“…The conventional grams per 1,000 cc calculation, in genetic relation of these deposits with igneous rocks is suggested partly because of close spatial association and partly because similar rock series elsewhere have associated mineral deposits of similar mineralogic character. The association of auriferous rocks with diorites and quartz diorites along the trend of the Alaska Range is a well-documented one, as shown in the Juneau gold belt (Spencer, 1906), a t Valdez Creek (Ross, 1933b), and in the Slana area (Richter and Matson, 1968). The association of tin-bearing greisen with granite is worldwide.…”