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《Gansu Geology》 2009-01
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FEATURES AND ORIGIN OF METALLOGENETIC FLUID OF DASHUI GOLD DEPOSIT IN GANSU PROVINCE

DAI Wen-jun1,CHEN Guo-zhong2,Ma Xiao-yun2(1.No.3 Geology and Mineral Exploration Team,Gansu Provincial Bureau of Geology and Mineral Exploration and Development,Lanzhou 730050,China;2.Faculty of Earth Resources,China University of Geosciences,Wuhan 430074,China)  
Dashui gold deposit is located in the south margin of west Qinling.On the basis of the study done by former experts,after studying systematically fluid inclusions of deposit,the authors supposes that the most in-clusions within calcite are gaseous and fluid inclusions.In the inclusions contained gaseous composition include CH4,CO and H2,which indicate the oxidizing environment,and the fluid composition is composed of anions as SO4-2 first and Cl-second,cations as K+ first,Na+ second.Au migrated in the complex of AuSO4 within the met-allogenetic fluid.The metallogenetic temperature is 120℃~220℃,within the range of low temperature.Salinity,w(NaCleq),is 2.7%~9.1%,and density is 0.875~0.970g/cm3.The results,δD=-101%~-61%,δ18O(SMOW)=-0.3%~19.42%,δ18OH2O=2.7%~9.1%,show that the metallogenetic fluid in early stage originated from magmatic water,and the metallogenetic fluid in later stage was the mixture of magmatic water and meteoric water,the value of δ13C indicate as the genesis hydrothermal.According to the result of comprehensive analysis,it is supposed that this deposit is a strata-bound,shallow-supershallow-seated,post-magamtic,hydrothermal metasomatic deposit which is a product of multi-stage tectonomagmatic process.
【CateGory Index】: P618.51
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