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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/169070
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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 |
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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 |
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language |
spa |
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info:eu-repo/semantics/altIdentifier/url/https://minmet-pimma-2019.congresos.unc.edu.ar/acta-final-del-congreso/ |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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Nacional |
dc.publisher.none.fl_str_mv |
Dahlquist, Juan Andrés |
publisher.none.fl_str_mv |
Dahlquist, Juan Andrés |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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