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
Idioma:inglés
OAI Identifier:oai:repositorio.anid.cl:10533/238113
Acceso en línea:https://hdl.handle.net/10533/238113
Access Level:acceso abierto
Descripción
Sumario: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