“…Magnetite in veinlets makes up more than 1 percent by volume of most porphyry copper-gold orebodies (Saegart and Lewis, 1977;Sillitoe, 1979). Magnetite forms stable assemblages with any of the minerals that characterize potassic or feldspar-stable alteration: chalcopyrite, biotite, anhydrite, K-feldspar, chlorite, or actinolite.…”