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根据间隙溶液及其周围的盐下陆源地层岩石的研究,阐明了把地表蒸发盐盐水改造为含矿溶液的机制;研究了含矿盐水变为成矿溶液的可能途径。
Based on the study of the interstitial solution and its surrounding salt rocks in the terrestrial source rocks, the mechanism of transforming surface salt water into ore-bearing solution was expounded and the possible ways of transforming ore-bearing brine into ore-forming solution were studied.