| 沽源盆地大官厂铀钼多金属矿床成矿机理及成矿预测 |
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| 引用本文： | 伍静,娄峰,李宏卫,肖成东,樊秉鸿,沈光银,薛清波.沽源盆地大官厂铀钼多金属矿床成矿机理及成矿预测[J].地学前缘,2011,18(1):133-140. |
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| 作者姓名： | 伍静 娄峰 李宏卫 肖成东 樊秉鸿 沈光银 薛清波 |
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| 作者单位： | 伍静,娄峰,李宏卫,Wu Jing,Lou Feng,Li Hongwei(中山大学,地球科学系,广东,广州,510275);肖成东,樊秉鸿,沈光银,薛清波,Xiao Chengdong,Fan Binghong,Shen Guangyin,Xue Qingbo(天津华北地质勘查总院,地质勘查总院,天津,300181) |
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| 基金项目： | 高等学校博士学科点基金 |
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| 摘 要： | 沽源火山盆地是中国华北地块北缘一条重要的铀钼多金属成矿带--燕辽成矿带的重要组成部分,长期以来受到地学界的广泛关注.由于该带矿床多数产于火山岩中,其成因一直被认为是与火山岩有关的矿床.文中根据花岗岩原地重熔理论及大官厂矿区地质、地球物理资料特征,提出大官厂矿区其下隐伏有花岗岩体,成矿作用主要与隐伏的花岗岩有关;同时分析...
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| 关 键 词： | 重熔界面 铀钼多金属矿床 大官厂 铀钼矿床 |
Mineralization mechanism of the Daguanchang U-Mo polymetallic deposit and its application in ore prospecting |
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| Wu Jing,Lou Feng,Li Hongwei,Xiao Chengdong,Fan Binghong,Shen Guangyin,Xue Qingbo.Mineralization mechanism of the Daguanchang U-Mo polymetallic deposit and its application in ore prospecting[J].Earth Science Frontiers,2011,18(1):133-140. |
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| Authors: | Wu Jing Lou Feng Li Hongwei Xiao Chengdong Fan Binghong Shen Guangyin Xue Qingbo |
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| Institution: | Wu Jing1,Lou Feng1,Li Hongwei1,Xiao Chengdong2,Fan Binghong2,Shen Guangyin2,Xue Qingbo2 1.Department of Earth Sciences,Sun Yat-Sen University,Guangzhou 510275,China2.North China Geological Exploration General Institute,Tianjin 300181,China |
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| Abstract: | The U-Mo polymetallic deposits located in the Guyuan volcanic basin in the northern rim of northern China terrain attract more and more attentions of geoscientists in China.The U-Mo polymetallic deposits were considered to have genetic relation to the ore-hosted volcanic rocks.On the basis of the in-situ-melting model of granite origin,together with geologic and geophysical features of the Daguanchang U-Mo polymetallic deposit,it is concluded that the Daguanchang U-Mo deposit was originated from the activit... |
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| Keywords: | remelting interface U-Mo polymetallic deposit ore genesis Daguanchang U-Mo deposit |
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