| 华南中新生代构造-岩浆活动驱动机制与铀成矿研究进展 |
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| 引用本文： | 王正庆,管太阳,林子瑜,冯志刚,谢焱石,陈亮.华南中新生代构造-岩浆活动驱动机制与铀成矿研究进展[J].华东地质学院学报,2013(4):349-356. |
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| 作者姓名： | 王正庆 管太阳 林子瑜 冯志刚 谢焱石 陈亮 |
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| 作者单位： | [1]南华大学核资源与核燃料工程学院,湖南衡阳421001 [2]中钢矿业开发有限公司,北京100080 [3]东华理工大学地球科学学院,江西南昌330013 |
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| 基金项目： | 湖南省教育厅项目“基于3s技术的诸广铀矿集区构造-花岗岩时空特征及其与铀成矿的关系”（10CIJ52）;中国核工业地质局项目“桃山一诸广成矿带铀成矿系统与勘查战略选Ⅸ”（2007YGD01） |
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| 摘 要： | 华南地区大规模金属成矿作用主要发生在中生代，区内的铀成矿作用明显不同于其它金属的成矿作用，如成矿时代上从中生代延续到新生代、矿岩时差大、铀矿聚集分布、铀源及矿化剂具慢源性等。基于众多铀成矿理论，从构造一岩浆活动的驱动力与铀成矿的关系出发，系统总结华南中新生代构造一岩浆活动与铀成矿的关系，认为当前华南铀成矿的动力学观点有四个，即构造体制转换铀成矿观、热点（地慢柱）铀成矿观、幔汁活动铀成矿观、原地重熔铀成矿观。
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| 关 键 词： | 华南 中新生代 构造-岩浆活动 驱动机制 铀成矿 |
Driving Mechanism of Structure-magmatic Activity and Uranium Mineralization of Mesozoic and Cenozoic,South China |
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| WANG Zheng-qing GUAN Tai-yang,LIN Zi-yu,FENG Zhi-gang XIE Yan-shi CHEN Liang.Driving Mechanism of Structure-magmatic Activity and Uranium Mineralization of Mesozoic and Cenozoic,South China[J].Journal of East China Geological Institute,2013(4):349-356. |
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| Authors: | WANG Zheng-qing GUAN Tai-yang LIN Zi-yu FENG Zhi-gang XIE Yan-shi CHEN Liang |
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| Institution: | 1. School of Nuclear Resources and Nuclear Fuel Engineering, University of South China, Hengyang, Hunan, 421001 ;2. Sinosteel Mining Co. Ltd, Beijing, 100080 ;3. College of Geoscience, East China Institute of Technology, Nanchang, Jiangxi, 330013 ) |
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| Abstract: | Large-scale mineralization in South China mainly occurs in Mesozoic. However, uranium mineralization in this area lasts from Mesozoic to Cenozoic with the features as follows ： （ Ⅰ ） the time gap of diagenesis and ura nium mineralization is large; （ Ⅱ ） the large uranium deposits are aggregated distribution; （Ⅲ）the uranium source and the mineralizer is mantle-derived; （IV） the uranium exploration has no great breakthrough for a long time. This paper takes the relation between the driving force of strueture-magmatic activity and uranium minerali zation as a starting point, combines with many uranium mineralization theories and studies the relation between structure-magmatic activity and uranium mineralization in South China systematically in Mesozoic and Cenozoic. According to the study, the relation between structure-magmatic activity and uranium mineralization in Mesozoic and Cenozoic of South China can be divided into four categories ： Tectonic regime transformation uranium minerali zation view, Hot spot （mantle plume） uranium mineralization view, Mantle ichor activity uranium mineralization view and ln-situ melting uranium mineralization view. |
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| Keywords: | South China Mesozoic and Cenozoic structure-magmatic activity driving mechanism uraniummineralization |
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