Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan

Autores
Medrano, Ornella; D'annunzio, María Celeste; Strazzere, Leonardo
Año de publicación
2019
Idioma
español castellano
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
Textural and paragenetic analysis of the Sur vein of the Cerro Norte Project, Casposo Mining District, San Juan. The Casposo mining district is located in the province of San Juan (Argentina) in the eastern sector of the Cordillera Frontal. Within this district epithermal lowsulphidation deposits are hosted by Vega de los Machos Formation (Caballé 1986) of lower Permian age. Cerro Norte has a system of E-O veins with dip between 60 and 85° to the North and the South and form three main outcrops: Norte, Centro and Sur veins. The latter is the reason for the present study. The Sur vein extends more than 400 m and its thickness varies from 0.20 m. up to 3 m. It is characterized by a bifurcation pattern. It comprises 6 events. Event 1 is characterized by crustiform-colloform quartz 1 (Fig. 1a and b) with moss (Fig. 1a) and spherulitic texture (Fig. 1b). This event presents mosaic textures (Fig. 1c) and flaming extinction (Fig. 1d) typical of recrystallization. Recrystallization, although it constitutes another event, could not be temporarily limited. Event 2 is formed by massive microcrystalline quartz of anhedral habit (Fig. 1e). Event 3 is the crystallization of calcite in the form of "blades". Event 4 shows the pseudomorphic replacement of calcite by quartz that forms the lattice-bladed texture (Fig. 1f). Event 5 represents the crystallization of drustiform habit quartz with zoned texture (Fig. 1g). Event 6 constitutes the formation of a hydrothermal breccia that includes clasts from previous events and cement crustiform-colloform quartz 2 (Fig. 1h), calcite, chlorite, freibergite-argentotennantite 1 (?), freibergite-argentotennantite 2 (?), pearceite-polybasite (?), freieslebenite (?), sphalerite, chalcopyrite, pyrite and native silver.
Fil: Medrano, Ornella. Universidad Nacional del Sur. Departamento de Geología; Argentina
Fil: D'annunzio, María Celeste. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Strazzere, Leonardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
XIII Congreso de Mineralogía, Petrología Ígnea y Metamórfica, y Metalogénesis
Córdoba
Argentina
Asociación Mineralógica Argentina
Comisión Científica de Petrología de la Asociación Geológica Argentina
Materia
CORDILLERA FRONTAL
VETA CARLOTA
EPITERMAL DE BAJA SULFURACIÓN
DISTRITO MINERO CASPOSO
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:11336/169070

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network_name_str CONICET Digital (CONICET)
spelling Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San JuanMedrano, OrnellaD'annunzio, María CelesteStrazzere, LeonardoCORDILLERA FRONTALVETA CARLOTAEPITERMAL DE BAJA SULFURACIÓNDISTRITO MINERO CASPOSOhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Textural and paragenetic analysis of the Sur vein of the Cerro Norte Project, Casposo Mining District, San Juan. The Casposo mining district is located in the province of San Juan (Argentina) in the eastern sector of the Cordillera Frontal. Within this district epithermal lowsulphidation deposits are hosted by Vega de los Machos Formation (Caballé 1986) of lower Permian age. Cerro Norte has a system of E-O veins with dip between 60 and 85° to the North and the South and form three main outcrops: Norte, Centro and Sur veins. The latter is the reason for the present study. The Sur vein extends more than 400 m and its thickness varies from 0.20 m. up to 3 m. It is characterized by a bifurcation pattern. It comprises 6 events. Event 1 is characterized by crustiform-colloform quartz 1 (Fig. 1a and b) with moss (Fig. 1a) and spherulitic texture (Fig. 1b). This event presents mosaic textures (Fig. 1c) and flaming extinction (Fig. 1d) typical of recrystallization. Recrystallization, although it constitutes another event, could not be temporarily limited. Event 2 is formed by massive microcrystalline quartz of anhedral habit (Fig. 1e). Event 3 is the crystallization of calcite in the form of "blades". Event 4 shows the pseudomorphic replacement of calcite by quartz that forms the lattice-bladed texture (Fig. 1f). Event 5 represents the crystallization of drustiform habit quartz with zoned texture (Fig. 1g). Event 6 constitutes the formation of a hydrothermal breccia that includes clasts from previous events and cement crustiform-colloform quartz 2 (Fig. 1h), calcite, chlorite, freibergite-argentotennantite 1 (?), freibergite-argentotennantite 2 (?), pearceite-polybasite (?), freieslebenite (?), sphalerite, chalcopyrite, pyrite and native silver.Fil: Medrano, Ornella. Universidad Nacional del Sur. Departamento de Geología; ArgentinaFil: D'annunzio, María Celeste. