| 塔里木盆地北缘塔里克铀矿点矿化成因及其找矿方向 |
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| 引用本文： | 阿种明,王军堂,杨小强,罗星刚.塔里木盆地北缘塔里克铀矿点矿化成因及其找矿方向[J].国外铀金地质,2008(3):139-142. |
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| 作者姓名： | 阿种明 王军堂 杨小强 罗星刚 |
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| 作者单位： | 核工业216大队,新疆乌鲁木齐830011 |
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| 摘 要： | 分析了塔里克铀矿点区域地质背景、矿点地质概况、含矿岩系和铀矿化特征及其成因类型，认为铀矿化成因属于层间氧化带型，“倒卷状”铀矿化为构造隆升前形成的“古矿化”。通过分析铀矿化带走向延伸特征和地貌特征，指出了找矿远景地段。
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| 关 键 词： | 塔里克铀矿点 成因 找矿方向 |
Prospecting direction and the genesis of Talike uranium ore occurrence in the northern Tarim Basin |
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| Authors: | A Zhong-ming WANG Jun-tang YANG Xiao-qiang LUO Xing-gang |
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| Institution: | (Geologic Party No.216, CNNC, Urumqi, Xinjiang 830011, China) |
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| Abstract: | The regional geological setting, brief geological outline of the ore occurrence, ore-bearing rock series, features and genetic types of uranium mineralization of Talike uranium ore occurrence are analyzed. It is considered that the genesis of uranium mineralization belongs to the inter-layered oxidation zone type. The＇ Inverted roll-front＇ uranium mineralization is a＇ palaeo-mineralization＇ formed before the structural uplift. Prospective areas are pointed out by analyzing the strike extension of uranium mineralization zone and geomorphic features. |
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| Keywords: | Talike uranium ore occurrence genesis prospecting direction |
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