Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina

Autores
Gutierrez, Adolfo Antonio; Mon, Ricardo; Arnous, Ahmad; Aranda Viana, Rodolfo Germán
Año de publicación
2021
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
This study shows the neotectonic deformation occurred in the southern piedmont of the Cumbres Calchaquíes, in the Amaicha and Tafí valleys. Neotectonic deformation manifests itself through faults, folds and diversions of drainage channels. The Amaicha valley is bounded to the north by the Tafí del Valle fault and to the south by the Los Cardones fault. The Cumbres Calchaquíes ride over the Sierra de Aconquija through the Los Cardones and Carapunco faults. The Carapunco fault also has a synestral component, responsible for generating an imbricated system of contractional fractures. In the study region many earthquakes of ≥ 3 and ≥ 4 magnitude coincide with regional faults evidencing its neotectonic activity. The seismic energy dissipated through materials with less cohesion that form the fill of the valleys, generating discrete fault scarps and strongly folded conglomerate strata. The foothills deposits of the Cumbres Calchaquíes absorbed most of the seismic energy released during the reactivation of the faults. Tectonic activity is deforming 630 a BP deposits in the Cumbres Calchaquíes piedmont.
Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán; Argentina
Fil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología; Argentina
Fil: Arnous, Ahmad. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina
Fil: Aranda Viana, Rodolfo Germán. Universidad Nacional de Tucumán; Argentina. 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
Materia
ANDES
EARTHQUAKES
NATURAL HAZARDS
NEOTECTONICS
SIERRAS PAMPEANAS
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:11336/159963
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of ArgentinaGutierrez, Adolfo AntonioMon, RicardoArnous, AhmadAranda Viana, Rodolfo GermánANDESEARTHQUAKESNATURAL HAZARDSNEOTECTONICSSIERRAS PAMPEANAShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This study shows the neotectonic deformation occurred in the southern piedmont of the Cumbres Calchaquíes, in the Amaicha and Tafí valleys. Neotectonic deformation manifests itself through faults, folds and diversions of drainage channels. The Amaicha valley is bounded to the north by the Tafí del Valle fault and to the south by the Los Cardones fault. The Cumbres Calchaquíes ride over the Sierra de Aconquija through the Los Cardones and Carapunco faults. The Carapunco fault also has a synestral component, responsible for generating an imbricated system of contractional fractures. In the study region many earthquakes of ≥ 3 and ≥ 4 magnitude coincide with regional faults evidencing its neotectonic activity. The seismic energy dissipated through materials with less cohesion that form the fill of the valleys, generating discrete fault scarps and strongly folded conglomerate strata. The foothills deposits of the Cumbres Calchaquíes absorbed most of the seismic energy released during the reactivation of the faults. Tectonic activity is deforming 630 a BP deposits in the Cumbres Calchaquíes piedmont.Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán; ArgentinaFil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología; ArgentinaFil: Arnous, Ahmad. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; ArgentinaFil: Aranda Viana, Rodolfo Germán. Universidad Nacional de Tucumán; Argentina. 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; ArgentinaSpringer Nature2021-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/159963Gutierrez, Adolfo Antonio; Mon, Ricardo; Arnous, Ahmad; Aranda Viana, Rodolfo Germán; Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina; Springer Nature; SN Applied Sciences; 3; 12; 12-20212523-3971CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1007/s42452-021-04874-0info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007/s42452-021-04874-0info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T15:10:07Zoai:ri.conicet.gov.ar:11336/159963instacron: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:34982025-10-15 15:10:07.894CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
title Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
spellingShingle Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
Gutierrez, Adolfo Antonio
ANDES
EARTHQUAKES
NATURAL HAZARDS
NEOTECTONICS
SIERRAS PAMPEANAS
title_short Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
