MupingRushan metallogenic belt is one of six major gold metallogenic zones in eastern Shandong (Jiaodong). Deep mineralization patterns in its northern part is unclear. Taking Xiwangcong area as the study object, by using regional geological analysis, controlled source audiofrequency magnetotelluric surveys and deep drilling, orecontrolling characteristics of faults with the trend of NNE have been revealed. Two deep mineralization spaces controlled by nearly parallel faults have been identified. A low resistivity mineralized alteration zone has been detected in the peripheral deep zone of Shuangshantun mining area. The three gold ore bodies controlled by drilling extend towards the NE side and are not enclosed. There is great potential in the deep part. It will provide new evidences of geophysics and structural coupling for mineral exploration in the deep part in Jiaodong area.