| 竹山下铀矿床成矿过程探讨 |
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| 引用本文： | 胡宝群,徐达忠.竹山下铀矿床成矿过程探讨[J].矿产与地质,1999,13(4):222-226. |
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| 作者姓名： | 胡宝群 徐达忠 |
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| 作者单位： | 华东地质学院,江西,临川,344000 |
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| 摘 要： | 对竹山下铀矿床中蚀变糜棱岩的矿物成分进行了研究，发现了一种新型Ｕ－Ｗ共生的蚀变糜棱岩型铀矿床，铀矿物主要是晶质铀矿；指出相应的成矿作用为燕山早期（１６５×１０６ａ±）气热高温热液铀成矿作用。
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| 关 键 词： | 铀矿床 蚀变糜棱岩 晶质铀矿 白钨矿 竹山下 |
| 修稿时间： | 1998年8月29日 |
STUDY ON THE MINERALIZATION PROCESS OF ZHUSHANXIA URANIUM DEPOSIT |
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| Hu Baoqun,Xu Dazhong.STUDY ON THE MINERALIZATION PROCESS OF ZHUSHANXIA URANIUM DEPOSIT[J].Mineral Resources and Geology,1999,13(4):222-226. |
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| Authors: | Hu Baoqun Xu Dazhong |
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| Abstract: | On the basis of studying the mineral composition of altered mylonite in zhushanxia uranium deposit,a new type of altered mylonite uranium deposit (U-W coexisting) has been found,and uranium exists as uraninite.It is concluded that the relative mineralization is pneamatohydrothermal uraniummineralization in early Yanshannian stafe (165106a). |
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| Keywords: | uranium deposit altered mylonite uraninite scheelite zhushanxia |
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