In Bachu Area, the major factor of impacting average velocity variety is multi big Angle unconformity interface that heave tectonic movement formed and big heave fault.
在巴楚地区，影响平均速度变化的主要因素是大的构造运动形成的多角度不整合界面和断距较大的断层。
For a normal earthquake this is when rock snaps, or rock grinds along a fault line, or rock layers drop or heave.
对于一个正常的地震，这是当岩石扣，或岩石研磨沿着断层线，或岩石层下降或隆起。
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