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Petroleum generation and migration in the Mesopotamian Basin and Zagros Fold Belt of Iraq: results from a basin-modeling study

机译:美索不达米亚盆地和伊拉克Zagros褶皱带的石油产生和迁移:盆地模型研究的结果

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A regional 3-D total petroleum-system model was developed to evaluate petroleum generation and migration histories in the Mesopotamian Basin and Zagros fold belt in Iraq. The modeling was undertaken in conjunction with Middle East petroleum assessment studies conducted by the USGS. Regional structure maps, isopach and facies maps, and thermal maturity data were used as input to the model. The oil-generation potential of Jurassic source-rocks, the principal known source of the petroleum in Jurassic, Cretaceous, and Tertiary reservoirs in these regions, was modeled using hydrous pyrolysis (Type II-S) kerogen kinetics. Results showed that oil generation in source rocks commenced in the Late Cretaceous in intrashelf basins, peak expulsion took place in the late Miocene and Pliocene when these depocenters had expanded along the Zagros foredeep trend, and generation ended in the Holocene when deposition in the foredeep ceased. The model indicates that, at present, the majority of Jurassic source rocks in Iraq have reached or exceeded peak oil generation and most rocks have completed oil generation and expulsion. Flow-path simulations demonstrate that virtually all oil and gas fields in the Mesopotamian Basin and Zagros fold belt overlie mature Jurassic source rocks (vertical migration dominated) and are situated on, or close to, modeled migration pathways. Fields closest to modeled pathways associated with source rocks in local intrashelf basins were charged earliest from Late Cretaceous through the middle Miocene, and other fields filled later when compression-related traps were being formed. Model results confirm petroleum migration along major, northwest-trending folds and faults, and oil migration loss at the surface.
机译:开发了区域3-D总石油系统模型,以评估美索不达米亚盆地和伊拉克Zagros褶皱带的石油生成和迁移历史。建模是与USGS进行的中东石油评估研究一起进行的。区域结构图,等值线和相图以及热成熟度数据被用作模型的输入。侏罗纪烃源岩是这些地区侏罗纪,白垩纪和第三纪储层中石油的主要已知来源,其生油潜力是利用含水热解(II-S型)干酪根动力学模拟的。结果表明,烃源岩的生油开始于陆架内盆地的白垩纪晚期,当这些沉积中心沿Zagros前缘的深部扩张时,中新世和上新世晚期发生了驱顶作用,而当前缘中的沉积停止后,则在全新世结束了驱油作用。 。该模型表明,目前,伊拉克的大多数侏罗纪烃源岩已经达到或超过了峰值产油量,并且大多数岩石已经完成了产油和驱逐。流动路径模拟表明,美索不达米亚盆地和Zagros褶皱带中的几乎所有油气田都覆盖在成熟的侏罗纪烃源岩(垂直运移为主)上,并且位于或接近模拟的运移路径。与白垩纪晚期至中新世中期相近的,与局部陆架内盆地烃源岩相关的与模拟路径最接近的油田,其后充填了与压缩相关的圈闭的其他油田。模型结果证实了沿主要的西北趋势褶皱和断层的石油运移,以及地表的石油运移损失。

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