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中条裂谷主要铜矿床的包裹体是以液相包裹体为主，含气液相包裹体亦较普遍，常含子矿物ＮａＣｌ；成矿温度以１４０—３００℃为主，晚期则高达４００—６２０℃；主要矿床的包裹体化学成分及化学序列相似，普遍富含Ｃｌ－，Ｎａ＋，Ｃａ２＋和Ｈ２Ｏ及ＣＯ２；成矿流体以高盐度（３２～４０Ｗｔ％ＮａＣｌ）为主，密度为１．０～１．１８ｇ／Ｃｍ３；各矿床成矿的物理条件不同，沉淀环境存在若干差异．矿床属海底中低温热液铜矿床．
The inclusions of the main copper deposits in the Middle Rift are dominated by liquid inclusions. Gas-bearing fluid inclusions are also common, often containing sub-mineral NaCl. The metallogenic temperature is mainly in the range of 140-300 ℃, while in the late stage, up to 400-620 ℃. The chemical composition and chemical sequence of the main ore deposit inclusions are similar, and are generally rich in Cl-, Na +, Ca2 +, H2O and CO2. The ore-forming fluids are mainly characterized by high salinity (32-40wt% NaCl) 1.0 ~ 1.18g / Cm3. The mineralization conditions of each deposit are different, and there are some differences in precipitation environment. The deposit is submarine low-temperature hydrothermal copper deposit.