| 岳阳市某地铀矿化特点及成因 |
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| 引用本文： | 李光明.岳阳市某地铀矿化特点及成因[J].湖南地质,1997,16(3):171-174. |
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| 作者姓名： | 李光明 |
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| 作者单位： | 岳阳楼区矿管办 |
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| 摘 要： | 铀矿产于上震旦统陡山沱组和下寒武统水井沱组中，含矿层为含黄铁矿碳泥质岩层，工业铀矿体赋存在层间挤压破碎带内，属同生沉积后生淋滤叠加复成矿床。
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| 关 键 词： | 成矿特点 铀矿床 矿化 |
Mineralization Feature of A Certain Uranium Deposit and Its Genesis in Yueyang City |
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| Li GuangmingThe Management Office of Mineral Resources of Yueyanglou Distract.Mineralization Feature of A Certain Uranium Deposit and Its Genesis in Yueyang City[J].Hunan Geology,1997,16(3):171-174. |
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| Authors: | Li GuangmingThe Management Office of Mineral Resources of Yueyanglou Distract |
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| Institution: | Li GuangmingThe Management Office of Mineral Resources of Yueyanglou Distract |
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| Abstract: | Uranium deposits occurs in Doushantuo formation of the upper series of Sinian system and Shuijingtuo formation of the lower series of Cambrian system.The ore bearing beds are pyrite bearing argillite.The industrial uranium orebody occurs in the interlayer compressional fracture zone.These deposits are composite,initially formed by syngenetic sedimentary and superimposed by epigenetic leaching. |
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| Keywords: | uranium deposit mineralization feature Yueyang city |
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