| 郴州—钦州铀成矿带南西段铀成矿条件及成矿潜力分析 |
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| 引用本文： | 李小英.郴州—钦州铀成矿带南西段铀成矿条件及成矿潜力分析[J].国外铀金地质,2010(3):144-148. |
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| 作者姓名： | 李小英 |
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| 作者单位： | 广西壮族自治区307核地质大队,广西贵港537100 |
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| 摘 要： | 郴州—钦州铀成矿带南西段是一条多次活动的构造-岩浆活动带,灵山—藤县、博白—岑溪断裂带呈NE向贯穿该成矿带。两条断裂带控制了岩体、中新生代盆地及铀矿床、矿点的分布。综合分析铀成矿条件及成矿潜力表明：该成矿带成矿条件有利,成矿潜力较大,有助于老矿床的扩大和找到新铀矿床。
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| 关 键 词： | 郴州—钦州铀成矿带南西段 成矿条件 成矿潜力 |
Analysis on uranium metallogenic condition and prospecting potential of southwestern segment of Chenzhou-Qinzhou uranium mineralization belt |
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| Authors: | LI Xiao-ying |
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| Institution: | LI Xiao-ying(Guangxi Nuclear Geological Party No.307,Guigang,Guangxi 537100,China) |
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| Abstract: | The southwestern segment of Chenzhou-Qinzhou uranium mineralization belt is a multi stage activities belt of structure-magmatism.The NE strike Linshan-Tengxian and Bobai-Cenxi fracture zones run through the metallogenic belt and control the distribution of pluton,Meso-Cenozoic basin and uranium deposits and occurrences.Comprehensive analysis on uranium metallogenic condition indicates that this metallogenic belt is favorable for uranium metallogenic condition and has great resource potential which is helpful to expand old deposits and discover new deposits. |
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| Keywords: | southwestern segment of Chenzhou-Qinzhou uranium metallogenic belt metallogenic condition metallogenic potential |
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