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。
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。
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。
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