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投稿时间:2014-03-18 修订日期:2014-03-21
投稿时间:2014-03-18 修订日期:2014-03-21
中文摘要: 西藏尕尔穷矿区位于班公湖-怒江成矿带西段,据前人研究表明,尕尔穷矿区成矿阶段的构造环境为造山环境。对尕尔穷铜金矿床的Ⅲ号矿体系统的矿相学研究表明,矿石矿物主要为磁铁矿、赤铁矿、黄铜矿、斑铜矿、自然金等;矿体围岩蚀变主要有硅化、碳酸盐化、绿泥石化、矽卡岩化、绿帘石化、绢云母化等。矿石组构表现出热液矿床特征。对比总结世界大多数典型IOCG矿床的特征,同时结合地球化学数据资料分析,认为尕尔穷Ⅲ号铜金矿应属于铁氧化物铜金(IOCG)矿体。Ⅲ号矿体成因的确定及尕尔穷矿床类型的补充拟定对于班公湖一怒江成矿带的区域找矿评价具有重要指示意义。
Abstract:Ga Erqiong mine is located in the west of Bangong–Nujiang metallogenic belt,According to the previous studies, its tectonic environment in Ga Erqiong mine is orogenic environment.The systematic mineralogical study of Ⅲ ore body in Ga Erqiong copper-gold deposit shows Ore minerals are mainly magnetite, hematite, chalcopyrite, bornite, native gold and so on; orebody wall rock alteration is variety, they mainly are silicified alteration, carbonated alteration, chlorited alteration, epidotizatied alteration, Sericited alteration, Skarnizatied alteration and other alterations. Ore fabrics show hydrothermal deposit’ characteristic. Contrasting with most typical IOCG deposits on world and combing geochemical analysis of data,we conclude that Ga Erqiong Ⅲ copper-gold ore body belong to IOCG ore body. Determination of the Ⅲ orebody's origin and complement of Gaerqiong deposit types are of great importance implication for exploration and evaluation atBangong-Nujiang metallogenic belt.
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基金项目:
作者 | 单位 | |
林 鑫 | 成都理工大学 中国地质科学院矿产资源研究所 | 501978783@qq.com |
唐菊兴* | 中国地质科学院矿产资源研究所 | tangjuxing@126.com |
张 志 | 成都理工大学 | |
宋俊龙 | 成都理工大学 | |
王红星 | 成都理工大学 |
引用文本:
林 鑫,唐菊兴,张 志,宋俊龙,王红星.西藏尕尔穷铜金矿床IOCG矿体地质特征与成因[J].有色金属(矿山部分),2014,66(4):.
LIN Xin,TANG Ju-xing,ZHANG Zhi,SONG Jun-long,WANG Hong-xing.Geological characteristics and origin of IOCG ore bodyin Gaerqiong Copper-gold deposit,Tibet[J].NONFERROUS METALS(Mining Section),2014,66(4):.
林 鑫,唐菊兴,张 志,宋俊龙,王红星.西藏尕尔穷铜金矿床IOCG矿体地质特征与成因[J].有色金属(矿山部分),2014,66(4):.
LIN Xin,TANG Ju-xing,ZHANG Zhi,SONG Jun-long,WANG Hong-xing.Geological characteristics and origin of IOCG ore bodyin Gaerqiong Copper-gold deposit,Tibet[J].NONFERROUS METALS(Mining Section),2014,66(4):.