| 新疆温泉县托克赛铅锌矿地质特征及找矿前景分析 |
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| 引用本文： | 成勇,闫存兴,俞彦龙,朱生善.新疆温泉县托克赛铅锌矿地质特征及找矿前景分析[J].矿产与地质,2011(6):481-485. |
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| 作者姓名： | 成勇 闫存兴 俞彦龙 朱生善 |
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| 作者单位： | 新疆维吾尔自治区有色地质矿产勘查院,乌鲁木齐830000 |
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| 摘 要： | 温泉县托克赛铅锌矿床处于捷克利—赛里木铜、铅锌、铌、钽、钨、磷成矿带上,赋矿地层为下元古界温泉群上亚群(Pt1 wqb),岩性主要为大理岩,矿体呈层状顺层产出,矿石主要呈条带状、纹层状构造,矿石矿物组合简单,属沉积—变质型铅锌矿床.通过与区域矿床的对比、分析,认为该成矿区具有寻找中—大型铅锌矿床的潜力.
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| 关 键 词： | 铅锌矿床 地质特征 找矿前景 托克赛 新疆 |
Geological characteristics and mineral prospect analysis of the Tuokesai lead-zinc ore deposit in Wenquan county, Xinjiang autonomous region |
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| Institution: | CHENG Yong, YAN Cun-xing, YU Yan-long,ZHU Shen-shan ( Xinjiang Institute of Geological Ezploration for Nonferrous Metal Resources, Urumqi, Xinjiang 830000, China ) |
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| Abstract: | 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 （Ptlwqb）, the petrology is mainly marble. ＇The ore body steadily extends along with the strutum 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-metamor- phic type. By comparison and analysis with regional ore deposits, it is considered that the region is prospec- tive for large-super lead-zinc ore deposit. |
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| Keywords: | lead-zinc ore deposit geological characteristics Tuokesai mineral prospect |
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