| 302矿床围岩蚀变与铀矿化的关系 |
| |
| 引用本文： | 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. |
| |
| 作者姓名： | 王英稳 丁德馨 |
| |
| 作者单位： | 1. 南华大学,核资源与安全工程学院,湖南,衡阳,421001;中核韶关锦原铀业有限公司,广东,仁化,512329
2. 南华大学,核资源与安全工程学院,湖南,衡阳,421001 |
| |
| 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.
|
| 关 键 词： | 铀矿床 矿体 围岩蚀变 |
| 文章编号： | 1673-0062(2007)03-0033-04 |
| 修稿时间： | 2007年9月25日 |
The Study on Relation Between the Character of Wall - Rock Alteration and Uranium - Mineralization at No. 302 Uranium Deposit |
| |
| WANG Ying-wen,DING De-xin.The Study on Relation Between the Character of Wall - Rock Alteration and Uranium - Mineralization at No. 302 Uranium Deposit[J].Journal of Nanhua University:Science and Technology,2007,21(3):33-36. |
| |
| Authors: | WANG Ying-wen DING De-xin |
| |
| Abstract: | 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. |
| |
| Keywords: | uranium deposit ore body wall-rock alteration |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《南华大学学报(自然科学版)》浏览原始摘要信息 |
| 点击此处可从《南华大学学报(自然科学版)》下载免费的PDF全文 |
|
