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Evaluation of the petroleum potentials and prospect of the Chad Basin Nigeria from heat flow and gravity data

机译:从热流和重力数据评估尼日利亚乍得盆地的石油潜力和前景

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An integrated study of the Chad Basin Nigeria has been carried out using heat flow, Bouguer gravity anomaly, depth to basement maps and interpreted seismic reflection data of the area. The seismic reflection data show two main structural elements: faults and folds whose primary structural orientation is northeast–southwest. Other features such as grabens and horst which are formed as a result of tensional stress and magnetic intrusive are also identified in the sections. The Bouger gravity anomaly ranges from ?10 to ?50?mgal with a northeast to southwest trend while the heat flow values ranges from 63.63 to 105.4?m?Wm?2 with an average of 80.6?m?Wm?2. The result shows that areas with relatively low heat flux in the southwest and northeast is associated with Bouguer gravity values ranging from ?30 to ?50?mgal. These parts of the basin also have a higher depth to basement and are associated with low sediment, buried hills and crest of folds. The range of heat flow values computed for this study shows that the basin sediments are thermally mature and therefore has high prospects for oil and gas generation. The graben in the basin is associated with low heat flow and very low negative Bouguer gravity anomaly. The study reveals that a decrease in heat flow is observed with an increasing sedimentary thickness. Thus, by studying the heat flow map, regions of gravity highs and lows can be identified within the Chad basin. Moreover, areas of gravity lows have greater thickness of sediments than areas of gravity highs. Low geothermal gradient causes the formation of oil to begin at fairly deep subsurface levels, but makes the oil window to be quite broad. The heat flow, Bouguer gravity values and seismically determined structural features suggest that the Chad Basin Nigeria has good prospects for hydrocarbon plays in Cretaceous rocks, with high potentials for both structural and stratigraphic traps. The southwestern and northeastern axis of the basin is therefore recommended for further drilling to deeper depth based on the results of this study.
机译:利用热流,布格重力异常,地下室深度图和该地区的地震反射数据,对尼日利亚乍得盆地进行了综合研究。地震反射数据显示了两个主要的构造要素:断层和褶皱,其主要构造方向是东北-西南。在这些部分中还指出了由于拉应力和磁性侵入而形成的其他特征,例如grab抓和发呆。 Bouger重力异常范围为10至50 mgal,呈东北向西南趋势,而热流值范围为63.63至105.4Ω·m·Wm·2,平均为80.6Ω·m·Wm·2。结果表明,西南和东北热通量较低的地区与布格重力值在30至50毫克当量之间。盆地的这些部分也具有较高的基底深度,并且与低沉积物,埋山丘和褶皱顶有关。为这项研究计算的热流值范围表明,盆地沉积物是热成熟的,因此具有很高的油气生成前景。盆地中的grab陷与低热流和极低的负布格重力异常有关。研究表明,随着沉积厚度的增加,热流减少。因此,通过研究热流图,可以在乍得盆地内确定重力的高低区域。此外,重力低点的区域比重力高点的区域具有更大的沉积物厚度。低的地热梯度会导致石油的形成从相当深的地下开始,但会使油窗变宽。热流,布格重力值和地震确定的构造特征表明,尼日利亚乍得盆地在白垩纪岩石中具有良好的油气藏前景,在构造和地层圈闭方面都具有很高的潜力。因此,根据这项研究的结果,建议将该盆地的西南和东北轴线进一步钻至更深的深度。

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