Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina
- Autores
- Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Altenberger, Uwe; Arnous, Ahmad
- Año de publicación
- 2023
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Investigations into the Andean orocline revealed a counterclockwise rotation of about 37° in the north and a clockwise rotation of about 29° in the south. This rotation would have started in the Eocene because the Nazca and South American plates converged. The transition zone between the Puna and the Sierras Pampeanas has a clockwise rotation pattern. Our new data show that the NE convergence of the Nazca and South American plates caused the counterclockwise rotation around the NW end of the Sierras Pampeanas. The temperature rise during a magmatic activity at 13 Ma would have favored a counterclockwise rotation of the mountain blocks of about 20° on a detachment zone within 10 to 15 km of depth. These range rotations generated local stress tensors trending NE and NW, facilitating the development of valleys, basins, mineralized dikes, mineral deposits, and alluvial fans separated from their origin. The Atajo fault shows both ductile and brittle characteristics. A mylonitic belt from the Sierra de Aconquija was juxtaposed on the rocks of the Ovejería Block and the Farallón Negro Volcanic Complex by reverse vertical displacement, and a dextral horizontal component of displacement resulted in curvatures that gave rise to pull-apart basins and step over features. The Santa Maria Valley, Campo del Arenal, Hualfín Valley, and Pipanaco salt flat most likely constituted a vast early Miocene basin rarely interrupted by low feature relief.
Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Fil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Fil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina
Fil: Altenberger, Uwe. Universitat Potsdam; Alemania
Fil: Arnous, Ahmad. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina - Materia
-
NEOTECTONIC
COUNTERCLOCKWISE ROTATION
ANDES
SIERRAS PAMPEANAS - 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:11336/222756
Ver los metadatos del registro completo
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Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, ArgentinaGutierrez, Adolfo AntonioMon, RicardoCisterna, Clara EugeniaAltenberger, UweArnous, AhmadNEOTECTONICCOUNTERCLOCKWISE ROTATIONANDESSIERRAS PAMPEANAShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Investigations into the Andean orocline revealed a counterclockwise rotation of about 37° in the north and a clockwise rotation of about 29° in the south. This rotation would have started in the Eocene because the Nazca and South American plates converged. The transition zone between the Puna and the Sierras Pampeanas has a clockwise rotation pattern. Our new data show that the NE convergence of the Nazca and South American plates caused the counterclockwise rotation around the NW end of the Sierras Pampeanas. The temperature rise during a magmatic activity at 13 Ma would have favored a counterclockwise rotation of the mountain blocks of about 20° on a detachment zone within 10 to 15 km of depth. These range rotations generated local stress tensors trending NE and NW, facilitating the development of valleys, basins, mineralized dikes, mineral deposits, and alluvial fans separated from their origin. The Atajo fault shows both ductile and brittle characteristics. A mylonitic belt from the Sierra de Aconquija was juxtaposed on the rocks of the Ovejería Block and the Farallón Negro Volcanic Complex by reverse vertical displacement, and a dextral horizontal component of displacement resulted in curvatures that gave rise to pull-apart basins and step over features. The Santa Maria Valley, Campo del Arenal, Hualfín Valley, and Pipanaco salt flat most likely constituted a vast early Miocene basin rarely interrupted by low feature relief.Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; ArgentinaFil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; ArgentinaFil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; ArgentinaFil: Altenberger, Uwe. Universitat Potsdam; AlemaniaFil: Arnous, Ahmad. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaScientific Research Publishing Inc.2023-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/222756Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Altenberger, Uwe; Arnous, Ahmad; Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina; Scientific Research Publishing Inc.; Open Journal of Geology; 13; 05; 5-2023; 345-3832161-7589CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.4236/ojg.2023.135018info:eu-repo/semantics/altIdentifier/url/https://www.scirp.org/journal/paperinformation?paperid=125255info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:56:24Zoai:ri.conicet.gov.ar:11336/222756instacron: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 09:56:24.499CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina |
title |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina |
spellingShingle |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina Gutierrez, Adolfo Antonio NEOTECTONIC COUNTERCLOCKWISE ROTATION ANDES SIERRAS PAMPEANAS |
title_short |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina |
title_full |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina |
title_fullStr |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina |
