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《MINERAL DEPOSITS》 1997-02
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GEOLOGICAL CHARACTERISTICS AND GENESIS OF THE ASHELE COPPER ZINC MASSIVE SULFIDE DEPOSIT,XINJIANG

Ye Qingtong,Fu Xijie (Institute of Mineral Deposits,Chinese Academy of Geological Sciences,Beijing 100037) Zhang Xiaohua (Section of Regionalization,Chinese Academy of Geological Sciences,Beijing 100037)  
The Ashele massive sulfide deposit occurs in the Ashele Devonian volcano sedimentary basin lying on the southern margin of Altay orogenic belt.The basin was formed as a result of rift evolution on the basis of Proterozoic Early Paleozoic continental crust,and experienced deformation of regional nappe structure.Mineralization took place at the interval between Early Middle Devonian volcanic activities of the bimodal spilite keratophyre volcanic suite.The deposit has two layer structure:a massive sulfide orebody in the upper part and a disseminated sulfide orebody in the lower part.In the massive sulfide orebody there exists vertical zonation of S→Cu,S→Cu,Zn,S→Cu,Pb,Zn→Cu,Zn,Pb,BaSO 4 which is a reflection of ore accumulation sequence at the bottom of the sea.Around the disseminated sulfide orebody are well developed wall rock alterations,which exhibit from the inside outward the zonation of sericite quartz metasomatite→chlorite sericite metasomatite→weakly hydrolytic pyroclastic rocks,suggesting characteristics of acid leaching.Studies of ore deposit geology,temperature pressture geochemistry and stable isotope geochemistry indicate that the ore forming fluids were composed of deeply circulating sea water and magmatic water,and that the ore forming materials were derived from the lower crust.In addition,the ore forming process has been discussed and a metallogenic model of mixed fluids comprising deeply circulating sea water and magmatic water has been established.
【Fund】: “八五”国家科技攻关项目
【CateGory Index】: P578.25
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