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中条山多金属成矿带的落家河铜矿床是不同于该地区已发现的其他类型铜矿床。本文通过对落家河铜矿床H-O-C-S同位素特征的研究,结合前人研究成果,认为落家河铜矿床的成矿流体为岩浆水和海水的混合。矿床的形成过程中岩浆热液参与了成矿。
The Luojiahe copper deposit in the Zhongtiaoshan polymetallic metallogenic belt is different from the other types of copper deposits that have been discovered in the area. Based on the study of the H-O-C-S isotopic characteristics of the Luojiahe copper deposit and the previous research results, it is considered that the ore-forming fluid of the Lujiahe copper deposit is a mixture of magmatic water and seawater. During the formation of ore deposits, magmatic hydrothermal fluids are involved in metallogenesis.