The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement

Autores
Norini, Gianluca; Baez, Walter Ariel; Becchio, Raul Alberto; Viramonte, Jose German; Giordano, Guido; Arnosio, José Marcelo; Pinton, Annamaria; Gropelli, Gianluca
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The structural evolution of the Puna Plateau is characterized by the activity of both orogen-parallel and orogen-oblique faults. Understanding the possible relationship between these two structural styles, their geodynamic implications and the influence on the migration of magmas is important to get insights into the tectonic and magmatic evolution of the Central Andes. In this study, we present a structural analysis of the orogen-oblique Calama-Olacapato-El Toro fault system and the surrounding orogen-parallel thrust faults in the central-eastern Puna Plateau. Morphostructural analysis and field mapping reveal the geometry, kinematics and dynamics of the tectonic features in the studied area. We propose a three-dimensional geometrical reconstruction of the main fault planes showing their attitude and intersections at depth. The study indicates that the crust underwent simultaneous deformation along both the vertical transcurrent Calama-Olacapato-El Toro fault system and the low-angle thrust faults, and that the back-arc portion of the Calama-Olacapato-El Toro fault system developed as a transfer zone among the main N-striking thrusts. Our model considers that both orogen-parallel and orogen-oblique fault systems should be regarded as parts of the same tectonic system, accommodating crustal shortening of a thickened crust. The study suggests that the tectonic control on the magma and fluid circulation in the crust is mainly related to the geometry of the fault planes and the orientation of the stress field, with a previously unrecognized important role played by the orogen-parallel thrust faults on the emplacement of the stratovolcanoes.
Fil: Norini, Gianluca. Consiglio Nazionale Delle Ricerche. Istituto per la Dinamica dei Processi Ambientali ; Italia;
Fil: Baez, Walter Ariel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET- Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;
Fil: Becchio, Raul Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET - Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;
Fil: Viramonte, Jose German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET - Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;
Fil: Giordano, Guido. Università degli Studi Roma Tre. Dipartimento di Scienze Geologiche; Italia;
Fil: Arnosio, José Marcelo. Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina; Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Cientifico Tecnológico - CONICET - Salta; Argentina;
Fil: Pinton, Annamaria. Università degli Studi Roma Tre. Dipartimento di Scienze Geologiche; Italia;
Fil: Gropelli, Gianluca. Consiglio Nazionale Delle Ricerche. Istituto per la Dinamica dei Processi Ambientali ; Italia;
Materia
Calama-Olacapato-El Toro Fault System
Volcano-Tectonics Interplay
3d Reconstruction of Fault Planes
Transfer Fault Systems
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:11336/2090
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/2090
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacementNorini, GianlucaBaez, Walter ArielBecchio, Raul AlbertoViramonte, Jose GermanGiordano, GuidoArnosio, José MarceloPinton, AnnamariaGropelli, GianlucaCalama-Olacapato-El Toro Fault SystemVolcano-Tectonics Interplay3d Reconstruction of Fault PlanesTransfer Fault Systemshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The structural evolution of the Puna Plateau is characterized by the activity of both orogen-parallel and orogen-oblique faults. Understanding the possible relationship between these two structural styles, their geodynamic implications and the influence on the migration of magmas is important to get insights into the tectonic and magmatic evolution of the Central Andes. In this study, we present a structural analysis of the orogen-oblique Calama-Olacapato-El Toro fault system and the surrounding orogen-parallel thrust faults in the central-eastern Puna Plateau. Morphostructural analysis and field mapping reveal the geometry, kinematics and dynamics of the tectonic features in the studied area. We propose a three-dimensional geometrical reconstruction of the main fault planes showing their attitude and intersections at depth. The study indicates that the crust underwent simultaneous deformation along both the vertical transcurrent Calama-Olacapato-El Toro fault system and the low-angle thrust faults, and that the back-arc portion of the Calama-Olacapato-El Toro fault system developed as a transfer zone among the main N-striking thrusts. Our model considers that both orogen-parallel and orogen-oblique fault systems should be regarded as parts of the same tectonic system, accommodating crustal shortening of a thickened crust. The study suggests that the tectonic control on the magma and fluid circulation in the crust is mainly related to the geometry of