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元古宙是世界范围内重要成矿期之一,也是华北陆块最重要的成矿期。渣尔泰山群地处华北地台北缘多金属成矿带,前人研究资料表明渣尔泰山裂陷槽沉积的中元古界渣尔泰山群是大型—超大型铜多金属矿的重要赋存层位。结合本次1:5万区域地质调查及周边研究成果,充分应用1:20万化学探矿结果。查明了渣尔泰山群在该区的分布及沉积特征,发现了多处矿点及矿化线索。如小石拐西南铁矿(化)点、南壕南侧铁矿(化)点等。已经具有一定的开采意义。
Proterozoic is one of the most important metallogenic stages in the world and is also the most important metallogenic stage of the North China terrane. The Zhaltai group is located in the polymetallic metallogenic belt on the northern margin of the North China Platform. According to previous studies, the Zardeokarst Taizhan Group deposited in the Zarita rift trough is an important deposit of large-superlarge copper polymetallic deposits Horizons. Combined with the 1: 50000 regional geological survey and the surrounding research results, full application of 1: 200000 chemical prospecting results. The distribution and sedimentary characteristics of the Zarita group in this area were identified, and many ore points and mineralization clues were discovered. Such as the small Shibei southwest iron ore (of) point, South South trench iron ore (chemical) point. Has a certain mining significance.