尼日利亚东北部上贝努埃海槽贡戈拉盆地白垩系贡贝砂岩储层潜力

B. Shettima, I. Buba, M. Sidi, Y. Abdulganiyu, H. Hamidu, U. Abubakar
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引用次数: 4

摘要

Benue上海槽贡戈拉盆地Campano - Maastrichtian Gombe砂岩为砂质岩性,横向展布,厚度达300m以上。根据二元图、岩相分析和下降头渗透率对储层进行岩石物理评价,平均孔隙度分别为15%、33%和23%。双变量图和降渗分析的平均渗透率分别为5.2D和100md。这些数值与北海和尼日尔三角洲已探明盆地的储层岩石具有可比性。贡贝砂岩在贡拉盆地具有潜在的储层潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reservoir Potentials of the Cretaceous Gombe Sandstone, Gongola Basin, Upper Benue Trough, North Eastern Nigeria
The Campano - Maastrichtian Gombe Sandstone of the Gongola Basin of the Upper Benue Trough is composed of arenaceous lithology that is laterally extensive and has reached a thickness of over 300m. The petrophysical evaluation of the formation on the basis of bivariate plots, petrographic analysis and falling head permeability indicated average porosity values of 15%, 33% and 23% respectively. Average permeability values of 5.2D and 100md were also obtained from bivariate plots and falling permeameter analysis respectively. These values are comparable to the reservoir rocks of proven petroleum basin of the North Sea and Niger Delta. Therefore, the Gombe Sandstone can serve as a potential reservoir rock in the Gongola Basin.
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