Sub Seismic Fault Identification within Carbonate Reservoirs with Borehole Images Logging-While-Drilling: Integrated Approach in Optimizing Well Placement; A Case Study from Offshore Abu Dhabi

Sultan Dahi Al-Hassani, S. Ahmed, O. Khan, Ibrahim Mohamed AL-Tameemi, Shahnawaz Khan, P. Marza, J. Abdulrahim, S. Shasmal, M. Alexander
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Abstract

Reservoirs located offshore Abu Dhabi can be complex in terms of sub-seismic structural features such as faults and localized deformations. With use of high-resolution resistivity image logs, a TST (true stratigraphic thickness) technique, along with 3D structural models, uncertainties related to sub seismic structural ambiguities are resolved and well trajectory is optimized while drilling. In this case study, real-time resistivity image logs were used while drilling. The sinusoid’s shape on images provided cutting down dip or up dip information. Dip trends were analyzed using a dip vector plot and to identify zones-of-interest. Dip attribute along with the log response were compared with the pre-job model and the inclination is adjusted accordingly during drilling. Several high angle features can be characterized as stratigraphic changes, fractures, or faults. The morphology and trend change observed in the dip vector plot of these features lead to the conclusion that these are sub-seismic resolution faults and deformation is associated with the fault. The stratigraphic drilling polarity and the TST were calculated using the formation dip data. Using a TST scale and splitting the logs into stratigraphic drilling polarity domains, the fault throw displacement is estimated. The model is updated to reflect the interpreted data. The fault plunge and trend are extrapolated away from the wellbore and to nearby wells.
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利用井眼图像识别碳酸盐岩储层亚地震断层:随钻测井优化配井的综合方法以阿布扎比为例
阿布扎比海上的储层在次地震构造特征(如断层和局部变形)方面可能很复杂。通过使用高分辨率电阻率成像测井、TST(真实地层厚度)技术以及3D结构模型,可以解决与次地震结构模糊性相关的不确定性,并在钻井过程中优化井眼轨迹。在本案例中,钻井时使用了实时电阻率成像测井。图像上正弦波的形状提供了向下倾斜或向上倾斜的信息。利用倾角矢量图分析倾角趋势,并确定感兴趣的区域。将倾角属性和测井响应与作业前模型进行比较,并在钻井过程中进行相应的倾角调整。几个高角度特性可以作为地层特征变化,骨折,或者缺点。根据这些特征的倾角矢量图的形态和趋势变化,得出这些断层是次地震分辨率断层,变形与断层有关的结论。利用地层倾角资料计算了地层钻井极性和TST。利用TST尺度,并将测井曲线划分为地层钻井极性域,估算了断层落差位移。更新模型以反映解释后的数据。断层的俯冲和走向从井筒外推到附近的井。
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