Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics
- Autores
- Mescua, Jose Francisco; Porras, Hernan; Duran, Patrick; Giambiagi, Laura Beatriz; de Moor, Maerten; Cascante, Monserrat; Salazar, Esteban; Protti, Marino; Poblete, Fernando
- Año de publicación
- 2017
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Contractional deformation in Costa Rica is usually attributed to the subduction of the aseismic Cocos Ridge. In this work, we review the evidences for contraction in the middle to late Miocene, prior to the arrival of the Cocos Ridge at the Middle America Trench. We find that the Miocene phase of contractional deformation is found in all of Costa Rica, probably extending to Nicaragua as well. The widespread distribution of this event requires a regional or plate geodynamic trigger. We analyze the possible mechanisms that could produce the onset of contractional deformation, using the better known case of subduction orogeny, the Andes, as an analog. We propose that a change in the direction of the Cocos plate since ∼19 Ma led to a change from oblique to orthogonal convergence, producing contractional deformation of the upper plate.
Fil: Mescua, Jose Francisco. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina
Fil: Porras, Hernan. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica
Fil: Duran, Patrick. Universidad de Costa Rica; Costa Rica
Fil: Giambiagi, Laura Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: de Moor, Maerten. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica
Fil: Cascante, Monserrat. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica
Fil: Salazar, Esteban. Servicio Nacional de Geología y Minería; Chile
Fil: Protti, Marino. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica
Fil: Poblete, Fernando. Universidad de O’Higgins; Chile - Materia
-
CENTRAL AMERICA
MIOCENE
SUBDUCTION - 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:11336/57316
Ver los metadatos del registro completo
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Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate GeodynamicsMescua, Jose FranciscoPorras, HernanDuran, PatrickGiambiagi, Laura Beatrizde Moor, MaertenCascante, MonserratSalazar, EstebanProtti, MarinoPoblete, FernandoCENTRAL AMERICAMIOCENESUBDUCTIONhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Contractional deformation in Costa Rica is usually attributed to the subduction of the aseismic Cocos Ridge. In this work, we review the evidences for contraction in the middle to late Miocene, prior to the arrival of the Cocos Ridge at the Middle America Trench. We find that the Miocene phase of contractional deformation is found in all of Costa Rica, probably extending to Nicaragua as well. The widespread distribution of this event requires a regional or plate geodynamic trigger. We analyze the possible mechanisms that could produce the onset of contractional deformation, using the better known case of subduction orogeny, the Andes, as an analog. We propose that a change in the direction of the Cocos plate since ∼19 Ma led to a change from oblique to orthogonal convergence, producing contractional deformation of the upper plate.Fil: Mescua, Jose Francisco. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; ArgentinaFil: Porras, Hernan. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa RicaFil: Duran, Patrick. Universidad de Costa Rica; Costa RicaFil: Giambiagi, Laura Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: de Moor, Maerten. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa RicaFil: Cascante, Monserrat. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa RicaFil: Salazar, Esteban. Servicio Nacional de Geología y Minería; ChileFil: Protti, Marino. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa RicaFil: Poblete, Fernando. Universidad de O’Higgins; ChileAmerican Geophysical Union2017-12info: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/11336/57316Mescua, Jose Francisco; Porras, Hernan; Duran, Patrick; Giambiagi, Laura Beatriz; de Moor, Maerten; et al.; Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics; American Geophysical Union; Tectonics; 36; 12; 12-2017; 2936-29490278-7407CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://doi.wiley.com/10.1002/2017TC004626info:eu-repo/semantics/altIdentifier/doi/10.1002/2017TC004626info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:33:20Zoai:ri.conicet.gov.ar:11336/57316instacron: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 09:33:20.999CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics |
title |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics |