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; ArgentinaFil: Strazzere, Leonardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; ArgentinaXIII Congreso de Mineralogía, Petrología Ígnea y Metamórfica, y MetalogénesisCórdobaArgentinaAsociación Mineralógica ArgentinaComisión Científica de Petrología de la Asociación Geológica ArgentinaDahlquist, Juan AndrésDahlquist, Juan Andrés2019info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/169070Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan; XIII Congreso de Mineralogía, Petrología Ígnea y Metamórfica, y Metalogénesis; Córdoba; Argentina; 2019; 338-339978-987-86-1704-6CONICET DigitalCONICETspainfo:eu-repo/semantics/altIdentifier/url/https://minmet-pimma-2019.congresos.unc.edu.ar/acta-final-del-congreso/Nacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:39:12Zoai:ri.conicet.gov.ar:11336/169070instacron: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 09:39:12.927CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
title Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
spellingShingle Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
Medrano, Ornella
CORDILLERA FRONTAL
VETA CARLOTA
EPITERMAL DE BAJA SULFURACIÓN
DISTRITO MINERO CASPOSO
title_short Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
title_full Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
title_fullStr Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
title_full_unstemmed Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
title_sort Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan
dc.creator.none.fl_str_mv Medrano, Ornella
D'annunzio, María Celeste
Strazzere, Leonardo
author Medrano, Ornella
author_facet Medrano, Ornella
D'annunzio, María Celeste
Strazzere, Leonardo
author_role author
author2 D'annunzio, María Celeste
Strazzere, Leonardo
author2_role author
author
dc.contributor.none.fl_str_mv Dahlquist, Juan Andrés
dc.subject.none.fl_str_mv CORDILLERA FRONTAL
VETA CARLOTA
EPITERMAL DE BAJA SULFURACIÓN
DISTRITO MINERO CASPOSO
topic CORDILLERA FRONTAL
VETA CARLOTA
EPITERMAL DE BAJA SULFURACIÓN
DISTRITO MINERO CASPOSO
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Textural and paragenetic analysis of the Sur vein of the Cerro Norte Project, Casposo Mining District, San Juan. The Casposo mining district is located in the province of San Juan (Argentina) in the eastern sector of the Cordillera Frontal. Within this district epithermal lowsulphidation deposits are hosted by Vega de los Machos Formation (Caballé 1986) of lower Permian age. Cerro Norte has a system of E-O veins with dip between 60 and 85° to the North and the South and form three main outcrops: Norte, Centro and Sur veins. The latter is the reason for the present study. The Sur vein extends more than 400 m and its thickness varies from 0.20 m. up to 3 m. It is characterized by a bifurcation pattern. It comprises 6 events. Event 1 is characterized by crustiform-colloform quartz 1 (Fig. 1a and b) with moss (Fig. 1a) and spherulitic texture (Fig. 1b). This event presents mosaic textures (Fig. 1c) and flaming extinction (Fig. 1d) typical of recrystallization. Recrystallization, although it constitutes another event, could not be temporarily limited. Event 2 is formed by massive microcrystalline quartz of anhedral habit (Fig. 1e). Event 3 is the crystallization of calcite in the form of "blades". Event 4 shows the pseudomorphic replacement of calcite by quartz that forms the lattice-bladed texture (Fig. 1f). Event 5 represents the crystallization of drustiform habit quartz with zoned texture (Fig. 1g). Event 6 constitutes the formation of a hydrothermal breccia that includes clasts from previous events and cement crustiform-colloform quartz 2 (Fig. 1h), calcite, chlorite, freibergite-argentotennantite 1 (?), freibergite-argentotennantite 2 (?), pearceite-polybasite (?), freieslebenite (?), sphalerite, chalcopyrite, pyrite and native silver.
