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.
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。
For different latitude areas, various patterns of tidal stress effects and relevant types of seismic faults have various distributing features.
对不同的纬度区域，不同的潮汐应力作用方式与之促滑的断层类型也有不同的分布特征。
Compressive faults occurred after principal earthquake with slow variation in propagation and release of stress wave, this might lead to higher after shock intensity and longer duration.
挤压型逆冲断层地震在主震之后，应力传播和释放过程比较缓慢，可能导致余震强度较大，持续时间较长。
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