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早已查明含钾盐类建造有钾盐和钾镁盐成分完全不同的两种类型:第一类为氧化物型。盐类矿物只有钾石盐和光卤石:第二类为硫酸盐型。在该种类型中,除了钾石盐和光卤石以外尚有硫镁矾、杂卤石、钾盐镁矾,无水钾镁矾等硫酸盐。据推测(1962;等,1978),这些建造形成于主要是海水补给的含盐海盆,同时,海水的成分是不变化的(至少在前寒武纪以后),其聚盐的古地理环境及大洋与陆地(由表生带)补给之间的相互关系,是在这类盆地中产生含钾盐类建造成矿特殊性的主要原因。但是其他因素在这种
It has been identified that potassium salts have two completely different types of potassium and magnesium salts: the first is oxide. Saline minerals only potassium salt and carnallite: The second type is sulfate type. In this type, in addition to potassium salt and carnallite, there are other salts such as kieserite, polyhalite, kieserite and anhydrous kieserite. It has been speculated (1962; et al., 1978) that these constructions were formed in saltwater basins that are primarily seawater recharges, while the composition of the seawater does not change (at least after the Precambrian), its palaeogeographic environment and The interrelationship between ocean and terrestrial (from the supergene) supply is the main cause of the mineralization that produces potash-bearing salts in such basins. But other factors lie in this