The Study of Structural Characteristic and Modern Activity of the Qingdao Pishkou Fault Zone

The space distribution, structureal charccteristic and the structure effects of the Pishikou fault in Qingdao were studied by the way of field observations and paining the profile pictures of the fault. Modern activity of the Pishikou fault in Qingdao was studied by the way of physiognomy, seism geology, Quaternary,and the structure chronology. The conclusion was got that the Pishikou fault tend to become steady since the late Pleistocene, and it's a inactive fault in later Quaternary.