| 黄泥湖铀矿床地质特征及成因探讨 |
| |
| 引用本文： | 钟启龙,张运涛,张小平,童日发,郭树英,李志明,温圣奇.黄泥湖铀矿床地质特征及成因探讨[J].铀矿地质,2011(5):282-285. |
| |
| 作者姓名： | 钟启龙 张运涛 张小平 童日发 郭树英 李志明 温圣奇 |
| |
| 作者单位： | 江西省核工业地质局264大队;中国地质大学(武汉); |
| |
| 摘 要： | 文章从区域地质、岩浆岩、构造、热液蚀变和铀成矿地质特征等方面,系统阐述了黄泥湖铀矿床成矿条件和控矿因素,提出该矿床成矿经历了沉积成矿、火山作用热水叠加成矿和热液作用改造富集3个阶段的观点。在此基础上,总结出该区＂以砂岩为基础、凹沟是条件、热盖是关键、斑岩旁侧有好矿＂的铀矿找矿新思路,对区内火山盆地铀矿找矿工作具有实际指导意义。
|
| 关 键 词： | 黄泥湖铀矿床 沉积成矿 热液改造 |
Discussion on geologic feature and genesis of Huangnihu uranium deposit |
| |
| ZHONG Qi-long,ZHANG Yun-tao,ZHANG Xiao-ping,TONG Ri-fa,GUO Shu-ying,LI Zhi-ming,WEN Sheng-qi.Discussion on geologic feature and genesis of Huangnihu uranium deposit[J].Uranium Geology,2011(5):282-285. |
| |
| Authors: | ZHONG Qi-long ZHANG Yun-tao ZHANG Xiao-ping TONG Ri-fa GUO Shu-ying LI Zhi-ming WEN Sheng-qi |
| |
| Institution: | ZHONG Qi-long1,2,ZHANG Yun-tao1,ZHANG Xiao-ping1,TONG Ri-fa1,GUO Shu-ying1,LI Zhi-ming1,WEN Sheng-qi1(1.Geologic Party No.264,Jiangxi Provincial Geology Bureau for Nuclear Industry,Ganzhou,Jiangxi 341000,China,2.China University of Geoscince,Wuhan,Hubei 430000,China) |
| |
| Abstract: | The forming condition and controlling factors of Huangnihua uranium deposit in Xuwu,Jiangxi were discussed in regional geology setting,magatism,structure,hydrothermal alteration and uranium mineralization features,it was proposed that the formation of the deposit had exprienced three stages of sandstone deposition,superimposition of thermal water action from volcanism and uranium enrichment of hydrothermal reworking.The exploration idea was summarized assandstone with furrows is the base and volcanic covers... |
| |
| Keywords: | Huangnihu uranium deposit sedimentary mineralization hydrpthermal reworking |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
