二期热卤水成矿作用常相互叠加，形成工业矿床。
The mineralization of the first and second period hot brine often superimposed to form industrial deposits.
碳酸盐岩地区的重晶石矿床，是在浅层条件下，以岩溶地下热卤水溶液为介质，岩溶作用为主导成矿作用形成的。
Barite deposits in carbonate rock area forms under shallow condition with karst hydrothermal brine solution as medium and karstification as leading factor of mineralization.
碳酸盐岩地区的重晶石矿床，是在浅层条件下，以岩溶地下热卤水溶液为介质，岩溶作用为主导成矿作用形成的。
Barite deposits in carbonate rock area forms under shallow condition with karst hydrothermal brine solution as medium and karstification as leading factor of mineralization.
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