Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin

Autores
van Kooten, Willemijn S. M. T.; Vallati, Michele; Sobel, Edward Robert; del Papa, Cecilia Eugenia; Payrola Bosio, Patricio Augusto; Starck, Daniel; Bande, Alejandro; Wayar Córdoba, Maria F.; Lapiana, Ayelén Trinidad; Glodny, Johannes
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The present‐day deformation style of the Eastern Cordillera in NW Argentina is stronglyinfluenced by the inversion of pre‐existing Paleozoic and Mesozoic structures. In particular, the extensional faults and lithological contrasts resulting from the Cretaceous–Paleogene Salta Rift phase form heterogeneities that were preferentially reactivated during the Andean orogeny. Constraining the timing and characteristics of reactivation is a key to understanding the interplay between tectonics and inherited crustal anisotropies. In this study, we combine structural and sedimentological field data with a low‐temperature thermochronology data set from the area surrounding the fault‐bounded Cianzo basin. The southeastern boundary is formed by the invertedHornocal fault, which was the basin‐bounding normal fault of the Lomas de Olmedo sub‐basin (Salta Rift basin). Lacustrine deposits of the Yacoraite Formation overspill on the footwall of this fault and mark tectonic quiescence during the post‐rift phase of the Salta Rift. Apatite (U‐Th‐Sm)/He and fission track ages in the Hornocal fault hanging wall show an onset of rapid cooling interpreted to be concomitant with fault inversion between the latest Oligocene and middle Miocene (∼24–15 Ma). Low‐temperature thermochronology data also constrain the timing of major folding in the eastern limb of the Cianzo syncline to pre‐10 Ma, whereas the western limb started tilting post‐10 Ma. Characterization of exhumation patterns related to fault activity surrounding the Cianzo basin.
Fil: van Kooten, Willemijn S. M. T.. Universitat Potsdam; Alemania
Fil: Vallati, Michele. Universitat Potsdam; Alemania
Fil: Sobel, Edward Robert. Universitat Potsdam; Alemania
Fil: del Papa, Cecilia Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Payrola Bosio, Patricio Augusto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina
Fil: Starck, Daniel. Independiente; Argentina
Fil: Bande, Alejandro. Tecpetrol S.A.; Argentina
Fil: Wayar Córdoba, Maria F.. Montgomery & Associates Consultores Argentina; Argentina
Fil: Lapiana, Ayelén Trinidad. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Glodny, Johannes. German Research Centre for Geosciences; Alemania
Materia
Out-of sequence deformation
Salta Group
Oligocene Miocene
Pre‐existing structures
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/260894

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oai_identifier_str oai:ri.conicet.gov.ar:11336/260894
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repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basinvan Kooten, Willemijn S. M. T.Vallati, MicheleSobel, Edward Robertdel Papa, Cecilia EugeniaPayrola Bosio, Patricio AugustoStarck, DanielBande, AlejandroWayar Córdoba, Maria F.Lapiana, Ayelén TrinidadGlodny, JohannesOut-of sequence deformationSalta GroupOligocene MiocenePre‐existing structureshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The present‐day deformation style of the Eastern Cordillera in NW Argentina is stronglyinfluenced by the inversion of pre‐existing Paleozoic and Mesozoic structures. In particular, the extensional faults and lithological contrasts resulting from the Cretaceous–Paleogene Salta Rift phase form heterogeneities that were preferentially reactivated during the Andean orogeny. Constraining the timing and characteristics of reactivation is a key to understanding the interplay between tectonics and inherited crustal anisotropies. In this study, we combine structural and sedimentological field data with a low‐temperature thermochronology data set from the area surrounding the fault‐bounded Cianzo basin. The southeastern boundary is formed by the invertedHornocal fault, which was the basin‐bounding normal fault of the Lomas de Olmedo sub‐basin (Salta Rift basin). Lacustrine deposits of the Yacoraite Formation overspill on the footwall of this fault and mark tectonic quiescence during the post‐rift phase of the Salta Rift. Apatite (U‐Th‐Sm)/He and fission track ages in the Hornocal fault hanging wall show an onset of rapid cooling interpreted to be concomitant with fault inversion between the latest Oligocene and middle Miocene (∼24–15 Ma). Low‐temperature thermochronology data also constrain the timing of major folding in the eastern limb of the Cianzo syncline to pre‐10 Ma, whereas the western limb started tilting post‐10 Ma. Characterization of exhumation patterns related to fault activity surrounding the Cianzo basin.Fil: van Kooten, Willemijn S. M. T.. Universitat Potsdam; AlemaniaFil: Vallati, Michele. Universitat Potsdam; AlemaniaFil: Sobel, Edward Robert. Universitat Potsdam; AlemaniaFil: del Papa, Cecilia Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaFil: Payrola Bosio, Patricio Augusto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; ArgentinaFil: Starck, Daniel. Independiente; ArgentinaFil: Bande, Alejandro. Tecpetrol S.A.; ArgentinaFil: Wayar Córdoba, Maria F.. Montgomery & Associates Consultores Argentina; ArgentinaFil: Lapiana, Ayelén Trinidad. