| 6720矿田断裂构造特征及其对铀矿化的控制 |
| |
| 引用本文： | 朱兆周,王佳雄.6720矿田断裂构造特征及其对铀矿化的控制[J].铀矿地质,1988(3). |
| |
| 作者姓名： | 朱兆周 王佳雄 |
| |
| 摘 要： | 本文分析了某区拉张深断裂带、构造网络特征及其对火山活动、热液活动和铀矿化的控制,划分了铀成矿阶段,概述了富矿形成的地质特征及其控制因素。
|
| 关 键 词： | 拉张深断裂 火山机构 富矿 |
THE CHARACTERISTICS OF FAULT STRUCTURE IN OREFIELD NO.6720 AND ITS CONTROL OVER URANIUM MINERALIZATION |
| |
| Zhu Zhaozhou Wang Jiaxiong.THE CHARACTERISTICS OF FAULT STRUCTURE IN OREFIELD NO.6720 AND ITS CONTROL OVER URANIUM MINERALIZATION[J].Uranium Geology,1988(3). |
| |
| Authors: | Zhu Zhaozhou Wang Jiaxiong |
| |
| Institution: | Zhu Zhaozhou Wang Jiaxiong |
| |
| Abstract: | The paper analyses the characteristics of extensional deep fault zone and structural network system in a certain area and its control over the volcanic activity, hydrothermal activity and uranium mineralization, the uranium minerogenetie stages are classified. The geological characteristics and its control factors in the formation of rich are also discussed. |
| |
| Keywords: | Extensional deep fault Volcanic apparatus Rich orc |
| 本文献已被 CNKI 等数据库收录！ |
