断层滑动 meaning in Chinese

fault slip

The kinematics of sudden faultslip have not yet been directly observed .
突然的断层滑动的运动情况迄今还没有人作过直接观测。
The focal mechanism is mainly left - lateral strike - slip , with a very small normal fault slip component
这次地震的震源机制基本上是左旋走滑，带有微小的正断层滑动分量。
This predictability most likely stems from the fact that water flowing from below subduction zones may exert significant control over when and where these faults slip silently
这样的可预测性，很可能来自于隐没带下方所流出的水，它对于何时、何地会发生无声的断层滑动，可能具有相当大的操控力。
The existence of silent earthquakes gives scientists a completely new angle on the slip process by permitting the detailed study of fault zones through every stage of their movement
然而，无声地震的存在却提供科学家一个全新的角度，来看待断层滑动的过程，让他们对断层带运动的每个阶段做更仔细的研究。
The importance of deciphering fault slip is difficult to overstate because when faults slip quickly , they can cause immense damage , sometimes at a great distance from the source
要去了解、解释断层滑动的重要性是无庸置疑的，因为一旦断层快速滑动，将会造成巨大的灾情，有时发生位置甚至离震源还有一大段距离。