矿区主要由东西向压性断层及与之伴生的近南北向张性断裂、北东和北西向扭性断层组成。区内褶皱构造主要有金厂峪复背斜及崔堡子复向斜,并伴有次一级小的背、向斜。金厂峪金矿床位于前述的复背斜轴部。
控矿构造以北北东向压扭性断裂最发育,表现形式为片岩带或片理化带。矿区内共有6条,片岩带的形态和交汇部位往往是控制单个矿体的主要构造。
The mining area is mainly composed of the East-West trending compressive fault and the near North and South trending faults, the North East and the North West to the fault. In the fold structures are mainly Jinchangyu complex Baoziwan anticline and Cui Xiang Xie, and Xiang Xie back, with a secondary small. Jinchangyu Gold Deposit is located in the complex anticline.
控矿构造以北北东向压扭性断裂最发育,表现形式为片岩带或片理化带。矿区内共有6条,片岩带的形态和交汇部位往往是控制单个矿体的主要构造。
The ore controlling structure of NNE trending compressoshear faults are most developed, form or schistositilization schist belt. In the mining area of a total of 6, the morphology and the intersection of schist belt is usually the main tectonic control single ore body.