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青山断裂总体呈东西走向,规模大,破碎带分带明显,具有多期次、多重力学性质的构造作用。具有由压→张→压扭→张扭性活动活动规律,早期为中浅构造位的韧脆性形变,晚期为浅构造位的脆性形变。
The Qingshan fault has an east-west trend, a large scale, and a clear zonation of the fractured zone. It is characterized by multiple periods and multiple mechanical properties. It is characterized by ductile and brittle deformation in the early stage of medium-shallow tectonic position and brittle deformation in the late stage of shallow tectonic stage.