“…Origin of gold interpreted to be from deep-crustal metamorphic fluids, or possibly a remobilized strata-bound deposit. Spencer, 1906;Twenhofel, 1952;Wayland, 1960;Herreid, 1962;Goldfarb and others, 1986Goldfarb and others, , 1988Goldfarb and others, , 1991Newberry andBrew, 1987, 1988;Light and others, 1989;Brew and others, 1991;Alaska Mineral Industry, 1993, p. 13 Kennedy and Walton, 1946;Johnson and others, 1982;Himmelberg andothers, 1987, Still, 1988;Brew and others, 1991; Significant Lode Deposits of Russian Far East, Alaska, and Canadian Cordillera sulfide Consists of sphalerite, galena, chalcopyrite, and tetrahedrite in a pyrite-rich matrix in massive pods, bands, laminations, and disseminations, associated with pyrite-carbonate-chert exhalite. Hanging wall of chlorite and sericrte sedimentary rocks.…”