Geochemical Characterization of Kazhdumi Source Rock in the Khaviz Oil Field, Southwest of Iran, Using Rock-Eval Pyrolysis

M. Khalatbari, M. Kamali, M. Arian, Buyuk Ghorbani
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引用次数: 2

Abstract

The Khaviz oil field located in Dezful embayment is one of Iran’s southwest oil fields. In this study, a total of 28 cutting samples from Kazhdumi formation (well No. KZ1, Khaviz oil field) were subject to geochemical investigation using Rock-Eval pyrolysis for the first time. The results of pyrolysis indicated that Kazhdumi source rock has significant hydrocarbon production potentiality and already entered the oil generation window. As inferred from the diagram of OI versus HI, Kazhdumi source rock contains organic matter type II kerogen deposited in paralic environment with anoxic to suboxic conditions. Using the diagram of S2 versus TOC, the absorbed carbon content, neutral carbon, and active carbon were calculated to be 0.42, 0.39, and 2.43 wt.% respectively.
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伊朗西南部Khaviz油田Kazhdumi烃源岩的岩石热解地球化学特征
位于Dezful海湾的Khaviz油田是伊朗西南部的油田之一。在本研究中,Kazhdumi地层(井1)共28个切割样品。KZ1, Khaviz油田)首次采用岩石热解方法进行了地球化学研究。热裂解结果表明,卡度米烃源岩具有显著的生烃潜力,已进入生油窗口。由OI - HI图可知,喀什杜米烃源岩为缺氧-亚缺氧的深水环境下的II型有机质干酪根。利用S2与TOC的关系图,计算出吸附碳、中性碳和活性碳分别为0.42、0.39和2.43 wt.%。
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