活跃水动力机制下深水浊积层的特征(尼日尔三角洲)

IF 3.7 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
V. Spina , S. Amoyedo , C. Wibberley , R. Tozer , C. Ribes , R. Maia , H. Atoyebi , E. Vincent
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引用次数: 0

摘要

埃吉纳油田位于尼日尔三角洲东部的深水区,其特征是一条东北-西南走向的反斜线,其中包含几个中新世至上新世的层状储层。值得注意的是,油田中的一个储层包括三个砂质层段,已被确定为深海浊积岩系统。最底层(区间 1)由一个叶状复合体组成,而最上层的区间 2 和区间 3 则由侵蚀通道复合体组成。这三个储层区间既有静态沟通,也有部分动态沟通。埃吉纳油气田受到连贯的伸展和斜滑断层网络的影响,目前的活动仅限于该构造的东部。大的位移断层(投掷>30米)抵消了单个储层区间,造成横向断开,成为流体跨断层流动的障碍。油井测试和四维地震数据显示,NNE-SSW向的小断层会在局部阻挡流体流动。然而,油井干扰测试表明,储层内部沟通良好。储油层间的侵蚀接触促进了层叠砂体之间的垂直沟通,而东北-西南方向的横向沟通则通过中继斜坡和断层尖部发生在分段断层周围。在整个油田,已经确定了 10 个油水接触点,总体趋势是向南加深。这种模式被解释为由活跃的水动力机制引起的倾斜接触,含水层超压从北向南逐渐降低(相差 31 米),与区域趋势一致。本文介绍了深水浊积岩储层在静态和动态条件下的地质(结构和沉积)异质性。本文介绍的工作显示了地质分析如何影响储层管理,推动油田开发的战略决策,如确定注水井机会或优化注水井位置,以有效支持生产者。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterization of a deep-water turbiditic reservoir under an active hydrodynamic regime (Niger delta)
The Egina Field, situated in the deep-water region of the eastern Niger Delta, is characterized by a NE-SW trending anticline that contains several Middle to Upper Miocene stacked reservoirs. Notably, one of the reservoirs in the field includes three sandy intervals, which have been identified as deep marine turbidite systems. The lowest level (Interval 1) comprises a lobe complex, while the uppermost Intervals 2 and 3 consist of erosive channel complexes. These three reservoir intervals exhibit both static and partial dynamic communication. The Egina Field is affected by a coherent network of extensional and oblique-slip faults, with current activity confined to the eastern sector of the structure. Large displacement faults (throw >30m) offset individual reservoir intervals, creating lateral disconnection and acting as barriers to fluid flow across faults. Minor NNE-SSW oriented faults can locally baffle the flow of fluids, as evidenced by well tests and 4D seismic data. Nonetheless, well interference tests suggest good communication within the reservoir. Vertical communication between the stacked sand bodies is facilitated through erosional contacts between reservoir intervals, while lateral communication occurs around segmented faults, via relay ramps and fault tips, in a NE-SW direction. Across the field, ten oil-water contacts have been identified, with a general trend of deepening towards the south. This pattern has been interpreted as a tilted contact caused by an active hydrodynamic regime, where aquifer overpressures gradually decrease from north to south (31 m of difference), aligning with the regional trend. This paper describes how the geological (structural and sedimentological) heterogeneities are paramount in deep-water turbiditic reservoirs, for both static and dynamic conditions. The work presented here shows how the geological analysis can impact reservoir management, driving strategic decisions on field development, as such as the identification of infill wells opportunities or the optimizing the placement of injectors wells, to effectively support producers.
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来源期刊
Marine and Petroleum Geology
Marine and Petroleum Geology 地学-地球科学综合
CiteScore
8.80
自引率
14.30%
发文量
475
审稿时长
63 days
期刊介绍: Marine and Petroleum Geology is the pre-eminent international forum for the exchange of multidisciplinary concepts, interpretations and techniques for all concerned with marine and petroleum geology in industry, government and academia. Rapid bimonthly publication allows early communications of papers or short communications to the geoscience community. Marine and Petroleum Geology is essential reading for geologists, geophysicists and explorationists in industry, government and academia working in the following areas: marine geology; basin analysis and evaluation; organic geochemistry; reserve/resource estimation; seismic stratigraphy; thermal models of basic evolution; sedimentary geology; continental margins; geophysical interpretation; structural geology/tectonics; formation evaluation techniques; well logging.
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