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaFil: Glodny, Johannes. German Research Centre for Geosciences; AlemaniaAmerican Geophysical Union2024-06info: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/11336/260894van Kooten, Willemijn S. M. T.; Vallati, Michele; Sobel, Edward Robert; del Papa, Cecilia Eugenia; Payrola Bosio, Patricio Augusto; et al.; Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin; American Geophysical Union; Tectonics; 43; 6; 6-2024; 1-320278-7407CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023TC007949info:eu-repo/semantics/altIdentifier/doi/10.1029/2023TC007949info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-04-15T10:07:36Zoai:ri.conicet.gov.ar:11336/260894instacron: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:34982026-04-15 10:07:37.216CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
title Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
spellingShingle Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
van Kooten, Willemijn S. M. T.
Out-of sequence deformation
Salta Group
Oligocene Miocene
Pre‐existing structures
title_short Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
title_full Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
title_fullStr Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
title_full_unstemmed Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
title_sort Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin
dc.creator.none.fl_str_mv van Kooten, Willemijn S. M. T.
Vallati, Michele
Sobel, Edward Robert
del Papa, Cecilia Eugenia
Payrola Bosio, Patricio Augusto
Starck, Daniel
Bande, Alejandro
Wayar Córdoba, Maria F.
Lapiana, Ayelén Trinidad
Glodny, Johannes
author van Kooten, Willemijn S. M. T.
author_facet van Kooten, Willemijn S. M. T.
Vallati, Michele
Sobel, Edward Robert
del Papa, Cecilia Eugenia
Payrola Bosio, Patricio Augusto
Starck, Daniel
Bande, Alejandro
Wayar Córdoba, Maria F.
Lapiana, Ayelén Trinidad
Glodny, Johannes
author_role author
author2 Vallati, Michele
Sobel, Edward Robert
del Papa, Cecilia Eugenia
Payrola Bosio, Patricio Augusto
Starck, Daniel
Bande, Alejandro
Wayar Córdoba, Maria F.
Lapiana, Ayelén Trinidad
Glodny, Johannes
author2_role author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Out-of sequence deformation
Salta Group
Oligocene Miocene
Pre‐existing structures
topic Out-of sequence deformation
Salta Group
Oligocene Miocene
Pre‐existing structures
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 present‐day deformation style of the Eastern Cordillera in NW Argentina is stronglyinfluenced by the inversion of pre‐existing Paleozoic and Mesozoic structures. In particular, the extensional faults and lithological contrasts resulting from the Cretaceous–Paleogene Salta Rift phase form heterogeneities that were preferentially reactivated during the Andean orogeny. Constraining the timing and characteristics of reactivation is a key to understanding the interplay between tectonics and inherited crustal anisotropies. In this study, we combine structural and sedimentological field data with a low‐temperature thermochronology data set from the area surrounding the fault‐bounded Cianzo basin. The southeastern boundary is formed by the invertedHornocal fault, which was the basin‐bounding normal fault of the Lomas de Olmedo sub‐basin (Salta Rift basin). Lacustrine deposits of the Yacoraite Formation overspill on the footwall of this fault and mark tectonic quiescence during the post‐rift phase of the Salta Rift. Apatite (U‐Th‐Sm)/He and fission track ages in the Hornocal fault hanging wall show an onset of rapid cooling interpreted to be concomitant with fault inversion between the latest Oligocene and middle Miocene (∼24–15 Ma). Low‐temperature thermochronology data also constrain the timing of major folding in the eastern limb of the Cianzo syncline to pre‐10 Ma, whereas the western limb started tilting post‐10 Ma. Characterization of exhumation patterns related to fault activity surrounding the Cianzo basin.
