这通常在几分钟之内发生，由于压力从一个点上跑到另一个点上，而此处的岩石层正阻挡着发生滑动，这样就导致了更多的晃动。
This often, within minutes, results in more jolts as the pressure that was at one point now moves to be pressure at the next point where rock fingers are holding the slippage.
沿着一些断层片段，岩石被固定在一定的位置而不能随板块运动而滑动。
Along segments of some faults, the rock becomes locked in place and cannot slide as the plates move.
滑动裂纹模型被广泛应用于岩石类材料压剪断裂分析及损伤分析。
The sliding crack model has been widely applied in the damage and fracture analysis of the rock-like materials.
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