| 下庄矿田湖子地区缓倾斜铀矿体的特征及成矿模式探讨 |
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| 引用本文： | 吴继光,张辉仁,冯志军,韩思旭.下庄矿田湖子地区缓倾斜铀矿体的特征及成矿模式探讨[J].东华理工大学学报（自然科学版）,2011(4):339-344. |
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| 作者姓名： | 吴继光 张辉仁 冯志军 韩思旭 |
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| 作者单位： | 广东省核工业地质局二九三大队 |
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| 基金项目： | 中央地勘基金项目(2009441002) |
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| 摘 要： | 下庄矿田湖子地区的铀矿体主要赋存在6009号硅化断裂带及其上盘次级构造带内,铀矿化以硅化带型为主,铀矿体产状陡倾；由钻探工程揭露,新发现的缓倾斜铀矿体位于6009号硅化断裂带与黄陂—张光营辉绿岩带的交汇区域,且具有较好的连续性,铀矿体产状缓倾,产状55°～ 65°NW∠17°～25°,矿体严格受平缓断裂控制,呈多层状分...
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| 关 键 词： | 湖子地区 铀成矿类型 缓倾斜铀矿体 成矿模式 |
Characteristic of Gently Inclined Uranium Ore Body and Metallogenic Model of Huzi Area in Xiazhuang Ore Field |
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| WU Ji-guang,ZHANG Hui-ren,FENG Zhi-jun,HAN Si-xu.Characteristic of Gently Inclined Uranium Ore Body and Metallogenic Model of Huzi Area in Xiazhuang Ore Field[J].Journal of East China Institute of Technology(Natural Science Edition),2011(4):339-344. |
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| Authors: | WU Ji-guang ZHANG Hui-ren FENG Zhi-jun HAN Si-xu |
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| Institution: | (Geological Team 293 in Guangdong Province of the Nuclear Industrial Ministry,Guangzhou,GD 5108000,China) |
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| Abstract: | The uranium ore bodies are mainly forming in silicated fault belt of No.6009 and its top of sub-structure.The uranium mineralization is a silicated zone type.The uranium ore body discovered recently is located in the intersection of silicified fracture zones of No.6009 and dolerite zone of Huangpi-Zhangguangying.The ore body has a good continuity and attitude of 55°～65°NW∠17°～25°.Furthermore,the ore body is controlled by gentle fracture,and distributed with multi-layers.The discovery of blind uranium ore body with gentle tilt in deep provide possible to find large-midium scale uranium in Huzi. |
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| Keywords: | Huzi area uranium metallogenic types uranium ore body with gentle tilt metallogenic model |
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