| 王英稳,丁德馨.302矿床围岩蚀变与铀矿化的关系[J].南华大学学报(自然科学版),2007,21(3):33~36.[.The Study on Relation Between the Character of Wall - Rock Alteration and Uranium - Mineralization at No. 302 Uranium Deposit[J].Journal of University of South China(Science and Technology),2007,21(3):33~36.] |
| 302矿床围岩蚀变与铀矿化的关系 |
| The Study on Relation Between the Character of Wall - Rock Alteration and Uranium - Mineralization at No. 302 Uranium Deposit |
| 修订日期：2007-09-25 |
| DOI： |
| 中文关键词: 铀矿床 矿体 围岩蚀变 |
| 英文关键词:uranium deposit,ore body,wall-rock alteration |
| 基金项目: |
| 王英稳 丁德馨 |
| 南华大学核资源与安全工程学院 南华大学核资源与安全工程学院 湖南衡阳 中核韶关锦原铀业有限公司 广东仁化 湖南衡阳 |
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| 中文摘要: |
| 储广山花岗岩体受郯庐断裂系遂川——热水走滑断裂带控制,区内塘湾断裂及一系列北西向断裂带发育,构成有利的成矿构造结,其中发现多个大型、超大型的铀矿田和铀矿床,其铀矿化受多因素控制,以构造、围岩和岩浆-热液活动为主,在时间上、空间上具有独特的展布规律,通过对该矿床的岩石、构造、矿体和围岩蚀变特征的分析,探讨了围岩蚀变与铀矿成矿的关系,为同类地区的找矿提供了依据. |
| 英文摘要: |
| The granite body in Chuguangshan is controlled by Tanlu fault system Suichuang-Reshuizoufa fault system,Quneitangwan fault zone and a series of north-west fault zones are developed to form favorable structural knot.Many large-scale and super large-scale uranium field and uranium deposit have been found where uranium mineralization is controlled by many factors,mainly made up of rock fabric,wall-rock and magma-hydrotherm activity.The spreading rules are particular in time and space distributing.The relation of wall-rock alteration and uranium mines formation was explored by analyzing the rock fabric,ore body and the characteristic of wall-rock alteration,which can provide basis for finding mineral. |
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