Phase equilibrium of sea water system forms the physicochemical basis of research on the origin of evaporite deposits.

海水体系相平衡的研究是蒸发岩矿床成因研究的物理化学基础。

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Till the late stage, the periodic sea-level changes resulted in the formation of the evaporite deposits in restricted shallow-water basin and mudstones and gravity-flow deposits in deep-water basins.

晚期因周期性的海平面变化导致形成局限浅水盆地、蒸发岩沉积和深水盆地泥岩和重力流沉积。

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