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.

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。

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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.

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。

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