• 责任者：Wu Zicheng (School of Geosciences and Info-Physics ; Central South University ; Changsha 410083 ; China) ; Liu Jishun
• 刊名：Mineral Deposits
• 出版年：2013
• 卷期：32(3)
• 关键词：铜矿 ; copper ores ; 钼矿 ; molybdenum ores ; 多金属矿 ; polymetallic ores ; 云南 ; Yunnan Province
• 页码：p.603-613
• 图表：9 illus., 6 tables, 32 refs.
• 分类号：1001
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

     In this paper, the authors summarized the metallogenic model of the Feimo Cu-Mo polymetalic deposit on the basis of geological, geochemical and isotopic geochronological characteristics of the ore deposit. The ore deposit genetically belongs to the sedimentation-metamorphism-magmatic hydrothermal solution superimposed deformation type Cu-Mo polymetallic deposit. The mineralization of the deposit was characterized by long period, multi-phase, poly-source, poly-stage and multi-genesis, and the ore-forming process experienced the sedimentary locating stage of Proterozoic, regional metamorphism-reformation-enrichment stage of Middle-Late Proterozoic, and subversive reformation superposition enrichment stage of Himalayan period.