Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition

Agua Rica is a world-class Cu (Mo–Au) deposit located in Catamarca, Argentina, in which the porphyry and high sulfidation epithermal stages are juxtaposed due to the telescoping of the mineralizing system. Pyrite is the most abundant sulfide in the analyz

Detalles Bibliográficos
Autor: Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2015
País:Chile
Institución:Agencia Nacional de Investigación y Desarrollo
Repositorio:Articulos_ANID
Idioma:inglés
OAI Identifier:oai:repositorio.anid.cl:10533/238113
Acceso en línea:https://hdl.handle.net/10533/238113
Access Level:acceso abierto
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spelling Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition Ore Geology Reviews Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V. Agua Rica is a world-class Cu (Mo–Au) deposit located in Catamarca, Argentina, in which the porphyry and high sulfidation epithermal stages are juxtaposed due to the telescoping of the mineralizing system. Pyrite is the most abundant sulfide in the analyz FONDAP 15090013 https://hdl.handle.net/10533/238113
title Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition
spellingShingle Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition
Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
title_short Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition
title_full Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition
title_fullStr Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition
title_full_unstemmed Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition
title_sort Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: textural features and metal zoning at the porphyry to epithermal transition
author Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
author_facet Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
author_role author
description Agua Rica is a world-class Cu (Mo–Au) deposit located in Catamarca, Argentina, in which the porphyry and high sulfidation epithermal stages are juxtaposed due to the telescoping of the mineralizing system. Pyrite is the most abundant sulfide in the analyz
publishDate 2015
format article
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url https://hdl.handle.net/10533/238113
language eng
eu_rights_str_mv openAccess
institution ANID
collection Articulos_ANID
reponame_str Articulos_ANID
instname_str Agencia Nacional de Investigación y Desarrollo
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publishDateSort 2015
author_browse Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
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