Reconstructing Deposition Environment Using Energy Regime Assessment of Stacked Sequences from Gamma Ray Log and 3D Seismic Data

O. Rotimi, Somto Chukwuka, K. Oyeyemi, T. Ogunkunle, A. Akande, Betty Ihekona, Oseremen Iyamah, Tope Shade Alege
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Abstract

Depositional sequence unbundling was done to understand the depositional environment from six wells through the analysis of gamma-ray logs using shale volume, and a 3D post-stack seismic. Identified hydrocarbon reservoir formations were laterally tracked to assess horizon continuity and spatial draping of the units. Horizon surfaces were built post-correlation to examine the bounded zones and reconcile sequences. Gamma-ray log motifs for the deposits indicate the presence of progradational, retrogradational, and aggradational sequence patterns that typifies prevalent energies at the time deposition, characteristic of deltaic environment. On the seismic sections, aggradational reflectors dominate over the other two. Although current well placements do not conform to structural attitude, petrophysical analysis done over the horizons indicate a significant increase in porosity and hydrocarbon saturation basin-ward (South-west), in the direction of the frontier prospect to site more wells.
利用伽马测井和三维地震资料叠加层序能量状态评价重建沉积环境
通过分析页岩体积的伽马射线测井曲线和三维叠后地震,对6口井的沉积层序进行了拆解,以了解沉积环境。对已识别的油气储层进行横向跟踪,以评估其层位连续性和空间垂度。建立了后相关的水平面来检查有界区域和协调序列。沉积物的伽马射线测井模式表明,沉积时存在进积、退积和堆积的层序模式,代表了沉积时的主流能量,具有三角洲环境的特征。在地震剖面上,叠加反射体占主导地位。尽管目前的井位不符合构造产状,但对地层进行的岩石物理分析表明,盆地方向(西南方向)的孔隙度和烃饱和度显著增加,在前沿勘探方向可以找到更多的井。
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