| 贵东岩体花岗岩中晶质铀矿的特征及其找矿意义 |
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| 引用本文： | 张成江.贵东岩体花岗岩中晶质铀矿的特征及其找矿意义[J].成都理工大学学报(自然科学版),1990(3). |
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| 作者姓名： | 张成江 |
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| 作者单位： | 成都地质学院三系 |
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| 摘 要： | 本文系统地研究了贵东岩体产铀矿与非产铀矿花岗岩中晶质铀矿的标型特征。据研究结果,贫钍晶质铀矿的含量高是产铀矿花岗岩的基本特征,其晶质铀矿的强烈溶蚀现象是铀活化转移的直接证据,可以将其作为寻找铀矿的标志之一。
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| 关 键 词： | 晶质铀矿 标型特征 找矿意义 花岗岩 |
THE FEATURES OF URANINITE IN GUIDONG GRANITE COMPLEX AND ITSSIGNIFICANCE TO SEARCH FOR URANIUM DEPOSIT |
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| Zhang Chengjiang.THE FEATURES OF URANINITE IN GUIDONG GRANITE COMPLEX AND ITSSIGNIFICANCE TO SEARCH FOR URANIUM DEPOSIT[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1990(3). |
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| Authors: | Zhang Chengjiang |
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| Institution: | Zhang Chengjiang |
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| Abstract: | The typomorphic features of uranium bearing and non-uranium granites inGuidong granite complex have been studied systematically. It has been proved that a largeamount of uraninite with lower thorium content is an important characteristic ofuranium mineralization granite, and that the strong corrosion or uraninite is one of the markto search for uranium deposit in this area. |
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| Keywords: | uraninite typomorphic feature significance to search for uranium deposit granite |
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