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。
Horizontal movement in 2004 have not formed orderly result of fault dislocation, 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。
The form and state of overlaying soil rupture depend on the types of the fault and its dip-slip angle and size of dislocation, and the thickness of overlaying soil and its distribution.
导致上覆土层的破裂的因素有基岩断层位错类型、断层面倾角、断层位错量及上覆土层的厚度与分布状况等。
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