christian
Ghiglione, Matias
Guillaume, Benjamin
Ramos, Miguel Esteban
Martinod, Joseph
Barberon, Vanesa
author_sort Suárez, Rodrigo Javier
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 4
container_start_page 364
container_title Terra Nova
container_volume 33
description 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 analyse 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 behaviour of the upper plate is disturbed at the first order by the trench-ridge intersection, leading to a heterogeneous stress field. Fil: Suárez, Rodrigo Javier. 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 Fil: Sue, Christian. Universite de Franche-Comte; Francia Fil: Ghiglione, Matias. 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 Fil: Guillaume, Benjamin. Universite de Rennes I; Francia Fil: Ramos, Miguel Esteban. 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. ...
format Article in Journal/Newspaper
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
geographic Antarctic
The Antarctic
Patagonia
Argentina
Guillaume
Pablo
Ramos
geographic_facet Antarctic
The Antarctic
Patagonia
Argentina
Guillaume
Pablo
Ramos
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op_doi https://doi.org/10.1111/ter.12521
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http://hdl.handle.net/11336/136256
Suárez, Rodrigo Javier; Sue, Christian; Ghiglione, Matias; Guillaume, Benjamin; Ramos, Miguel Esteban; et al.; Seismotectonic implications of the South Chile ridge subduction beneath the Patagonian Andes; Wiley Blackwell Publishing, Inc; Terra Nova (print); 2021; 14-2-2021; 1-34
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/136256 2025-01-16T19:38:48+00:00 Seismotectonic implications of the South Chile ridge subduction beneath the Patagonian Andes Suárez, Rodrigo Javier Sue, Christian Ghiglione, Matias Guillaume, Benjamin Ramos, Miguel Esteban Martinod, Joseph Barberon, Vanesa application/pdf http://hdl.handle.net/11336/136256 eng eng Wiley Blackwell Publishing, Inc info:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1111/ter.12521 info:eu-repo/semantics/altIdentifier/doi/10.1111/ter.12521 http://hdl.handle.net/11336/136256 Suárez, Rodrigo Javier; Sue, Christian; Ghiglione, Matias; Guillaume, Benjamin; Ramos, Miguel Esteban; et al.; Seismotectonic implications of the South Chile ridge subduction beneath the Patagonian Andes; Wiley Blackwell Publishing, Inc; Terra Nova (print); 2021; 14-2-2021; 1-34 0954-4879 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ EARTHQUAKE FOCAL MECHANISM INTRAPLATE SEISMIC GAP PATAGONIA SLAB WINDOW SOUTH CHILE RIDGE https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1111/ter.12521 2023-09-24T20:26:44Z 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 analyse 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 behaviour of the upper plate is disturbed at the first order by the trench-ridge intersection, leading to a heterogeneous stress field. Fil: Suárez, Rodrigo Javier. 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 Fil: Sue, Christian. Universite de Franche-Comte; Francia Fil: Ghiglione, Matias. 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 Fil: Guillaume, Benjamin. Universite de Rennes I; Francia Fil: Ramos, Miguel Esteban. 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. ... Article in Journal/Newspaper Antarc* Antarctic CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic The Antarctic Patagonia Argentina Guillaume ENVELOPE(70.150,70.150,-49.350,-49.350) Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Ramos ENVELOPE(-59.700,-59.700,-62.500,-62.500) Terra Nova 33 4 364 374
spellingShingle EARTHQUAKE FOCAL MECHANISM
INTRAPLATE SEISMIC GAP
PATAGONIA SLAB WINDOW
SOUTH CHILE RIDGE
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Suárez, Rodrigo Javier
Sue, Christian
Ghiglione, Matias
Guillaume, Benjamin
Ramos, Miguel Esteban
Martinod, Joseph
Barberon, Vanesa
Seismotectonic implications of the South Chile ridge subduction beneath the Patagonian Andes
title 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_short 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
topic EARTHQUAKE FOCAL MECHANISM
INTRAPLATE SEISMIC GAP
PATAGONIA SLAB WINDOW
SOUTH CHILE RIDGE
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet EARTHQUAKE FOCAL MECHANISM
INTRAPLATE SEISMIC GAP
PATAGONIA SLAB WINDOW
SOUTH CHILE RIDGE
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/136256