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中条山区铜矿床是在中条古裂谷地质构造环境中演化形成的。本文从涑水杂岩期－绛县期－中条期－西阳河期等不同时代地质历史演化，分别探讨了中条山区不同类型铜矿床时空分布和成因上的内在联系。它们早期形成的矿源层受不同时代的层位和岩性控制，但在后期的２０００～２１００Ｍａ和１８００～１９００Ｍａ较大规模的构造－热事件，对不同类型铜矿床进行了叠加和改造，使铜质进一步富集，最终形成工业矿床
The Zhongtiao Mountain copper deposit is evolved in the middle rift ancient rift geological tectonic environment. In this paper, the geo-historical evolution of different age deposits in the Yushui complex-Jiangxian-Zhongzhang-Xiyanghe period is discussed respectively, and the internal relations of the spatiotemporal distribution and genesis of the different types of copper deposits in the Zhongtiaoshan Mountains are discussed respectively. The early formation of the source rocks was controlled by the horizon and lithology of different ages. However, in the later large-scale tectono-thermal events of 2000 ~ 2100Ma and 1800 ~ 1900Ma, different types of copper deposits were superimposed and reconstructed, Copper further enrichment, the final formation of industrial deposits