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Sedimentary features of Jishan Sandbody in huimin sag

机译:惠民凹陷鸡山砂体的沉积特征

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The sedimentary environment of Jishan sandbody is always disputed by geologists. The sandbody is in Huimin sag of Jiyang depression of Bohaiwan gasin. With the help of the theory and method of sequences Stratigraphy, core analysis, logging curves and mineral analysis and so on. This paper presents that the Jishan sandbody is turbidite facies according to the research on the sandbody. The source area is Chengning arch in the north, and the flow direction is southeast. The conditions of oil generation, Migration and accumulation are very good. It forms many kinds of oil-bearing reservoirs such as Lithologic, lithologic-block and fault-block oil reservoirs and so on.
机译:地质学家一直对鸡山砂体的沉积环境存在争议。砂体在渤海湾瓦斯盆地济阳depression陷惠民凹陷。借助层序地层学,岩心分析,测井曲线和矿物分析等理论和方法的帮助。根据对砂体的研究,认为鸡山砂体为浊积相。源区为北部的成宁拱,流向为东南。产油,运移和聚集的条件非常好。形成了岩性,岩性,断块等多种含油储层。

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