Gold in porphyry copper deposits: Experimental determination of the distribution of gold in the Cu-Fe-S system at 400 degrees to 700 degrees C

Experiments in the system Au-Cu-Fe-S were carried out at temperatures of 40 0 degrees to 700 degrees C to determine how much gold could be accommodated by bornite and chalcopyrite, the two most common ore minerals in porphyry copper-gold deposits. Our results show that for all temperatures bornite co ntains one order of magnitude more gold than chalcopyrite (or intermediate solid solution (iss), its high-temperature equivalent). The range of gold c oncentrations in bornite and chalcopyrite (or iss) decreases with decreasin g temperature from 1,280 to 8,200 ppm Au in bornite and 100 to 125 ppm Au i n iss at 600 degrees C, to 235 to 364 ppm Au in bornite and 5 to 16 ppm Au in chalcopyrite (or iss) at 500 degrees C, and to 13 to 80 ppm Au in bornit e and 2 to 4 ppm Au in chalcopyrite (or iss) at 400 degrees C. The amount o f gold in bornite is also strongly dependent on the composition of bornite, being highest in "stoichiometric" bornite compositions (Cu5FeS4),and decre asing toward Cu-rich and Cu-poor compositions. Phase equilibrium constraints for solutions with geologically reasonable re duced sulfur contents indicate that high-temperature porphyry copper-gold d eposits will contain bornite and magnetite, whereas lower temperature depos its (whether primary or overprinted by phyllic alteration) will contain cha lcopyrite and pyrite. If gold is present in the ore-forming solutions, more of it will be deposited in high-temperature porphyry copper-gold deposits where it will be closely associated with bornite. Coexisting magnetite in t hese deposits should generate magnetic anomalies. Lower temperature deposit s will contain less gold, which is hosted by pyrite as well as chalcopyrite , and will lack magnetic anomalies. Comparison of the amount of gold hosted by natural porphyry copper-gold ores to that hosted by bornite and chalcop yrite in our experiments suggests that significant amounts of gold can be l ost from these deposits into surrounding hydrothermal systems.