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He and Ar isotopic compositions in fluid inclusions of Hubei Jilongshan Au-Cu deposit and their geological implications

Jia Baojian1,2,Li Shengrong1,Yang Qingyu3,Xu Yongzhong4,Yang Chengdong1,Pang Ajuan1,Yan Yutong1(1.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(Beijing); school of geosciences and resources,China University of Geosciences(Beijing); 2.Zhejiang provincial institute of geological resources; 3.Hubei Jinlongshan Gold Mining Co.,Ltd;4.China National Gold Group Corporation)  
Jilongshan Au-Cu deposit is a typical skarn deposit located in the southeastern Hubei metallographic zone subordinated by the Middle-Lower Yangtze River Fe-Cu polymetallic metallogenic belt.Little study of metallogenic fluid sources has been made on this deposit.By studying 5 pyrite samples collected from different skarn belts of this deposit,this paper analyzed the helium and argon isotopic compositions of fluid inclusions for the first time.It is shown that the 3He/4He ratios are 0.025-0.051 Ra with the average of 0.031 Ra and the 40Ar/36Ar ratios are 261.2-580.2 Ra with the average of 377.2 Ra.The data obtained suggest that the metallogenic fluids in this deposit mostly comprise rainfalls with extracted crust materials while mantle fluids play little role.
【Fund】: 国家自然科学基金重大研究计划重点支持项目(90914002);; 中国地质调查局地质调查工作项目(1212011220926)
【CateGory Index】: P618.51;P618.41
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