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《Geoscience》 2014-01
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Mineral Composition of Bianjiadayuan Pb-Zn-Ag Polymetallic Deposit in Inner Mongolia and Its Origin Significance

WANG Xi-long;LIU Jia-jun;ZHAI De-gao;YANG Yong-qiang;WANG Jian-ping;ZHANG Qi-bin;ZHANG An-li;LI Yan-lin;WANG Xiao-liang;YANG Zeng-hai;State Key Laboratory of Geological Processes and Mineral Resources,School of Earth Sciences and Resources,China University of Geosciences;Lituo Mining Industry Group of Chifeng;243 Brigade of Inner Mongolia Nuclear Geology;  
Located in the southern Daxing'anling metallogenic belt,Bianjiadayuan Pb-Zn-Ag deposit is a new discovery in recent years of higher ore grade lead-zinc-silver polymetallic deposit. Detailed microscopic identification and electron analysis show that metalliferous minerals of this deposit mainly consist of galena,sphalerite, pyrite,chalcopyrite,pyrrhotite, arsenopyrite and stannine. Silver minerals mainly consist of tetrahedrite, freibergite and pyrrhotite. In addition,we also found a large number of falkmanites in the mine,which are intimately accompanied by galena,chalcopyrite and tetrahedrite. Falkmanite crystals show as needle,pillar, bunchiness and anhedral grain forms,and their grain sizes commonly vary from 5 to 150 μm. Electron microprobe analysis also shows that its corresponding formula is( Pb4. 77Cu0. 05Fe0. 04Zn0. 06)4. 92Sb3. 91S11. 00,and its sim-plified formula is Pb5Sb4S11. Falkmanite is generally the product of the late mineralization with a low tempreture. The formation of falkmanite may be favored by a low temperature,increasing fS2and reduced fluid conditions in the ore-forming process.
【Fund】: 中国地质调查局地质矿产调查评价专项“覆盖区矿产综合预测”(1212011085471);; 国家自然科学基金项目(40973035 41072070 41272110);; 高等学校学科创新引智计划(B07011)
【CateGory Index】: P618.4
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