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《东华理工学院学报》 2005-01
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Subsequent Transformation and Evolution of Ore Bearing Structure in Erlian

LIU Wu-sheng~(1,2), LIU Jin-hui~1, WANG Zheng-bang~2, XIE You-xin~2(1.East China Institute of Technology, Fuzhou, JX 344000, China; 2.Beijing Research Institute of Uranium Geology, Beijing 100029, China)  
According to the analysis of the historic geology, tectonic movement and deposition characteristics in Erlian basin, its subsequent transformation can be divided into four stages, and each stage has different characteristics. They are late Cretaceous epoch stage(K_2), Palaeocene-Eocene epoch stage(E_(1—2)), Oligecene-Miocene epoch stage(E_3—N_1), and Paliocene-Quaternary period stage(N_2—Q). Then according to paleostructure, paleohydrogeologic map and paleoclimate, subsequent transformation of cap rock of each stage is also separated into two basic types: deoxidational and oxidizational type. for the first type, gas-oil area, migratory direction area of reducing medium and area presenting subsequent transformation in reducing environment are divided; for the another one, groundwater bearing oxygen and uranium migratory direction and interlaminar pressure water migratory direction are offered. What have been doing above have actual meanings for evaluating uranium metallogenesis of Erlian basin.
【Fund】: 内蒙-东北区地 1 /250万系列编图与成矿预测(地D0101)
【CateGory Index】: P542.2
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