吐哈盆地十红滩铀矿床成矿因素及成矿规律分析  

Analysis of metallogenic factors and regularities of Shihongtan uranium deposit in Turpan-Hami basin

作　　者：周伟 强利刚 陈宏斌 曹雷 

机构地区：[1]核工业二〇三研究所,咸阳712000

出　　处：《西部资源》2018年第2期197-199,201,共4页Western Resources

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.

关 键 词：吐哈盆地 十红滩铀矿床 成矿因素 成矿规律 

分 类 号：P619.14[天文地球—矿床学]