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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/57316
Acceder
id CONICETDig_1edeb04453a0947d8eaa7053291a8a49
oai_identifier_str oai:ri.conicet.gov.ar:11336/57316
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling 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 Técnicas2025-10-22T11:01:20Zoai: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:34982025-10-22 11:01:20.694CONICET 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
_version_ 1846781195520573440
score 12.982451

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