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
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/260894
Ver los metadatos del registro completo
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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 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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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 |
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eng |
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eng |
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American Geophysical Union |
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American Geophysical Union |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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