Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Fie...

Autores: Giambiagi, Laura Beatriz; Spagnotto, Silvana Liz; Suriano, Julieta; Lossada, Ana Clara; Mescua, Jose Francisco; Quiroga Carrasco, Rodrigo Adolfo; Barrionuevo, Matías
Año de publicación: 2019
Idioma: inglés
Tipo de recurso: documento de conferencia
Estado: versión publicada
Descripción: The estimation of contemporary stress field, crustal deformation and sedimentation during the evolution of the southern Central Andes, between 20º and 36ºS, is crucial for the understanding of plate-driving and gravitational forces, acting during the construction of a subduction-related orogenic system, and the mechanical behaviour of the continental plate. While the synergies between crustal deformation, exhumation and sedimentation processes are well-known to first order, it is challenging to evaluate the interplay between constructive deep mechanisms building the Andes, the stress field, exhumation and basin development.The goal of our study is to do a systematic analysis of the stress field evolution, in the time interval between 20 Ma to the Quaternary. For this purpose, the temporal and spatial stress field variations as a parameter crucial to understanding the relationship between deep and shallow crustal deformation and associated exhumation and sedimentation is used.Reduced stress tensors, n=293, from more than 4,000 fault-slip data were obtained. This data set is integrated with 9,240 published fault-slip data from other authors, into a database to obtain a total of 865 location sites with kinematic data or reduced stress tensors. Data from geophysical logs, dyke and sill analysis, and the compilation of 1,293 earthquake (>2 Mw) focal mechanisms to image the current stress field in the High Andes and the forelands.The integration of these data suggests that, on the one hand, spatiotemporal changes in the state of stress in the crust indicate a shift from compression to strike-slip or normal tectonics, associated with σ3/σ2 and σ2/σ1 permutations respectively, in the highest portions of the Andes, due to an increase in the absolute magnitude of the vertical stress component as the crust thickens and the gravitational potential energy increases. This change in local stress regime is closely linked with changes in the style of basin formation, for example from either foreland or broken foreland to pull-apart settings.On the other hand, the results of paleo and present stress field analysis show a remarkably consistent maximum horizontal stress direction (either σ1 or σ2) subperpendicular to the plate convergence direction and/or subperpendicular to spatial variations of the gravitational component of stress. This suggests that, during the latest stage of Andean construction of the last 20 my, the SHmax orientation is mainly controlled by plate boundary forces, topography and lithospheric density structure.
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: Spagnotto, Silvana Liz. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Luis. Facultad de Ciencias Físico- Matemáticas y Naturales; Argentina
Fil: Suriano, Julieta. 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: Lossada, Ana Clara. 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: 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: Quiroga Carrasco, Rodrigo Adolfo. 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: Barrionuevo, Matías. 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
8th International Symposium on Andean Geodynamics
Quito
Ecuador
Escuela Politécnica Nacional
Institut de Recherche pour le Développement
Materia: CENTRAL ANDES
Stress Field
Exhumation
Sedimentation
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:11336/234281

Acceder

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repository_id_str	3498
network_name_str	CONICET Digital (CONICET)
spelling	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution ProjectGiambiagi, Laura BeatrizSpagnotto, Silvana LizSuriano, JulietaLossada, Ana ClaraMescua, Jose FranciscoQuiroga Carrasco, Rodrigo AdolfoBarrionuevo, MatíasCENTRAL ANDESStress FieldExhumationSedimentationhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The estimation of contemporary stress field, crustal deformation and sedimentation during the evolution of the southern Central Andes, between 20º and 36ºS, is crucial for the understanding of plate-driving and gravitational forces, acting during the construction of a subduction-related orogenic system, and the mechanical behaviour of the continental plate. While the synergies between crustal deformation, exhumation and sedimentation processes are well-known to first order, it is challenging to evaluate the interplay between constructive deep mechanisms building the Andes, the stress field, exhumation and basin development.The goal of our study is to do a systematic analysis of the stress field evolution, in the time interval between 20 Ma to the Quaternary. For this purpose, the temporal and spatial stress field variations as a parameter crucial to understanding the relationship between deep and shallow crustal deformation and associated exhumation and sedimentation is used.Reduced stress tensors, n=293, from more than 4,000 fault-slip data were obtained. This data set is integrated with 9,240 published fault-slip data from other authors, into a database to obtain a total of 865 location sites with kinematic data or reduced stress tensors. Data from geophysical logs, dyke and sill analysis, and the compilation of 1,293 earthquake (>2 Mw) focal mechanisms to image the current stress field in the High Andes and the forelands.The integration of these data suggests that, on the one hand, spatiotemporal changes