首页> 外文期刊>Arabian journal of geosciences >Evolution of petroleum generation and expulsion of the oil-source rock in the north-western Say'un-Masilah Basin as inferred from 1D basin models of a single well (Al-Qarn-01)
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Evolution of petroleum generation and expulsion of the oil-source rock in the north-western Say'un-Masilah Basin as inferred from 1D basin models of a single well (Al-Qarn-01)

机译:北方南部南部的油源岩石的石油生成和驱逐油源岩的演变为1D盆地(Al-Qarn-01)的1D盆地模型推断出来

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The Madbi Shale Formation is the main oil-source rock for conventional petroleum extraction in the east-central Say'un-Masilah Basin. This study explores the generation and expulsion potential of oil from the Madbi source rock system in a deep well location (Al-Qarn-01) in the north-western Say'un-Masilah Basin using geological and geochemical modelling. One-dimensional (1D) basin models were constructed to the estimate thermal regime in the basin and the evolution of oil cracking and expulsion from the organic-rich intervals in the Madbi Formation over the geological time. In the studied Al-Qarn-01 well, the organic-rich intervals in the Madbi Formation are thermally mature, ranging from peak- to late-mature oil window stages; thus, half or more of the kerogen was converted to oil at these maturity stages. The basin modelling results of the studied well (Al-Qarn-01) show that oil was generated and expelled from Madbi source rock intervals in two main phases according to the conversion ratio (TR %) of kerogen. The main conversion of kerogen to oil (TR = 10-50%) occurred between Late Cretaceous and Early Oligocene (80-33 Ma) periods, corresponding to the peak-oil window (0.70-1.00 Easy %R-o)(.)Furthermore, significant amounts of oil were expelled from the source rock, which subsequently migrated into the overlying reservoir rocks in the Early Oligocene time during the initial Tertiary rifting. The late-mature oil window (1.00-1.10 Easy %R-o) commenced during this time, with TRs of 50-77%.
机译:Madbi Shale Mape Mail是东部地区的常规石油萃取的主要油源岩石。本研究探讨了北 - 西部的北部的地理位置(Al-Qarn-01)中的Madbi Source Rock System的发电和驱逐潜力,使用地质和地球化学建模。一维(1D)盆地模型被构建为盆地中的估计热调节和油裂的进化和从地质时间的MADBI形成中的有机富含间隔的进化。在研究的Al-Qarn-01孔中,Madbi形成中的有机丰富的间隔是热成熟的,从峰值到后期的油窗阶段。因此,在这些成熟阶段将半个或多个基因酮转化为油。研究井(Al-Qarn-01)的盆地建模结果表明,根据基因的转化比(Tr%),在两个主要相中产生并从Madbi源岩间隔中产生油。在晚餐和早期的寡核苷酸(80-33mA)期间,Kerogen对油(Tr = 10-50%)的主要转化率发生,对应于峰油窗口(0.70-1.00易%RO)(。),从源岩中排出大量的油,随后在初始三级裂转期间在早期的寡聚酮中迁移到覆盖储层岩中。在此期间,晚熟的油窗口(1.00-1.10易于%R-O),TRS为50-77%。

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