| 潘湘和,何友宇,蒋国清,覃金宁,刘旭.某铀矿床稀土元素地球化学特征[J].南华大学学报(自然科学版),2014,28(4):40~43, 55.[PAN Xiang-he,HE You-yu,JIANG Guo-qing,QIN Jin-ning,LIU Xu.Geochemical Characteristics of REE in a Uranium Deposit[J].Journal of University of South China(Science and Technology),2014,28(4):40~43, 55.] |
| 某铀矿床稀土元素地球化学特征 |
| Geochemical Characteristics of REE in a Uranium Deposit |
| 投稿时间：2014-07-20 |
| DOI： |
| 中文关键词: 铀矿床 稀土元素特征 稀土元素配分曲线 |
| 英文关键词:uranium deposit characteristics of REE REE distribution curve |
| 基金项目: |
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| 摘要点击次数: 799 |
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| 中文摘要: |
| 通过对某铀矿床各构造地球化学带的稀土元素特征参数和球粒陨石标准化配分曲线的分析和研究,结果表明此矿床矿石与岩浆岩有着相同的稀土元素特征,铀主要来自于矿区内富铀花岗岩岩体.稀土元素相关的特征值变化表明该矿床在成矿过程中,成矿环境从相对还原环境向相对氧化环境改变,成矿温度逐渐降低. |
| 英文摘要: |
| Analysis and research are based on REE geochemical parameters and chondrite-normalized REE distribution curve of each geochemical and tectonic belt in a uranium deposit.The results show that magmatite have the same characteristics of REE with ore in this deposit,and the uranium mainly come from the mining area granite which is rich in uranium.Variation of REE features show that metallogenic environment change from relatively reducing environment to relatively oxidizing conditions and the temperature of mineralization is decreased gradually in the mineralization. |
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