本文通过对四川卤水特征的研究,结合贵州汞、锑矿床包裹体液成分分析认为,当黄卤富含某些重金属与含大量还原硫的黑卤相遇混合,是卤水成矿的重要机制之一。两者物理性质、化学组份的差异,为成矿作用提供了不同的条件。断裂是卤水成矿的通道,硅化为早期矿化的标志,碳酸盐化为晚期矿化的产物。 Based on the study of the characteristics of brine in Sichuan Province and the analysis of body fluid composition in mercury and antimony deposits in Guizhou Province, it is considered that the inclusion of some heavy metals in yellow brine and mixed black halogens containing a large amount of reduced sulfur is one of the important mechanisms for the mineralization of brine. The difference between the two physical properties and the chemical composition provides different conditions for metallogenesis. Fracturing is the channel of brine mineralization, silicification is a hallmark of early mineralization, and carbonatation is a product of late mineralization.