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庙山金矿位于秦岭造山带西秦岭中部花岗岩带,属北中秦岭陆表海盆中段。赋存于高桥—洮坪大断裂西段。通过对金矿体地质及矿带特征较为客观认识的基础上,分析总结矿体控矿因素指导深部探矿。经深部坑探,矿体氧化深度较深(最深178m),矿体向深部有变富变厚的趋势。庙山金矿属断裂破碎带控制的中低温热液蚀变岩型金矿。
Miaoshan gold deposit is located in the central Qinling orogenic belt West Qinling granite belt, belonged to the North Qinling Mountains in the middle of the surface water table. Occurred in Takahashi - Ping large fault western section. Based on the more objective understanding of the geology and ore belt characteristics of the gold ore body, the ore prospecting and controlling factors are analyzed and summarized to guide the deep prospecting. After deep pit exploration, the depth of ore body oxidation is deepest (the deepest is 178m), and the ore body tends to become rich and thick toward the depth. Miaoshan gold deposit is controlled by the middle and low temperature hydrothermal alteration rock type gold deposit.