摘要
本文通过对钱家店凹陷姚家组地球化学环境的研究,把该区地化环境划分了原生氧化、原生还原、后生还原及后生氧化四种类型,总结了姚家组地化环境的变化与铀成矿的关系。
This paper studies the geochemical environment of Yaojia Fm in the Qianjiadian Basin,The environment of the area was divided into four types: primary oxidation, original reduction, reconstituted and postnatal oxidation,The relationship between the changes of the geochemical environment and uranium mineralization was summarized.
出处
《世界有色金属》
2017年第14期288-289,共2页
World Nonferrous Metals
基金
中国地质调查局北方中新生代盆地及华东南铀矿远景区地质矿产调查"松辽盆地东部九台-双城地区铀矿资源调查评价"(编号:12120115017001)资助