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庄河－凤城断裂走向北东，形成于早中生代，属辽南区域性切壳断裂构造，规模大、变形强、活动期次多，对成岩成矿有重要控制作用。
The Zhuanghe-Fengcheng fault goes to the north-east and formed in the early Mesozoic. It belongs to the regional crust-faulted structure in southern Liaoning. It has large scale, strong deformation and many active periods, which play an important controlling role in diagenesis and mineralization.