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红旗沟金矿床主要产于元古宇色洛河群地层和花岗岩-绿岩带中,矿化类型主要为石英脉型-蚀变岩型,矿体受北西向构造控制,矿床成因类型属沉积-变质(再造)金矿床。区域地球化学场趋势显示该区为金矿集中区,大多数土壤地球化学测量结果具有直接指导地表工程布置和有可能发现矿体及矿化体的作用。
The Hongqigou gold deposit is mainly produced in the Proterozoic Silurian Group strata and the granite-greenstone belt. The mineralization type is mainly quartz vein-altered rock type, and the ore body is controlled by the NW structure. The genesis of the deposit belongs to sedimentary- Metamorphic (re-created) gold deposits. The trend of regional geochemical field shows that the area is a gold concentrate area. Most of the soil geochemical survey results have direct guidance to the surface engineering arrangement and may find the role of ore bodies and mineralized bodies.