Analysis of airborne potential field data for hydrocarbon exploration in Southern Nigeria

Ayodeji Hansen Ayoola, Olawale Olakunle Osinowo
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引用次数: 5

Abstract

The reservoir component of the petroleum system of the Niger – Delta has historically been accessed at depths ranging between 3.5 and 4.5 km, even though the Delta's sedimentary thickness is put at a maximum of 12 km as the basin has never been drilled to basement. The conventional assumption of the depth extent of reservoir facies within the Delta have been put to question as recent forays past the known limits yielded hydrocarbon production. Filtered, transformed, and enhanced airborne gravity and magnetic data acquired over the Niger Delta, southern Nigeria, were therefore analyzed to gain insight into the interval that has remained unexplored. A careful consideration of the zone suggests that the unexplored interval may accommodate interesting rock units and structures that could support the generation and preservation of hydrocarbon within some parts of the interval. Combined Spectral Depth Analysis (SDA) and 3D Euler Deconvolution employed to determine depth range to basement within the entire Niger Delta indicate that depth to basement rocks beneath the sedimentary unit ranges from 10–15 km, thus suggesting the presence of a Cretaceous sedimentary interval beneath the current drill depths that might be at least 6 km thick. Structural analyses of the basement rocks as well as the basement topography could reveal interesting structural pattern which when reactivated possibly engendered sedimentary structures within the sediments overlying them. Relevant information, such as generated from this study is expected to motivate interest to focus exploration target beyond the current drilling depth.

尼日利亚南部油气勘探机载势场数据分析
尼日尔三角洲油气系统的储层部分历史上在3.5至4.5公里的深度范围内被发现,尽管三角洲的沉积厚度最大为12公里,因为盆地从未钻探到基底。由于最近的勘探突破了已知的油气产量极限,对三角洲内储层相深度范围的传统假设受到了质疑。因此,对尼日利亚南部尼日尔三角洲采集的航空重磁数据进行了过滤、转换和增强分析,以深入了解尚未勘探的层段。对该区域的仔细考虑表明,未勘探的层段可能包含有趣的岩石单元和结构,这些岩石单元和结构可能支持层段某些部分的油气生成和保存。综合光谱深度分析(SDA)和三维欧拉反褶积(3D Euler Deconvolution)用于确定整个尼日尔三角洲到基底的深度范围,表明沉积单元下的基底岩石深度在10-15公里之间,从而表明在当前钻探深度下存在白垩纪沉积层,厚度可能至少为6公里。对基底岩石和基底地形的结构分析可以揭示有趣的结构模式,当这些结构模式被重新激活时,可能会在其上的沉积物中形成沉积结构。相关信息,例如从这项研究中产生的信息,有望激发人们对当前钻井深度以外的重点勘探目标的兴趣。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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