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《Gansu Geology》 2009-01
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WEI Bing-an(219 Team,Gansu Provincial Bureau of Nuclear Geology,Tianshui 741025,China)  
Shuidonggou gold deposit in Tianshui city is located in the southern side of the great reversed "S" type structure in the junction area of Caledonian orogenic belt of Qilian and north Qinling,where gold mineral-ization is controlled strictly by EW-striking fractures.The walk-rock alteration is characterized by silicification,limonitization,pyritization and sericitization.The gold-bearing minerals mainly are limonite,pyrite and arsenopy-rite.The results of study show that the basic conditions of deposit formation include meta-sandstone,ductile-brit-tle fractures and intermediate-acid intrusive rock,the EW-striking tectonic alteration zone and the areas where geochemical anomalies have been recognized are the favorite for prospecting gold.
【CateGory Index】: P618.51
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