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《Journal of Jilin University(Earth Science Edition)》 2011-06
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A Comparative Study of Ore-Forming Structures in Bairendaba and Weilasituo Silver-Polymetallic Deposits of Inner Mongolia

SUN Ai-qun1,NIU Shu-yin1,2,MA Bao-jun1,NIE Feng-jun3, JIANG Si-hong3,ZHANG Jian-zhen1,WANG Bao-de1,CHEN Chao1,2 1.Shijiazhuang University of Economics,Shijiazhuang 050031,China 2.School of the Earth Sciences and Resources,China University of Geoscicences,Beijing 100083,China 3.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China  
The Bairendaba and Weilasituo Ag-Pb-Zn deposits are two large-size deposits in the same orefield,with the prospective reserves of Ag being over 10 000 tons and Pb and Zn about 600 million tons.The magmatism of these two ore deposits was controlled by mantle branch in southern Da Hinggan Mountains.Since Mesozoic,intensive magmatism has generated the channel for the upwelling of deep source materials and resulted in the formation of a series of fracture systems related to igneous activities,which served as important ore-controlling structures for the migration and concentration of hydrothermal fluids.Studies demonstrate that different scales of structures dominate the mineralization distribution of this ore deposit.The orefield is controlled by the northeast principal detachment zone on the south margin of the mantle branch in southern Da Hinggan Mountains,the deposits are controlled by a series of secondary detachment belts,and the ore bodies are controlled by tensile or tensile-shearing faults.Geochemical studies indicate that ore-forming materials were mainly derived from the depth,with the participation of some crustal materials during the upwelling of hydrothermal fluids.
【Fund】: 危机矿山研究项目(20089948 20109901);; 国家重点自然科学基金项目(41030421);; 国家自然科学基金项目(40872137);; 石家庄经济学院招标项目(2008JZ01)
【CateGory Index】: P618.2
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