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酒店地区褶皱、断裂构造发育、区域变质和热动力变质作用较强,具矿体多、矿化均匀、品位低、厚度较稳定的特点,该矿床主要产于志留系下统梅子亚组的石英片岩中,受层位控制,与韧性剪切带和石英脉关系密切,一般韧性剪切作用越强、石英脉群越发育的地段,金矿化越强,该区地质环境和产出特征在陕南地区具有一定的代表性,对浅变质片岩类金成矿规律的研究,具有重要的理论意义和现实意义。
In the area of the hotel, the fold, faulting structure, regional metamorphism and thermodynamic metamorphism are strong, with many ore bodies, even mineralization, low grade and relatively stable thickness. The deposit is mainly produced in the following areas of the Silurian plum subgroup The quartz schist is controlled by horizon, closely related to the ductile shear zone and quartz vein, the stronger the ductile shearing, the more developed quartz vein group, the stronger the gold mineralization, the geological environment and the output characteristics It is of great theoretical and practical significance to study the regularity of gold mineralization in the shallow metamorphic schist since it has certain representativeness in southern Shaanxi.