GEOLOGY, GEOCHEMISTRY, AND GEOCHRONOLOGY OF THE CONTACT COPPER PROSPECT: AN INVESTIGATION OF A POTENTIAL PORPHYRY ROOT, NEVADA, USA
Hydrothermal fluids at Contact Copper evolved from early, oxidizing, and circumneutral pH conditions associated with sodic-calcic and potassic alteration to later, relatively reducing, and slightly more acidic conditions associated with phyllic and intermediate argillic alteration. Early hydrothermal alteration is texturally destructive and quartz-leaching, producing a vuggy texture, but late hydrothermal alteration is associated with quartz veins.
A-type veins at Contact Copper are represented by 1) barren, whispy, quartz-dominant veins with local alteration envelopes; or 2) quartz veins with trace chalcopyrite±bornite and weak alteration halos of albite, epidote, actinolite±potassium feldspar±white mica. B-type veins are 1) quartz+chlorite±molybdenite±sphalerite veins with alteration envelopes of albite, epidote, actinolite±white mica; or 2) quartz+molybdenite±chalcopyrite veins with alteration halos of potassium feldspar and/or albite±epidote±white mica. The youngest vein types observed are chlorite±chalcopyrite veinlets with thin halos of white mica. The Al-OH absorption feature of white micas occurs between 2198 and 2202nm near vein centers and between 2204 and 2213nm at distance, implying a transition from muscovitic illite to aluminoceladonite.
Crosscutting relationships and geochronology suggest that early hydrothermal alteration occurred before the complete solidification of the Contact pluton at 160.6±1.5Ma (U-Pb age, 2σ errors) and continued until at least 157.9±0.6Ma (Re-Os age, 2σ errors). Mineralized andesite porphyry dikes (160.0±1.4Ma; U-Pb age, 2σ errors) mingled and mixed with granodiorite mush and likely contributed volatiles and metals which migrated upwards and reacted with solidified wallrock, forming mineralized quartz veins at a structurally higher level of the pluton.