海相砂质滩坝储层内部构型模式及表征—以哈得逊油田东河砂岩为例
- 收稿日期:
2023-12-05
- 网络出版日期:
2024-05-14
摘要: 【意义】海相砂质滩坝储层构型特征复杂,储层内部发育渗流优势通道及渗流屏障,对储层内部构型特征认识不清,制约了油藏的剩余油挖潜。【方法】本文应用野外露头、卫星照片及沉积数值模拟等多技术手段,以哈得逊东河砂岩为研究目标,探讨了海相砂质滩坝储层的构型模式,在模式指导下对东河砂岩储层进行了构型精细表征。【结果】复合滩坝内部单一坝砂的沉积构型受控于岸线形态、海岸坡度、波浪方向及高度等多种因素,可形成不同形态的锥形坝、弯月坝、正向线性坝、斜交坝等单一坝体构型模式,在单一坝体边界识别的基础上,以构型模式为指导,在研究区C1小层识别出不同规模的坝体13个,包括弯月坝5个、正向线性坝7个、斜交坝1个,不同坝体间定量规模存在差异,弯月坝长度约1.5-3km,斜交坝长度约4.5-5km,正向线性坝体长度大于6km。坝砂间呈进积型及退积型叠置模式,C1小层坝体间呈进积侧向分隔型及进积侧向叠置型,海岸线迁移速率影响了砂坝间的叠置关系。数值模拟结果及露头资料表明砂坝内部增生体发育模式存在差异,其内部夹层分布模式包括顶积式分布、顶积-侧积式、间隔式3类,在C1小层识别出3类坝体内部夹层分布模式,16号坝体内部夹层呈“顶积-侧积式”的两段式分布特征,19号坝体内部夹层呈“侧积式”分布,顶积式与侧积式夹层的倾角分布区间约1-3°、3-7°,14、15号坝体间夹层呈“间隔式”分布,总结了哈得逊东河砂岩储层砂坝内部夹层的发育模式。【结论】对海相砂质滩坝储层内部构型的精细表征,可有效指导剩余油的挖潜。
Architecture patterns and characterization of marine sandy beach-bar reservoirs- Taking the Donghe Sandstone in Hudson Oilfield as an Example
- Received Date:
2023-12-05
- Available Online:
2024-05-14
Abstract: [Significance] The architecture of marine sandy beach-bar reservoirs is complex, and dominant seepage channels and barriers are developed inside the reservoirs. There is a lack of architecture models for underground reservoirs, which cannot effectively guide the recovery of remaining oil. [Method] In this paper, we have proposed the architecture pattern of marine sandy beach-bar reservoirs by outcrops, satellite photos and numerical simulation with the Hudson Donghe sandstone as the research objective. Under the guidance of the mode, the architecture of the Donghe sandstone reservoir is finely characterized. [Result] The results show that: the depositional architecture of a single sand bar inside composite beach-bar is controlled by many factors such as shoreline shape, coastal slope, wave direction, and height, multiple types of sandbars can be formed, such as conical bar, tight moon bar, positive linear bar, nonlinear inclined bar, and sandy beak bar. Based on the identification of single sandbar boundaries and guided by the architecture mode, 13 sandbars of different sizes were identified in the C1 layer of the study area, including five tight moon bar, seven forward linear bars and one oblique bar, there are differences in quantitative scale between different sanbars. The length of tight moon bar is about 1.5-3 km, the length of the oblique bar is about 4.5-5 km, and the length of the positive linear bar is more than 6 km. The sandbars exhibits both progradational and retrogradational stacking patterns, while the bars in C1 small layer exhibits progradational lateral separation and progradational lateral stacking patterns. The migration rate of the coastline affects the stacking relationship between the sandbars. The numerical simulation results and outcrop data indicate that there are differences in the development patterns of the internal accretion bodies. The distribution patterns of the internal interlayers include top accretion, top accretion-side accretion, and interval type. In the C1 small layer, three types of distribution patterns of the internal interlayers were identified. The internal interlayers in the No. 16 sandbar exhibit a two-stage distribution feature of "top accretion-side accretion", while the internal interlayers in the No. 19 sandbar exhibit a "side accretion". The angle distribution range of the top and side accretion interlayers is about 1-3 ° and 3-7 °, and the interlayers between dam No. 14 and 15 sandbars are distributed in an "interval" pattern. The development pattern of the interlayers inside the bars of Hudson Donghe sandstone reservoir is summarized. [Conclusion] Fine characterization of the internal architecture of marine sandy beach-bar reservoirs can effectively guide the recovery of remaining oil.