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通过对区内成矿地质背景及矿床特征的分析,阐述了本区处于华北地台南缘卢氏-栾川台缘断褶带内,秦岭纬向系构造带与北东向新华夏系构造带太行山隆起带的交汇复合部位;矿体产于新元古界栾川群煤窑沟组、鱼库沟组的石英岩、二云片岩、白云石大理岩和下古生界陶湾群三岔口组、秋木沟组钙质砾岩、白云质石英大理岩等地层中;该区大地构造位置独特,地质构造复杂,岩浆活动频繁,围岩蚀变强烈、地球化学异常明显,形成了以Pb、Zn、Mo、Ag等为主的丰富的内生金属矿产,充分证明了该区成矿地质条件良好,找矿远景乐观。
Based on the analysis of the metallogenic geological background and the characteristics of the ore deposits in the area, the paper expounds that the area is located in the rupture zone of the Lashi - Luanchuantai rim on the southern margin of the North China Platform, the Qinlingling zonal system belt and the NE- Taihangshan uplift of the intersection of the composite parts; ore body produced in the Neoproterozoic Luanchuan group Meiyaogou, Yukuanggou quartzite, two-micaodolite, dolomite marble and the Lower Paleozoic Tao Wanqu Sanchakou group, autumn The Mogou Formation calcareous conglomerate, the dolomitic quartz marble and other strata; the tectonic location of the area is unique, the geological structure is complex, the magmatic activity is frequent, the wall rock is strongly altered and the geochemistry anomaly is obvious. Mo, Ag and other rich endogenous metal deposits, fully proved that the area of good geological conditions of mineralization, ore prospecting optimistic.