• The restraining barrier is more steady than the interbed in vertical .

    纵向上隔层分布稳定,夹层分布零散。

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  • The prediction of thin bed and thin interbed thicknesses is an important link for the reservior lateral prediction.

    薄层、薄互层厚度预测是储层横向预测的一重要环节。

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  • The dynamic process of bottom-water bypassing interbed and fleeing upward is simulated by using sintered planner models.

    采用烧结的平面物理模型,实验模拟底水绕过上窜夹层的动态过程。

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  • Among various factors of affecting development result of the horizontal well, the influence of intrastratal interbed is more important.

    在影响水平井开发效果的多种因素中,层内夹层的影响是比较重要的方面。

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  • In this paper, we build a forward modeling of seismic response to thin-interbed and find the suitable condition of spectral decomposition.

    试图通过正演模型开展薄互层地震响应特征分析来探讨分频技术的适用条件。

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  • Nanjing silty clay with fine sand interbed is a sediment deposited alternately by silty clay and fine sand, appearing to be a "thousand layers cake";

    南京粉质粘土与粉砂互层土为粉质粘土与粉细砂交互沉积,呈现“千层饼”状外貌;

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  • Therefore, the application of high-resolution thin-interbed inversion based on the model in sand body description and reservoir prediction has been studied.

    为此,在该区开展了基于模型的高分辨率薄互层反演技术进行砂体描述和储层预测的研究。

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  • The noise in the information from the wells in the thin sand-mudstone interbed area with dense well network should be removed by coarsening well information.

    对密井网的砂泥岩薄互层区采用井信息进行粗化去除部分干扰信息;

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  • The Taiyuan Formation develops three types of strata assemblages, including clastic rock type, limestone type and interbed of clastic rock and limestone type.

    太原组地层发育了碎屑岩型、灰岩型和互层型三种组合。

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  • Deformation will be concerted of the fourth weak interbed exceptant bank slope rock mass and weak interbed will be potential, the most dangerous failure plane.

    第四层软弱夹层以外的岸坡岩体变形较协调,这一软弱夹层是岸坡潜在的最危险的破坏面;

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  • Transitional tervain from siliceous rock to clayrock, both interbed and altered clayrock are favourable strata of all kinds of elements concentrated mineralization underneath the Cambrian.

    寒武系底部硅质岩向粘土岩过渡地带 ,或两者的互层以及蚀变粘土岩是多种元素富集成矿的有利岩层。

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  • Transitional tervain from siliceous rock to clayrock, both interbed and altered clayrock are favourable strata of all kinds of elements concentrated mineralization underneath the Cambrian.

    寒武系底部硅质岩向粘土岩过渡地带 ,或两者的互层以及蚀变粘土岩是多种元素富集成矿的有利岩层。

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