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

dc.creatorFranchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
dc.date2020-03-11T20:26:45Z
dc.date2022-07-07T23:44:59Z
dc.date2020-03-11T20:26:45Z
dc.date2022-07-07T23:44:59Z
dc.date2015
dc.date.accessioned2023-08-22T11:56:32Z
dc.date.available2023-08-22T11:56:32Z
dc.identifier15090013
dc.identifier15090013
dc.identifierhttps://hdl.handle.net/10533/238113
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8346156
dc.descriptionAgua 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
dc.descriptionFONDAP
dc.descriptionFONDAP
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.oregeorev.2014.10.022
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleTrace 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.titleOre Geology Reviews
dc.typeArticulo
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion


Este ítem pertenece a la siguiente institución