概述现代盐湖矿床,是第四纪以来可溶盐分通过迁移,集聚于成盐盆地;矿化水的浓缩和盐类矿物的沉积而形成的。迄今,有不少盐湖的盐类沉积作用现在还在继续进行着。现代盐湖矿床,按其赋存形状分为固体矿床和液体矿床两种类型。后者又可分为地表卤水(指湖水)、晶间卤水(指赋存在盐层孔隙、晶间或夹层内的地下卤水)两类。我国多数盐湖都是固、液并存的矿床。 Summary Modern Salt Lake deposits, since the Quaternary soluble salt by migration, gathered in the salt-forming basin; the concentration of mineralized water and salt mineral deposition formed. So far, there are quite a few salt lake sediments that are still going on. Modern Salt Lake deposits, according to their occurrence is divided into two types of solid deposits and liquid deposits. The latter can be divided into surface brine (refers to the lake), intergranular brine (refers to the presence of salt pore, intergranular or intercalation underground brine) categories. Most of our salt lakes are solid and liquid deposits.