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对区内5个成矿带进行研究,提出云开隆起脆性剪切带阵列控制着金矿化分布的态势;印支期重熔花岗岩和燕山晚期花岗岩迭加的脆性或脆韧性剪切带是金矿床集中部位;金矿成矿斑岩体的定性判别标志,新发现加里东晚期斑岩型矿床;岩浆热液矿床沿构造岩浆岩带、隆起与坳陷交接部位、坳陷里的构造凸起边缘或隆起里的凹陷周缘和NNE-NE与NW—NWW走向的壳层逆掩断裂交织的菱形块上升部位或各自的相对上升盘分布,岩浆侵入体出现在构造复合部位,特别是NE向深断裂和EW向、NW向构造复合部位;含矿层位为前寒武纪—二叠纪地层;查明燕山运动期间三次铜、铅、锌（银）区域成岩成矿岩浆活动。
Based on the study of five metallogenic belts in the area, it is proposed that the brittle or brittle-ductile shear zone superimposed by the Indosinian reclaimed granite and the late Yanshanian granite should be controlled by the array of brittle-shear zones in the cloud- The central part of the gold deposit; the gold ore-forming porphyry qualitative identification markers, the new discovery of Caledonian porphyry deposits late; magmatic hydrothermal deposits along the tectonic magmatic belt, uplift and the junction of the depression, the depression in the structural convex From the edge of the rim or uplift in the perimeter of the dimple and the NNE-NE and NW-NWW crust, the upwelling of the uplifted intercalated diamond blocks or their relative uplifting disk distribution, magmatic intrusions occur in the tectonic complex, especially the NE Deep fault, EW strike and NW strike. The ore bearing layer is Precambrian-Permian strata. The diagenetic and ore-forming magmatic activities of the three copper, lead and zinc (silver) regions during the Yanshan movement are identified.