Articulo
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
Registro en:
15090013
15090013
Autor
Franchini, M., McFarlane, C., Maydagan, L., Reich, M., Lentz, D.R., Meinert, L., Bouhier, V.
Institución
Resumen
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 FONDAP