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《Acta Petrologica Sinica》 2017-05
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Spatial-temporal distribution of Mesozoic igneous rock and their relationship with hydrothermal uranium deposits in eastern China

WU JianHua;GUO GuoLin;GUO JiaLei;ZHANG Qi;WU RenGui;YU DaGan;State Key Laboratory Breeding Base of Nuclear Resources and Environment,East China University of Technology;Collage of Earth Science,East China University of Technology;Institute of Geology and Geophysics,Chinese Academy of Sciences;  
It was characterized by extensive development of Mesozoic magmatism and widely distributed a large number of hydrothermal uranium deposits in eastern China.According to the spatial distribution of igneous rocks and uranium deposits from north to the south,it can be divided into 8 volcanic intrusive belts of Great Xing'an Range,Lesser Xing'an-Changbaishan,northern Hebeiwestern Liaoning,northern Dabieshan,the Middle-Lower Reaches of Yangtze River,southeastern Yangtze Block,Wuyi-yunkai areas,the Southeast Coastal areas,and 9 hydrothermal uranium metallogenic belts of Guyuan-Hongshanzi,Qinglong-Xingcheng,LuzongQixia,Ganhang,Wuyi Mountain,Taoshan-Zhuguang,Chenzhou-qinzhou,the Middle Hunan Province,and 5 uranium metallogenic perspective zones of Manzhouli-Erguna,Zhalantun,Yichun,Jinzhai,Tianmo Mountain.The temporal distribution of the magmatic activity of those volcanic intrusive belts can be subdivided into 8 stages,such as 250~233 Ma,228~205 Ma,195~175 Ma,165~150Ma,145~130 Ma,126~115 Ma,110~100 Ma,97~80 Ma,which can also be classified two-phase metallogenic systems,early stage characterized by high temperature and deep source origin,and late stage with low temperature and shallow origin.Granite type hydrothermal uranium deposits can be divided into 11 ore deposit types,and volcanic type hydrothermal uranium deposits can be divided into 15 ore deposit types.Exploration results show that granite hydrothermal type uranium deposit has a close relationship with specific periods of magmatite activity,but irrelevant with lithology and lithofacies of igneous rocks.Granite type hydrothermal uranium deposits are mainly existed in the Triassic granite,and that those volcanic type hydrothermal uranium deposits are mainly hosted in inner and outer contact zones of the early Early Cretaceous volcanic rocks.
【Fund】: 国家自然科学基金项目(41372071);; 中国核工业集团公司项目(中核地计[2008]74号)联合资助
【CateGory Index】: P588.1;P619.14
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【Citations】
Chinese Journal Full-text Database 10 Hits
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【Co-citations】
Chinese Journal Full-text Database 2 Hits
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6 Liu Jinlong;Sun Fengyue;Lin Bolei;Wang Guan;Xu Qinglin;Ao Cong;College of Earth Sciences,Jilin University;;Geochronology and Geochemistry of Trachyandesite of Naozhi Gold Deposit in Yanbian Region,Southern Jinlin Province and Its Geological Significance[J];吉林大学学报(地球科学版);2015-05
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8 ZHONG Zhi-fei;WU Jian-hua;College of Earth Science,East China Institute of Technology;State Key Laboratory Breeding Base of Nuclear Resources and Environment,East China Institute of Technology;;Geochronology,Geochemical Characteristics and Genesis significance of Adakitic Trachyte in Huichang Basin,Jiangxi Province[J];东华理工大学学报(自然科学版);2015-02
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