graben faulting

基本解释

The development and evolution of the basin was controlled by graben faulting mainly in vertical movement of E-W direction.
以东西向垂直运动为主体的构造活动控制了盆地的发展和演化。
The intermountain graben basin that had been formed by the faulting movement was also considered as an active place of seismicity.
山区因断裂活动产生的山间断陷盆地也是地震活动场所。
The evolution of a half graben basin bounded by normal faulting in the upper crust with a Byerlee-type strength envelope has been modelled by elastoplastic finite element analysis.
利用新近完成的粘弹塑构造模拟软件包对盆地的动力学演化进行了一系列模拟。
d.wanfangdata.com.cn