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石膏与岩盐则逐渐变薄或完全被溶解掉。Gypsum and halite are simply thinned or removed altogether.

盐构造是由于岩盐和其他蒸发岩的流动形变所形成的地质体。Salt structure is a geologic body formed by flow iir1 deformation of halite and other evaporitic rocks.

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盐岩又是良好的盖层，且在高温、高压下呈塑性状态。Meanwhile, halite is also a good cap rock, and would be in plastic state under high temperature and high pressure condition.

采用常蠕变速率假定，研究了盐岩地层中石油套管的长期蠕变变形和强度问题。The long-time creep deformation and strength of the casing in halite stratum were studied assuming the constant creep velocity.

在这种环境下，石膏或硬石膏可以堆积成许多米厚的岩层，而没有任何石盐伴生沉淀。Under the circumstances, gypsum or anhydrite could accumulate to form beds many meters thick, without any co-precipitation of halite.

碱湖矿层剖面上，天然碱与芒硝呈互为消长关系，天然碱和石盐则呈正相关。Trona is negatively correlated with mirabilite in the mineral bed sections of soda lakes. Trona and halite show a positive correlation.

在这种环境下，石膏或硬石膏可以堆积成许多米厚的岩层，而没有任何石盐伴生沉淀。Under the circumstances, gypsum or anhydrite Co. ld accumulate to form beds many meters thick, without any Co. precipitation of halite.

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东濮凹陷的一大特点是其北部纵向上发育4套盐岩，它们构成油气富集的优良盖层。A typical feature of Dongpu depression is that 4 sets of halite are vertically developed in the north, which forms the favorable cap of hydrocarbon accumulation.

盐湖盐类沉积有碳酸盐类、硫酸盐类和氯化物型盐类、主要盐类矿物为芒硝、钾芒硝、天然碱、泡碱、碳钾钠矾、石盐等。Saline deposits of salt lake consist of more than 10 salt minerals, but the glauber salt, glaserite, pgrotechnite, hanksite, natron, trona and halite are mainly salt minerals.

研究表明，在缺少井间约束条件的情况下，充分利用盐岩的沉积特征，采用地质约束条件下的盐岩随机建模，可以实现对盐岩分布的科学预测。According to the obvious facies sequence and the concentric distribution of salt bed, a stochastic modeling method under geological constraints was applied in the study of F Halite bed.

它主要用于测量桩基钻孔的井径与井筒偏斜，也可用于帷幕、沉井井筒测量以及海岸工程、岩盐水溶开采的井下溶腔测量等。Besides the diameter and inclination of pile foundation drill-hole, it can also be applied to other engineering, such as segmentation sinking, caisson sinking and halite mining by water-solution.