近源浅水三角洲沉积特征及沉积模式研究以八面河油田沙三上亚段5砂组为例

    Sedimentary characteristics and model of proximal shallow water delta in the Eocene upper Es3s5 unit of Bamianhe Oilfield

    • 摘要: 浅水三角洲已成为油气地质领域研究的重点对象,进一步深化其沉积模式与砂体展布规律,对加快该类储层的油气勘探与开发具有重要意义。本文以八面河油田沙三上亚段5砂组为例,综合岩芯、测录井、分析化验等地质资料,研究近物源体系浅水三角洲的沉积特征,建立区域特色的沉积模式。结果表明,在构造背景、古物源、古气候等因素影响下,八面河油田沙三上亚段5砂组岩性以细砂岩为主,自下而上砂体规模逐渐增加,整体呈进积特征,主要发育水下分流河道、水下天然堤、席状砂等沉积微相,河口坝基本不发育,水下分流河道呈交织状连片分布,并在浅水区形成大面积席状砂。

       

      Abstract: Shallow water delta has become a key object in the field of oil and gas geology. Further Understanding of its sedimentary model and sand body distribution is of great significance to accelerate the oil and gas exploration and development of this kind of reservoir. The sedimentary characteristics of shallow water delta in such a proximal shallow delta system were studied and the regional characteristic sedimentary model was established for the upper Es3s5 sand unit of the Eocene Shahejie Formation in Bamianhe Oilfield by integrating the geological data from borehole, logging and chemical analysis. Results show that, under the tectono-structural background, the ancient material source, paleoclimate and other factors, the upper Es3s5 sand unit was formed and composed of mainly fine sandstone, and the sand body size increased gradually from bottom to top, showing progradation characteristics as a whole. The sedimentary microfacies such as underwater distributary channel, underwater natural levee sheet sand and so on were mainly developed. The estuary bar was merely developed, and the underwater distributary channel was distributed in an intertwined and contiguous manner, and a large area of sand sheet was formed in the shallow water area.

       

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