The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes

Autores
Torres Carbonell, Pablo Juan; Cao, Sebastián José; Gonzalez Guillot, Mauricio Alberto; Mosqueira González, María Victoria; Dimieri, Luis Vicente; Duval, Florian; Scaillet, Stéphane
Año de publicación
2020
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
New detailed structural data from the Fuegian Andes including new ages and cross-cutting relationships with intrusive rocks, as well as an appraisal of published structural data, support that this orogen evolved as a basement-involved thrust-fold belt after initial formation in an arc-continent collision scenario. New structural data from a deformed 84 Ma intrusive indicate that structures from the collisional event in the Argentine Fuegian Andes are of Campanian age, comprising only the youngest and less intense deformation of the orogenic wedge. In the internal thrust-fold belt, these structures are cut by intrusives with new ages of 74 Ma (Ar/Ar on hornblende). The superposition of thrusts on these early structures indicates a subsequent event in which a thrust-fold belt formed since the Maastrichtian-Danian. Additional new data confirm brittle-ductile thrusting in the central belt, with thrusts joining a common upper detachment in the base of the Lower Cretaceous rocks. These thrusts formed a first-order duplex system that transferred the shortening accommodated in the foreland until the Miocene.
Fil: Torres Carbonell, Pablo Juan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Cao, Sebastián José. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Gonzalez Guillot, Mauricio Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Mosqueira González, María Victoria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Dimieri, Luis Vicente. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Duval, Florian. Université d´Orléans; Francia. Centre National de la Recherche Scientifique; Francia
Fil: Scaillet, Stéphane. Centre National de la Recherche Scientifique; Francia
Materia
ARC-CONTINENT COLLISION
THRUST-FOLD BELT
AR/AR DATING
DEFORMATION CHRONOLOGY
FUEGIAN ANDES
Nivel de accesibilidad
acceso embargado
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:11336/110499

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network_name_str CONICET Digital (CONICET)
spelling The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost AndesTorres Carbonell, Pablo JuanCao, Sebastián JoséGonzalez Guillot, Mauricio AlbertoMosqueira González, María VictoriaDimieri, Luis VicenteDuval, FlorianScaillet, StéphaneARC-CONTINENT COLLISIONTHRUST-FOLD BELTAR/AR DATINGDEFORMATION CHRONOLOGYFUEGIAN ANDEShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1New detailed structural data from the Fuegian Andes including new ages and cross-cutting relationships with intrusive rocks, as well as an appraisal of published structural data, support that this orogen evolved as a basement-involved thrust-fold belt after initial formation in an arc-continent collision scenario. New structural data from a deformed 84 Ma intrusive indicate that structures from the collisional event in the Argentine Fuegian Andes are of Campanian age, comprising only the youngest and less intense deformation of the orogenic wedge. In the internal thrust-fold belt, these structures are cut by intrusives with new ages of 74 Ma (Ar/Ar on hornblende). The superposition of thrusts on these early structures indicates a subsequent event in which a thrust-fold belt formed since the Maastrichtian-Danian. Additional new data confirm brittle-ductile thrusting in the central belt, with thrusts joining a common upper detachment in the base of the Lower Cretaceous rocks. These thrusts formed a first-order duplex system that transferred the shortening accommodated in the foreland until the Miocene.Fil: Torres Carbonell, Pablo Juan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Cao, Sebastián José. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; ArgentinaFil: Gonzalez Guillot, Mauricio Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; ArgentinaFil: Mosqueira González, María Victoria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Dimieri, Luis Vicente. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; ArgentinaFil: Duval, Florian. Université d´Orléans; Francia. Centre National de la Recherche Scientifique; FranciaFil: Scaillet, Stéphane. Centre National de la Recherche Scientifique; FranciaPergamon-Elsevier Science Ltd2020-10-12info:eu-repo/date/embargoEnd/2020-12-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/110499Torres Carbonell, Pablo Juan; Cao, Sebastián José; Gonzalez Guillot, Mauricio Alberto; Mosqueira González, María Victoria; Dimieri, Luis Vicente; et al.; The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 102; 12-10-20200895-9811CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0895981120302212info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2020.102678info:eu-repo/semantics/embargoedAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:04:37Zoai:ri.conicet.gov.ar:11336/110499instacron: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 10:04:37.348CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
title The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
spellingShingle The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
Torres Carbonell, Pablo Juan
ARC-CONTINENT COLLISION
THRUST-FOLD BELT
AR/AR DATING
DEFORMATION CHRONOLOGY
FUEGIAN ANDES
title_short The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