the fault planes and the orientation of the stress field, with a previously unrecognized important role played by the orogen-parallel thrust faults on the emplacement of the stratovolcanoes.Fil: Norini, Gianluca. Consiglio Nazionale Delle Ricerche. Istituto per la Dinamica dei Processi Ambientali ; Italia;Fil: Baez, Walter Ariel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET- Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;Fil: Becchio, Raul Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET - Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;Fil: Viramonte, Jose German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET - Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;Fil: Giordano, Guido. Università degli Studi Roma Tre. Dipartimento di Scienze Geologiche; Italia;Fil: Arnosio, José Marcelo. Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina; Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Cientifico Tecnológico - CONICET - Salta; Argentina;Fil: Pinton, Annamaria. Università degli Studi Roma Tre. Dipartimento di Scienze Geologiche; Italia;Fil: Gropelli, Gianluca. Consiglio Nazionale Delle Ricerche. Istituto per la Dinamica dei Processi Ambientali ; Italia;Elsevier2013-11-26info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/2090Norini, Gianluca; Baez, Walter Ariel; Becchio, Raul Alberto; Viramonte, Jose German; Giordano, Guido; et al.; The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement; Elsevier; Tectonophysics; 608; 26-11-2013; 1280-12970040-1951enginfo:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0040195113003788info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2013.06.013info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:49:27Zoai:ri.conicet.gov.ar:11336/2090instacron: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 09:49:27.818CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
title The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
spellingShingle The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
Norini, Gianluca
Calama-Olacapato-El Toro Fault System
Volcano-Tectonics Interplay
3d Reconstruction of Fault Planes
Transfer Fault Systems
title_short The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
title_full The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
title_fullStr The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
title_full_unstemmed The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
title_sort The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement
dc.creator.none.fl_str_mv Norini, Gianluca
Baez, Walter Ariel
Becchio, Raul Alberto
Viramonte, Jose German
Giordano, Guido
Arnosio, José Marcelo
Pinton, Annamaria
Gropelli, Gianluca
author Norini, Gianluca
author_facet Norini, Gianluca
Baez, Walter Ariel
Becchio, Raul Alberto
Viramonte, Jose German
Giordano, Guido
Arnosio, José Marcelo
Pinton, Annamaria
Gropelli, Gianluca
author_role author
author2 Baez, Walter Ariel
Becchio, Raul Alberto
Viramonte, Jose German
Giordano, Guido
Arnosio, José Marcelo
Pinton, Annamaria
Gropelli, Gianluca
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Calama-Olacapato-El Toro Fault System
Volcano-Tectonics Interplay
3d Reconstruction of Fault Planes
Transfer Fault Systems
topic Calama-Olacapato-El Toro Fault System
Volcano-Tectonics Interplay
3d Reconstruction of Fault Planes
Transfer Fault Systems
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 structural evolution of the Puna Plateau is characterized by the activity of both orogen-parallel and orogen-oblique faults. Understanding the possible relationship between these two structural styles, their geodynamic implications and the influence on the migration of magmas is important to get insights into the tectonic and magmatic evolution of the Central Andes. In this study, we present a structural analysis of the orogen-oblique Calama-Olacapato-El Toro fault system and the surrounding orogen-parallel thrust faults in the central-eastern Puna Plateau. Morphostructural analysis and field mapping reveal the geometry, kinematics and dynamics of the tectonic features in the studied area. We propose a three-dimensional geometrical reconstruction of the main fault planes showing their attitude and intersections at depth. The study indicates that the crust underwent simultaneous deformation along both the vertical transcurrent Calama-Olacapato-El Toro fault system and the low-angle thrust faults, and that the back-arc portion of the Calama-Olacapato-El Toro fault system developed as a transfer zone among the main N-striking thrusts. Our model considers that both orogen-parallel and orogen-oblique fault systems should be regarded as parts of the same tectonic system, accommodating crustal shortening of a thickened crust. The study suggests that the tectonic control on the magma and fluid circulation in the crust is mainly related to the geometry of the fault planes and the orientation of the stress field, with a previously unrecognized important role played by the orogen-parallel thrust faults on the emplacement of the stratovolcanoes.
