Compressive faults occurred after principal earthquake with slow variation in propagation and releaseofstress 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。
2
As tectonic stretching is not a releaseofstress or tension, trapped lava exploded upwards through volcanos. Volcanic fallout was a substantial problem for nearly a decade after the shift.