在岩块拆离滑脱过程中所形成的主拆离滑脱带、次级拆离滑脱带及层间滑动断裂成为较发育的构造扩容空间。
The main and second detachment belts as well as interformational faults were formed during the gliding of rock masses, and became well developed structural expanding space.
两个板块的运动被认为是由碰撞-滑动断裂引起的，两部分地壳正在以水平移动的方式向着相反的方向碾压运动。
The motions of these plates create what are known as strike-slip faults, where two sections of Earth's crust are grinding past each other in opposite directions.
地震时发生的断层滑动确实会造成作用在该地区其他断层上的压力的改变，从而改变这些断层发生断裂的可能性。
The fault slip that happens in an earthquake changes the stress acting on other faults in the area, and may influence how close they are to failure themselves.
应用推荐