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《Geology-geochemistry》 2001-02
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THE GEOLOGICAL SETTING, CHARACTERS AND ORIGIN OF MISSISSIPPI VALLEY-TYPE Pb-ZnDEPOSITS IN SICHUAN AND YUNNAN PROVINCES

Wang Jiangzhen+{1,2)} Li Chaoyang+{1)} Li Zeqin+{1,2)} Liu Jiajun+{1)}1) (Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002)2) (Chengdu University of Technology, 610059)  
Along the border of Southeast Sichuan and East Yunnan (Fig.1) there are numerous Mississippi Valley-type Pb-Zn deposits. Some characteristics of the deposits are: (1) the deposits are hosted in Late Proterozoic and Mississippian rocks, especially in dolomite; (2) fluid-inclusion studies of the deposits show that the homogenization temperatures fall predominantly between 140-200℃; (3) around the deposits the Proterozoic limestone has altered to dolomite. Regional dolomitization covers a large area; (4) there are some aquifers in the region. The most important one for the ore fluids is Late Proterozoic sandstone, named the Doushantuo Formation.; It has been suggested that all the deposits were formed by regional migration of ore-forming brines. Hydrologic modeling of regional brine migration is that when the Longmenshan-Jingpingshan orogenic belt, situated west of the area, uplifted in the Yenshanian and Himalayan movements (Jurassic to Eogene), the gravity drove the ore-forming fluids from the orogenic belt to the locus of mineralization and resulted in the formation of the deposits.;
【Fund】: ZK95 1 B1 411项目和KZCX2 10 1项目
【CateGory Index】: P618.4
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