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柴家庄金矿位于西秦岭褶皱系北秦岭加里东褶皱带李子园—吊把子金矿带上,赋存于柴家庄二长花岗岩体外接触带的丹凤群地层中,严格受NE向及NNW向断裂控制。矿床形成经历了火山沉积期、区域变质期、构造热液成矿期及岩浆热液成矿期4个阶段,属沉积变质—岩浆期后热液叠加改造的变质热液金矿床。岩体外接触带0～2km范围内的NE向、NNW向断裂构造带是找矿的最佳方向。
The Chaijiazhuang gold deposit is located in the Liqiyuan-Zhuanzi gold belt in the Caledonian fold belt of the North Qinling in the western Qinling fold system and occurs in the Danfeng Group strata in the in-vitro contact zone of the Chaijiazhuang monzonitic granite. It is strictly controlled by NE And NNW fracture control. The deposit formed four phases of volcanic sedimentary period, regional metamorphism, tectono-hydrothermal mineralization and magmatic hydrothermal mineralization, belonging to metamorphic-hydrothermal gold deposit after sedimentary metamorphism-hydrothermal alteration. The NE-direction and NNW-trending faults in the outer contact zone of the rock mass within the range of 0 ~ 2km are the best prospecting directions.