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.
利用岩石破坏过程分析软件——RFPA2D对该模型进行数值模拟，模拟结果显示了重力坝破坏的三种模式：表层滑动、深层滑动及混合滑动。
The failure process of the model was simulated by RFPA2D software. Simulation results show three failure modes of gravity dam, such as surficial slide, deep slide and mixed slide.
这类岩石缺乏面理构造，是由于矿物颗粒的脆性碎裂，旋转以及颗粒边界的磨擦滑动和扩展而造成的。
These rocks are lack of foliation and resulted from the brittle fragmentation of mineral grains with rotation of grain fragments accompanied by fractional grain boundary sliding and dilatancy.
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。
The movement of the plates strains the rock at and near plate boundaries and produces zones of faults around these boundaries.
当床上用品的倾角小于岩石内摩擦角，岩层分离和一些岩石块，在每一块岩石地层滑动沿节理面作为一个整体。
When the dip of bedding is less than the friction Angle of rock, the rock stratum will separate and some rock blocks in every rock stratum may slide along joint surface as a whole.
当床上用品的倾角小于岩石内摩擦角，岩层分离和一些岩石块，在每一块岩石地层滑动沿节理面作为一个整体。
When the dip of bedding is less than the friction Angle of rock, the rock stratum will separate and some rock blocks in every rock stratum may slide along joint surface as a whole.
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