The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina

Autores
Sato, Ana María; González, Pablo Diego; Stipp Basei, Miguel Angelo; Passarelli, C. R.; Tickyj, H.; Ponce, José Manuel
Año de publicación
2003
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The Sierra de San Luis is located in the southern part of the Eastern Sierras Pampeanas. The most conspicuous orogenic events (arc magmatism, deformation and metamorphism) took place during the Lower Paleozoic Famatinian orogeny, overprinting the metamorphic and sedimentary rocks already delineated by the previous Pampean orogeny (Proterozoic? to Early Cambrian). The granitoids were c1assified into pre-, syn- and post-orogenic plutons on the basis of their structural relationship with the penetrative NNE-SSW trending Ordovician structures, attributed to the main Famatinian phase (Ortiz Suarez et al., 1992; Llambias et al., 1998). Available data constrain the low- to high-grade regional metamorphism associated with the deformation mainly within the Early to Middle Ordovician (see synthesis in Sato et al., 2002).
Centro de Investigaciones Geológicas
Laboratorio de Entrenamiento Multidisciplinario para la Investigación Tecnológica
Materia
Geología
Sierras Pampeanas
Famatinian orogeny
granitoids
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/164914
Acceder
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repository_id_str 1329
network_name_str SEDICI (UNLP)
spelling The Famatinian granitoids of Southwestern Sierra de San Luis, ArgentinaSato, Ana MaríaGonzález, Pablo DiegoStipp Basei, Miguel AngeloPassarelli, C. R.Tickyj, H.Ponce, José ManuelGeologíaSierras PampeanasFamatinian orogenygranitoidsThe Sierra de San Luis is located in the southern part of the Eastern Sierras Pampeanas. The most conspicuous orogenic events (arc magmatism, deformation and metamorphism) took place during the Lower Paleozoic Famatinian orogeny, overprinting the metamorphic and sedimentary rocks already delineated by the previous Pampean orogeny (Proterozoic? to Early Cambrian). The granitoids were c1assified into pre-, syn- and post-orogenic plutons on the basis of their structural relationship with the penetrative NNE-SSW trending Ordovician structures, attributed to the main Famatinian phase (Ortiz Suarez et al., 1992; Llambias et al., 1998). Available data constrain the low- to high-grade regional metamorphism associated with the deformation mainly within the Early to Middle Ordovician (see synthesis in Sato et al., 2002).Centro de Investigaciones GeológicasLaboratorio de Entrenamiento Multidisciplinario para la Investigación Tecnológica2003info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionObjeto de conferenciahttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdf290-293http://sedici.unlp.edu.ar/handle/10915/164914enginfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:43:41Zoai:sedici.unlp.edu.ar:10915/164914Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:43:42.106SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
title The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
spellingShingle The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
Sato, Ana María
Geología
Sierras Pampeanas
Famatinian orogeny
granitoids
title_short The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
title_full The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
title_fullStr The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
title_full_unstemmed The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
title_sort The Famatinian granitoids of Southwestern Sierra de San Luis, Argentina
dc.creator.none.fl_str_mv Sato, Ana María
González, Pablo Diego
Stipp Basei, Miguel Angelo
Passarelli, C. R.
Tickyj, H.
Ponce, José Manuel
author Sato, Ana María
author_facet Sato, Ana María
González, Pablo Diego
Stipp Basei, Miguel Angelo
Passarelli, C. R.
Tickyj, H.
Ponce, José Manuel
author_role author
author2 González, Pablo Diego
Stipp Basei, Miguel Angelo
Passarelli, C. R.
Tickyj, H.
Ponce, José Manuel
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Geología
Sierras Pampeanas
Famatinian orogeny
granitoids
topic Geología
Sierras Pampeanas
Famatinian orogeny
granitoids
dc.description.none.fl_txt_mv The Sierra de San Luis is located in the southern part of the Eastern Sierras Pampeanas. The most conspicuous orogenic events (arc magmatism, deformation and metamorphism) took place during the Lower Paleozoic Famatinian orogeny, overprinting the metamorphic and sedimentary rocks already delineated by the previous Pampean orogeny (Proterozoic? to Early Cambrian). The granitoids were c1assified into pre-, syn- and post-orogenic plutons on the basis of their structural relationship with the penetrative NNE-SSW trending Ordovician structures, attributed to the main Famatinian phase (Ortiz Suarez et al., 1992; Llambias et al., 1998). Available data constrain the low- to high-grade regional metamorphism associated with the deformation mainly within the Early to Middle Ordovician (see synthesis in Sato et al., 2002).
Centro de Investigaciones Geológicas
Laboratorio de Entrenamiento Multidisciplinario para la Investigación Tecnológica
description The Sierra de San Luis is located in the southern part of the Eastern Sierras Pampeanas. The most conspicuous orogenic events (arc magmatism, deformation and metamorphism) took place during the Lower Paleozoic Famatinian orogeny, overprinting the metamorphic and sedimentary rocks already delineated by the previous Pampean orogeny (Proterozoic? to Early Cambrian). The granitoids were c1assified into pre-, syn- and post-orogenic plutons on the basis of their structural relationship with the penetrative NNE-SSW trending Ordovician structures, attributed to the main Famatinian phase (Ortiz Suarez et al., 1992; Llambias et al., 1998). Available data constrain the low- to high-grade regional metamorphism associated with the deformation mainly within the Early to Middle Ordovician (see synthesis in Sato et al., 2002).
publishDate 2003
dc.date.none.fl_str_mv 2003
dc.type.none.fl_str_mv info:eu-repo/semantics/conferenceObject
info:eu-repo/semantics/publishedVersion
Objeto de conferencia
http://purl.org/coar/resource_type/c_5794
info:ar-repo/semantics/documentoDeConferencia
format conferenceObject
status_str publishedVersion
dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/164914
url http://sedici.unlp.edu.ar/handle/10915/164914
dc.language.none.fl_str_mv eng
language eng
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
dc.format.none.fl_str_mv application/pdf
290-293
dc.source.none.fl_str_mv reponame:SEDICI (UNLP)
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collection SEDICI (UNLP)
instname_str Universidad Nacional de La Plata
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institution UNLP
repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
repository.mail.fl_str_mv alira@sedici.unlp.edu.ar
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