| 华南古岩溶型铀矿床矿物学及其矿床成因意义 |
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| 引用本文： | 闵茂中,王湘云,沈保培,文光斗,樊涛,江仪,张国文,黎旭畅.华南古岩溶型铀矿床矿物学及其矿床成因意义[J].中国岩溶,1997,16(3):251-258. |
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| 作者姓名： | 闵茂中 王湘云 沈保培 文光斗 樊涛 江仪 张国文 黎旭畅 |
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| 作者单位： | 南京大学地球科学系,南京大学地球科学系,核工业中南３０３大队,核工业中南３０３大队,核工业中南３０３大队,核工业中南３０７大队,核工业中南３０７大队,核工业中南３０７大队 |
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| 摘 要： | 华南古岩溶铀矿床的矿物学特征为：表生矿物发育，原生成矿矿物少见；矿化脉体几乎没有；矿石中铀主要呈吸附状态，其次呈显微和超显微沥青铀矿存在，与古岩溶有关铀矿床则出现典型低中温热液矿物组合，矿化脉体期次分明，矿石中铀基本呈可见状沥青矿存在，沥青铜矿具有有热液成因标型。鉴于该类矿床成矿前主岩溶为冷水成因，而热液成矿流体是与岩溶无关的体系，故属古岩溶热液叠造成矿。
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| 关 键 词： | 古岩溶 铀矿床 矿物学 矿床成因 |
MINERALOGY OF PALEOKARST-HOSTED URANIUM DEPOSITS AND ITS GENETIC
SIGNIFICATIONS IN SOUTH CHINA |
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| Min Maozhong,Wang Xiangyun,Shen Baopei,Wen Guangdou,Fan Tao,Jiang Yi,Zhang Guowen and Li Xuchang.MINERALOGY OF PALEOKARST-HOSTED URANIUM DEPOSITS AND ITS GENETIC
SIGNIFICATIONS IN SOUTH CHINA[J].Carsologica Sinica,1997,16(3):251-258. |
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| Authors: | Min Maozhong Wang Xiangyun Shen Baopei Wen Guangdou Fan Tao Jiang Yi Zhang Guowen and Li Xuchang |
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| Institution: | Department of Earth Sciences, Nanjing University,Department of Earth Sciences, Nanjing University,N o. 303 Geological Party , Bureau of Geology and Exploration of Centra l-South China,N o. 303 Geological Party , Bureau of Geology and Exploration of Centra l-South China,N o. 303 Geological Party , Bureau of Geology and Exploration of Centra l-South China,N o. 307 Geological Party , Bureau of Geology and Exploration of Central-South China,N o. 307 Geological Party , Bureau of Geology and Exploration of Central-South China and N o. 307 Geological Party , Bureau of Geology and Exploration of Central-South China |
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