College of Energy and Mining Engineering, Shandong University of Science and Technology, Qingdao, 266590, China.
Institute of Geophysics, Polish Academy of Sciences, Warszawa, 01-452, Poland.
Sci Rep. 2022 Jun 30;12(1):11102. doi: 10.1038/s41598-022-14831-5.
Discoveries of heavy crude oil in the Neoproterozoic rocks (Infracambrian rock sequence) from the Bikaner-Nagaur Basin of India emphasize the significance of studying and exploring the Neoproterozoic source rock potential in the southeastern part of Pakistan. This study evaluates the potential of the source rock in the Infracambrian rock sequence (Salt Range Formation) based on surface geochemical surveys, Rock-Eval pyrolysis, source biomarkers, geophysical characterization, and seismic inversion using machine learning for maturity index estimation. Core samples of Infracambrian rock were extracted for Rock-Eval pyrolysis and biomarker characterization. Additionally, 81 geomicrobial soil and gas samples were collected from the surface to explore the petroleum system and potential source rocks in the subsurface. Advanced interpretation techniques were used to investigate the origin and concentration of hydrocarbon gases at the surface, including Rock-Eval pyrolysis, thermal maturity, source biomarkers, and the environment of deposition of organic matter. The results show that the investigated samples are characterized by restricted marine clay devoid of sedimentary carbonate facies with thermal maturity in the early stage of the oil generation window. The seismic inverted maturity index profile demonstrates a reasonable correlation of thermal maturity with the biomarkers and Rock-Eval pyrolysis. Further scrutiny of the surface geochemical samples confirms the presence of higher concentrations of thermogenic C-C hydrocarbons in the vicinity of anticlinal structures, suggesting the existence of an effective migration path along deep-seated faults to the surface. This study concludes that the Infracambrian rocks on the eastern flank of Pakistan are thicker, thermally mature, and have deep-seated structural closures, indicating a greater probability of heavy and light oil in this area than in the Bikaner-Nagaur Basin, India.
在印度比卡内尔-那加乌尔盆地的新元古代岩石(下寒武统地层)中发现重质稠油,这强调了研究和勘探巴基斯坦东南部新元古代烃源岩潜力的重要性。本研究基于地表地球化学调查、岩石热解分析、源生物标志物、地球物理特征以及使用机器学习进行成熟度指数估算的地震反演,评估了下寒武统地层(盐岭组)中源岩的潜力。提取了下寒武统岩石的岩心样本进行岩石热解分析和生物标志物特征分析。此外,从地表采集了 81 个地球微生物土壤和气体样本,以探索地下的石油系统和潜在源岩。先进的解释技术用于研究地表碳氢气体的来源和浓度,包括岩石热解分析、热成熟度、源生物标志物和有机质沉积环境。结果表明,所研究的样品具有限制型海洋粘土特征,缺乏沉积碳酸盐相,热成熟度处于生油窗的早期阶段。地震反演的成熟度指数剖面表明,热成熟度与生物标志物和岩石热解分析具有合理的相关性。对地表地球化学样本的进一步研究证实了在背斜构造附近存在更高浓度的热成因 C-C 碳氢化合物,这表明沿着深部断层存在有效的运移途径到达地表。本研究得出结论,巴基斯坦东侧的下寒武统岩石较厚、热成熟度较高且具有深部构造封闭性,表明该地区比印度比卡内尔-那加乌尔盆地更有可能存在重质油和轻质油。