GEOLOGY AND GEOCHEMISTRY OF JIANGXILONG GOLD-ANTIMONY DEPOSIT IN WESTERN HUNAN PROVINCE
YIN Hua-feng1, XIANG Tian1, YANG Hong-chao1, BAO Zhen-xiang2, BAO Jue-min2
1. No. 245 Team, Hunan Bureau of Geologic Exploration for Nonferrous Metals, Jishou 416007, Hunan Province, China; 2. Western Hunan Research and Development Center for Mineral Resources, Jishou 416007, Hunan Province, China
Abstract：The Jiangxilong gold-antimony deposit in Western Hunan Province, occurring in the epimetamorphic rock series of Wuqianxi formation, Banxi group, Neoproterozoic, is a cogentic (associated) Au-Sb deposit. The metallogenesis is strictly controlled by NE-trending shear fault zone. The ore-bodies are steeply-dipped crossing veins, stably reappearing in the direction of dip and striking. The gold occurs in the near altered wallrock. Arsenopyrite is the main gold carrier. The enrichment of antinomy is closely related to silicification. The Au-bearing antimony ore is with high As. The result of ore dressing experiment focused on antimony shows that the main recovered mineral is antimonite, with recoverable of gold.
尹华锋, 向田, 杨洪超, 鲍振襄, 包觉敏. 湖南江溪垄金锑矿床地质地球化学特征及开发应用[J]. 地质与资源, 2007, 16(4): 275-279.
YIN Hua-feng, XIANG Tian, YANG Hong-chao, BAO Zhen-xiang, BAO Jue-min. GEOLOGY AND GEOCHEMISTRY OF JIANGXILONG GOLD-ANTIMONY DEPOSIT IN WESTERN HUNAN PROVINCE. GEOLOGY AND RESOURCES, 2007, 16(4): 275-279.
2007, Vol. 16 
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