摘要
宝龙山铀矿床水文地质条件比较复杂,文章概括了该区含水层及隔水层的基本情况,着重分析了含矿含水层及其隔水顶板的特征,简述了其与铀成矿的关系。依据该区的水文地球化学特征,尤其是矿化度、水化学类型及铀含量分布规律,说明了区内地下水整体流向由西南向东北方向;西辽河及架玛吐、兴隆-协代花岗岩古隆起为地下水局部补给区,F3断裂、宝龙山剥蚀天窗及新开河为局部排泄区。
Hydrogeological condition of Baolongshan uranium deposit is quite complex,by sumarrizing the condition of aquifer and inpermiable layer with the focus on their roof feature,this article describes its relationship with uranium mineralization.Based on the study result of hydrogeochemical characteristics of this area such as of salinity,hydochemical type and the distribution of uranium content,the ground water was found flows from southwest to north east,and the uplift granite in Westliaohe and Jiamatu,Xinglong-xiedai are regarded as local recharge area,while F3 fracture,Baolongshan fenster and Xinkaiuhe are regarded as local discharge area.
出处
《铀矿地质》
CAS
CSCD
2015年第5期517-523,535,共8页
Uranium Geology
