Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation
- Autores
- Ghiglione, Matias; Barberon, Vanesa; Ramos, Miguel Esteban; Tobal, Jonathan Elías; Garcia Morabito, Ezequiel; Suárez, Rodrigo Javier; Martinod, Joseph; Sue, Christian
- Año de publicación
- 2018
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- We present an appraisal of structural domains in the SPA (Southern Patagonian Andes) between 46° and 52°S, recognizing a thickskinnedBD (Basement domain) and a hybrid thick- and thin-skinned systems in the FTB (fold and thrust belt).Two major structural segments can be clearly defined north and south of 48°30´: (1) Northern segment: With a steady orogenicwidth of around 340-360km, is characterized by a well-developed basement domain, and a narrow FTB. The inner domain of theFTB is very narrow.The comparison of our geometrical data with exhumation patterns from thermochronological studies evidences importantcorrelations: (1) The wide basement in the northern sector coincides with exhumation ages younger than 3 Ma throughout thisdomain. It has been proposed that this sector was dominated by highly efficient alpine glacial erosion, producing this characteristicyoung exhumation pattern (Thomson 2010). In terms of the critical wedge theory, enhanced erosive exhumation in the highlandof the retro wedge produces active tectonic uplift of the basement domain; while the basement is constantly subdued under thecritical angle, the thrust front does not advance, and the FTB is underdeveloped, in agreement with our empirical observations. (2)The abrupt and steady increase in width and shortening of the FTB towards the southern sector coincides with older basementcooling ages which indicate much reduced late Cenozoic erosion despite dominantly glacial conditions here since the latestMiocene (Thomson et al., 2010). Although orogen width does seem to be around 25% wider between 48°30´and 50°SL, it showsa gradual decline towards the south. Older exhumation ages in the Basement domain coincides with a thicker sedimentary coverand erosion focused in the retroarc, as expected by the critical wedge theory, predicting the development of a wider FTB.
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: Barberon, Vanesa. 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: 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. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
Fil: Tobal, Jonathan Elías. 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: Garcia Morabito, Ezequiel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio. Universidad Nacional de Río Negro. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio; Argentina
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: Martinod, Joseph. Université de Savoie Mont-blanc; Francia
Fil: Sue, Christian. Universite de Franche-Comte; Francia
XV Congreso Geológico Chileno
Concepción
Chile
Universidad de Concepción
Colegio de Geólogos de Chile
Sociedad Geológica de Chile - Materia
-
STRUCTURE
EXHUMATION
THERMOCHRONOLOGICAL
PATAGONIA - 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:11336/268071
Ver los metadatos del registro completo
id |
CONICETDig_b28c163cd7e24a255d48889a7452c7ab |
---|---|
oai_identifier_str |
oai:ri.conicet.gov.ar:11336/268071 |
network_acronym_str |
CONICETDig |
repository_id_str |
3498 |
network_name_str |
CONICET Digital (CONICET) |
spelling |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformationGhiglione, MatiasBarberon, VanesaRamos, Miguel EstebanTobal, Jonathan ElíasGarcia Morabito, EzequielSuárez, Rodrigo JavierMartinod, JosephSue, ChristianSTRUCTUREEXHUMATIONTHERMOCHRONOLOGICALPATAGONIAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We present an appraisal of structural domains in the SPA (Southern Patagonian Andes) between 46° and 52°S, recognizing a thickskinnedBD (Basement domain) and a hybrid thick- and thin-skinned systems in the FTB (fold and thrust belt).Two major structural segments can be clearly defined north and south of 48°30´: (1) Northern segment: With a steady orogenicwidth of around 340-360km, is characterized by a well-developed basement domain, and a narrow FTB. The inner domain of theFTB is very narrow.The comparison of our geometrical data with exhumation patterns from thermochronological studies evidences importantcorrelations: (1) The wide basement in the northern sector coincides with exhumation ages younger than 3 Ma throughout thisdomain. It has been proposed that this sector was dominated by highly efficient alpine glacial erosion, producing this characteristicyoung exhumation pattern (Thomson 2010). In terms of the critical wedge theory, enhanced erosive exhumation in the