中东地区主要碳酸盐岩沉积模式、储层特征及主控因素
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    摘要:

    中东地区碳酸盐岩储层占全球油气可采储量的近半数,其宏观-微观非均质性显著影响油藏开发效果。本研究基于阿联酋、阿曼、伊拉克、伊朗等地区典型油藏多尺度动静态资料,系统划分出缓坡、镶边台地、陆表海缓坡、蒸发台地和淹没台地五种沉积模式,并揭示其演化规律。缓坡与陆表海缓坡早期以加积为主,内缓坡高能带发育生物礁/颗粒滩形成沉积隆起;在海侵背景下,生物礁滩体规模增大,形成障壁礁滩体,最终演变为镶边台地;海退或构造抬升形成蒸发台地,海侵或沉降则转化为淹没台地。储层特征分析表明:缓坡模式主储层为内缓坡颗粒滩;镶边台地以台缘礁滩为主,潟湖潮道相储层高渗但非均质性强;陆表海缓坡发育似球粒颗粒灰岩,储层连续性好且非均质性弱;蒸发台地潮上带白云岩-膏岩-灰岩互层形成复杂储层结构;淹没台地以浮游有孔虫粒泥灰岩为主,呈现高孔低渗特征。研究成果规范了中东碳酸盐岩沉积模式分类体系,阐明了模式间动态演化机制,为优质储层预测和开发方案优化提供了理论依据。

    Abstract:

    The Middle East contains nearly half of global recoverable hydrocarbon reserves, primarily hosted in carbonate reservoirs characterized by multi-scale heterogeneity. Integrating multi-domain static and dynamic data from key oilfields in the United Arab Emirates, Oman, Iraq, and Iran, this study proposes a unified classification framework comprising five typical carbonate sedimentary models: ramp, rimmed platform, epicontinental sea ramp, evaporative platform and submerged platform. These systems exhibit dynamic transitions controlled by sea-level fluctuations and tectonic activities. The ramp and epeiric ramp systems initially develop through aggradation. The inner ramp with high water energy develops biological reefs or shoals to form sedimentary uplifts. Transgressive phases promote barrier reef-shoal expansion, ultimately evolving into rimmed platforms. Evaporative platforms form through sea-level fall or tectonic uplift, whereas subsequent transgression or tectonic subsidence transforms them into a submerged platform model. The ramp model takes the inner ramp shoal as the main reservoir. The rimmed platform model takes the platform margin reef-shoal as the main reservoir. The reservoir of the tidal channel facies in the lagoon has high permeability but strong heterogeneity. The epicontinental sea ramp model develops typical spherulitic granular limestone with good reservoir continuity, large scale and weak heterogeneity. The evaporative platform model has obvious evaporation in the supratidal zone. Dolomite, gypsum and limestone coexist to form a complex internal reservoir structure. The submerged platform model mainly develops planktonic foraminiferal wackestone reservoir. The intrafossil pores of planktonic foraminifera are developed, but the connectivity is poor, showing the characteristics of high porosity and low permeability and weak heterogeneity. By establishing genetic linkages between sedimentary models and reservoir architectures, this study provides a predictive tool for identifying high-quality reservoirs and optimizing development strategies in the Middle East carbonate provinces.

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  • 收稿日期:2025-04-09
  • 最后修改日期:2025-07-06
  • 录用日期:2025-07-07
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