Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina

Autores
Sardi, Fernando Guillermo; Toselli, Alejandro Jose
Año de publicación
2003
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Sistema de Famatina is located in the northwestern sector of Argentina, sharing territories with La Rioja and Catamarca provinces. The Sistema de Famatina display N-S orientation being represented by metamorphites (Negro Peinado/La Aguadita Formations) of the Pampean Cycle. The marine clastic and volcaniclastic sedimentary rocks, the volcanic-subvolcanic bodies of basic and acid composition and the widespread outcrops of granitoids belong to the posterior Famatinian Cycle. The Sierra de Velasco is located eastwards of the Sistema de Famatina in La Rioja province. This is the largest orographic unit of the Sierras Pampeanas, nearly totaly represented by Famatinian granitoids with porfiric and equigranular textures. Epigenic mineralizations (Cu, Mo, W, Be) are recorded in the region, related to the different magmatic units. These igneous manifestations are formed by a volcano-sedimentary secuences of El Chuschin Formation and the Ñuñorco and Paimán Granites in the Sistema de Famatina, and the Huaco Granite in the Sierra de Velasco.
Fil: Sardi, Fernando Guillermo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Toselli, Alejandro Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; 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:11336/81643
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern ArgentinaSardi, Fernando GuillermoToselli, Alejandro Josehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Sistema de Famatina is located in the northwestern sector of Argentina, sharing territories with La Rioja and Catamarca provinces. The Sistema de Famatina display N-S orientation being represented by metamorphites (Negro Peinado/La Aguadita Formations) of the Pampean Cycle. The marine clastic and volcaniclastic sedimentary rocks, the volcanic-subvolcanic bodies of basic and acid composition and the widespread outcrops of granitoids belong to the posterior Famatinian Cycle. The Sierra de Velasco is located eastwards of the Sistema de Famatina in La Rioja province. This is the largest orographic unit of the Sierras Pampeanas, nearly totaly represented by Famatinian granitoids with porfiric and equigranular textures. Epigenic mineralizations (Cu, Mo, W, Be) are recorded in the region, related to the different magmatic units. These igneous manifestations are formed by a volcano-sedimentary secuences of El Chuschin Formation and the Ñuñorco and Paimán Granites in the Sistema de Famatina, and the Huaco Granite in the Sierra de Velasco.Fil: Sardi, Fernando Guillermo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; ArgentinaFil: Toselli, Alejandro Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; ArgentinaInstituto Superior de Correlación Geológica2003-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/mswordapplication/pdfhttp://hdl.handle.net/11336/81643Sardi, Fernando Guillermo; Toselli, Alejandro Jose; Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina; Instituto Superior de Correlación Geológica; Serie de Correlación Geológica; 17; 12-2003; 227-2311514-4186CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www.insugeo.org.ar/publicaciones/docs/scg_17/37.htminfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:48:35Zoai:ri.conicet.gov.ar:11336/81643instacron: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 09:48:35.275CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
title Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
spellingShingle Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
Sardi, Fernando Guillermo
title_short Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
title_full Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
title_fullStr Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
title_full_unstemmed Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
title_sort Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina
dc.creator.none.fl_str_mv Sardi, Fernando Guillermo
Toselli, Alejandro Jose
author Sardi, Fernando Guillermo
author_facet Sardi, Fernando Guillermo
Toselli, Alejandro Jose
author_role author
author2 Toselli, Alejandro Jose
author2_role author
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 Sistema de Famatina is located in the northwestern sector of Argentina, sharing territories with La Rioja and Catamarca provinces. The Sistema de Famatina display N-S orientation being represented by metamorphites (Negro Peinado/La Aguadita Formations) of the Pampean Cycle. The marine clastic and volcaniclastic sedimentary rocks, the volcanic-subvolcanic bodies of basic and acid composition and the widespread outcrops of granitoids belong to the posterior Famatinian Cycle. The Sierra de Velasco is located eastwards of the Sistema de Famatina in La Rioja province. This is the largest orographic unit of the Sierras Pampeanas, nearly totaly represented by Famatinian granitoids with porfiric and equigranular textures. Epigenic mineralizations (Cu, Mo, W, Be) are recorded in the region, related to the different magmatic units. These igneous manifestations are formed by a volcano-sedimentary secuences of El Chuschin Formation and the Ñuñorco and Paimán Granites in the Sistema de Famatina, and the Huaco Granite in the Sierra de Velasco.
Fil: Sardi, Fernando Guillermo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
Fil: Toselli, Alejandro Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán. Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán. Facultad de Ciencias Naturales e Instituto Miguel Lillo. Departamento de Geología. Cátedra Geología Estructural. Instituto Superior de Correlación Geológica; Argentina
description The Sistema de Famatina is located in the northwestern sector of Argentina, sharing territories with La Rioja and Catamarca provinces. The Sistema de Famatina display N-S orientation being represented by metamorphites (Negro Peinado/La Aguadita Formations) of the Pampean Cycle. The marine clastic and volcaniclastic sedimentary rocks, the volcanic-subvolcanic bodies of basic and acid composition and the widespread outcrops of granitoids belong to the posterior Famatinian Cycle. The Sierra de Velasco is located eastwards of the Sistema de Famatina in La Rioja province. This is the largest orographic unit of the Sierras Pampeanas, nearly totaly represented by Famatinian granitoids with porfiric and equigranular textures. Epigenic mineralizations (Cu, Mo, W, Be) are recorded in the region, related to the different magmatic units. These igneous manifestations are formed by a volcano-sedimentary secuences of El Chuschin Formation and the Ñuñorco and Paimán Granites in the Sistema de Famatina, and the Huaco Granite in the Sierra de Velasco.
publishDate 2003
dc.date.none.fl_str_mv 2003-12
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/11336/81643
Sardi, Fernando Guillermo; Toselli, Alejandro Jose; Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina; Instituto Superior de Correlación Geológica; Serie de Correlación Geológica; 17; 12-2003; 227-231
1514-4186
CONICET Digital
CONICET
url http://hdl.handle.net/11336/81643
identifier_str_mv Sardi, Fernando Guillermo; Toselli, Alejandro Jose; Ordovician mineralizations in the Sistema de Famatina and Sierra de Velasco, northwestern Argentina; Instituto Superior de Correlación Geológica; Serie de Correlación Geológica; 17; 12-2003; 227-231
1514-4186
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://www.insugeo.org.ar/publicaciones/docs/scg_17/37.htm
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/msword
application/pdf
dc.publisher.none.fl_str_mv Instituto Superior de Correlación Geológica
publisher.none.fl_str_mv Instituto Superior de Correlación Geológica
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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