highlandof the retro wedge produces active tectonic uplift of the basement domain; while the basement is constantly subdued under thecritical angle, the thrust front does not advance, and the FTB is underdeveloped, in agreement with our empirical observations. (2)The abrupt and steady increase in width and shortening of the FTB towards the southern sector coincides with older basementcooling ages which indicate much reduced late Cenozoic erosion despite dominantly glacial conditions here since the latestMiocene (Thomson et al., 2010). Although orogen width does seem to be around 25% wider between 48°30´and 50°SL, it showsa gradual decline towards the south. Older exhumation ages in the Basement domain coincides with a thicker sedimentary coverand erosion focused in the retroarc, as expected by the critical wedge theory, predicting the development of a wider FTB.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"; ArgentinaFil: Barberon, Vanesa. 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: 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. Instituto de Estudios Andinos "Don Pablo Groeber"; ArgentinaFil: Tobal, Jonathan Elías. 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: Garcia Morabito, Ezequiel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio. Universidad Nacional de Río Negro. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio; ArgentinaFil: 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"; ArgentinaFil: Martinod, Joseph. Université de Savoie Mont-blanc; FranciaFil: Sue, Christian. Universite de Franche-Comte; FranciaXV Congreso Geológico ChilenoConcepciónChileUniversidad de ConcepciónColegio de Geólogos de ChileSociedad Geológica de ChileUniversidad de Concepción2018info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/268071Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation; XV Congreso Geológico Chileno; Concepción; Chile; 2018; 1208-1208CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://congresogeologicochileno.cl/wp-content/uploads/2018/12/Libro-de-Actas-XVCongresoGeologicoChileno2018-2.pdfInternacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:57:47Zoai:ri.conicet.gov.ar:11336/268071instacron: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 09:57:47.288CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation |
title |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation |
spellingShingle |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation Ghiglione, Matias STRUCTURE EXHUMATION THERMOCHRONOLOGICAL PATAGONIA |
title_short |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation |
title_full |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation |
title_fullStr |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation |
title_full_unstemmed |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation |
title_sort |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation |
dc.creator.none.fl_str_mv |
Ghiglione, Matias Barberon, Vanesa Ramos, Miguel Esteban Tobal, Jonathan Elías Garcia Morabito, Ezequiel Suárez, Rodrigo Javier Martinod, Joseph Sue, Christian |
author |
Ghiglione, Matias |
author_facet |
Ghiglione, Matias Barberon, Vanesa Ramos, Miguel Esteban Tobal, Jonathan Elías Garcia Morabito, Ezequiel Suárez, Rodrigo Javier Martinod, Joseph Sue, Christian |
author_role |
author |
author2 |
Barberon, Vanesa Ramos, Miguel Esteban Tobal, Jonathan Elías Garcia Morabito, Ezequiel Suárez, Rodrigo Javier Martinod, Joseph Sue, Christian |
author2_role |
author author author author author author author |
dc.subject.none.fl_str_mv |
STRUCTURE EXHUMATION THERMOCHRONOLOGICAL PATAGONIA |
topic |
STRUCTURE EXHUMATION THERMOCHRONOLOGICAL PATAGONIA |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
We present an appraisal of structural domains in the SPA (Southern Patagonian Andes) between 46° and 52°S, recognizing a thickskinnedBD (Basement domain) and a hybrid thick- and thin-skinned systems in the FTB (fold and thrust belt).Two major structural segments can be clearly defined north and south of 48°30´: (1) Northern segment: With a steady orogenicwidth of around 340-360km, is characterized by a well-developed basement domain, and a narrow FTB. The inner domain of theFTB is very narrow.The comparison of our geometrical data with exhumation patterns from thermochronological studies evidences importantcorrelations: (1) The wide basement in the northern sector coincides with exhumation ages younger than 3 Ma throughout thisdomain. It has been proposed that this sector was dominated by highly efficient alpine glacial erosion, producing this characteristicyoung exhumation pattern (Thomson 2010). In terms of the