Cotabambas: Late Eocene Porphyry Copper-Gold Mineralization Southwest of Cuzco, Peru
José Perelló, Carlos Neyra, Héctor Posso, Alberto Zárate, Pedro Ramos, Alberto Caballero, Ricardo Martini, Nicolás Fuster, Ricardo Muhr, 2005. "Cotabambas: Late Eocene Porphyry Copper-Gold Mineralization Southwest of Cuzco, Peru", Andean Metallogeny: New Discoveries, Concepts, and Updates, Richard H. Sillitoe, José Perelló, César E. Vidal
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The Cotabambas porphyry copper-gold cluster includes at least four porphyry centers in an area of 5 × 3 km, namely Ccalla, Azulccacca, Huaclle, and Ccarayoc, of which the first two are the best known. The geology of the area is dominated by two large granodiorite and diorite plutons and smaller stocks and dikes of microdiorite and andesite, all of which form part of the middle Eocene to early Oligocene Andahuaylas-Yauri batholith. At Cotabambas, granodiorite (K-Ar age of 39.8 ± 1.5 Ma) intrudes diorite (K-Ar age of 43.2 ± 1.1 Ma) and both, in turn, are intruded by a series of composite, structurally controlled porphyry stocks and dikes of granodioritic to quartz monzodioritic composition associated with porphyry copper-gold mineralization. The main structural features include several intersecting north-northeast- and west-northwest-trending faults, which are interpreted to have controlled the emplacement and architecture of the porphyry centers.
Most of the copper-gold mineralization at Cotabambas is associated with early-stage potassic alteration, including multiphase, magnetite-rich stockworks with quartz, K-feldspar, biotite, chalcopyrite, and bornite. Apatite and anhydrite are common constituents. An early, copper-bearing potassic-calcic assemblage made up of quartz, K-feldspar, biotite, actinolite, hornblende, diopside-hedenbergite, and magnetite is also preserved locally. Early, biotite-rich alteration from Ccalla yielded a K-Ar age of 35.7 ± 0.9 Ma. These mineral associations are overprinted by greenish-colored, intermediate argillic assemblages dominated by quartz, chlorite, illite, smectite, halloysite, and greenish soapy sericite, which have partially to completely destroyed earlier formed chalcopyrite-bornite associations but have contributed pyrite as disseminated grains and veinlets. These associations are spatially related to a series of inter- to late mineral porphyries.
All the previously described rocks and alteration assemblages are cut by a large, late mineral, domelike body of dacitic composition and an associated dike swarm. Both dome and dikes developed incipient alteration to calcite, illite, and chlorite and host a set of centimeter-wide veins with open spaces filled by quartz, calcite, sphalerite, and galena.
Supergene mineralization is present as patchily distributed copper oxides near surface underlain by an irregular supergene enrichment blanket dominated by sooty chalcocite. Supergene kaolinite and alunite are common. A K-Ar age of 3.3 ± 0.2 Ma on alunite shows a late Pliocene age for supergene enrichment and leaching processes in the region.
The mineralization at Cotabambas is assigned to the porphyry copper-gold class because (1) gold grades are typically >0.3 ppm; (2) copper-gold mineralization is accompanied by abundant (>5 vol %) hydrothermal magnetite in potassic alteration; (3) hydrothermal amphibole and pyroxene are present in potassic-calcic alteration; (4) copper and gold display a sympathetic relationship, and all observed Au occurs as micron-sized inclusions in chalcopyrite; (5) intense pyrite-rich intermediate argillic alteration overprints earlier formed potassic and calcic-potassic alteration and associated copper-gold mineralization; and (6) molybdenum contents are low (<0.01%).
The coincident K-Ar and fission-track (apatite) ages (38.6 ± 3.4 and 33.3 ±1.4 Ma) for plutons from the Cotabambas area, together with the late Eocene age of Cotabambas (see above) and regional data, confirm that porphyry copper emplacement in the Andahuaylas-Yauri belt of southeastern Peru took place simultaneously with intense shortening, surface uplift, and rapid exhumation during the middle to late Eocene Incaic orogeny.
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A variety of metals and deposit types define the metallogeny of the Andes from Colombia through Ecuador, Peru, and Bolivia to Argentina and Chile, although porphyry copper and epithermal gold deposits undoubtedly predominate and will continue to do so. Discoveries over the last 30 yrs or so, predominantly in the central Andes and especially Chile, have been made using routine, field-based geologic and complementary geochemical methods, a situation that is considered unlikely to change radically in the foreseeable future. The only clearcut evolutionary change is the increased number of deposits being discovered beneath pre- and postmineral cover. The predictive capacity of conceptual geology has had minimal impact on the Andean discovery record but is thought to offer much promise for the future. This introductory article selects mineralization styles and relationships as well as some broader metallogenic parameters as simple examples of geologic concepts that may assist exploration. Emphasis is placed on porphyry copper ± molybdenum ± gold and high-, intermediate-, and lowsulfidation epithermal gold ± silver deposits, although reference is also made to several carbonate rock-hosted precious and base metal deposit types and styles as well as subvolcanic tin, volcanogenic massive sulfide, and slate-belt and intrusion-related gold deposits. Particular emphasis is placed on the potential for exceptionally high grade porphyry copper, porphyry gold, epithermal gold, and subvolcanic tin deposits. Deposits resulting from the oxidation, enrichment, and chemical transport of copper and zinc and mechanical transport of gold and silver during supergene weathering are also briefly highlighted.
Si bien la metalogenia de los Andes de Colombia, Ecuador, Perú, Bolivia y Chile se encuentra definida por una gama de metales y estilos de mineralización, son los depósitos tipo pórfido de cobre y epitermal de oro los que dominan en el presente y continuarán prevaleciendo en el futuro. Los descubrimientos de los últimos 30 años, predominantemente en los Andes centrales y especialmente en Chile, han sido realizados mediante métodos geológicos rutinarios de campo, generalmente complementados satisfactoriamente por métodos geoquímicos. Se estima que esta situación difícilmente experimentará variaciones radicales en un futuro cercano. El único cambio destacable en esta historia evolutiva está dado por el aumento apreciable de descubrimientos de depósitos cubiertos, bajo cobertura pre o postmineral. A nivel andino, la capacidad predictiva de la geología conceptual ha tenido un impacto mínimo en el número total de descubrimientos, aunque se piensa que su uso debiera garantizar buenas perspectivas futuras. El presente artículo