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本文根据淄河铁矿氧、硫同位素地质特征及其矿田地质,分析了该铁矿的成矿作用,提出了“沉积—热卤水改造—氧化淋滤”的成因观点,以期商榷。
Based on the geological characteristics of oxygen and sulfur isotopes and the geology of their orefields, this paper analyzes the mineralization of the iron ore and proposes the genesis view of “sedimentary-thermal brine transformation-oxidation leaching”.