in the state of stress in the crust indicate a shift from compression to strike-slip or normal tectonics, associated with σ3/σ2 and σ2/σ1 permutations respectively, in the highest portions of the Andes, due to an increase in the absolute magnitude of the vertical stress component as the crust thickens and the gravitational potential energy increases. This change in local stress regime is closely linked with changes in the style of basin formation, for example from either foreland or broken foreland to pull-apart settings.On the other hand, the results of paleo and present stress field analysis show a remarkably consistent maximum horizontal stress direction (either σ1 or σ2) subperpendicular to the plate convergence direction and/or subperpendicular to spatial variations of the gravitational component of stress. This suggests that, during the latest stage of Andean construction of the last 20 my, the SHmax orientation is mainly controlled by plate boundary forces, topography and lithospheric density structure.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; ArgentinaFil: Spagnotto, Silvana Liz. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Luis. Facultad de Ciencias Físico- Matemáticas y Naturales; ArgentinaFil: Suriano, Julieta. 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: Lossada, Ana Clara. 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"; ArgentinaFil: 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: Quiroga Carrasco, Rodrigo Adolfo. 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: Barrionuevo, Matías. 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; Argentina8th International Symposium on Andean GeodynamicsQuitoEcuadorEscuela Politécnica NacionalInstitut de Recherche pour le DéveloppementInternational Society for Animal Genetics2019info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectSimposioBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/234281Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project; 8th International Symposium on Andean Geodynamics; Quito; Ecuador; 2019; 1-1CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.igepn.edu.ec/8isag-abstracts/plenary-talksinfo:eu-repo/semantics/altIdentifier/url/https://www.igepn.edu.ec/servicios/eventos/8isagInternacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:29:24Zoai:ri.conicet.gov.ar:11336/234281instacron: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 10:29:24.925CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project
title	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project
spellingShingle	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project Giambiagi, Laura Beatriz CENTRAL ANDES Stress Field Exhumation Sedimentation
title_short	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project
title_full	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project
title_fullStr	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project
title_full_unstemmed	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project
title_sort	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project
dc.creator.none.fl_str_mv	Giambiagi, Laura Beatriz Spagnotto, Silvana Liz Suriano, Julieta Lossada, Ana Clara Mescua, Jose Francisco Quiroga Carrasco, Rodrigo Adolfo Barrionuevo, Matías
author	Giambiagi, Laura Beatriz
author_facet	Giambiagi, Laura Beatriz Spagnotto, Silvana Liz Suriano, Julieta Lossada, Ana Clara Mescua, Jose Francisco Quiroga Carrasco, Rodrigo Adolfo Barrionuevo, Matías
author_role	author
author2	Spagnotto, Silvana Liz Suriano, Julieta Lossada, Ana Clara Mescua, Jose Francisco Quiroga Carrasco, Rodrigo Adolfo Barrionuevo, Matías
author2_role	author author author author author author
dc.subject.none.fl_str_mv	CENTRAL ANDES Stress Field Exhumation Sedimentation
topic	CENTRAL ANDES Stress Field Exhumation Sedimentation
purl_subject.fl_str_mv	https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv	The estimation of contemporary stress field, crustal deformation and sedimentation during the evolution of the southern Central Andes, between 20º and 36ºS, is crucial for the understanding of plate-driving and gravitational forces, acting during the construction of a subduction-related orogenic system, and the mechanical behaviour of the continental plate. While the synergies between crustal deformation, exhumation and sedimentation processes are well-known to first order, it is challenging to evaluate the interplay between constructive deep mechanisms building the Andes, the stress field, exhumation and basin development.The goal of our study is to do a systematic analysis of the stress field evolution, in the time interval between 20 Ma to the Quaternary. For this purpose, the temporal and spatial stress field variations as a parameter crucial to understanding the relationship between deep and shallow crustal deformation and associated exhumation and sedimentation is used.Reduced stress tensors, n=293, from more than 4,000 fault-slip data were obtained. This data set is integrated with 9,240 published fault-slip data from other authors, into a database to obtain a total of 865 location sites with kinematic data or reduced stress tensors. Data from geophysical logs, dyke and sill analysis, and the compilation of 1,293 earthquake (>2 Mw) focal mechanisms to image the current stress field in the High Andes and the forelands.The integration of these data suggests that, on the one hand, spatiotemporal changes in the state of stress in the crust indicate a shift from compression to strike-slip or normal tectonics, associated with σ3/σ2 and σ2/σ1 permutations respectively, in the highest portions of the Andes, due to an increase in the absolute magnitude of the vertical stress component as the crust thickens and the gravitational potential energy increases. This change in local stress regime is closely linked with changes in the style of basin formation, for example from either foreland or broken foreland to pull-apart settings.On the other hand, the results of paleo and present stress field analysis show a remarkably consistent maximum horizontal stress direction (either σ1 or σ2) subperpendicular to the plate convergence direction and/or subperpendicular to spatial variations of the gravitational component of stress. This suggests that, during the latest stage of Andean construction of the last 20 my, the SHmax orientation is mainly controlled by plate boundary forces, topography and lithospheric density structure. 