“…The suite is similar to that measured in groundwater around other porphyry Cu deposits (e.g. Learned et al, 1985;Leybourne and Cameron, 2010), where elevated Cu, Zn, and SO 4 concentrations can be attributed to weathering of chalcopyrite, sphalerite, and iron-sulfides. Molybdenum and Re (a common trace element primarily hosted within molybdenite in porphyry Cu systems; McCandless et al, 1993), are likely derived from molybdenite, although chalcopyrite and pyrite (e.g.…”