新疆且末县屈库勒克东金(锑)矿床地质特征研究  

The geological characteristics of the East gold (antimony) deposit in Qukuleke County, Xinjiang

作　　者：孙彦佰 金正斌 段报瑞 李少阳 赵锐龙 SUN Yan-bai;JIN Zheng-bin;DUAN Bao-rui;LI Shao-yang;ZHAO Rui-long(Qiemo County Bangtai Mining Investment Co.,Ltd.,Bazhou 841900,China)

机构地区：[1]且末县邦泰矿业投资有限公司,新疆巴州841900

出　　处：《世界有色金属》2024年第6期131-133,共3页World Nonferrous Metals

摘　　要：屈库勒克东金(锑)矿是东昆仑地区重要的金锑矿床,对东昆仑寻找该类型矿床提供了研究对象。文章在系统总结矿床地质特征的基础上,总结得出:上石炭统哈拉米兰河上亚群是主要的矿源层,受区域中酸性岩浆岩和构造的影响,导致地层的Au、Zn、Mo、Ag、Pb等元素活化富集,进而在上石炭统哈拉米兰河群上亚群碳酸盐岩-沉积碎屑岩中封闭形成具有工业价值的矿体。The East Gold(Antimony)Mine is an important gold-antimony deposit in East Kunlun area,which provides a research object for the search for this type of deposit in East Kunlun.On the basis of systematically summarizing the geological characteristics of the deposits,this paper concludes that the Upper Carboniferous Harraman River subgroup is the main ore source layer,which is affected by the acidic magmatic rocks and structures in the region,resulting in the activation and enrichment of Au,Zn,Mo,Ag,Pb and other elements in the strata,and then stores and closes in the carbonate-sedimentary clastic rocks of the Upper Carboniferous Harraman River Group to form an ore body with industrial value.

关 键 词：金锑矿床 地质特征 矿化规律 

分 类 号：P618.51[天文地球—矿床学]