多年来,人们一直认为云南勐野并钾盐矿床是正常海水蒸发而成的。笔者对该矿床进行了长期的、反复的调查研究,认为它是深部的塑状盐流侵位于白垩系上统勐野并组红色陆相地层的产物,而塑状盐流很可能是直接源于地幔的“火成盐体”。 Over the years, people have always thought that the Yunnan Mengno and Potash deposits are formed by normal seawater evaporation. The author conducted a long-term, repeated investigation and study of the deposit and concluded that it is the result of deep plastic salt intrusion into the Cretaceous Manyeo Formation red terrigenous formation. The plastic salt flow is likely to be a direct source In the mantle of “fire into salt body.”