中国大陆区多数活动断裂虽未见有引起地表变形的明显断层蠕滑运动现象,但仍不乏断层蠕滑运动的种种地质形迹,如区域性有序的地裂运动,沿断裂分布的线性变形带,以及与地质滑动速率相比大大偏低的地震滑动速率等.认识并查明断层蠕滑运动这一重要活动习性,在理论上和实际中均有重要意义. Although most of the active faults in mainland China have not seen the obvious fault creep movement that causes surface deformation, there are still many geological features of fault creep movement such as the regional orderly ground-fissure movement, the linear deformation zone along the fracture distribution , As well as the seismic slip rate, which is much lower than the geologic slip rate, etc. Understanding and identifying the important activity habit of the fault creep movement is of great significance both theoretically and practically.