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首页> 外文期刊>Research journal of applied science, engineering and technology >Hydrocarbon Potentials, Thermal and Burial History in Herwa-1 Well from the Nigerian Sector of the Chad Basin: An Implication of 1-D Basin Modeling Study
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Hydrocarbon Potentials, Thermal and Burial History in Herwa-1 Well from the Nigerian Sector of the Chad Basin: An Implication of 1-D Basin Modeling Study

机译:乍得盆地尼日利亚地区Herwa-1井的油气潜力,热力和埋藏历史:对一维盆地建模研究的启示

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This research study attempt to evaluate the hydrocarbon potentials, thermal and burial history and the timing of hydrocarbon generation in Herwa-1 well within the Nigerian Sector of the Chad basin. Organic geochemical study of some ditch cuttings samples from Herwa-1 well and a One-dimensional basin modeling study was carried out. The result of the geochemical analysis revealed a moderate to good TOC greater than 0.5wt% in Fika and Gongila formation, the Hydrogen Index (HI) ranges from 150-300 (mgHC/g) and the Tmax values falls within the range of greater than or equal to 430°C. The hydrocarbon potentials in Herwa-1 well was further supported with the values of S1+S2 which is greater than or equal to 2 mg/g of rock in almost all the samples, suggesting a good hydrocarbon potentials. The 1-D basin model was constructed for Herwa-1 well in order to assess the burial history and thermal maturity of the potential source rocks in the Nigerian sector of the Chad basin. The modeling results indicate that maximum burial occurred in the late Miocene and suggesting erosion might have been the cause of the thinning of the Tertiary sediments in the present time. The calibration of Vitrinite reflectance against Temperature revealed the present day heat flow to be at 60 mW/m2 and Paleo heat flow falls within the range of 68 mW/m2. However, it is also revealed that Oil Window begins at (0.60-1.30% VRr) at the depth of (2000-3000 m) in the middle Cretaceous and the Gas Window start during the late Cretaceous to Tertiary with a value of (1.3-2.5% VRr) at a depth greater than (3500 m).
机译:这项研究试图评估乍得盆地尼日利亚地区Herwa-1井的油气潜力,热和埋藏历史以及生烃时间。对Herwa-1井部分沟屑进行了有机地球化学研究,并进行了一维盆地模拟研究。地球化学分析的结果表明,在Fika和Gongila地层中,TOC大于0.5wt%,氢指数(HI)为150-300(mgHC / g),Tmax值大于或等于430°C。在几乎所有样品中,S1 + S2值均大于或等于2 mg / g岩石,进一步支持了Herwa-1井中的烃潜力。为评估Herwa-1井的一维盆地模型,以评估其在乍得盆地尼日利亚地区的潜在烃源岩的埋藏历史和热成熟度。模拟结果表明,最大的埋藏发生在中新世晚期,表明侵蚀可能是当前第三纪沉积物变薄的原因。校准玻璃陶瓷对温度的反射率表明,目前的热流量为60 mW / m2,古热流量为68 mW / m2。但是,还发现白垩纪中段(2000-3000 m)深度处的油窗始于(0.60-1.30%VRr),白垩纪晚期至第三纪的气窗始于(6.3- 2.5%VRr)深度大于(3500 m)。

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