| 河南潢川盆地冯楼砂岩型铀矿点成矿地质条件分析 |
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| 引用本文： | 黄宏业,范少云,翦勋平,曹晓满.河南潢川盆地冯楼砂岩型铀矿点成矿地质条件分析[J].铀矿地质,2004,20(1):23-28. |
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| 作者姓名： | 黄宏业 范少云 翦勋平 曹晓满 |
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| 作者单位： | 核工业230研究所,湖南,长沙,410011 |
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| 摘 要： | 本文以水成铀矿理论为依据 ,通过对冯楼铀矿点的构造、岩性岩相、古气候特征以及后生改造、铀源、水文地质等条件进行分析 ,指出冯楼矿点为与火山岩建造有关的层间氧化带砂岩型铀矿 ,为在我国中部地区进一步寻找可地浸砂岩型铀矿提供了线索和可以借鉴的依据。
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| 关 键 词： | 冯楼铀矿点 层间氧化带 砂岩型铀矿 |
| 文章编号： | 1000-0658(2004)01-0023-06 |
| 修稿时间： | 2003年3月2日 |
Analysis on metallogenic-geologic condition of Fenglou sandstone-type uranium occurrence,Huangchuan basin,Henan province |
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| HUANG Hong-ye,FAN Shao-yun,JIAN Xun-ping,CHAO Xiao-man.Analysis on metallogenic-geologic condition of Fenglou sandstone-type uranium occurrence,Huangchuan basin,Henan province[J].Uranium Geology,2004,20(1):23-28. |
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| Authors: | HUANG Hong-ye FAN Shao-yun JIAN Xun-ping CHAO Xiao-man |
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| Abstract: | Based on the theory of hydrogenic uranium deposit,by analyzing the structrual,lithology-lithofacies,paleoclimatic features,as well as epigenetic reworking,uranium source,and hydrogeologic conditions,authors of this paper suggest that Fonglou uranium occurrence is of interlayer oxidation zone sandstone-type uranium occurrence associated with volcanic formation.This conclusion provides clues and bases for the further prospecting for in-situ leachable sandstone-type uranium deposits in the central area of China. |
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| Keywords: | Feonglou uranium occurrence interlayer oxidation zone sandstone-type uranium deposit |
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