由于应力弛张作用，使两地体间的构造分界线（灵山构造带）后期表现为左旋断层性质。
For the sake of stress relaxation, the tectonic boundary between these two different terrains (i. e. the Lingshan structure zone) expressed as a dextral fault in late period.
运动激波在密度间断层传播时，引起密度分界面的变形，相应激波形状发生改变。
When a planar shock wave is sweeping a density layer, the deformation of the density interface and the wave configurations can occur.
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