盐下砂储层图像域最小二乘偏移与深度域反演

L. Leon, M. Hegazy, O. Zdraveva, M. Majdoub, Charles Inyang, K. Hargrove, K. Pasch, John Hollins
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引用次数: 1

摘要

由于复杂的地质条件和地面地震采集几何结构的限制,导致地震图像受到光照等波传播效应变化的影响。因此,可变光照的印记损害了地震图像中振幅和相位的可靠性。此外,目前的常规振幅反演方法假设地震振幅代表了地球的声学和弹性特性,并且不能补偿可变的照明效应。我们提出了一个来自墨西哥湾盐下的案例研究,展示了图像域的最小二乘迁移,其点扩展函数(PSF)能够同时校正照明效果,并产生位于盐基附近的薄砂床的高分辨率图像。我们讨论了我们的方法,以减轻散射效应,目前在psf产生的高对比度阻抗边界在地球模式内。最后,我们展示了叠后深度域反演的结果,提供了真实振幅图像和声阻抗体积,可以对先前确定的钻井目标的可行性进行可靠评估,并相应地增强了前景解释。
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Image-Domain Least-Squares Migration and Depth-Domain Inversion for Subsalt Sand Reservoirs
Summary A combination of complex geology and limitations imposed by the surface seismic acquisition geometry results in seismic images contaminated by variabilities in wave propagation effects such as illumination. Consequently, imprints of variable illumination compromise the reliability of the amplitude and phase within the seismic image. Additionally, today's conventional methods of amplitude inversion assume that the seismic amplitudes are representative of the earth's acoustic and elastic properties and do not compensate for variable illumination effects. We present a subsalt case study from the Gulf of Mexico demonstrating least-squares migration in the image domain with point-spread functions (PSF) ability to simultaneously correct for illumination effects and produce a higher-resolution image of thin sand beds located in close proximity to base of salt. We discuss our approach for mitigating scattering effects present in the PSFs arising from high-contrast impedance boundaries within the earth model. Finally, we show the results from a poststack depth-domain inversion, providing true amplitude images and acoustic impedance volumes and allowing reliable assessment of the viability of previously identified drilling targets and enabling corresponding augmentation of prospect interpretation.
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