吐哈盆地十红滩铀矿床成矿因素及成矿规律分析
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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,summed up the metallogenic regularities of Shihongtan uranium deposit.
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,summed up the metallogenic regularities of Shihongtan uranium deposit.
引文
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[5]孙超.鄂尔多斯盆地北部大营铀矿床直罗组下段粘土矿物变化特征探讨[J].西部资源,2016(04):88-92.
[2]李占游,李保侠,邓小卫,等。新疆吐哈盆地十红滩铀矿床南矿带32~31勘探线地质普查报告[R].咸阳:核工业二〇三研究所,2002.
[3]权建平,徐高中,李卫红,等。十红滩砂岩型铀矿床成矿控制因素与成矿模式研究[J].铀矿地质,2006,22(1):10~16.
[4]傅成铭。吐哈盆地十红滩铀矿床控矿因素及找矿耙区研究铀矿地质[J].铀矿地质,2005,21(2):85~91.
[5]孙超.鄂尔多斯盆地北部大营铀矿床直罗组下段粘土矿物变化特征探讨[J].西部资源,2016(04):88-92.