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...
Published in: | Terra Nova |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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Online Access: | http://hdl.handle.net/11336/136256 |
_version_ | 1821772084103086080 |
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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 |
id | ftconicet:oai:ri.conicet.gov.ar:11336/136256 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(70.150,70.150,-49.350,-49.350) ENVELOPE(-63.717,-63.717,-64.283,-64.283) ENVELOPE(-59.700,-59.700,-62.500,-62.500) |
op_collection_id | ftconicet |
op_container_end_page | 374 |
op_doi | https://doi.org/10.1111/ter.12521 |
op_relation | 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 |
op_rights | info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
publisher | Wiley Blackwell Publishing, Inc |
record_format | openpolar |
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 |