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内蒙古长汉卜罗银铅锌矿床地质特征及找矿方向
引用本文:蒋炜,;林龙军,;张云国,;李占龙,;潘彦好.内蒙古长汉卜罗银铅锌矿床地质特征及找矿方向[J].矿产与地质,2014(4):443-448.
作者姓名:蒋炜  ;林龙军  ;张云国  ;李占龙  ;潘彦好
作者单位:[1]有色金属矿产地质调查中心,北京100012; [2]中色地科矿产勘查股份有限公司,北京100012
摘    要:长汉卜罗银铅锌矿床位于华北克拉通北缘。矿体受EW、NE向断裂控制,主要以脉状、透镜状赋存于流纹斑岩、花岗闪长岩、安山岩内及不同岩性接触带。金属矿物以方铅矿、闪锌矿、黄铁矿为主,其次为黄铜矿、毒砂、黝铜矿、银黝铜矿等。围岩蚀变主要在矿脉两侧发育,包括黄铁矿化、绢云母化、硅化、绿泥石化、绿帘石化、碳酸盐化等。在找矿方向上应加强对EW向和NE向断裂破碎带中矿体的寻找,同时在矿区深部南东方向具有更好的找矿前景。

关 键 词:银铅锌矿床  地质特征  找矿方向  长汉卜罗  内蒙古

Geological characteristics and prospecting direction of Changhanboluo Ag-Pb-Zn deposit in Inner Mongolia
Institution:JIANG Wei,LIN Long-jun,ZHANG Yun-guo,LI Zhan-long,PAN Yan-hao(1. Nonferrous Metals Resource Geological Survey of China , Beij ing 100012; 2. Sinotech Mineral Exploration Co. , Ltd. , Beijing 100012 )
Abstract:Changhanboluo Ag-Pb-Zn deposit is located in the northern fringe of North China Craton.The ore-bodies are controlled by EW-and NE-trending faults and occur in veined or lenticular shape inside rhyolite porphyry,granodiorite,andesite and the contact zones of different rocks.The metal minerals mainly include galena,sphalerite and pyrite,with minor chalcopyrite,arsenopyrite,tetrahedrite and freibergite.Wall rock alteration is well developed on both sides of the veins,dominated by pyritization,sericitization,silication, chloritization,epidotization,carbonatation,etc.It is suggested that the future prospecting works shall focus on the orebodies inside the EW-and NE-trending faulted fracture zones,and the southeast part in deep level of the mining area has more favorable prospecting prospect.
Keywords:Ag-Pb-Zn deposit  geological characteristic  prospecting direction  Changhanboluo  Inner Mong olia
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