| Reference | {Deposit:: LINQING, MA, 1982, THE GEOLOGICAL CHARACTERISTICS OF DAMINGSHAN SEDIMENTARY-MAGMATIC-HYDROTHERMAL WOLFRAMITE DEPOSIT, GUANGXI ZHUANG AUTONOMOUS REGION, CHINA, IN J.V. HEPWORTH AND HONG ZHANG YU (EDS.), TUNGSTEN GEOLOGY, CHINA; ESCAP/RMRDC, BANDUNG, INDONESIA, P. 375-384.}{Deposit:: BING, WAN, 1982, THE DAMINGSHAN STRATA-BOUND TUNGSTEN DEPOSITS IN GUANGXI ZHUANG AUTONOMOUS REGION, CHINA, IN J.V. HEPWORTH AND HONG ZHANG YU (EDS.), TUNGSTEN GEOLOGY, CHINA; J.V. HEPWORTH, AND HONG ZHANG YU (EDS.), TUNGSTEN GEOLOGY, CHINA; ESCAP/RMRDC, BANDUNG, INDONESIA, P. 403-412.}{Deposit:: ANSTETT, T.F., BLEIWAS, D.I., AND HURDELBRINK, R.J., 1985, TUNGSTEN AVAILABILITY - MARKET ECONOMY COUNTRIES, U.S. BUREAU; OF MINES, INFORMATION CIRCULAR 9025, 51 P.} |