Source Rock Characterization for the Hydrocarbon Generative Potential and Thermal Maturity of Carboniferous Strata in the Tendrara–Missour Basin, Northeastern Morocco

IF 1.1 4区 工程技术 Q3 CHEMISTRY, ORGANIC
Achour Margoum, Youssef Elbouazaoui, Mohammed Et-Touhami, Rabah Bouchta, Abdelwahid Chakor Alami
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Abstract

The Tendrara–Missour Basin in eastern Morocco hosts the country's largest gas field, featuring a proven petroleum system with Paleozoic source rocks and a Triassic siliciclastic reservoir sealed by Late Triassic and Early Jurassic salt formations. This study evaluated the hydrocarbon generative potential and thermal maturity of Carboniferous source rocks via geochemical analysis of 215 samples from four wells (OSD-1, TE-1, TE-2, and TE-3). The results indicate that the majority of the samples were characterized by a poor to fair content of organic matter, with the total organic carbon (TOC) values less than 1%. These samples were composed mainly of type III (gas prone) and type IV (non-generative) kerogen, with the hydrogen index (HI) < 150 mg HC/g TOC. However, certain intervals, particularly in the OSD-1 well, displayed excellent source rock characteristics with the TOC values exceeding 4% and a mixture of the type II/III kerogen with the HI values exceeding 150 mg HC/g TOC. The maturity levels across the well ranged from immature to post-mature, with vitrinite values varied within 0.58–2.56%. The burial history modeling in the OSD-1 and TE-3 wells indicated that the hydrocarbon generation from the Carboniferous source rocks started during the Late Carboniferous–Permian period, i.e., during the Hercynian orogeny. Volumetric calculations based on the Monte Carlo simulation estimated the generative potential of the Carboniferous source rocks to be approximately 200 000 tons/km2 (P50). The accumulated volumes derived from the Carboniferous source rocks (P50) are estimated at approximately 300 million barrels of oil and 2.5 trillion cubic feet (TCF) of gas.

Abstract Image

Abstract Image

摩洛哥东北部Tendrara-Missour盆地石炭系烃源岩生烃潜力及热成熟度表征
摩洛哥东部的Tendrara-Missour盆地拥有该国最大的天然气田,其已探明的油气系统包括古生代烃源岩和三叠纪的硅碎屑储层,这些储层被晚三叠世和早侏罗世的盐层封闭。本研究通过对4口井(OSD-1、TE-1、TE-2和TE-3) 215个样品的地球化学分析,评估了石炭系烃源岩的生烃潜力和热成熟度。结果表明,大部分样品有机质含量较差,总有机碳(TOC)值小于1%。这些样品主要由III型(易气)和IV型(非生烃)干酪根组成,氢指数(HI)为150 mg HC/g TOC。然而,某些层段,特别是在OSD-1井中,显示出良好的烃源岩特征,TOC值超过4%,HI值超过150 mg HC/g TOC的II/III型干酪根混合物。整个井的成熟度水平从未成熟到后成熟不等,镜质组值在0.58-2.56%之间变化。OSD-1井和TE-3井埋藏史模拟表明,石炭系烃源岩生烃始于晚石炭-二叠世,即海西期造山运动。基于蒙特卡罗模拟的体积计算估计,石炭系烃源岩的生成潜力约为20万吨/平方公里(P50)。石炭系烃源岩(P50)的累积体积估计约为3亿桶石油和2.5万亿立方英尺(TCF)天然气。
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来源期刊
Petroleum Chemistry
Petroleum Chemistry 工程技术-工程:化工
CiteScore
2.50
自引率
21.40%
发文量
102
审稿时长
6-12 weeks
期刊介绍: Petroleum Chemistry (Neftekhimiya), founded in 1961, offers original papers on and reviews of theoretical and experimental studies concerned with current problems of petroleum chemistry and processing such as chemical composition of crude oils and natural gas liquids; petroleum refining (cracking, hydrocracking, and catalytic reforming); catalysts for petrochemical processes (hydrogenation, isomerization, oxidation, hydroformylation, etc.); activation and catalytic transformation of hydrocarbons and other components of petroleum, natural gas, and other complex organic mixtures; new petrochemicals including lubricants and additives; environmental problems; and information on scientific meetings relevant to these areas. Petroleum Chemistry publishes articles on these topics from members of the scientific community of the former Soviet Union.
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