From Indo-China Movement to Yenshan Movement, it was a left-lateral normal fault.
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。
