碳酸盐-硅质岩混合储层层序地层框架中的沉积和成岩异质性:波斯湾渐新世-中新世阿斯玛里地层案例研究

IF 2.7 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Yasaman Ahmadi, Hamzeh Mehrabi, Mohammad Hasani, Mohsen Ranjbaran
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引用次数: 0

摘要

混合硅质碎屑岩-碳酸盐岩储层(如扎格罗斯盆地的阿斯玛里地层)具有显著的异质性,影响着油气勘探和生产。本研究采用多种方法,包括岩相分析、岩石物理测量、岩心 CT 扫描、X 射线衍射和筛分分析,对波斯湾西北部 Asmari 地层的沉积和成岩异质性进行了研究。主要目的是在层序地层框架内确定这些异质性的起源、规模和可预测性,以加强储层特征描述。地貌分析显示,沉积环境从沙坝到海岸面、潮周、泻湖和浅滩,碳酸盐沉积被与海平面波动相关的碎屑涌入打断。通过岩相分析,确定了包括白云石化、溶解、胶结和断裂在内的成因过程,并强调了这些过程对储层质量的影响。为了量化这些异质性并划分储层流动单元,采用了温兰分类法、水力流动单元(HFU)分析法和洛伦兹分带法等方法。结果表明,沉积异质性主要由海平面变化驱动,范围从小到大,并可在层序地层背景下进行预测。二源变化对孔隙度和渗透率有很大影响,白云石化会提高储层潜力,而压实和胶结则会降低储层潜力。压裂,尤其是在下阿斯玛里碳酸盐岩中,可提高渗透率。研究得出结论,准确识别和模拟储层的三维异质性可以极大地改进波斯湾的勘探和开发战略。更好地了解优质储层带和防渗挡板层的空间分布,将有助于更精确地布井、优化油气回收并降低勘探风险。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Depositional and diagenetic heterogeneities in sequence stratigraphic framework of a mixed carbonate-siliciclastic reservoir: A case study from Oligocene–Miocene Asmari Formation in the Persian Gulf
Mixed siliciclastic–carbonate reservoirs, such as the Asmari Formation in the Zagros Basin, present significant heterogeneities that influence hydrocarbon exploration and production. This study examines the depositional and diagenetic heterogeneities of the Asmari Formation in the northwest Persian Gulf through a multi-methodological approach, including petrographic analysis, petrophysical measurements, core CT-scanning, X-ray diffraction, and sieve analysis. The primary goal is to identify the origins, scales, and predictability of these heterogeneities within a sequence stratigraphic framework to enhance reservoir characterization. Facies analysis reveals depositional environments ranging from sabkha to shoreface, peritidal, lagoonal, and shoal settings, with carbonate sedimentation interrupted by clastic influxes associated with sea-level fluctuations. Diagenetic processes, including dolomitization, dissolution, cementation, and fracturing, were identified through petrographic analysis, highlighting their effects on reservoir quality. To quantify these heterogeneities and delineate reservoir flow units, methods such as Winland classification, hydraulic flow unit (HFU) analysis, and Lorenz zonation were applied. Results show that depositional heterogeneities, predominantly driven by sea-level changes, range from small to large scales and can be predicted within a sequence stratigraphic context. Diagenetic modifications substantially affect porosity and permeability, with dolomitization improving reservoir potential, while compaction and cementation tend to reduce it. Fracturing, particularly in the lower Asmari carbonates, enhances permeability. The study concludes that accurately recognizing and modeling reservoir heterogeneities in three dimensions can significantly improve exploration and development strategies in the Persian Gulf. A better understanding of the spatial distribution of high-quality reservoir zones and impermeable baffle layers will facilitate more precise well placement, optimize hydrocarbon recovery, and mitigate exploration risks.
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来源期刊
Journal of Asian Earth Sciences
Journal of Asian Earth Sciences 地学-地球科学综合
CiteScore
5.90
自引率
10.00%
发文量
324
审稿时长
71 days
期刊介绍: Journal of Asian Earth Sciences has an open access mirror journal Journal of Asian Earth Sciences: X, sharing the same aims and scope, editorial team, submission system and rigorous peer review. The Journal of Asian Earth Sciences is an international interdisciplinary journal devoted to all aspects of research related to the solid Earth Sciences of Asia. The Journal publishes high quality, peer-reviewed scientific papers on the regional geology, tectonics, geochemistry and geophysics of Asia. It will be devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be included. Papers must have international appeal and should present work of more than local significance. The scope includes deep processes of the Asian continent and its adjacent oceans; seismology and earthquakes; orogeny, magmatism, metamorphism and volcanism; growth, deformation and destruction of the Asian crust; crust-mantle interaction; evolution of life (early life, biostratigraphy, biogeography and mass-extinction); fluids, fluxes and reservoirs of mineral and energy resources; surface processes (weathering, erosion, transport and deposition of sediments) and resulting geomorphology; and the response of the Earth to global climate change as viewed within the Asian continent and surrounding oceans.
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