• 责任者：Chen Bailin (Institute of Geomechanics ; Chinese Academy of Geological Sciences ; Beijing 100081 ; China) ; Zhao Hengle
• 刊名：Mineral Deposits
• 出版年：2012
• 卷期：31(1)
• 关键词：银矿 ; silver ores ; 铅矿 ; lead ores ; 阿尔金山 ; Altun Mountains
• 页码：p.13-26
• 图表：12 illus., 6 tables, 31 refs.
• 分类号：1001
• 出版序号：20130230
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

Located in Ruoqiang County of Xinjiang, the Abei ore deposit is a medium-size Ag-Pb deposit recently discovered in eastern Altun Mountains. Tectonically, it is sandwiched between NE-trending Altun strike-slip fault and EW-trending northern Altun marginal fault. In combination with an analysis of the regional tectonic evolution and features of the ore-controlling structure, the authors hold that the Abei Ag-Pb ore deposit is a magmatic hydrothermal ore deposit controlled by high-angle brittle fracture and related to intermediate-acid magmatic activity during the closure and collision of Hongliugou-Lapeiquan back-arc basin in late Early Paleozoic.