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地球科学进展  2014, Vol. 29 Issue (12): 1372-1382    DOI: 10.11867/j.issn.1001-8166.2014.12.1372
综述与评述     
中国东部中生代流纹岩—粗面岩组合与热液型铀矿研究新进展
巫建华1, 解开瑞2, 吴仁贵2, 郭国林1, 刘帅1
1.东华理工大学核资源与环境国家重点实验室培育基地,江西 南昌 330013; 2.东华理工大学地球科学学院,江西 南昌 330013
The New Progress in the Study of Mesozoic Rhyolite-Trachyte Assemblage and Hydrothermal-type Uranium Mineralization in Eastern China
Wu Jianhua1, Xie Kairui2, Wu Rengui2, Guo Guolin1, Liu Shuai1
1.State Key Laboratory Breeding Base of Nuclear Resources and Environment, East China Institute of Technology, Nanchang 330013, China; 2.College of Earth Science, East China Institute of Technology, Nanchang 330013, China
 全文: PDF(2755 KB)  
摘要:

中国东部中生代火山活动强烈,热液型铀矿分布广泛。空间上,自北而南可划分出大兴安岭、小兴安岭—张广才岭、冀北—辽西、长江中下游、赣杭、武夷山区和东南沿海7个火山岩带和满洲里—额尔古纳、扎兰屯、伊春、沽源—红山子、青龙—兴城、庐枞—栖霞、赣杭和武夷山8个铀成矿带或铀成矿远景带;时间上,从早到晚可划分出早侏罗世—中侏罗世早期、中侏罗世晚期—晚侏罗世早期、早白垩世早期、早白垩世中期、早白垩世晚期和晚白垩世早期6个不同时期的岩石组合,其中早白垩世早期高钾钙碱性流纹岩—碱性粗面岩组合与已知铀矿关系密切,高钾钙碱性流纹岩能为浅成低温成矿系统提供铀,碱性粗面岩可能是深源高温成矿系统富铀碱性成矿流体的开路先锋。

关键词: 流纹岩&#x02014粗面岩组合中国东部热液型铀矿早白垩世早期    
Abstract:

The most intense area of Mesozoic volcanism and main region of hydrothermal-type uranium deposits is located in Eastern China. From the northern to the southern part, it can be divided into seven volcanic belts of Great Xing’an Range, Lesser Xing’an-Zhangguangcai Ranges, Northern Hebei-Western Liaoning, the Lower Yangtze Region, Ganhang areas, Wuyi Mountain areas,the Southeast Coastal areas, five uranium metallogenic belts of Guyuan-Hongshanzi, Qinglong-Xingcheng, Luzong-Qixia, Ganhang, Wuyi Mountain, and Three uranium metallogenic perspective belts of Manzhouli-Erguna, Zhalantun, Yichun. The volcanism of all these volcanic belts can be subdivided into six stages: The Early Jurassic to early Middle Jurassic, late Middle Jurassic to early Late Jurassic, early Early Cretaceous, middle Early Cretaceous, late Early Cretaceous and early Late Cretaceous. High-K calc-alkaline rhyolite-alkali trachyte rock assemblage of the early Early Cretaceous has a close connection with the explored uranium deposits. High-K calc-alkaline rhyolites have high content of uranium, and can provide the epithermal ore forming system with uranium; Alkali trachyte associated with mantle-derived magmatism can provide alkaline ore-forming fluid of rich uranium for deep temperature mineralizing system or act as pioneers of alkaline ore-forming fluid of rich uranium.

Key words: Rhyolite-trachyte assemblage    Hydrothermal-type uranium deposits    Eastern China.    Early Early Cretaceous
收稿日期: 2014-05-23 出版日期: 2014-12-20
:  P619.14  
基金资助:

国家自然科学基金项目“沽源—红山子铀成矿带流纹岩—粗面岩组合的成因及其与铀成矿的关系”(编号:41372071); 中国核工业集团公司项目“中国中—新生代铀成矿作用研究”(编号:中核地计[2008]74号)资助

作者简介: 巫建华(1960-),男,江西宜丰人,教授,主要从事火山地质学与铀矿地质学研究
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引用本文:

巫建华, 解开瑞, 吴仁贵, 郭国林, 刘帅. 中国东部中生代流纹岩—粗面岩组合与热液型铀矿研究新进展[J]. 地球科学进展, 2014, 29(12): 1372-1382.

Wu Jianhua, Xie Kairui, Wu Rengui, Guo Guolin, Liu Shuai. The New Progress in the Study of Mesozoic Rhyolite-Trachyte Assemblage and Hydrothermal-type Uranium Mineralization in Eastern China. Advances in Earth Science, 2014, 29(12): 1372-1382.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2014.12.1372        http://www.adearth.ac.cn/CN/Y2014/V29/I12/1372

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