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首页> 外文期刊>Marine and Petroleum Geology >Study of hydrocarbon generation and 1D-2D modeling of hydrocarbon migration at the Karanj and Parsi oilfields, Southern Dezful Embayment, SW Iran
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Study of hydrocarbon generation and 1D-2D modeling of hydrocarbon migration at the Karanj and Parsi oilfields, Southern Dezful Embayment, SW Iran

机译:Karanj和Parsi油田的烃迁移碳氢化合物发电和1D-2D建模研究,SW Iran

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摘要

This study is a 2D basin modeling to determine the petroleum system (i.e. Cretaceous-Neogene play) of the Karanj and Parsi oilfields in the Southern Dezful Embayment, SW Iran. This system is characterized by occurrence of source rocks of Middle Cretaceous, Late Cretaceous and Paleocene to Eocene (Kazhdumi, Pabdeh and Gurpi Formation), reservoirs of Upper Cretaceous and Late Oligocene-Early Miocene (Ilam-Sarvak and Asmari formations), and seals of Paleocene and Miocene (Pabdeh and Gachsaran Formation). Considering temperature, transformation ratio and vitrinite reflectance, the maturity of source rocks (Kazhdumi, Pabdeh and Gurpi Formation) was investigated. A maturity history analysis showed that the maturity of Kazhdumi, Pabdeh and Gurpi Formation started during 70-60 and 4 Ma, respectively. Generation and expulsion of hydrocarbons started similar to 16 Ma in the Kazhdumi Formation and similar to 3 Ma in the Pabdeh Formation that continued up to the present. The analysis of the transformation ratio indicates transformation of significant amounts of Kazhdumi source rocks for generating hydrocarbons. Migration of hydrocarbons from the Kazhdumi Formation is mainly vertically upward. From Pabdeh Formation migration is both vertically upward (to the Asmari reservoir) and downwards (to the flam-Sarvak reservoir). However, some local traps have formed due to the hydrocarbon accumulation above the faults. Our results reveal that petroleum generation, migration and entrapment occurred at proper timing which facilitated the migration of hydrocarbons and their accumulation in the reservoirs.
机译:本研究是一个2D盆地模型,以确定南德德德·伊朗南部的卡伦和巴西油田的石油系统(即白垩纪 - Neogene发挥)。该系统的特征在于,发生中白垩纪,晚期白垩纪和古产物的源岩(Kazhdumi,Pabdeh和Gurpi形成),上白垩纪和晚期寡烯 - 早期内海(ILAM-Sarvak和Asmari地层)的储层和密封件古茂和新世(Pabdeh和Gachsaran Mablation)。考虑温度,转化率和耐久性反射率,研究了源岩的成熟度(Kazhdumi,Pabdeh和Gurpi形成)。到期历史分析表明,kazhdumi,pabdeh和gurpi形成的成熟程度分别在70-60和4 mA期间开始。在kazhdumi形成中,碳氢化合物的产生和驱逐类似于16 mA,并且在pabdeh形成中类似于3 ma,继续至今。转化率分析表明,用于产生烃的大量Kazhdumi源岩的转化。碳氢化合物从kazhdumi形成的迁移主要是垂直向上。从Pabdeh形成迁移既垂直向上(到Asmari水库)和向下(到Flam-Sarvak Chockoir)。然而,由于故障以上的碳氢化合物积累,一些局部陷阱形成了一些局部陷阱。我们的结果表明,在适当的时间表中发生了石油,迁移和夹带,促进了碳氢化合物的迁移及其在水库中的积累。

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