| 新疆乌恰县萨热克砂岩铜矿床地质特征与找矿前景 |
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| 引用本文： | 胡庆雯,刘宏林.新疆乌恰县萨热克砂岩铜矿床地质特征与找矿前景[J].矿产与地质,2008,22(2):131-134. |
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| 作者姓名： | 胡庆雯 刘宏林 |
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| 作者单位： | 有色金属矿产地质调查中心新疆地质调查所,乌鲁木齐,830011 |
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| 摘 要： | 萨热克铜矿位于托云中新生代拉分盆地西南缘与东阿赖褶皱带之间的次级中生代断陷盆地中。矿床受NE向向斜构造和层间断裂控制，矿体呈层状赋存于白垩系特定的层位和碎屑岩建造中。根据矿区矿化富集规律和地质地球化学勘查成果，认为该区具有中一大型铜矿的找矿潜力。
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| 关 键 词： | 萨热克铜矿床 矿床特征 砂岩 找矿前景 乌恰县 新疆 |
Geological characteristics and prospecting perspective of the Sareke sandstone Cu deposit in Wuqia County,Xinjiang |
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| HU Qing-wen,LIU Hong-lin.Geological characteristics and prospecting perspective of the Sareke sandstone Cu deposit in Wuqia County,Xinjiang[J].Mineral Resources and Geology,2008,22(2):131-134. |
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| Authors: | HU Qing-wen LIU Hong-lin |
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| Institution: | (Xinjiang Geological Survey of China Nonferrous Metals Resources Geological Survey, Urumqi 830011, China) |
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| Abstract: | The Sareke Cu deposit located in the secondary Mesozoic fault basin between southwestern edge of Meso-cenozoic pull-apart basin in Tuoyun and Eastern Alai fold belt. The deposit is controlled by both NE trending syncline structure and interlayer fracture, and the orebodies occurred in beds which located in given horizon and elastic rocks construction of Cretaceous. According to mineralization and enriching rules of this area with geological and geochemical exploring fruits, it has believed there is prospecting potential for middle-large scale Cu deposit in this ore area. |
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| Keywords: | Sareke Cu deposit geological characteristics sandstone prospecting perspective Wuqia County Xinjiang |
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