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沃溪断层最早形成于雪峰期 ,为铲式正断层 ;加里东期表现为右旋斜冲性质 ,西部错失鱼儿山矿体上部层脉 ,错失矿体在鱼儿山以东 ;印支—燕山期表现为左旋正滑性质。它既不是导矿构造 ,也不是容矿构造 ;其总体构造效应为正断层。
The Wuxi fault was first formed in the Xuefeng period as a shovel-type normal fault. In the Caledonian period, it was characterized by dextral syncronism. In the western part, the upper strata of the Yueshan orebody were missed and the ore body was missed to the east of Yuer’er Mountain. The Yanshanian period shows the L-normal slippery nature. It is neither the ore-bearing structure nor the ore-bearing structure; its general tectonic effect is the normal fault.