摘要
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入型坳陷盆地,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。
Santanghu basin is an infiltration depression basin with forward direction hydrogeological and hydrogeochemical zonation. The basin has a well developed aquifer and favorable mudsandmud 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 Dart of redox zone.
出处
《铀矿地质》
CAS
CSCD
2012年第4期227-232,共6页
Uranium Geology
关键词
三塘湖盆地
水文地质条件
铀成矿前景
Santanghu basim hydrogeological conditiom uranium mineralization prospect