Formation and development of ground fissure are controlled by neotectonics.

地裂缝的形成和发展受新构造运动控制。

By using the approach of morphostructure and tectonic chronology analysis, neotectonic activity evidences and characteristics as well as its ralation to uranium mineralization were researched.

通过构造地貌和构造年代学的分析方法，对其表现特徵和运动特徵及其与铀成矿之间的关系进行研究。