- 责任者：Shu Duoyou (103 Geological Party ; Guizhou Bureau of Geology and Mineral Exploration & Development ; Tongren 554550 ; China) ; Zhang Mingqiao
- 刊名：Guizhou Geology
- 出版年：2011
- 卷期：28(2)
- 关键词：钒矿 ; vanadium ores ; 贵州 ; Guizhou Province
- 页码：p.114-117,140
- 图表：2 illus., 10 refs.
- 分类号：1001
- issnNo：ISSN1000-5943
- isbnNo：CN52-1059/P
Gongetun-Qingyang area is located transitional slope belt of Yangtze Platform and Jiangnan old land, the metallogenic condition in this area is good and many middle scale sedimentary vanadium deposits were founded. By study the relation of geologic characters and stratum, lithology of vanadium occurrence, the concentrating regulation of vanadium ore, it’s known the new discovered ore bodies occurs in the carbonate shale and claystone 0.98 m form the bottom, the taste of surface oxide ore V2O5 is higher than it in deep side. The concentration of vanadium is positive-correlation relation with Al2O3, and the relation with carbonate is not obvious, vanadium mainly exists as isomorphism in the clay mineral: illite lattice. It’s thought that the vanadium exploration targets in this area are stratum position, lithology, paleogeographic environment and microchemical features.