title_full_unstemmed |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina |
title_sort |
Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina |
dc.creator.none.fl_str_mv |
Gutierrez, Adolfo Antonio Mon, Ricardo Cisterna, Clara Eugenia Altenberger, Uwe Arnous, Ahmad |
author |
Gutierrez, Adolfo Antonio |
author_facet |
Gutierrez, Adolfo Antonio Mon, Ricardo Cisterna, Clara Eugenia Altenberger, Uwe Arnous, Ahmad |
author_role |
author |
author2 |
Mon, Ricardo Cisterna, Clara Eugenia Altenberger, Uwe Arnous, Ahmad |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
NEOTECTONIC COUNTERCLOCKWISE ROTATION ANDES SIERRAS PAMPEANAS |
topic |
NEOTECTONIC COUNTERCLOCKWISE ROTATION ANDES SIERRAS PAMPEANAS |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Investigations into the Andean orocline revealed a counterclockwise rotation of about 37° in the north and a clockwise rotation of about 29° in the south. This rotation would have started in the Eocene because the Nazca and South American plates converged. The transition zone between the Puna and the Sierras Pampeanas has a clockwise rotation pattern. Our new data show that the NE convergence of the Nazca and South American plates caused the counterclockwise rotation around the NW end of the Sierras Pampeanas. The temperature rise during a magmatic activity at 13 Ma would have favored a counterclockwise rotation of the mountain blocks of about 20° on a detachment zone within 10 to 15 km of depth. These range rotations generated local stress tensors trending NE and NW, facilitating the development of valleys, basins, mineralized dikes, mineral deposits, and alluvial fans separated from their origin. The Atajo fault shows both ductile and brittle characteristics. A mylonitic belt from the Sierra de Aconquija was juxtaposed on the rocks of the Ovejería Block and the Farallón Negro Volcanic Complex by reverse vertical displacement, and a dextral horizontal component of displacement resulted in curvatures that gave rise to pull-apart basins and step over features. The Santa Maria Valley, Campo del Arenal, Hualfín Valley, and Pipanaco salt flat most likely constituted a vast early Miocene basin rarely interrupted by low feature relief. Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina Fil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina Fil: Cisterna, Clara Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina Fil: Altenberger, Uwe. Universitat Potsdam; Alemania Fil: Arnous, Ahmad. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina |
description |
Investigations into the Andean orocline revealed a counterclockwise rotation of about 37° in the north and a clockwise rotation of about 29° in the south. This rotation would have started in the Eocene because the Nazca and South American plates converged. The transition zone between the Puna and the Sierras Pampeanas has a clockwise rotation pattern. Our new data show that the NE convergence of the Nazca and South American plates caused the counterclockwise rotation around the NW end of the Sierras Pampeanas. The temperature rise during a magmatic activity at 13 Ma would have favored a counterclockwise rotation of the mountain blocks of about 20° on a detachment zone within 10 to 15 km of depth. These range rotations generated local stress tensors trending NE and NW, facilitating the development of valleys, basins, mineralized dikes, mineral deposits, and alluvial fans separated from their origin. The Atajo fault shows both ductile and brittle characteristics. A mylonitic belt from the Sierra de Aconquija was juxtaposed on the rocks of the Ovejería Block and the Farallón Negro Volcanic Complex by reverse vertical displacement, and a dextral horizontal component of displacement resulted in curvatures that gave rise to pull-apart basins and step over features. The Santa Maria Valley, Campo del Arenal, Hualfín Valley, and Pipanaco salt flat most likely constituted a vast early Miocene basin rarely interrupted by low feature relief. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023-05 |
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/11336/222756 Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Altenberger, Uwe; Arnous, Ahmad; Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina; Scientific Research Publishing Inc.; Open Journal of Geology; 13; 05; 5-2023; 345-383 2161-7589 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/222756 |
identifier_str_mv |
Gutierrez, Adolfo Antonio; Mon, Ricardo; Cisterna, Clara Eugenia; Altenberger, Uwe; Arnous, Ahmad; Cenozoic Age Counterclockwise Rotation in the Northwest End of the Sierras Pampeanas, Argentina; Scientific Research Publishing Inc.; Open Journal of Geology; 13; 05; 5-2023; 345-383 2161-7589 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.4236/ojg.2023.135018 info:eu-repo/semantics/altIdentifier/url/https://www.scirp.org/journal/paperinformation?paperid=125255 |
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.publisher.none.fl_str_mv |
Scientific Research Publishing Inc. |
publisher.none.fl_str_mv |
Scientific Research Publishing Inc. |
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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CONICET Digital (CONICET) |
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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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1844613694475993088 |
score |
13.070432 |