spellingShingle |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics Mescua, Jose Francisco CENTRAL AMERICA MIOCENE SUBDUCTION |
title_short |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics |
title_full |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics |
title_fullStr |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics |
title_full_unstemmed |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics |
title_sort |
Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics |
dc.creator.none.fl_str_mv |
Mescua, Jose Francisco Porras, Hernan Duran, Patrick Giambiagi, Laura Beatriz de Moor, Maerten Cascante, Monserrat Salazar, Esteban Protti, Marino Poblete, Fernando |
author |
Mescua, Jose Francisco |
author_facet |
Mescua, Jose Francisco Porras, Hernan Duran, Patrick Giambiagi, Laura Beatriz de Moor, Maerten Cascante, Monserrat Salazar, Esteban Protti, Marino Poblete, Fernando |
author_role |
author |
author2 |
Porras, Hernan Duran, Patrick Giambiagi, Laura Beatriz de Moor, Maerten Cascante, Monserrat Salazar, Esteban Protti, Marino Poblete, Fernando |
author2_role |
author author author author author author author author |
dc.subject.none.fl_str_mv |
CENTRAL AMERICA MIOCENE SUBDUCTION |
topic |
CENTRAL AMERICA MIOCENE SUBDUCTION |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Contractional deformation in Costa Rica is usually attributed to the subduction of the aseismic Cocos Ridge. In this work, we review the evidences for contraction in the middle to late Miocene, prior to the arrival of the Cocos Ridge at the Middle America Trench. We find that the Miocene phase of contractional deformation is found in all of Costa Rica, probably extending to Nicaragua as well. The widespread distribution of this event requires a regional or plate geodynamic trigger. We analyze the possible mechanisms that could produce the onset of contractional deformation, using the better known case of subduction orogeny, the Andes, as an analog. We propose that a change in the direction of the Cocos plate since ∼19 Ma led to a change from oblique to orthogonal convergence, producing contractional deformation of the upper plate. Fil: Mescua, Jose Francisco. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina Fil: Porras, Hernan. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica Fil: Duran, Patrick. Universidad de Costa Rica; Costa Rica Fil: Giambiagi, Laura Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: de Moor, Maerten. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica Fil: Cascante, Monserrat. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica Fil: Salazar, Esteban. Servicio Nacional de Geología y Minería; Chile Fil: Protti, Marino. Observatorio Vulcanológico y Sismológico de Costa Rica; Costa Rica Fil: Poblete, Fernando. Universidad de O’Higgins; Chile |
description |
Contractional deformation in Costa Rica is usually attributed to the subduction of the aseismic Cocos Ridge. In this work, we review the evidences for contraction in the middle to late Miocene, prior to the arrival of the Cocos Ridge at the Middle America Trench. We find that the Miocene phase of contractional deformation is found in all of Costa Rica, probably extending to Nicaragua as well. The widespread distribution of this event requires a regional or plate geodynamic trigger. We analyze the possible mechanisms that could produce the onset of contractional deformation, using the better known case of subduction orogeny, the Andes, as an analog. We propose that a change in the direction of the Cocos plate since ∼19 Ma led to a change from oblique to orthogonal convergence, producing contractional deformation of the upper plate. |
publishDate |
2017 |
dc.date.none.fl_str_mv |
2017-12 |
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/11336/57316 Mescua, Jose Francisco; Porras, Hernan; Duran, Patrick; Giambiagi, Laura Beatriz; de Moor, Maerten; et al.; Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics; American Geophysical Union; Tectonics; 36; 12; 12-2017; 2936-2949 0278-7407 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/57316 |
identifier_str_mv |
Mescua, Jose Francisco; Porras, Hernan; Duran, Patrick; Giambiagi, Laura Beatriz; de Moor, Maerten; et al.; Middle to Late Miocene Contractional Deformation in Costa Rica Triggered by Plate Geodynamics; American Geophysical Union; Tectonics; 36; 12; 12-2017; 2936-2949 0278-7407 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://doi.wiley.com/10.1002/2017TC004626 info:eu-repo/semantics/altIdentifier/doi/10.1002/2017TC004626 |
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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1844613023340167168 |
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13.070432 |