Hydrocarbon potential evaluation of Middle Benue Basin, East Central Nigeria using high resolution aeromagnetic data

Olawale Olakunle Osinowo , Adesoji Olumuyiwa Akanji , Oluseun Adetola Sanuade , Olatubosun Oluwaseyi Esho
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引用次数: 1

Abstract

Relatively cheap and non-intrusive magnetic geophysical technique has been employed to reduce the hydrocarbon exploration uncertainty in the Middle Benue Basin which straddles the northeastern and southeastern parts of Nigeria. Various derivatives and magnetic attributes extracted from the filtered, transformed and enhanced aeromagnetic data of the basin highlighted valuable information employed to appraise the hydrocarbon generating and preservation potentials of the basin, thus delineating the prospective regions where further search light of expensive and intrusive geophysical exploration tools could be focused. The trough delineated from the analyzed aeromagnetic data comprised of a massive 350 km NE-SW trending fan shaped sedimentary body bounded to the northwest and southeast by Basement Complex rocks. Active structural framework with dominant NE-SW fault systems which appeared to be the landward extension of the Chain and Charcot offshore fractures characterize the basement rocks that underlay the sediments. Sedimentary thickness of up to 3.68 km in some parts of the basin obtained from depth weighting analyses, indicate the possibility of hydrocarbon generation through the maturation of organic matter from available source rock(s). Analytic signal grids confirmed the occurrence of already documented volcanic intrusions in addition to newly delineated ones. These volcanics which are often renowned for compromising the hydrocarbon potential of a sedimentary basin are widespread in the western and southern parts the basin. Combination of adequately thick sedimentary units which overly structurally active basement rocks in regions of limited (very few/non) occurrence of volcanic intrusions delineate the north central region for further petroleum exploration prospect evaluation.

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利用高分辨率航磁数据评价尼日利亚中东部贝努埃盆地中部的油气潜力
在横跨尼日利亚东北部和东南部的中贝努埃盆地,采用了相对便宜的非侵入性磁地球物理技术来减少碳氢化合物勘探的不确定性。从经过过滤、转换和增强的盆地航磁数据中提取的各种衍生物和磁性属性突出了用于评估盆地碳氢化合物生成和保存潜力的宝贵信息,从而划定了可以进一步关注昂贵和侵入性地球物理勘探工具的潜在区域。根据分析的航磁数据描绘的槽由一个350公里的东北-西南走向的扇形沉积体组成,该沉积体以基底杂岩为西北和东南边界。活跃的结构框架,具有主要的NE-SW断层系统,似乎是Chain和Charcot近海断裂向陆地延伸,是沉积物下伏基岩的特征。通过深度加权分析获得的盆地某些部分的沉积厚度高达3.68km,表明通过有效烃源岩中有机质的成熟产生碳氢化合物的可能性。分析信号网格证实,除了新划定的火山入侵外,还发生了已有记录的火山入侵。这些火山岩通常以损害沉积盆地的碳氢化合物潜力而闻名,广泛分布在盆地的西部和南部。在火山侵入体出现有限(很少/不出现)的区域内,足够厚的沉积单元(结构过于活跃的基岩)的组合描绘了中北部区域,以进行进一步的石油勘探前景评估。
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