Abstract：The Baiganhu W-Sn deposit,occurring in the metamorphic rock series of Paleoproterozoic Jinshuikou Group,is closely related to the Caledonian acidic intrusive rocks.The studied area is with a high geochemical background of W-element.The enrichment coefficients of W range from 9.57 to 25.30 in various geologic bodies.Total 17 ore bodies have been discovered with scheelite ore of skarn type and wolframite ore of quartz vein type.The deposit belongs to the stratabound hydrothermal superimposed type of W-Sn deposit.
李宏茂, 刘忠, 时友东, 王速, 王正科. 新疆东昆仑白干湖钨锡矿床地质特征[J]. 地质与资源, 2005, 14(1): 33-36.
LI Hong-mao, LIU Zhong, SHI You-dong, WANG Su, WANG Zheng-Ke. THE GEOLOGIC FEATURES OF BAIGANHU W-Sn DEPOSIT IN EAST KUNLUN MOUNTAINS,XINJIANG. GEOLOGY AND RESOURCES, 2005, 14(1): 33-36.
2005, Vol. 14 
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