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。

矿区含金复脉带是由石英脉、钠长石英脉、钠长石脉、次生石英岩等断续分布于片岩带中。长1500m、宽460～900m，在本矿床6个复脉带中共圈出大小16个工业矿体。矿体多集中于Ⅱ、Ⅲ、Ⅳ带中。以Ⅱ2、Ⅲ3、Ⅳ4矿体最富，Ⅱ5规模最大。金矿平均品位10.6g/t。

The mine area is composed of the East and west of the East and the west, and the north and west to the East. 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.
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.
Gold mining area complex vein zone is composed of quartz, albite quartz vein, sodium feldspar veins, secondary quartzite intermittent distribution in schist belt in. Long 1500m, width of 460 ~ 900m, in the 6 mineral deposits Fumai the circle size of 16 industrial orebody. The ore bodies are concentrated in the middle of the second, third and fourth. The ore bodies of 2, 3, 5 and 4 are the most abundant, and the second is the largest. Gold average grade 10.6g/t.