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《地质科学》 1996-01
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CHRONOLOGY STUDY OF KANGGULTAGE GOLD METALLOGENIC BELT, EAST TIANSHAN

Ji Jinsheng; Zhang Lianchang; Zeng Zhangren Lu Dengrong; Yang Xingke (XI'an Collage and Mineral Resource Xi'an 710054)Yang Jianguo(Institute of Geology and Mineral Resouce Xi'an 710054)  
he Kanggultage gold metallogenic belt is located in east Tianshan volcanic rock distrct of Early-middle Carboniferous. The gold deposits of epithermaltype,dutile shear zone-type and quartz vein were found in the belt, for example,Xitan, Kanggul, Xifengshan etc.In Xitan gold deposit, it is indicated that the Rb-Sr isochron age of host volcanic rock is 290 Ma, while the age of mineralization is 276-244 Ma. There are similar (87Sr/86Sr)i (0.7059-0. 7044) between the host rock and ore. Xitan gold deposit is of epithermal type.Using the methods of Rb-Sr isochron age, 40Ar/39Ar age spectrum and U-Ph age for Kanggul gold deposit, it is showed that the age if host volcanic rock is 300-280 Ma, while the age of mineralization is 267-220 Ma. There are smillar (87Sr/86Sr),(0. 7125-0. 7079)between the host rock and ore.Kanggul gold deposit is controlled by ductile shear zone.Based on chronology study of Kanggultage gold metallogenic belt, the age of host volcanic rock is 300-280Ma,the time of mineralization is late Variscan early Indo-Chinese epoch(270-220 Ma),in which multi-stage mineralization took place. There are time-space relationships between the granitoid intrusion and gold mineralization.
【Fund】: 国家305重点科技攻关项目
【CateGory Index】: P618.510.2
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