Fil: van Kooten, Willemijn S. M. T.. Universitat Potsdam; Alemania
Fil: Vallati, Michele. Universitat Potsdam; Alemania
Fil: Sobel, Edward Robert. Universitat Potsdam; Alemania
Fil: del Papa, Cecilia Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Payrola Bosio, Patricio Augusto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Bio y Geociencias del NOA. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Museo de Ciencias Naturales. Instituto de Bio y Geociencias del NOA; Argentina
Fil: Starck, Daniel. Independiente; Argentina
Fil: Bande, Alejandro. Tecpetrol S.A.; Argentina
Fil: Wayar Córdoba, Maria F.. Montgomery & Associates Consultores Argentina; Argentina
Fil: Lapiana, Ayelén Trinidad. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Glodny, Johannes. German Research Centre for Geosciences; Alemania
description The present‐day deformation style of the Eastern Cordillera in NW Argentina is stronglyinfluenced by the inversion of pre‐existing Paleozoic and Mesozoic structures. In particular, the extensional faults and lithological contrasts resulting from the Cretaceous–Paleogene Salta Rift phase form heterogeneities that were preferentially reactivated during the Andean orogeny. Constraining the timing and characteristics of reactivation is a key to understanding the interplay between tectonics and inherited crustal anisotropies. In this study, we combine structural and sedimentological field data with a low‐temperature thermochronology data set from the area surrounding the fault‐bounded Cianzo basin. The southeastern boundary is formed by the invertedHornocal fault, which was the basin‐bounding normal fault of the Lomas de Olmedo sub‐basin (Salta Rift basin). Lacustrine deposits of the Yacoraite Formation overspill on the footwall of this fault and mark tectonic quiescence during the post‐rift phase of the Salta Rift. Apatite (U‐Th‐Sm)/He and fission track ages in the Hornocal fault hanging wall show an onset of rapid cooling interpreted to be concomitant with fault inversion between the latest Oligocene and middle Miocene (∼24–15 Ma). Low‐temperature thermochronology data also constrain the timing of major folding in the eastern limb of the Cianzo syncline to pre‐10 Ma, whereas the western limb started tilting post‐10 Ma. Characterization of exhumation patterns related to fault activity surrounding the Cianzo basin.
publishDate 2024
dc.date.none.fl_str_mv 2024-06
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/11336/260894
van Kooten, Willemijn S. M. T.; Vallati, Michele; Sobel, Edward Robert; del Papa, Cecilia Eugenia; Payrola Bosio, Patricio Augusto; et al.; Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin; American Geophysical Union; Tectonics; 43; 6; 6-2024; 1-32
0278-7407
CONICET Digital
CONICET
url http://hdl.handle.net/11336/260894
identifier_str_mv van Kooten, Willemijn S. M. T.; Vallati, Michele; Sobel, Edward Robert; del Papa, Cecilia Eugenia; Payrola Bosio, Patricio Augusto; et al.; Structural Inheritance in the Eastern Cordillera, NW Argentina: Low‐Temperature Thermochronology of the Cianzo Basin; American Geophysical Union; Tectonics; 43; 6; 6-2024; 1-32
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/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023TC007949
info:eu-repo/semantics/altIdentifier/doi/10.1029/2023TC007949
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/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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