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: Spagnotto, Silvana Liz. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de San Luis. Facultad de Ciencias Físico- Matemáticas y Naturales; Argentina Fil: Suriano, Julieta. 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: Lossada, Ana Clara. 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: 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: Quiroga Carrasco, Rodrigo Adolfo. 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: Barrionuevo, Matías. 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 8th International Symposium on Andean Geodynamics Quito Ecuador Escuela Politécnica Nacional Institut de Recherche pour le Développement
description	The estimation of contemporary stress field, crustal deformation and sedimentation during the evolution of the southern Central Andes, between 20º and 36ºS, is crucial for the understanding of plate-driving and gravitational forces, acting during the construction of a subduction-related orogenic system, and the mechanical behaviour of the continental plate. While the synergies between crustal deformation, exhumation and sedimentation processes are well-known to first order, it is challenging to evaluate the interplay between constructive deep mechanisms building the Andes, the stress field, exhumation and basin development.The goal of our study is to do a systematic analysis of the stress field evolution, in the time interval between 20 Ma to the Quaternary. For this purpose, the temporal and spatial stress field variations as a parameter crucial to understanding the relationship between deep and shallow crustal deformation and associated exhumation and sedimentation is used.Reduced stress tensors, n=293, from more than 4,000 fault-slip data were obtained. This data set is integrated with 9,240 published fault-slip data from other authors, into a database to obtain a total of 865 location sites with kinematic data or reduced stress tensors. Data from geophysical logs, dyke and sill analysis, and the compilation of 1,293 earthquake (>2 Mw) focal mechanisms to image the current stress field in the High Andes and the forelands.The integration of these data suggests that, on the one hand, spatiotemporal changes in the state of stress in the crust indicate a shift from compression to strike-slip or normal tectonics, associated with σ3/σ2 and σ2/σ1 permutations respectively, in the highest portions of the Andes, due to an increase in the absolute magnitude of the vertical stress component as the crust thickens and the gravitational potential energy increases. This change in local stress regime is closely linked with changes in the style of basin formation, for example from either foreland or broken foreland to pull-apart settings.On the other hand, the results of paleo and present stress field analysis show a remarkably consistent maximum horizontal stress direction (either σ1 or σ2) subperpendicular to the plate convergence direction and/or subperpendicular to spatial variations of the gravitational component of stress. This suggests that, during the latest stage of Andean construction of the last 20 my, the SHmax orientation is mainly controlled by plate boundary forces, topography and lithospheric density structure.
publishDate	2019
dc.date.none.fl_str_mv	2019
dc.type.none.fl_str_mv	info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject Simposio Book http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia
status_str	publishedVersion
format	conferenceObject
dc.identifier.none.fl_str_mv	http://hdl.handle.net/11336/234281 Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project; 8th International Symposium on Andean Geodynamics; Quito; Ecuador; 2019; 1-1 CONICET Digital CONICET
url	http://hdl.handle.net/11336/234281
identifier_str_mv	Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Field Evolution Project; 8th International Symposium on Andean Geodynamics; Quito; Ecuador; 2019; 1-1 CONICET Digital CONICET
dc.language.none.fl_str_mv	eng
language	eng
dc.relation.none.fl_str_mv	info:eu-repo/semantics/altIdentifier/url/https://www.igepn.edu.ec/8isag-abstracts/plenary-talks info:eu-repo/semantics/altIdentifier/url/https://www.igepn.edu.ec/servicios/eventos/8isag
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.coverage.none.fl_str_mv	Internacional
dc.publisher.none.fl_str_mv	International Society for Animal Genetics
publisher.none.fl_str_mv	International Society for Animal Genetics
dc.source.none.fl_str_mv	reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str	CONICET Digital (CONICET)
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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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Contemporary stress field, crustal deformation, exhumation and sedimentation during the building of the Central Andes over the last 20 my: Advances in the Central Andean Stress Fie...

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