Platinum-group elements geochemistry of Tulaergen Cu-Ni sulphide deposit in East Tianshan,Xinjiang,northwest China

摘要：

　　The Tulaergen Cu-Ni sulphide deposit hosted in ultramafic intrusion is located in the east of Juluotage ductile shear zone at the northern of the East Tianshan,NW China.The sulphide ores are mainly disseminated,massive and net-textured.Pd/Ir ratios of Tulaergen rocks and ores range from 17 to 1426,and those of some massive,disseminated and net-textured ores are more than 100,which indicate that the ores may be altered by late hydrothermal fluids.The primary magma of the Tulaergen intrusion is a high-MgO basalt.Our calculations indicate that if the primary magma similar to picrite contains 10.86 ppb Pt,9.54 ppb Pd,0.76 ppb Ir and 200 ppm Cu,0.012% prior sulphide removal would result in the obviously declined contents of PGE in residual magma with 0.99 ppb Pt,0.87 ppb Pd,and 0.07 ppb Ir.

作者: Yan-Rong Liu Xin-Biao Lü Yu-Jian Wang Fu-Gui Wang Zhan Gao Wei-Dong Hui

作者单位: Faculty of Earth Resources,China University of Geosciences,Wuhan,China;Key Laboratory of Western Min Faculty of Earth Resources,China University of Geosciences,Wuhan,China Hexin Mining Co.,Ltd,Hami,China

会议类型: 国际会议

会议名称: 第十二届镍矿床国际会议

会议地点: 贵阳

会议语种:英文

页码: 58-61

在线出版日期: 2012-06-16（万方平台首次上网日期，不代表论文的发表时间）