The changes on static stress, acquired according to the half-space elastic dislocation theory, can exist on fault plane for a long time until the next strong earthquake.
依据半弹性空间地震位错理论获得的静应力变化量,可以长期存在于邻近断层面上,直至下一次地震发生。
2
Horizontal movement in 2004 have not formed orderly result of faultdislocation, relative concentration of strain or locking of fault.
2004年水平运动没有形成断层错动、应变相对集中或断层闭锁的有序结果。
3
Stacking fault energy plays an important role in the decompounds of dislocation and the martensitic transformation behavior of shape mechanism as forming nucleus with stacking fault.