| 湖南明月峰铀矿深源性及控矿因素探讨 |
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| 引用本文： | 林锦荣,蔡根庆,刘建桥.湖南明月峰铀矿深源性及控矿因素探讨[J].地质论评,1999,45(7):756-760. |
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| 作者姓名： | 林锦荣 蔡根庆 刘建桥 |
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| 作者单位： | 核工业北京地质研究院,100029 |
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| 摘 要： | 本文通过对明月峰地区铀成矿条件综合分析，认为该区铀矿成矿热液具深源性，而非岩浆期后热液，也非花岗岩蚀变浸出；总结出该区铀成矿控矿因素，即铀成矿的构造环境、岩石蚀变组合及元素群体组合。
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| 关 键 词： | 铀矿 拆离构造 控矿因素 湖南 |
Study of Uranium from Deep Crust or Mantle and Ore controlling Factors in Mingyuefeng Area, Hunan |
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| Lin Jinrong,Cai Genqing and Liu Jianqiao.Study of Uranium from Deep Crust or Mantle and Ore controlling Factors in Mingyuefeng Area, Hunan[J].Geological Review,1999,45(7):756-760. |
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| Authors: | Lin Jinrong Cai Genqing and Liu Jianqiao |
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| Institution: | Beijing Research Institute of Uranium Geology,Beijing,100029 |
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| Abstract: | Based on comprehensive analysis of uranium mineralization, it is proposed in thi s paper that or eforming hydrothermal solutions originated from deep crust or mantle in the Min gyuefeng ar ea, and they are not postmagmatic hydrothermal or generated from alterat ed granite. Thi s paper also summarizes favorable structural settings and association charact eristics of wall rock alteration and elements association of uranium mineraliza t ion. |
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