Fil: Medrano, Ornella. Universidad Nacional del Sur. Departamento de Geología; Argentina
Fil: D'annunzio, María Celeste. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Strazzere, Leonardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
XIII Congreso de Mineralogía, Petrología Ígnea y Metamórfica, y Metalogénesis
Córdoba
Argentina
Asociación Mineralógica Argentina
Comisión Científica de Petrología de la Asociación Geológica Argentina
description Textural and paragenetic analysis of the Sur vein of the Cerro Norte Project, Casposo Mining District, San Juan. The Casposo mining district is located in the province of San Juan (Argentina) in the eastern sector of the Cordillera Frontal. Within this district epithermal lowsulphidation deposits are hosted by Vega de los Machos Formation (Caballé 1986) of lower Permian age. Cerro Norte has a system of E-O veins with dip between 60 and 85° to the North and the South and form three main outcrops: Norte, Centro and Sur veins. The latter is the reason for the present study. The Sur vein extends more than 400 m and its thickness varies from 0.20 m. up to 3 m. It is characterized by a bifurcation pattern. It comprises 6 events. Event 1 is characterized by crustiform-colloform quartz 1 (Fig. 1a and b) with moss (Fig. 1a) and spherulitic texture (Fig. 1b). This event presents mosaic textures (Fig. 1c) and flaming extinction (Fig. 1d) typical of recrystallization. Recrystallization, although it constitutes another event, could not be temporarily limited. Event 2 is formed by massive microcrystalline quartz of anhedral habit (Fig. 1e). Event 3 is the crystallization of calcite in the form of "blades". Event 4 shows the pseudomorphic replacement of calcite by quartz that forms the lattice-bladed texture (Fig. 1f). Event 5 represents the crystallization of drustiform habit quartz with zoned texture (Fig. 1g). Event 6 constitutes the formation of a hydrothermal breccia that includes clasts from previous events and cement crustiform-colloform quartz 2 (Fig. 1h), calcite, chlorite, freibergite-argentotennantite 1 (?), freibergite-argentotennantite 2 (?), pearceite-polybasite (?), freieslebenite (?), sphalerite, chalcopyrite, pyrite and native silver.
publishDate 2019
dc.date.none.fl_str_mv 2019
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
Congreso
Book
http://purl.org/coar/resource_type/c_5794
info:ar-repo/semantics/documentoDeConferencia
status_str publishedVersion
format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/169070
Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan; XIII Congreso de Mineralogía, Petrología Ígnea y Metamórfica, y Metalogénesis; Córdoba; Argentina; 2019; 338-339
978-987-86-1704-6
CONICET Digital
CONICET
url http://hdl.handle.net/11336/169070
identifier_str_mv Análisis textural y paragenético de laveta sur del proyecto Cerro Norte, distrito minero Casposo, San Juan; XIII Congreso de Mineralogía, Petrología Ígnea y Metamórfica, y Metalogénesis; Córdoba; Argentina; 2019; 338-339
978-987-86-1704-6
CONICET Digital
CONICET
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://minmet-pimma-2019.congresos.unc.edu.ar/acta-final-del-congreso/
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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/
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dc.publisher.none.fl_str_mv Dahlquist, Juan Andrés
publisher.none.fl_str_mv Dahlquist, Juan Andrés
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
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