| 滇西可地浸砂岩型铀矿特征,成因类型及成矿模式 |
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| 引用本文： | 陈友良.滇西可地浸砂岩型铀矿特征,成因类型及成矿模式[J].铀矿地质,1998,14(4):193-199. |
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| 作者姓名： | 陈友良 |
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| 作者单位： | 西南地质局280研究所!四川广汉，618300 |
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| 摘 要： | 文阐述了滇西新生代盆地可地浸砂岩型铀矿的矿床特征，讨论了铀矿床的成因类型，认为属“潜水顺层氧化带型”铀矿床。根据铀矿床的形成机制，对滇西地区新生代盆地的砂岩型铀矿成矿模式进行了探讨。
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| 关 键 词： | 滇西地区 铀矿特征 成因类型 成矿模式 |
DISCUSSION ON CHARACTERISTICS, GENESIS TYPE AND GENETIC MODEL OF IN-SITU LEACHABLE SANDSTONE TYPE URANIUM DEPOSITS IN WESTERN YUNNAN |
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| Chen Youliang.DISCUSSION ON CHARACTERISTICS, GENESIS TYPE AND GENETIC MODEL OF IN-SITU LEACHABLE SANDSTONE TYPE URANIUM DEPOSITS IN WESTERN YUNNAN[J].Uranium Geology,1998,14(4):193-199. |
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| Authors: | Chen Youliang |
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| Abstract: | This paper expounds the characteristics of in-situ leachable sandstone type uranium deposits in Cenozoic basins in western Yunnan, discusses the genesis type of uranium deposits, and attributes them to phreatic interlayered oxidation zone. A genetic model for the sandstone type uranium deposits in Cenozoic basins of western Yunnan is proposed. |
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| Keywords: | Western Yunnan Characteristics of uranium deposits Genesis type Genetic Model |
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