title_full Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
title_fullStr Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
title_full_unstemmed Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
title_sort Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina
dc.creator.none.fl_str_mv Gutierrez, Adolfo Antonio
Mon, Ricardo
Arnous, Ahmad
Aranda Viana, Rodolfo Germán
author Gutierrez, Adolfo Antonio
author_facet Gutierrez, Adolfo Antonio
Mon, Ricardo
Arnous, Ahmad
Aranda Viana, Rodolfo Germán
author_role author
author2 Mon, Ricardo
Arnous, Ahmad
Aranda Viana, Rodolfo Germán
author2_role author
author
author
dc.subject.none.fl_str_mv ANDES
EARTHQUAKES
NATURAL HAZARDS
NEOTECTONICS
SIERRAS PAMPEANAS
topic ANDES
EARTHQUAKES
NATURAL HAZARDS
NEOTECTONICS
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 This study shows the neotectonic deformation occurred in the southern piedmont of the Cumbres Calchaquíes, in the Amaicha and Tafí valleys. Neotectonic deformation manifests itself through faults, folds and diversions of drainage channels. The Amaicha valley is bounded to the north by the Tafí del Valle fault and to the south by the Los Cardones fault. The Cumbres Calchaquíes ride over the Sierra de Aconquija through the Los Cardones and Carapunco faults. The Carapunco fault also has a synestral component, responsible for generating an imbricated system of contractional fractures. In the study region many earthquakes of ≥ 3 and ≥ 4 magnitude coincide with regional faults evidencing its neotectonic activity. The seismic energy dissipated through materials with less cohesion that form the fill of the valleys, generating discrete fault scarps and strongly folded conglomerate strata. The foothills deposits of the Cumbres Calchaquíes absorbed most of the seismic energy released during the reactivation of the faults. Tectonic activity is deforming 630 a BP deposits in the Cumbres Calchaquíes piedmont.
Fil: Gutierrez, Adolfo Antonio. Universidad Nacional de Tucumán; Argentina
Fil: Mon, Ricardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología; Argentina
Fil: Arnous, Ahmad. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina
Fil: Aranda Viana, Rodolfo Germán. Universidad Nacional de Tucumán; Argentina. 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
description This study shows the neotectonic deformation occurred in the southern piedmont of the Cumbres Calchaquíes, in the Amaicha and Tafí valleys. Neotectonic deformation manifests itself through faults, folds and diversions of drainage channels. The Amaicha valley is bounded to the north by the Tafí del Valle fault and to the south by the Los Cardones fault. The Cumbres Calchaquíes ride over the Sierra de Aconquija through the Los Cardones and Carapunco faults. The Carapunco fault also has a synestral component, responsible for generating an imbricated system of contractional fractures. In the study region many earthquakes of ≥ 3 and ≥ 4 magnitude coincide with regional faults evidencing its neotectonic activity. The seismic energy dissipated through materials with less cohesion that form the fill of the valleys, generating discrete fault scarps and strongly folded conglomerate strata. The foothills deposits of the Cumbres Calchaquíes absorbed most of the seismic energy released during the reactivation of the faults. Tectonic activity is deforming 630 a BP deposits in the Cumbres Calchaquíes piedmont.
publishDate 2021
dc.date.none.fl_str_mv 2021-12
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/11336/159963
Gutierrez, Adolfo Antonio; Mon, Ricardo; Arnous, Ahmad; Aranda Viana, Rodolfo Germán; Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina; Springer Nature; SN Applied Sciences; 3; 12; 12-2021
2523-3971
CONICET Digital
CONICET
url http://hdl.handle.net/11336/159963
identifier_str_mv Gutierrez, Adolfo Antonio; Mon, Ricardo; Arnous, Ahmad; Aranda Viana, Rodolfo Germán; Piedmont deposits as seismic energy dissipators, Sierras Pampeanas of Argentina; Springer Nature; SN Applied Sciences; 3; 12; 12-2021
2523-3971
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1007/s42452-021-04874-0
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007/s42452-021-04874-0
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 Springer Nature
publisher.none.fl_str_mv Springer Nature
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
_version_ 1846083249512644608
score 13.22299

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