critical wedge theory, enhanced erosive exhumation in the highlandof the retro wedge produces active tectonic uplift of the basement domain; while the basement is constantly subdued under thecritical angle, the thrust front does not advance, and the FTB is underdeveloped, in agreement with our empirical observations. (2)The abrupt and steady increase in width and shortening of the FTB towards the southern sector coincides with older basementcooling ages which indicate much reduced late Cenozoic erosion despite dominantly glacial conditions here since the latestMiocene (Thomson et al., 2010). Although orogen width does seem to be around 25% wider between 48°30´and 50°SL, it showsa gradual decline towards the south. Older exhumation ages in the Basement domain coincides with a thicker sedimentary coverand erosion focused in the retroarc, as expected by the critical wedge theory, predicting the development of a wider FTB. 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: Barberon, Vanesa. 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: 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. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Tobal, Jonathan Elías. 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: Garcia Morabito, Ezequiel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio. Universidad Nacional de Río Negro. Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio; Argentina 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: Martinod, Joseph. Université de Savoie Mont-blanc; Francia Fil: Sue, Christian. Universite de Franche-Comte; Francia XV Congreso Geológico Chileno Concepción Chile Universidad de Concepción Colegio de Geólogos de Chile Sociedad Geológica de Chile |
description |
We present an appraisal of structural domains in the SPA (Southern Patagonian Andes) between 46° and 52°S, recognizing a thickskinnedBD (Basement domain) and a hybrid thick- and thin-skinned systems in the FTB (fold and thrust belt).Two major structural segments can be clearly defined north and south of 48°30´: (1) Northern segment: With a steady orogenicwidth of around 340-360km, is characterized by a well-developed basement domain, and a narrow FTB. The inner domain of theFTB is very narrow.The comparison of our geometrical data with exhumation patterns from thermochronological studies evidences importantcorrelations: (1) The wide basement in the northern sector coincides with exhumation ages younger than 3 Ma throughout thisdomain. It has been proposed that this sector was dominated by highly efficient alpine glacial erosion, producing this characteristicyoung exhumation pattern (Thomson 2010). In terms of the critical wedge theory, enhanced erosive exhumation in the highlandof the retro wedge produces active tectonic uplift of the basement domain; while the basement is constantly subdued under thecritical angle, the thrust front does not advance, and the FTB is underdeveloped, in agreement with our empirical observations. (2)The abrupt and steady increase in width and shortening of the FTB towards the southern sector coincides with older basementcooling ages which indicate much reduced late Cenozoic erosion despite dominantly glacial conditions here since the latestMiocene (Thomson et al., 2010). Although orogen width does seem to be around 25% wider between 48°30´and 50°SL, it showsa gradual decline towards the south. Older exhumation ages in the Basement domain coincides with a thicker sedimentary coverand erosion focused in the retroarc, as expected by the critical wedge theory, predicting the development of a wider FTB. |
publishDate |
2018 |
dc.date.none.fl_str_mv |
2018 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject Congreso 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/11336/268071 Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation; XV Congreso Geológico Chileno; Concepción; Chile; 2018; 1208-1208 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/268071 |
identifier_str_mv |
Structure and tectonic evolution of the South Patagonian fold and thrust belt: pairing between subduction dynamics, climate and tectonic deformation; XV Congreso Geológico Chileno; Concepción; Chile; 2018; 1208-1208 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://congresogeologicochileno.cl/wp-content/uploads/2018/12/Libro-de-Actas-XVCongresoGeologicoChileno2018-2.pdf |
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 |
dc.coverage.none.fl_str_mv |
Internacional |
dc.publisher.none.fl_str_mv |
Universidad de Concepción |
publisher.none.fl_str_mv |
Universidad de Concepción |
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_ |
1844613725984653312 |
score |
13.070432 |