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重晶石是渗流热卤水成矿的重要成因标志 丘赫洛夫(1974)曾指出:“硫酸钡沉积,极大多数可能是卤水在海底卸载所致”(见文献[3]).我们同意重晶石的生成大多与卤水有关,并认为它是渗流热卤水成矿的重要成因标志之一.
Barite is an important genetic indicator of percolation hot brine mineralization Chukhlov (1974) pointed out: “Barium sulfate deposition, most likely due to unloading of brine in the sea” (see [3]). We agree that the formation of barite is mostly related to brine, and it is considered as one of the important genetic markers of percolation hot brine mineralization.