库米什盆地木拉阿米特凹陷铀成矿水文地质条件分析  

Analysis on hydrogeological conditions of uranium formation in Mulaamite Sag in Kumux Basin

作　　者：王成渭[1] 陈黎昀[1] 王军堂[1] 

机构地区：[1]核工业216大队,新疆乌鲁木齐830011

出　　处：《世界核地质科学》2008年第1期30-34,共5页World Nuclear Geoscience

摘　　要：在综合分析资料的基础上,从基础地质条件出发,全面分析了木拉阿米特凹陷的水文地质条件、含水岩组特征、水文地球化学特征与层间氧化带及铀矿化的关系,初步认为库鲁克塔格山前地带具有较好的发育层间氧化带及铀矿化的前景。Based on the comprehensive analysis on the materials, hydrogeological conditions, features of water-bearing rock formation, relationship amoung the hydrogeochemical features and interlayer oxidation zone and uranium formation are analyzed from the point of view of basic geological conditions, it is preliminarily considered that Kuluketage fore-mountain zone has a good potential to develop the interlayer oxidation belt and uranium mineralization.

关 键 词：水文地质条件 水文地球化学特征 远景区段 

分 类 号：P619.14[天文地球—矿床学] P641.2[天文地球—地质学]