摘要
吐哈盆地十红滩铀矿床为一典型的层间氧化带砂岩型铀矿床。通过对其地质特征研究分析,认为其形成及其展布主要受到层间氧化带、区域构造、沉积体系及沉积层位等成矿作用的控制,在分析这些成矿作用的基础上,总结出了十红滩铀矿床的成矿规律。
The Shihongtan uranium deposit is a typical interlayer oxidation zone sandstone-type uranium deposit.Based on the study of geologic characteristics, authors suggest that the ore-formation and distribution is mainly controlled by metallogenic factors, such as interlayer oxidation zone, regional structure, sedimentary system, sedimentary horizon etc.On the basis of analyzing these sedimentary, sunmmed up the metallogenic regularities of Shihongtan uranimn deposit.
出处
《西部资源》
2018年第2期197-199,201,共4页
Western Resources
关键词
吐哈盆地
十红滩铀矿床
成矿因素
成矿规律
Turpan-Hami basin
Shihongtan uranium deposit
metallogenic factors
metallogenic regularities
