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

Detalhes bibliográficos
Autor: Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2015
País:Chile
Idioma:inglés
OAI Identifier:oai:repositorio.anid.cl:10533/238113
Acesso em linha:https://hdl.handle.net/10533/238113
Access Level:acceso abierto
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spelling Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.201510.1016/j.oregeorev.2014.10.022https://hdl.handle.net/10533/238113http://purl.org/coar/access_right/c_abf2Trace 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 transitionFranchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.2020-03-11T20:26:45Z2022-07-07T23:44:59Z2020-03-11T20:26:45Z2022-07-07T23:44:59Z2015Agua 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 analyzFONDAPFONDAP1509001315090013virtual::39710-1WOS:000348620500019https://hdl.handle.net/10533/238113eng10.1016/j.oregeorev.2014.10.022https://doi.org/10.1016/j.oregeorev.2014.10.022Atribución-NoComercial-SinDerivadas 3.0 Chilehttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/info:eu-repo/semantics/openAccessTrace 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 transitionOre Geology ReviewsArticuloinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttps://hdl.handle.net/10533/238113FONDAPhttp://purl.org/coar/resource_type/c_2df8fbb1af9f301e-501e-40b1-ba24-0e199f38a218virtual::39710-1af9f301e-501e-40b1-ba24-0e199f38a218virtual::39710-110533/238113oai:repositorio.anid.cl:10533/2381132023-07-24 16:30:54.151https://repositorio.anid.clRepositorio ANIDaletelier@anid.cl
dc.title.none.fl_str_mv 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
dc.title.journal.none.fl_str_mv Ore Geology Reviews
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
dc.creator.none.fl_str_mv Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
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
dc.date.issued.none.fl_str_mv 2015
dc.date.accessioned.none.fl_str_mv 2020-03-11T20:26:45Z
2022-07-07T23:44:59Z
dc.date.available.none.fl_str_mv 2020-03-11T20:26:45Z
2022-07-07T23:44:59Z
dc.type.none.fl_str_mv Articulo
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dc.identifier.folio.none.fl_str_mv 15090013
15090013
dc.identifier.idwos.none.fl_str_mv WOS:000348620500019
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/10533/238113
identifier_str_mv 15090013
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url https://hdl.handle.net/10533/238113
dc.language.iso.none.fl_str_mv eng
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dc.relation.doi.none.fl_str_mv 10.1016/j.oregeorev.2014.10.022
dc.relation.uri.none.fl_str_mv https://doi.org/10.1016/j.oregeorev.2014.10.022
dc.rights.none.fl_str_mv Atribución-NoComercial-SinDerivadas 3.0 Chile
http://creativecommons.org/licenses/by-nc-nd/3.0/cl/
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