东营凹陷沙二段沉积特征再认识及油气精细勘探意义
Re-Understandings of Sedimentary Features and Hydrocarbon Implications of the Second Member (Es2) Interval of Shahejie Formation, Dongying Sag
DOI: 10.12677/AG.2023.138084, PDF,    科研立项经费支持
作者: 李 扬, 彭威龙:中国石化石油勘探开发研究院,北京;石 磊:中海石油深圳分公司南海东部石油研究院,广东 深圳
关键词: 东营凹陷浪控三角洲滩坝古气候隐蔽圈闭Dongying Sag Wave-Dominated Delta Sand Shoals and Bank Paleoclimate Subtle Trap
摘要: 东营凹陷沙二段是勘探程度较高的陆相盆地含油气层系,基于岩芯观察、测录井及地震资料系统分析,开展了沙二段沉积特征再认识研究。认为沙二段不仅发育建设期三角洲,同样发育改造期和破坏期三角洲沉积类型。其中沙二下亚段表现为早期建设性、中期快速湖侵期改造–破坏性和晚期建设性三角洲特征;沙二上亚段先后发育干旱气候–弱物源–改造性三角洲和湿润气候–建设/改造性三角洲。三角洲沉积特征及其演化主要由盆地抬升与剥蚀过程、古气候及物源输入、古地理及古风浪等因素控制。改造型(如河口坝、沿岸砂坝复合体)和破坏型(滩坝)三角洲砂体在东营凹陷富油气盆地中较为广泛发育,是寻找隐蔽圈闭及增储上产值得关注的重要领域。
Abstract: The second member (Es2) of Shahejie Formation, Dongying Sag, is a high-maturity hydrocarbon interval in China. Based on core observations, well and seismic data, this study conducted a sedimentary investigation for Es2 of Shahejie Formation. The results showed that besides the development of constructive river-derived delta, both the reworked and destroyed delta formed in Dongying paleo-lake. The lake experienced early constructive, medium reworked to destroyed, late constructive delta in the lower phase of Es2, Shahejie Formation. The upper interval of Es2 experienced weak source input and reworked delta process under arid paleo-climate settings, followed by constructive and reworked delta process under humid paleo-climate environment. The sedimentary system is controlled by tectonic activities, deposits source inputting, paleo-climate and paleo-wind directions during Eocene to Oligocene time. The reworked sandbodies, such as mouth-bars, banks along shoreline, and sand shoals, see as important targets for oil exploration in mature hydrocarbon basins.
文章引用:李扬, 彭威龙, 石磊. 东营凹陷沙二段沉积特征再认识及油气精细勘探意义[J]. 地球科学前沿, 2023, 13(8): 879-890. https://doi.org/10.12677/AG.2023.138084

参考文献

[1] 宋明水, 王永诗, 李友强. 成熟探区“层勘探单元”划分与高效勘探[J]. 石油勘探与开发, 2018, 45(3): 520-527.
[2] 王居峰. 济阳坳陷东营凹陷古近系沙河街组沉积相[J]. 古地理学报, 2005, 7(1): 45-58.
[3] 姜在兴.沉积学 [M]. 第2版. 北京: 石油工业出版社, 2010.
[4] 秦祎, 朱世发, 朱筱敏, 等. 东营凹陷南缓坡浅水三角洲沉积特征与源-汇过程[J]. 地球科学, 2017, 42(11): 2081-2094.
[5] 胜利油田石油地质志编写组. 中国石油地质志(卷六) [M]. 北京: 石油工业出版社, 1993.
[6] 杨家福. 胜坨油田砂体沉积类型与储层特征[J]. 石油学报, 1988, 9(2): 43-56.
[7] 宋明水. 胜坨油田成藏条件及勘探开发关键技术[J]. 石油学报, 2021, 42(1): 129-142.
[8] 苏宗富, 邓宏文, 陶宗普, 等. 济阳坳陷古近系区域层序地层格架地层特征对比[J]. 古地理学报, 2006, 8(1): 89-102.
[9] 姚益民. 济阳坳陷的沙二段及其相关的不整合面[J]. 石油勘探与开发, 1988(3): 1-10.
[10] 王永诗, 郝雪峰, 胡阳. 富油凹陷油气分布有序性与富集差异性——以渤海湾盆地济阳坳陷东营凹陷为例[J]. 石油勘探与开发, 2018, 45(5): 41-50.
[11] 崔文富, 沈志晗, 姜在兴, 贺丽容, 王成, 张家志, 等. 东营凹陷胜坨油田一区沙河街组二段1砂组砂体微相研究[J]. 地学前缘, 2023, 30(3): 452-464.
[12] 朱宗浩, 范乃敏, 罗华仪. 胜利油区第三纪气候[J]. 山东地质, 2000, 16(1): 22-28.
[13] Ao, H., Dupont-Nivet, G., Rohling, E.J., et al. (2020) Orbital Climate Variability on the Northeastern Tibetan Plateau across the Eocene-Oligocene Transition. Nature Communications, 11, Article No. 5249. [Google Scholar] [CrossRef] [PubMed]
[14] Liu, Z., Huang, C., Algeo, T.J., et al. (2018) High-Resolution As-trochronological Record for the Paleocene-Oligocene (66-23Ma) from the Rapidly Subsiding Bohai Bay Basin, Northeastern China. Palaeogeography, Palaeoclimatology, Palaeoecology, 510, 78-92. [Google Scholar] [CrossRef
[15] 姜在兴, 主编. 风场-物源-盆地系统沉积动力学: 沉积体系成因解释与分布预测新概念[M]. 北京: 科学出版社, 2016.
[16] Graham, S.A., Carroll, A.R. and Ping, L. (2010) Tectonic and Stratigraphic Evolution of Nonmarine Basins of China. Basin Research, 22, 1-2. [Google Scholar] [CrossRef