| 322矿田主控因素新说 |
| |
| 引用本文： | 刘翔,杨崇秋.322矿田主控因素新说[J].华东地质学院学报,1996,19(4):355-362. |
| |
| 作者姓名： | 刘翔 杨崇秋 |
| |
| 作者单位： | [1]核工业中南地质局地质处 [2]核工业中南地质局三0二大队 |
| |
| 摘 要： | ３２２地区北东向断裂构造具压剪性，左行左滑的特点，它对３２２矿田的定位具有明显的控制作用，是铀矿作用的主控因素，由于北东向断层的左行走滑，在丰州一带生成拉盆地，北东向断裂，丰州盆地的形成，演化，控制了矿田内各矿床的形成。
|
| 关 键 词： | 铀矿床 断裂构造 控矿因素 |
New Interpretation of The Dominant Ore-controlling Factor of The Uranium ore field No. 322 |
| |
| Liu Xiang, Yang Chongqiu.New Interpretation of The Dominant Ore-controlling Factor of The Uranium ore field No. 322[J].Journal of East China Geological Institute,1996,19(4):355-362. |
| |
| Authors: | Liu Xiang Yang Chongqiu |
| |
| Abstract: | The NE-trending fault structures in ore field NO. 322 are characterized by compresso-shearing, left-Lateral left-slipping, having an obvious control over the Localication of the ore field No. 322,and are the dominant ore-controlling factor of the ore field NO. 322,Resulting from the sinistral displacement of the NE-trending fault,there is a pull-apart basin in the Feng Zhou area. The formation and evolution of the NE-trending fault zone and the Feng Zhou basin control the formation of uranium deposits Of ore field No. 322. |
| |
| Keywords: | strike-slip fault pull-apart basin ore-controlling condition uranium ore field |
| 本文献已被 CNKI 维普 等数据库收录！ |
