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内蒙古西乌珠穆沁旗花敖包特银铅锌矿矿床地质特征及成因初探
引用本文:李振祥,谢振玉,刘召,李淑果.内蒙古西乌珠穆沁旗花敖包特银铅锌矿矿床地质特征及成因初探[J].地质与资源,2008,17(4):278.
作者姓名:李振祥  谢振玉  刘召  李淑果
作者单位:1. 内蒙古自治区第十地质勘查院, 内蒙古 赤峰 024005;2. 辽宁省矿产勘查院, 辽宁 沈阳 110032
摘    要:花敖包特大型脉状银铅锌多金属矿床赋存于下二叠统寿山沟组(P1s)裂隙破碎带中,属中低温次火山热液成因.矿床处于大兴安岭中南部的锡林浩特-霍林郭勒多金属成矿带上,断裂构造发育,火山活动强烈,银铅锌多金属多期成矿.矿体赋存于北西、北东及近南北向的构造破碎带里,矿体呈脉状严格受断裂构造控制.矿体规模中等,形态较复杂,厚度较稳定,组分较均匀.围岩蚀变发育,可出现3期,具明显的分带性.成矿期为晚侏罗世.

关 键 词:银铅锌矿  次火山热液  多期成矿  晚侏罗世  花敖包特  
收稿时间:2008-09-23

GEOLOGY AND GENESIS OF THE HUAAOBAOTE LEAD-ZINC DEPOSIT IN INNER MONGOLLA
LI Zhen-xiang,XIE ZhenVyu,LIU Zhao,LI Shu-guo.GEOLOGY AND GENESIS OF THE HUAAOBAOTE LEAD-ZINC DEPOSIT IN INNER MONGOLLA[J].Geology and Resources,2008,17(4):278.
Authors:LI Zhen-xiang  XIE ZhenVyu  LIU Zhao  LI Shu-guo
Institution:1. No. 10 Institute of Geological Exploration, Inner Mongolia Bureau of Geology and Mineral Resources, Chifeng 024005, Inner Mongolia, China;2. Liaoning Institute of Mineral Resources Exploration, Shenyang 110032, China
Abstract:The large-scale Huaaobaote vein type of Ag-Pb-Zn polymetal deposit in Xi Ujimqin Qi, Inner Mongolia, occurring in the fracture zone in Lower Permian Shoushan formation, is of subvolcanic meso-epithermal genesis. The deposit is located in the Xilinhot-Huolin Gol polymetal metallogenetic belt in the middle-south of Daxinganling Mountains, with developed faults and intense volcanic activities. The metallogenesis of Ag-Pb-Zn polymetal is in multiple stages. The vein-shaped ore bodies are in medium scale, comple...
Keywords:Ag-Pb-Zn deposit  subvolcanic solution  multi-staged metallogenesis  Late Jurassic  Inner Mongolia  
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