Abstract：Abundant nonferrous metallic, precious metallic, rare earth metallic and nonmetallic mineral resources are hosted in the Early Cambrian black rock series in south China. Among them, the vanadium deposits located on the southeast margin of Yangtze platform are with great potential. The vanadium deposits in Hunan Province occur in the organic-rich carbonaceous, siliceous, phosphate black rock series at the bottom of Lower Cambrian. The ore bodies are broadly distributed in simple layers, with stable occurrence, shallow depth and huge reserves. The metallogenesis started with hydrothermal deposition epoch and ended with normal sedimentation epoch, which alternatively perform as the peak epochs for the mineralization of vanadium. The deposit is characterized by both hydrothermal deposition and microbiologic metallogenesis, genetically belonging to bio-geochemical deposition.
刘光昭, 尹华锋, 刘玉峰, 付益平. 湖南下寒武统黑色岩系中的钒矿床[J]. 地质与资源, 2008, 17(3): 194-201.
LIU Guang-zhao, YIN Hua-feng, LIU Yu-feng, FU Yi-ping. VANADIUM DEPOSITS IN THE LOWER CAMBRIAN BLACK ROCK SERIES IN HUNAN PROVINCE. GEOLOGY AND RESOURCES, 2008, 17(3): 194-201.
2008, Vol. 17 
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