Zhuo Wen , Guangqing Yao , Xiaobo Zhao , Xiao Lei , Xinguang Wang , Haodong Tang , Xinyang Wu , Zhongming Huang
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引用次数: 0
Abstract
The fan delta front deposit is a notable reservoir type in the basin margin and typically exhibits high heterogeneity in reservoir architecture. With the deepening of exploration and development of oil and gas fields, the study of lower-order depositional architectures is relatively weak, and their implication on remaining oil distribution and enrichment are poorly understood. Field outcrops of the fan delta front deposit exhibit first-hand data of lithofacies, association, and depositional architectures, effectively providing insights for underground reservoir research to guide the development of oil fields, such as high water–cut oil fields in the late development period. Herein, we considered the fan delta front outcrops of the Sangyuan section as an object to reveal the depositional architectures located in the Luanping Basin, northeast China. Using meticulous artificial fieldwork and unmanned aerial vehicle observation, we focused on the 4th-order (single sandbody) and 3rd-order (composite laminaset groups) architectural units. Based on field observations, quantitative statistics, and model matching and guidance, architectural models of the fan delta front in the Sangyuan section were established in response to the high-frequency lake-level. In addition, genetic types of remaining oil controlled by architectural features in Wenchang B oil field during the high water–cut stage were further discussed, and suitable strategies and measures are proposed to produce different types of remaining oil. Results indicate that there are twelve basic types of lithofacies and three types of a single sandbody developed in the Sangyuan section, and evidently, the dimensions and spatial stacking patterns of 4th-order architectural units are closely related to high-frequency lake-level fluctuation, that is, with the rise of lake-level, the thickness and width of a single sandbody gradually decrease, whereas the width–thickness ratio gradually increases. Meanwhile, the spatial stacking patterns of sandbody gradually evolution from the downcut type to the superposition or butted type and finally to the isolated type. A single sandbody is divided into one or more composite laminate groups by the interfaces of 3rd-order architectural elements, which are identified according to the flow regime and sedimentary structures. Different orders of architectural units have different controlling effects over remaining oil distribution and enrichment, and the corresponding technical measures are proposed to enhance the remaining oil recovery. The above mentioned analyses can provide a valuable reference for oil and gas production in the late stage of an oil field with a similar depositional environment.
扇三角洲前缘沉积是盆地边缘的一种显著储层类型,其储层结构通常表现出高度的异质性。随着油气田勘探开发的深入,对低阶沉积构造的研究相对薄弱,对其对剩余油分布和富集的影响认识不足。扇三角洲前沿沉积的野外露头展示了岩性、关联和沉积构造的第一手资料,有效地为地下储层研究提供了启示,以指导油田开发,如开发后期的高水切油田。在此,我们以三原剖面扇三角洲前缘露头为对象,揭示了位于中国东北滦平盆地的沉积构造。通过细致的人工野外工作和无人机观测,我们重点研究了四阶(单体砂体)和三阶(复合层组)建筑单元。在野外观测、定量统计、模型匹配与指导的基础上,建立了三袁段扇三角洲前沿响应高频湖面的建筑模型。此外,还进一步讨论了高水切阶段文昌 B 油田建筑特征控制的剩余油遗传类型,并提出了生产不同类型剩余油的合适策略和措施。研究结果表明,三元断面发育有12种基本岩性类型和3种单一砂体类型,且4阶建筑单元的尺寸和空间叠加模式明显与高频湖面波动密切相关,即随着湖面的上升,单一砂体的厚度和宽度逐渐减小,而宽厚比逐渐增大。同时,沙体的空间堆积形态由下切型逐渐演变为叠加型或对接型,最后演变为孤立型。根据流态和沉积结构的不同,单个砂体被三阶建筑单元的界面划分为一个或多个复合层组。不同阶次的建筑单元对剩余油分布和富集有不同的控制作用,并提出相应的技术措施来提高剩余油采收率。上述分析可为具有类似沉积环境的油田后期油气生产提供有价值的参考。
期刊介绍:
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