首页> 外文期刊>Journal of natural gas science and engineering >Basin and petroleum system modeling of the Cretaceous and Jurassic source rocks of the gas and oil reservoirs in Darquain field, south west Iran
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Basin and petroleum system modeling of the Cretaceous and Jurassic source rocks of the gas and oil reservoirs in Darquain field, south west Iran

机译:伊朗西南部Darquain油田天然气和油藏的白垩纪和侏罗纪烃源岩的盆地和石油系统模拟

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In south west Iran, in the Abadan Plain, there are several giant gas and oil reserves in Jurassic and Cretaceous carbonates, such as Darquain, where there are excellent source rocks in the Early Cretaceous and Jurassic successions. In present study, petroleum generation and migration from these source rocks were evaluated. Maturity state of organic matter was determined with Organic petrography and results were used for calibration of thermal model. Basin modeling was used for investigation of petroleum generation and migration history. Burial history and 3D thermal model were constructed for the study area using Temis suite and Genex software. Modeling shows source rocks of Jurassic, such as Sargelu and Neyriz are in gas maturity state, oil generation phase passed before Cenozoic. It appears that gas from Jurassic source rocks accumulated in Najmeh and did not reach to Cretaceous Fahliyan reservoir. Cretaceous reservoir in Fahliyan Formation has been charged by the Garau Formation. This source rock reached to oil window in Early Cretaceous time and began hydrocarbon expulsion at the end of Cretaceous when the Darquain structure formed. Migration paths of hydrocarbons shifted from NE to SW direction about 11 Ma in response to changes in regional structural dip contemporary with the Zagros Orogeny. Modeling results indicate that the quantity of gas and oil generated in the kitchen area was more than the reservoirs' capacity. Therefore, the surplus hydrocarbon could have migrated laterally out of reservoir area. (C) 2015 Elsevier B.V. All rights reserved.
机译:在伊朗西南部的阿巴丹平原上,侏罗纪和白垩纪的碳酸盐岩中有数个巨大的天然气和石油储藏,例如达尔金,早白垩纪和侏罗纪的演替中有极好的烃源岩。在本研究中,对这些烃源岩的生油和运移进行了评估。用有机岩相学确定有机物的成熟状态,并将其结果用于热模型的校准。盆地建模被用来调查石油的产生和迁移历史。使用Temis套件和Genex软件为研究区域构建了埋葬历史和3D热模型。建模表明,侏罗纪的烃源岩,例如Sargelu和Neyriz处于天然气成熟状态,生油阶段早于新生代。看来侏罗纪烃源岩中的天然气聚集在纳杰姆,没有到达白垩纪的法赫利扬储层。 Fahliyan组的白垩纪储层由Garau组充注。该烃源岩在白垩纪早期就到达了油窗,并在达奎因构造形成时在白垩纪末期开始了烃排泄。响应Zagros造山带的当代区域构造倾角变化,碳氢化合物的迁移路径从东北向西南方向移动了约11 Ma。建模结果表明,厨房区域产生的天然气和石油数量超过了水库的容量。因此,多余的碳氢化合物可能已经横向移出了储层区域。 (C)2015 Elsevier B.V.保留所有权利。

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