Sequence stratigraphy and petrophysical evaluation controls on fluvial to fluvio-marine reservoirs in the syn- and post-rift sediments: Insights into in the Kharita and Bahariya Formations, West Beni Suef basin

IF 2.2 4区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of African Earth Sciences Pub Date : 2025-06-01 Epub Date: 2025-02-19 DOI:10.1016/j.jafrearsci.2025.105568
Amer A. Shehata , Mohammad Abdelfattah Sarhan , Ramadan Abdelrehim , Kamal Abdelrahman , Mohammed S. Fnais , Amir Ismail
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Abstract

Hydrocarbon occurrence in rift basins is largely governed by tectonic styles and basin-fill stratigraphy, with abundant potential reservoirs found throughout the syn-rift and post-rift successions. This study conducts a sequence stratigraphic analysis and petrophysical evaluation of the Albian-Cenomanian syn- and post-rift successions in the Beni Suef (BS) rift basin. The Albian Fluviatile Kharita Formation is deposited in the syn-rift phase, while the fluvio-marine Bahariya Formation is deposited in the post-rift phase of the BS basin. The studied succession is divided into three depositional sequences: SQLKH-1 & SQUKH-2 in the Kharita Formation and SQBAH-3 in the Bahariya Formation. SQLKH-1 and SQUKH-2 are siliciclastic-dominated units developed in a long-lasting fluviatile setting with some shallow marine shale deposits in the lower levels of SQLKH-1, while the SQBAH-3 is a siliciclastic unit with carbonate interbeds developed initially in fluvio-deltaic setting and become shallow marine upwards. Petrophysical analysis has been conducted to evaluate hydrocarbon potential and reservoir characteristics of the Kharita and Bahariya formations across several wells. With effective porosity values between 0.09 and 0.14 and average shale volumes of about 0.10, the Kharita Formation exhibits good reservoir quality but limited hydrocarbon saturation, indicating potential suitability for CO2 sequestration rather than hydrocarbon production. The Bahariya Formation demonstrates superior reservoir potential, with low shale volumes (<10%) and effective porosity ranging from 10% to 20%, highlighting its suitability for hydrocarbon exploration. The considerable variation in water saturation between wells from 25% to 75% highlights localized heterogeneity. Potential hydrocarbon accumulation zones are identified in wells with lower water saturation, like Azhar A2 and Azhar E−2X. These results highlight the importance of site-specific reservoir management to maximize production and the Bahariya Formation's superior suitability for hydrocarbon exploration when compared to the Kharita Formation.
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层序地层学和岩石物性评价对同裂谷和后裂谷沉积中河流-河流-海相储层的控制作用——以西贝尼苏韦夫盆地哈里塔组和巴哈里亚组为例
裂谷盆地油气赋存状态主要受构造样式和盆填地层控制,在同裂谷和后裂谷序列中发现了丰富的潜在储集层。本文对贝尼苏夫裂谷盆地的阿尔-塞诺曼尼亚同裂谷和后裂谷序列进行了层序地层学分析和岩石物理评价。阿尔比安河相哈里塔组沉积于同裂谷期,而河相-海相巴哈里亚组沉积于裂谷后期。研究层序分为三个层序:SQLKH-1 &;Kharita组的sqkh -2和Bahariya组的sqba -3。SQLKH-1和sqkh -2是在长期的河流沉积环境中发育的以硅屑为主的单元,在SQLKH-1下部有浅海页岩沉积,而sqah -3则是在河流-三角洲环境中初步发育碳酸盐互层的硅屑单元,向上发育为浅海沉积。通过对几口井的岩石物理分析,评价了Kharita和Bahariya地层的油气潜力和储层特征。哈里塔组有效孔隙度值在0.09 ~ 0.14之间,页岩平均体积约为0.10,储层质量良好,但含油气饱和度有限,可能适合封存CO2而非生产油气。巴哈里亚组页岩体积低(10%),有效孔隙度在10% ~ 20%之间,具有较好的储层潜力,适合油气勘探。井间含水饱和度从25%到75%之间的巨大差异突出了局部非均质性。在含水饱和度较低的井(如Azhar A2和Azhar E - 2X)中确定了潜在的油气聚集带。这些结果强调了针对特定地点的油藏管理对于最大限度地提高产量的重要性,以及与Kharita组相比,Bahariya组更适合油气勘探。
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来源期刊
Journal of African Earth Sciences
Journal of African Earth Sciences 地学-地球科学综合
CiteScore
4.70
自引率
4.30%
发文量
240
审稿时长
12 months
期刊介绍: The Journal of African Earth Sciences sees itself as the prime geological journal for all aspects of the Earth Sciences about the African plate. Papers dealing with peripheral areas are welcome if they demonstrate a tight link with Africa. The Journal publishes high quality, peer-reviewed scientific papers. It is devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be considered. Papers must have international appeal and should present work of more regional than local significance and dealing with well identified and justified scientific questions. Specialised technical papers, analytical or exploration reports must be avoided. Papers on applied geology should preferably be linked to such core disciplines and must be addressed to a more general geoscientific audience.
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