首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Source rock characterization of the Cretaceous Sarvak Formation in the eastern part of the Iranian sector of Persian Gulf
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Source rock characterization of the Cretaceous Sarvak Formation in the eastern part of the Iranian sector of Persian Gulf

机译:波斯湾伊朗断层东部白垩纪萨尔瓦克组烃源岩特征

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摘要

Cenomanian Middle Sarvak rock samples were collected from various parts of the eastern Iranian sector of the Persian Gulf and analyzed for quantity, quality, maturity and depositional environment of the organic matter by Rock-Eval pyrolysis, gas chromatography (GC), gas chromatography-mass spectrometry (GC-MS), pyrolysis-gas chromatography-mass spectrometry (Py-GC-MS), kerogen stable carbon isotopic signatures, elemental composition and petrography. The results indicate that the organic matter has mainly good to very good hydrocarbon generation potential corresponding to kerogen types I, II and II-S. The maturity increases from immature in the western section to early mature in the eastern section of the study area. In addition, biomarker parameters indicate a marine carbonate depositional environment for the Middle Sarvak Formation and deposition under anoxic condition. According to hydrocarbon potential, maturity and oil-source rock correlation, the Middle Sarvak is the main source rock charging the Late Cretaceous Upper Sarvak/Ilam reservoirs of south-eastern part of the Persian Gulf. (C) 2016 Elsevier Ltd. All rights reserved.
机译:从波斯湾伊朗东部东部各地区收集了西诺曼尼亚中萨瓦克岩石样品,并通过Rock-Eval热解,气相色谱(GC),气相色谱-质谱分析了有机物的数量,质量,成熟度和沉积环境。光谱法(GC-MS),热解-气相色谱-质谱(Py-GC-MS),干酪根稳定的碳同位素特征,元素组成和岩石学。结果表明,有机质主要具有良好至非常好的烃生成潜力,对应于干酪根类型I,II和II-S。研究区的成熟度从西部的不成熟期增加到东部的早期成熟期。另外,生物标志物参数表明了在缺氧条件下中萨瓦克组和沉积的海洋碳酸盐沉积环境。根据烃的潜力,成熟度和油源岩的相关性,中部萨尔瓦克是充填波斯湾东南部晚白垩世上萨尔瓦克/伊兰储层的主要烃源岩。 (C)2016 Elsevier Ltd.保留所有权利。

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