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中国海相含铀沉积建造分布与铀成矿分析
引用本文:蔡煜琦,宋继叶,虞航,姚春玲,朱鹏飞.中国海相含铀沉积建造分布与铀成矿分析[J].国外铀金地质,2010(4):187-194.
作者姓名:蔡煜琦  宋继叶  虞航  姚春玲  朱鹏飞
作者单位:[1]核工业北京地质研究院,北京100029 [2]东华理工大学,江西抚州344000
摘    要:中国海相含铀沉积建造分布非常广泛,产有重要的碳硅泥岩型铀矿床(点)。文章较为详细阐述了上震旦统、下寒武统、中—下志留统、中—上泥盆统、下石炭统和上二叠统海相含铀沉积建造类型及分布;利用全国1∶2 500000地质图数据库,编制了各时期海相含铀建造分布图,分析了海相含铀沉积建造与铀成矿的关系。

关 键 词:海相  含铀沉积建造  铀成矿

Analysis on the distribution of marine uranium-bearing sedimentary formation and uranium metallogenesis in China
Authors:CAI Yu-qi  SONG Ji-ye  YU Hang  YAO Chun-ling  ZHU Peng-fei
Institution:1.Beijing Research Institute of Uranium Geology,Beijing 100029,China; 2.East China Institute of Technology,Fuzhou,Jiangxi 344000,China)
Abstract:Marine uranium-bearing sedimentary formation distributes quite widely in China,and hosts the important carbonaceous-siliceous-argilaceous rock uranium deposits(occurrences).Marine uranium-bearing sedimentary formation in Upper Sinian,Lower Cambrian,Middle-Lower Silurian,Middle-Upper Devonian,Lower Carboniferous and Upper Permian is elaborated more detailedly in their types and distribution in China.With the 1:2 500 000 scaled geological map database,the distribution of marine uranium-bearing formation in the different periods and phases is drawn up and analyzed for their relationship to uranium metallogenesis.
Keywords:marine  uranium-bearing sedimentary formation  uranium metallogenesis
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