title_full The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
title_fullStr The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
title_full_unstemmed The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
title_sort The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes
dc.creator.none.fl_str_mv Torres Carbonell, Pablo Juan
Cao, Sebastián José
Gonzalez Guillot, Mauricio Alberto
Mosqueira González, María Victoria
Dimieri, Luis Vicente
Duval, Florian
Scaillet, Stéphane
author Torres Carbonell, Pablo Juan
author_facet Torres Carbonell, Pablo Juan
Cao, Sebastián José
Gonzalez Guillot, Mauricio Alberto
Mosqueira González, María Victoria
Dimieri, Luis Vicente
Duval, Florian
Scaillet, Stéphane
author_role author
author2 Cao, Sebastián José
Gonzalez Guillot, Mauricio Alberto
Mosqueira González, María Victoria
Dimieri, Luis Vicente
Duval, Florian
Scaillet, Stéphane
author2_role author
author
author
author
author
author
dc.subject.none.fl_str_mv ARC-CONTINENT COLLISION
THRUST-FOLD BELT
AR/AR DATING
DEFORMATION CHRONOLOGY
FUEGIAN ANDES
topic ARC-CONTINENT COLLISION
THRUST-FOLD BELT
AR/AR DATING
DEFORMATION CHRONOLOGY
FUEGIAN ANDES
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv New detailed structural data from the Fuegian Andes including new ages and cross-cutting relationships with intrusive rocks, as well as an appraisal of published structural data, support that this orogen evolved as a basement-involved thrust-fold belt after initial formation in an arc-continent collision scenario. New structural data from a deformed 84 Ma intrusive indicate that structures from the collisional event in the Argentine Fuegian Andes are of Campanian age, comprising only the youngest and less intense deformation of the orogenic wedge. In the internal thrust-fold belt, these structures are cut by intrusives with new ages of 74 Ma (Ar/Ar on hornblende). The superposition of thrusts on these early structures indicates a subsequent event in which a thrust-fold belt formed since the Maastrichtian-Danian. Additional new data confirm brittle-ductile thrusting in the central belt, with thrusts joining a common upper detachment in the base of the Lower Cretaceous rocks. These thrusts formed a first-order duplex system that transferred the shortening accommodated in the foreland until the Miocene.
Fil: Torres Carbonell, Pablo Juan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Cao, Sebastián José. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Gonzalez Guillot, Mauricio Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Mosqueira González, María Victoria. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Dimieri, Luis Vicente. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Duval, Florian. Université d´Orléans; Francia. Centre National de la Recherche Scientifique; Francia
Fil: Scaillet, Stéphane. Centre National de la Recherche Scientifique; Francia
description New detailed structural data from the Fuegian Andes including new ages and cross-cutting relationships with intrusive rocks, as well as an appraisal of published structural data, support that this orogen evolved as a basement-involved thrust-fold belt after initial formation in an arc-continent collision scenario. New structural data from a deformed 84 Ma intrusive indicate that structures from the collisional event in the Argentine Fuegian Andes are of Campanian age, comprising only the youngest and less intense deformation of the orogenic wedge. In the internal thrust-fold belt, these structures are cut by intrusives with new ages of 74 Ma (Ar/Ar on hornblende). The superposition of thrusts on these early structures indicates a subsequent event in which a thrust-fold belt formed since the Maastrichtian-Danian. Additional new data confirm brittle-ductile thrusting in the central belt, with thrusts joining a common upper detachment in the base of the Lower Cretaceous rocks. These thrusts formed a first-order duplex system that transferred the shortening accommodated in the foreland until the Miocene.
publishDate 2020
dc.date.none.fl_str_mv 2020-10-12
info:eu-repo/date/embargoEnd/2020-12-12
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/11336/110499
Torres Carbonell, Pablo Juan; Cao, Sebastián José; Gonzalez Guillot, Mauricio Alberto; Mosqueira González, María Victoria; Dimieri, Luis Vicente; et al.; The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 102; 12-10-2020
0895-9811
CONICET Digital
CONICET
url http://hdl.handle.net/11336/110499
identifier_str_mv Torres Carbonell, Pablo Juan; Cao, Sebastián José; Gonzalez Guillot, Mauricio Alberto; Mosqueira González, María Victoria; Dimieri, Luis Vicente; et al.; The Fuegian thrust-fold belt: From arc-continent collision to thrust-related deformation in the southernmost Andes; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 102; 12-10-2020
0895-9811
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.sciencedirect.com/science/article/abs/pii/S0895981120302212
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2020.102678
dc.rights.none.fl_str_mv info:eu-repo/semantics/embargoedAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv embargoedAccess
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.publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
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instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
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repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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