Fil: Norini, Gianluca. Consiglio Nazionale Delle Ricerche. Istituto per la Dinamica dei Processi Ambientali ; Italia;
Fil: Baez, Walter Ariel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET- Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;
Fil: Becchio, Raul Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET - Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;
Fil: Viramonte, Jose German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico - CONICET - Salta. Instituto de Investigaciones en Energía No Convencional; Argentina; Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina;
Fil: Giordano, Guido. Università degli Studi Roma Tre. Dipartimento di Scienze Geologiche; Italia;
Fil: Arnosio, José Marcelo. Universidad Nacional de Salta. Facultad De Ciencias Naturales. Instituto Geonorte; Argentina; Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Cientifico Tecnológico - CONICET - Salta; Argentina;
Fil: Pinton, Annamaria. Università degli Studi Roma Tre. Dipartimento di Scienze Geologiche; Italia;
Fil: Gropelli, Gianluca. Consiglio Nazionale Delle Ricerche. Istituto per la Dinamica dei Processi Ambientali ; Italia;
description The structural evolution of the Puna Plateau is characterized by the activity of both orogen-parallel and orogen-oblique faults. Understanding the possible relationship between these two structural styles, their geodynamic implications and the influence on the migration of magmas is important to get insights into the tectonic and magmatic evolution of the Central Andes. In this study, we present a structural analysis of the orogen-oblique Calama-Olacapato-El Toro fault system and the surrounding orogen-parallel thrust faults in the central-eastern Puna Plateau. Morphostructural analysis and field mapping reveal the geometry, kinematics and dynamics of the tectonic features in the studied area. We propose a three-dimensional geometrical reconstruction of the main fault planes showing their attitude and intersections at depth. The study indicates that the crust underwent simultaneous deformation along both the vertical transcurrent Calama-Olacapato-El Toro fault system and the low-angle thrust faults, and that the back-arc portion of the Calama-Olacapato-El Toro fault system developed as a transfer zone among the main N-striking thrusts. Our model considers that both orogen-parallel and orogen-oblique fault systems should be regarded as parts of the same tectonic system, accommodating crustal shortening of a thickened crust. The study suggests that the tectonic control on the magma and fluid circulation in the crust is mainly related to the geometry of the fault planes and the orientation of the stress field, with a previously unrecognized important role played by the orogen-parallel thrust faults on the emplacement of the stratovolcanoes.
publishDate 2013
dc.date.none.fl_str_mv 2013-11-26
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/11336/2090
Norini, Gianluca; Baez, Walter Ariel; Becchio, Raul Alberto; Viramonte, Jose German; Giordano, Guido; et al.; The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement; Elsevier; Tectonophysics; 608; 26-11-2013; 1280-1297
0040-1951
url http://hdl.handle.net/11336/2090
identifier_str_mv Norini, Gianluca; Baez, Walter Ariel; Becchio, Raul Alberto; Viramonte, Jose German; Giordano, Guido; et al.; The Calama-Olacapato-El Toro fault system in the Puna Plateau, Central Andes: Geodynamic implications and stratovolcanoes emplacement; Elsevier; Tectonophysics; 608; 26-11-2013; 1280-1297
0040-1951
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0040195113003788
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2013.06.013
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
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
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 13.070432

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