Quantitative Seismic Interpretation Workflow for Sweet Spot Identification in Organic-Rich Mudrocks

M. A. Ibrahim, T. Mukerji, A. Scheirer
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Abstract

Estimating the lateral heterogeneity of geochemical properties of organic rich mudrocks is important for unconventional resource plays. Mature regions can rely on abundant well data to build empirical relationships and on traditional geostatistical methods to estimate properties between wells. However, well penetration in emerging plays are sparse and so these methods will not yield good results. In this case, quantitative seismic interpretation (QSI) might be helpful in estimating the desired properties. In this study, we use QSI based on a rock physics template in estimating the uncertainty of the geochemical properties of organic mudrocks of the Shublik Formation, North Slope, Alaska. A rock physics template incorporating lithology, pore fraction, kerogen fraction, and thermal maturity is constructed and validated using well data. The template clearly shows that the inversion problem is non-unique. Inverted impedances cubes are estimated from three seismic angle gathers (near with angles between 0° and 15°, mid with angle gathers between 15° and 30°, and far with angle gathers between 30° and 45°). The inversion is done using a model-based implementation with an initial earth model derived from the seismic velocity model used in the processing phase. By combining the rock physics template and the results of seismic inversion, multiple realizations of total organic content (TOC), matrix porosity, and brittleness index are generated. These parameters can be used for sweet spot detection. Lithological results can also be used as an input for basin and petroleum system modeling.
富有机质泥岩甜点识别定量地震解释工作流程
评价富有机质泥岩地球化学性质的横向非均质性对非常规资源区具有重要意义。成熟地区可以依靠丰富的井资料建立经验关系,也可以利用传统的地质统计学方法估计井间的性质。然而,新兴区块的井眼渗透率很低,因此这些方法不会产生很好的效果。在这种情况下,定量地震解释(QSI)可能有助于估计所需的属性。在这项研究中,我们使用基于岩石物理模板的QSI来估计阿拉斯加北坡Shublik组有机泥岩地球化学性质的不确定性。结合岩性、孔隙分数、干酪根分数和热成熟度,构建并验证了岩石物理模板。该模板清楚地显示了反演问题的非唯一性。反向阻抗立方体是根据三个地震角集估计的(近角集在0°到15°之间,中角集在15°到30°之间,远角集在30°到45°之间)。反演使用基于模型的实现,并使用从处理阶段使用的地震速度模型导出的初始地球模型。将岩石物理模板与地震反演结果相结合,生成总有机含量(TOC)、基质孔隙度和脆性指数的多种实现。这些参数可用于甜点检测。岩性结果也可以作为盆地和油气系统建模的输入。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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