松辽盆地东南缘地浸砂岩型铀矿成矿条件分析

Abstract

Abstract: The analyses of the sedimentary facies, rock geochemistry and reformation after the sedimentation from the Upper Cretaceous Quantou Formation to Nenjiang Formation indicate that the beneficial sandbodies of the uranium deposit are mainly Quantou Formation’s braided channel and Qingshankou Formation’s delta sandstone types. By summarizing and analyzing the geological setting, uranium source, paleoclimate, hydrology, lithologiclithofacies conditions in the region, it is indicated that the Quantou Formation in Fanjiatun-Jiutai area and the Qingshankou Formation in Yangdachenzi area are potential metallogenic prospective areas for insitu leachable sandstone type uranium deposit in the region, which develop braided channel or delta marginal sandstones, and possess favorable forming conditions of interlayer oxidation zone, and constituting supply-passage-discharge system of abundant uranium source.

Key words: Songliao Basin, Upper Cretaceous, suti leachable sandstone type uranium deposit, metallogenic condition

CLC Number:

P619.14

YU Wen-bin, DONG Qing-shui, ZOU Ji-bin, FENG Ben-zhi. Analysis of Metallogenic Conditions of InSitu Leachable Sandstone Type Uranium Deposit in the Southeastern Margin of Songliao Basin[J].J4, 2006, 36(04): 543-548.

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Analysis of Metallogenic Conditions of InSitu Leachable Sandstone Type Uranium Deposit in the Southeastern Margin of Songliao Basin