The growth of laboratory earthquake from aseismic slip,tremor and foreshock activities on the existence of fault barrier

【作者】 王丽凤； 卓燕群； 马胜利；

【机构】 中国地震局地质研究所；

【摘要】 <正>Nucleation phase on the planar fault has been recognized as a aseismic sliding process in both laboratory and theory. However, the natural fault is usually not ideal plane, which may fundamentally change the view point of nucleation process, and brings complexity that leading to dynamical rupture of faults.更多还原