Quantifying the mineral magnetic signature of petroleum systems and their source rocks: A study on the Inner Moray Firth, UK North Sea

IF 2.8 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Geophysical Journal International Pub Date : 2024-07-23 DOI:10.1093/gji/ggae254
J R Perkins, A R Muxworthy, A J Fraser, P Hu
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Abstract

Summary This study aims to expand on existing connections between magnetic minerals and hydrocarbons within petroleum systems. Previous studies have focussed on single-source petroleum systems whereas this study, for the first time, analyses a multi-source petroleum system to investigate potential correlations between different kerogen type source rocks and magnetic minerals. To do this, the study investigates the magnetic mineral characteristics of the Inner Moray Firth (IMF), UK North Sea, through room-, low-, and high-temperature techniques, and correlates this to published basin and petroleum systems modelling results that show a three-source hydrocarbon mix. Magnetic mineral analysis identifies extensive evidence for magnetite, goethite, and siderite, alongside more minor lepidocrocite and iron sulphides. Although we find that magnetite is ubiquitous within the IMF, its abundance is relatively low, and, in contrast, the relatively magnetically weak goethite is more likely the most abundant magnetic mineral throughout the IMF. In agreement with previous studies, we find magnetic enhancement at oil-water contacts (OWCs); however, here, we identify two different magnetic enhancement processes at OWCs in wells, which are dependent on the amount of sulphur available in the local environment. Wells with low levels of sulphur have increasing levels of magnetite towards the OWC, with the magnetic enhancement occurring at the top of the water-saturated section. Sulphur-rich environments display an increase in iron sulphides near the OWC at the bottom of the oil-saturated sediments. Additionally, we confirm the presence of siderite as indicator of upward vertical migration. Combining with petroleum system model predictions, we find direct links between iron hydroxide presence and Type I and II-III kerogen source rocks, and iron sulphide presence with Type II kerogen source rocks. This study shows the potential for further utilisation of magnetic mineral analysis within hydrocarbon exploration and petroleum system definition.
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量化石油系统及其源岩的矿物磁特征:英国北海内莫里峡湾研究
摘要 本研究旨在拓展石油系统中磁性矿物与碳氢化合物之间的现有联系。以往的研究侧重于单源石油系统,而本研究则首次分析了多源石油系统,以研究不同的角质源岩和磁性矿物之间的潜在关联。为此,该研究通过室温、低温和高温技术研究了英国北海内莫里峡湾(IMF)的磁性矿物特征,并将其与已公布的盆地和石油系统建模结果(显示了三源碳氢化合物组合)相关联。磁性矿物分析确定了磁铁矿、鹅铁矿和菱铁矿的大量证据,以及更少量的鳞铁矿和硫化铁。尽管我们发现磁铁矿在 IMF 中无处不在,但其丰度相对较低,相比之下,磁性相对较弱的鹅铁矿更有可能是整个 IMF 中最丰富的磁性矿物。与之前的研究一致,我们在油水接触点(OWCs)发现了磁性增强现象;不过,在这里,我们在油井的 OWCs 发现了两种不同的磁性增强过程,这取决于当地环境中的硫含量。硫含量低的油井中,磁铁矿的含量向 OWC 方向不断增加,磁性增强发生在水饱和段的顶部。硫含量丰富的环境显示,在石油饱和沉积物底部的 OWC 附近,硫化铁含量增加。此外,我们还证实菱铁矿的存在是向上垂直迁移的指标。结合石油系统模型的预测,我们发现氢氧化铁的存在与 I 类和 II-III 类角质源岩有直接联系,硫化铁的存在与 II 类角质源岩有直接联系。这项研究显示了在油气勘探和石油系统定义中进一步利用磁性矿物分析的潜力。
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来源期刊
Geophysical Journal International
Geophysical Journal International 地学-地球化学与地球物理
CiteScore
5.40
自引率
10.70%
发文量
436
审稿时长
3.3 months
期刊介绍: Geophysical Journal International publishes top quality research papers, express letters, invited review papers and book reviews on all aspects of theoretical, computational, applied and observational geophysics.
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