新疆三塘湖盆地水文地质条件及铀成矿前景分析

摘要

Santanghu basin is an infiltration depression basin with forward direction hydrogeological and hydrogeochemical zonation. The basin has a well developed aquifer and favorable mud-sand-mud pattern and abundant uranium source. The distribution pattern of uranium in the ground water is favorable for the precipitation and enrichment of uranium in transitional part of redox zone.%新疆三塘湖盆地是具有正向水文地质和水文地球化学分带的渗-型坳陷盆地,区内含水层发育良好,具有较好的泥-砂-泥结构模式,盆地铀源丰富,地下水中铀元素的分布规律有利于其在氧化还原过渡带中沉积富集,具有较好的铀成矿前景.