Therefore, there is some significance for studying the law of salt-gypsum rock creep in drilling engineering.
因此，开展盐膏岩蠕变规律的研究具有十分重要的工程意义。
The carbonate source rock is controlled by system tracts and facies. The carbonate source rock is mainly developed in high system tract in low ramp or is survived with gypsum-salt rock together.
碳酸盐岩烃源岩的形成是受层序体系域和沉积相控制，分布于下斜坡的高位体系域或与膏盐岩伴生。
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