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中条山及其邻区,夹持在新太古代涑水杂岩与中元古代西阳河群之间的古元古代地层,包括:绛县群横岭关亚群和铜矿峪亚群、中条群下亚群和上亚群、担山石群、宋家山群、银鱼沟群等,呈推覆构造形成的堆垛地层系统,具有侧向地层对比的关系,揭示了中条山沉积改造型铜矿床独特的成矿作用。1)横岭关亚群、铜矿峪亚群、中条群上、下亚群、担山石群、宋家山群、银鱼沟群等有相似的地层序列,主要为碎屑岩、泥质岩、碳酸盐岩夹火山岩,南部的担山石群变质砂砾岩具有边缘相特征。这些群和亚群之间均为断层接触关系,非角度不整合
Zhongtiao Mountains and its adjacent areas, sandwiched between the Neoarchean Yongshen Complex and the Mesoproterozoic Xiyanghe Group ancient Paleozoic strata, including: Jiangxian group Hengling Guan sub-group and copper mine sub-group, in Lower subgroups and sub-subgroups of Upper and Lower Subgroups, the Dan Shan Group, the Song Jiashan Group and the YinYuGou Group are the stacking stratigraphic systems formed by the nappe structure and have the relationship of lateral stratigraphic correlation, revealing the sedimentary transformation of Zhongtiaoshan Type copper deposit unique mineralization. 1) There are similar stratigraphic sequences of Henglinguan sub-group, Tongkuangyu sub-group, Zhongtiao group, sub-sub-group, Danshan rock group, Songjiashan group and Yinyugou group, which are mainly clastic rocks, argillaceous rocks, Carbonate rocks volcanic rocks, southern Shanshan metamorphic sandy conglomerate with edge phase characteristics. These groups and sub-groups are between the fault contact relationship, non-angle of non-integration