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本文在分析断层等不连续面冲击地压现象的基础上,用岩体的振动与断层间的刚体错动的叠加来描述不连续面冲击地压发生过程.提出阶层上下两盘刚体滑动的稳定与非稳定的形式;分析了振幅越来越大的不稳定振动.断层冲击地区发生时,岩体位移是岩体的振动与断层间的刚体错动的叠加.指出了发生断层冲击地区的影响因素及原因,
Based on the analysis of the phenomenon of rockburst in discontinuities such as faults and faults, the paper deals with the rockburst and the superimposition of rigid body faults between faults to describe the rockburst occurrence process of discontinuities. The stable and unsteady forms of two rigid bodies in the upper and lower classes are proposed. The unstable vibration with larger amplitude is analyzed. When a fault occurs in the area, the displacement of the rock mass is the superposition of the vibration of the rock mass and the dislocation of the rigid body between the faults. It points out the influencing factors and reasons of the fault impact area,