Strike of seismogenic fault 发震断层走向
dislocation type of seismogenic fault 震源错动类型
alternate activity of seismogenic fault 发震断层交替活动
Seismogenic active fault 地震活断层
The analytical results of the aftershock focal mechanism show that the seismogenic fault dip angle is slowing down with depth,and is gradually steepening from southwest to northeast,which could be used to explain the increases of strike-slip component.
余震震源机制分析结果表明,发震断层的倾角随深度的增加而变缓,且从西南向北东逐渐变陡可以用来解释走滑分量增加的成因。
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