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(Pt1wqb),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。
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.
出处
《矿产与地质》
2011年第6期481-485,共5页
Mineral Resources and Geology
关键词
铅锌矿床
地质特征
找矿前景
托克赛
新疆
lead-zinc ore deposit, geological characteristics, Tuokesai, mineral prospect
