热模拟在伊朗波斯湾Gadvan组地球化学表征中的应用

Q4 Earth and Planetary Sciences
A. Vaezian, M. Ziaii, M. Kamali, A. Kadkhodaie-Ilkhchi
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引用次数: 0

摘要

本研究对位于伊朗边界的波斯湾中部地区的Gadvan组烃源岩的生烃潜力进行了研究。利用Rock-Eval热解结果对6口井的干酪根类型和成熟度进行了研究,并与Pars Basin Modeler (PBM)建模软件程序的结果进行了比较。氢指数(HI)与最高温度的交叉图表明,研究区Gadvan组处于早、中期成熟阶段,可能是一个倾向于天然气的烃源岩。在此基础上,通过一口井确定了加德万组的埋藏史和热史。利用Easy %Ro和时间-温度指数(TTI)两种方法重建了Gadvan地层所有井的热模型,并研究了其热成熟度水平。TTI法和Easy %Ro法的结果吻合较好,两者都证实了岩石评价分析的结果。综合分析表明,Gadvan组在研究区属于低含气烃源岩,其成熟度在波斯湾南部逐渐提高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Application of Thermal Modelling for Geochemical Characterization of Gadvan Formation, Persian Gulf, Iran
In the this research, the hydrocarbon generation potential of the Gadvan Formation as a probable source rock was investigated in the central part of the Persian Gulf at the borders of Iran. Type and maturity level of kerogen were investigated in six wells using the results of Rock-Eval pyrolysis and compared with results yielded by the modelling software program known as Pars Basin Modeler (PBM). The cross-plot of hydrogen index (HI) versus maximum temperature suggests that the Gadvan Formation reached early to mid-maturity stages in the studied area, which means that it could act as a gas prone source rock. Furthermore, the burial and thermal history of the Gadvan Formation was determined in one well. Two methods, Easy %Ro and time-temperature index (TTI) were used for the reconstruction of thermal modelling and studying the thermal maturity level in all of the drilled wells reaching the Gadvan Formation. The results of the TTI and Easy %Ro methods were in good agreement and both of confirmed the results of Rock Eval analysis. An integrated approach using different techniques showed that the Gadvan Formation can be classified as a poor gas bearing source rock in the studied area, while its maturity increases towards the southern parts of the Persian Gulf.
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来源期刊
International Journal of Mining and Geo-Engineering
International Journal of Mining and Geo-Engineering Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
0.80
自引率
0.00%
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0
审稿时长
12 weeks
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