摘要
为了探讨六盘山盆地是否存在地浸砂岩型铀成矿的环境,从盆地地质背景、找矿目的层、铀矿化特征进行研究,重点对层间氧化带的铀成矿条件进行分析.结果表明,下白垩统和尚铺组、李洼峡组具有地浸砂岩型铀成矿前景.
In order to investigate whether there is an environment for situ leachable sandstone-type uranium mineralization in Liupanshan basin,the geological background and prospecting target layer and uranium mineralization characteristics were studied.The conditions of uranium mineralization of interlayer oxidation zone are analysis emphases.Results show that the prospect zone for situ leachable sandstone type uranium mineralization is Heshangpu Fm,Liwaxia Fm in Lower Cretaceous.
出处
《宁夏工程技术》
CAS
2013年第3期205-208,共4页
Ningxia Engineering Technology
关键词
六盘山盆地
铀矿化
成矿条件
地浸砂岩型铀矿
Liupanshan basin
uranium mineralization
conditions of mineralization
situ leachable sandstone type uranium deposit
