• 责任者：Cheng Yong (Xinjiang Institute of Geological Exploration for Nonferrous Metal Resources ; Urumqi 830000 ; China) ; Yan Cunxing
• 刊名：Mineral Resources and Geology
• 出版年：2011
• 卷期：25(6)
• 关键词：铅锌矿床 ; lead-zinc deposit ; 新疆 ; Xinjiang
• 页码：p.481-485
• 图表：4 illus., 2 photos, 1 table, 4 refs.
• 分类号：1001
• issnNo：ISSN1001-5663
• isbnNo：CN45-1174/TD

 The Tuokesai lead-zinc ore deposit in Wenquan County locates in Jiekeli-Sailimu metallogenic belt of copper, lead-zinc, niobium, tantalum, tungsten, phosphorus, ore-bearing stratum of which is sub-formation of lower Proterozoic Wenquan Formation, the petrology is mainly marble. The ore body steadily extends along with the stratum strike, occurring in bed. The ore rocks are mainly striped and laminated structure with simple ore mineral association assemblage. The ore deposit belongs to sedimental-metamorphic type. By comparison and analysis with regional ore deposits, it is considered that the region is prospective for large-super lead-zinc ore deposit.