Petroleum source rock characterization and hydrocarbon generating potential of sediments from Surghar range, Kohat plateau, Upper Indus Basin

IF 4.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Physics and Chemistry of the Earth Pub Date : 2025-06-01 Epub Date: 2025-01-04 DOI:10.1016/j.pce.2025.103853
Fraz Khalid , Arif Nazir , Saeed Abbas , Munawar Iqbal
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Abstract

This study focusses on the investigation of hydrocarbon generating potential of the Surghar Range Kohat Plateau, Upper Indus. The potential source rock of Paleocene, Cretaceous and Jurassic rocks including the Patala, Hangu, Chichali, SamnaSuk, Shinawari, Datta formations were assessed through geochemical analysis of their well cuttings. These analyses include Rock-Eval Pyrolysis, TOC, Kerogen type, thermal maturity and depositional environment. The TOC, wt. % reveals that sixteen samples of M-03 well of Patala Formation (0.91−10.62 wt %) show excellent quality, while other formations belong to N-02 and C-02 exhibit have fair to good quality of OM. The hydrogen index (HI) values of M-03 oil well for the Patala formation are ranging from 200 to 318 exhibit Type II/III Kerogen. HI value of N-02 well for the Patala Formation are greater than 300 indicates Type II Kerogen whereas other samples show OM of Type III Kerogen. The thermal maturity of the Patala Formation of M-03, N-02 and C-02 oil wells falls in early stage oil window and all the other analyzed formations are thermally immature. Genetic potential is generally in good range except for small number of samples from Chichali, SamanaSuk, Shinawari and Datta formations, which indicate poor genetic potential values. This study uniquely identifies the kerogen types and thermal maturity of under study formations, providing critical insights for understanding their economic viability. By highlighting the differences in organic matter quality across formations, it fills a gap in the existing literature and supports informed decision-making for future exploration efforts.
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上印度河盆地科哈特高原苏尔加尔山脉沉积物烃源岩特征及生烃潜力
本文重点研究了印度河上游的苏尔哈尔山脉、科哈特高原的生烃潜力。通过岩屑地球化学分析,评价了Patala、Hangu、Chichali、SamnaSuk、Shinawari、Datta等古新世、白垩系和侏罗系地层的潜在烃源岩。这些分析包括岩石热解、TOC、干酪根类型、热成熟度和沉积环境。帕塔拉组M-03井16个样品的TOC wt. % (0.91 ~ 10.62 wt %)质量优良,其余N-02和C-02组样品的OM质量一般。M-03油井Patala组氢指数(HI)在200 ~ 318之间,为ⅱ/ⅲ型干酪根。帕塔拉组N-02井的HI值大于300为ⅱ型干酪根,其余样品的OM值为ⅲ型干酪根。M-03、N-02和C-02油井帕塔拉组热成熟度处于早期油窗阶段,其余储层均为热不成熟层。除Chichali、SamanaSuk、Shinawari和Datta地层的少数样品外,遗传潜力一般在良好范围内,这些样品表明遗传潜力价值较差。该研究独特地识别了所研究地层的干酪根类型和热成熟度,为了解其经济可行性提供了关键见解。通过突出不同地层有机质质量的差异,它填补了现有文献的空白,并为未来的勘探工作提供了明智的决策。
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来源期刊
Physics and Chemistry of the Earth
Physics and Chemistry of the Earth 地学-地球科学综合
CiteScore
5.40
自引率
2.70%
发文量
176
审稿时长
31.6 weeks
期刊介绍: Physics and Chemistry of the Earth is an international interdisciplinary journal for the rapid publication of collections of refereed communications in separate thematic issues, either stemming from scientific meetings, or, especially compiled for the occasion. There is no restriction on the length of articles published in the journal. Physics and Chemistry of the Earth incorporates the separate Parts A, B and C which existed until the end of 2001. Please note: the Editors are unable to consider submissions that are not invited or linked to a thematic issue. Please do not submit unsolicited papers. The journal covers the following subject areas: -Solid Earth and Geodesy: (geology, geochemistry, tectonophysics, seismology, volcanology, palaeomagnetism and rock magnetism, electromagnetism and potential fields, marine and environmental geosciences as well as geodesy). -Hydrology, Oceans and Atmosphere: (hydrology and water resources research, engineering and management, oceanography and oceanic chemistry, shelf, sea, lake and river sciences, meteorology and atmospheric sciences incl. chemistry as well as climatology and glaciology). -Solar-Terrestrial and Planetary Science: (solar, heliospheric and solar-planetary sciences, geology, geophysics and atmospheric sciences of planets, satellites and small bodies as well as cosmochemistry and exobiology).
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