Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny

Autores
Ciccioli, Patricia Lucia; Marenssi, Sergio Alfredo; Rossello, Eduardo Antonio; Limarino, Carlos Oscar
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volcanic mountains belts in South America reaching up to 6200 m in height. Despite the fact that the uplift of the Nevados del Famatina was (and is) closely related to the Andean Orogeny, these mountains are located about 400 km from the Chile trench and up to 100 km from the main Andean Cordillera (Cobbold et al., 2007). The origin of the high and isolated Nevados del Famatina is related to a Neogene tectonic syntaxis due to the relationship between the left-lateral Valle Fértil wrench fault and the right-lateral Tucuman wrench fault (Rossello et al., 2011). The Vinchina Basin, a highly subsiding basin that accumulated more than 10,000 m of continental sediments during the Neogene developed between the magmatic arc, located in the Andean Cordillera, and the Famatina Mountain. The study of the sedimentary fill of the Vinchina Basin allows reconstructing not only the evolution of the magmatic arc (and its associated deformation) but also the timing and effect of the uplift of the Nevados del Famatina.
Fil: Ciccioli, Patricia Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Marenssi, Sergio Alfredo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Rossello, Eduardo Antonio. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Limarino, Carlos Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Materia
Sedimentary Pattern
Transcurrent
Vinchina
Argentina
Nivel de accesibilidad
acceso abierto
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:11336/18646
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogenyCiccioli, Patricia LuciaMarenssi, Sergio AlfredoRossello, Eduardo AntonioLimarino, Carlos OscarSedimentary PatternTranscurrentVinchinaArgentinahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volcanic mountains belts in South America reaching up to 6200 m in height. Despite the fact that the uplift of the Nevados del Famatina was (and is) closely related to the Andean Orogeny, these mountains are located about 400 km from the Chile trench and up to 100 km from the main Andean Cordillera (Cobbold et al., 2007). The origin of the high and isolated Nevados del Famatina is related to a Neogene tectonic syntaxis due to the relationship between the left-lateral Valle Fértil wrench fault and the right-lateral Tucuman wrench fault (Rossello et al., 2011). The Vinchina Basin, a highly subsiding basin that accumulated more than 10,000 m of continental sediments during the Neogene developed between the magmatic arc, located in the Andean Cordillera, and the Famatina Mountain. The study of the sedimentary fill of the Vinchina Basin allows reconstructing not only the evolution of the magmatic arc (and its associated deformation) but also the timing and effect of the uplift of the Nevados del Famatina.Fil: Ciccioli, Patricia Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Marenssi, Sergio Alfredo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Rossello, Eduardo Antonio. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Limarino, Carlos Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaIstituto Nazionale Di Oceanografia E Di Geofisica2013-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/18646Ciccioli, Patricia Lucia; Marenssi, Sergio Alfredo; Rossello, Eduardo Antonio; Limarino, Carlos Oscar; Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny; Istituto Nazionale Di Oceanografia E Di Geofisica; Bollettino Di Geofisica Teorica Ed Applicata; 54; Supplement 2; 11-2013; 217-2200006-6729CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www3.ogs.trieste.it/bgta/provapage.php?id_articolo=664info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:03:13Zoai:ri.conicet.gov.ar:11336/18646instacron: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:34982025-10-22 11:03:14.215CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
title Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
spellingShingle Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
Ciccioli, Patricia Lucia
Sedimentary Pattern
Transcurrent
Vinchina
Argentina
title_short Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
title_full Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
title_fullStr Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
title_full_unstemmed Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
title_sort Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny
dc.creator.none.fl_str_mv Ciccioli, Patricia Lucia
Marenssi, Sergio Alfredo
Rossello, Eduardo Antonio
Limarino, Carlos Oscar
author Ciccioli, Patricia Lucia
author_facet Ciccioli, Patricia Lucia
Marenssi, Sergio Alfredo
Rossello, Eduardo Antonio
Limarino, Carlos Oscar
author_role author
author2 Marenssi, Sergio Alfredo
Rossello, Eduardo Antonio
Limarino, Carlos Oscar
author2_role author
author
author
dc.subject.none.fl_str_mv Sedimentary Pattern
Transcurrent
Vinchina
Argentina
topic Sedimentary Pattern
Transcurrent
Vinchina
Argentina
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 Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volcanic mountains belts in South America reaching up to 6200 m in height. Despite the fact that the uplift of the Nevados del Famatina was (and is) closely related to the Andean Orogeny, these mountains are located about 400 km from the Chile trench and up to 100 km from the main Andean Cordillera (Cobbold et al., 2007). The origin of the high and isolated Nevados del Famatina is related to a Neogene tectonic syntaxis due to the relationship between the left-lateral Valle Fértil wrench fault and the right-lateral Tucuman wrench fault (Rossello et al., 2011). The Vinchina Basin, a highly subsiding basin that accumulated more than 10,000 m of continental sediments during the Neogene developed between the magmatic arc, located in the Andean Cordillera, and the Famatina Mountain. The study of the sedimentary fill of the Vinchina Basin allows reconstructing not only the evolution of the magmatic arc (and its associated deformation) but also the timing and effect of the uplift of the Nevados del Famatina.
Fil: Ciccioli, Patricia Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Marenssi, Sergio Alfredo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Rossello, Eduardo Antonio. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Limarino, Carlos Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; Argentina
description The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volcanic mountains belts in South America reaching up to 6200 m in height. Despite the fact that the uplift of the Nevados del Famatina was (and is) closely related to the Andean Orogeny, these mountains are located about 400 km from the Chile trench and up to 100 km from the main Andean Cordillera (Cobbold et al., 2007). The origin of the high and isolated Nevados del Famatina is related to a Neogene tectonic syntaxis due to the relationship between the left-lateral Valle Fértil wrench fault and the right-lateral Tucuman wrench fault (Rossello et al., 2011). The Vinchina Basin, a highly subsiding basin that accumulated more than 10,000 m of continental sediments during the Neogene developed between the magmatic arc, located in the Andean Cordillera, and the Famatina Mountain. The study of the sedimentary fill of the Vinchina Basin allows reconstructing not only the evolution of the magmatic arc (and its associated deformation) but also the timing and effect of the uplift of the Nevados del Famatina.
publishDate 2013
dc.date.none.fl_str_mv 2013-11
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/11336/18646
Ciccioli, Patricia Lucia; Marenssi, Sergio Alfredo; Rossello, Eduardo Antonio; Limarino, Carlos Oscar; Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny; Istituto Nazionale Di Oceanografia E Di Geofisica; Bollettino Di Geofisica Teorica Ed Applicata; 54; Supplement 2; 11-2013; 217-220
0006-6729
CONICET Digital
CONICET
url http://hdl.handle.net/11336/18646
identifier_str_mv Ciccioli, Patricia Lucia; Marenssi, Sergio Alfredo; Rossello, Eduardo Antonio; Limarino, Carlos Oscar; Sedimentary patterns in the Vinchina basin: interplay between compressional and transcurrent tectonism during the andean orogeny; Istituto Nazionale Di Oceanografia E Di Geofisica; Bollettino Di Geofisica Teorica Ed Applicata; 54; Supplement 2; 11-2013; 217-220
0006-6729
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www3.ogs.trieste.it/bgta/provapage.php?id_articolo=664
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
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Istituto Nazionale Di Oceanografia E Di Geofisica
publisher.none.fl_str_mv Istituto Nazionale Di Oceanografia E Di Geofisica
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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score 12.982451

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