Hydrocarbon production potential of paralic reservoirs from the Niger Delta basin: Evidence from ichnological studies

O.O. Efemena, C. Ugwueze
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Abstract

Reservoir ichnological study was employed to improve on the inconsistencies and poor interpretation of hydrocarbon-bearing strata within the multipartite maturing terrain of the onshore Niger Delta basin. Ichnofacies characterization revealed two distinctive trace fossil suites that both reflected different feeding behaviours and responses to substrate consistency, which assisted in the high-resolution assessment of facies constituting the paralic reservoirs. Fifteen potential reservoir intervals were subdivided into productive and non-productive as revealed on core slabs as well as well log signatures. Fluctuating river sediment influx has been considered to be detrimental to the colonization of the channel deposits and barrier bars, which resulted in excellent hydrocarbon reservoirs in the study area. The sandstone facies, characterized by sparse bioturbation and extensive bedding, displays imprints of Ophiomorpha, Thalassinoides, and Palaeophycus. The removal of these imprints has minimized subtle heterogeneities, resulting in more uniform reservoir characteristics. This uniformity has favored the accumulation of hydrocarbons within the point bars.Biogenicchurning of bedded sediment generated a poorer sorting index thereby reducing the reservoir quality at 9866-9840ft, 9154-9120ft, and 9090- 060ft depth intervals, which has been interpreted to represent poor reservoir potentials. However, it is advised that future investigations should focus on the forced regressive shoreface and delta front reservoirs of the studied interval for its internal continuity that may contain maximum production potential. 
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尼日尔三角洲盆地副岩储层的碳氢化合物生产潜力:岩石学研究的证据
采用储层痕量化石研究来改善尼日尔三角洲陆上盆地多岩层成熟地形中含烃地层的不一致性和解释不清的问题。痕量化石特征研究揭示了两种截然不同的痕量化石组合,它们都反映了不同的取食行为和对基质一致性的反应,这有助于对构成副岩储层的岩相进行高分辨率评估。根据岩心板和测井记录的特征,将 15 个潜在储层区间细分为生产性和非生产性储层。波动的河流沉积物流入量被认为不利于河道沉积物和屏障条石的定殖,这导致了研究区域极佳的碳氢化合物储层。砂岩面具有稀疏的生物扰动和广泛的层理特征,显示出 Ophiomorpha、Thalassinoides 和 Palaeophycus 的印记。这些印记的去除最大程度地减少了细微的异质性,从而使储层特征更加统一。这种均匀性有利于碳氢化合物在点条内的积累。层状沉积物的生物燃烧产生了较差的分选指数,从而降低了 9866-9840 英尺、9154-9120 英尺和 9090- 060 英尺深度区间的储层质量,这被解释为储层潜力较差。不过,建议今后的勘探工作应重点关注所研究区间的强制回归岸面和三角洲前沿储层,因为其内部连续性可能蕴含着最大的生产潜力。
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