Improving pre-salt targets using wave-equation velocity analysis

D. Donno, Sergio Barragan, F. Jouno, A. Khalil
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引用次数: 1

Abstract

Despite continuous improvements in model-building technologies, imaging below salt remains challenging. Reflection full-waveform inversion (RFWI) is effective at providing low-wavenumber velocity updates beyond the penetration depth of diving waves, however it is still susceptible to amplitude mismatch between input and modeled data. It also suffers from limitations imposed by narrow-azimuth (NAZ) seismic acquisition. To reduce the adverse impact of amplitude differences between input and modeled data, we present here a stack-power waveequation migration velocity analysis (WEMVA) method. Differently than RFWI, this method uses an objective function defined in the image domain. Therefore, it depends more on the kinematic part of the propagated wavefields, resulting in a more reliable inversion scheme. We also introduce a regularization term that reduces the footprints created in the velocity updates by NAZ seismic data. We demonstrate the effectiveness of this method by using synthetic and field data with NAZ acquisition geometries. Finally, we discuss some of its limitations, and suggest ideas for further improvements.
利用波动方程速度分析改进盐下目标
尽管模型构建技术不断改进,但盐层下的成像仍然具有挑战性。反射全波形反演(RFWI)在提供潜水波穿透深度以外的低波数速度更新方面是有效的,但它仍然容易受到输入和建模数据之间振幅不匹配的影响。它还受到窄方位角(NAZ)地震采集的限制。为了减少输入数据和模型数据之间振幅差异的不利影响,我们提出了一种堆栈-功率波方程偏移速度分析(WEMVA)方法。与RFWI不同的是,该方法使用在图像域中定义的目标函数。因此,它更多地依赖于传播波场的运动部分,从而产生更可靠的反演方案。我们还引入了一个正则化项,以减少NAZ地震数据在速度更新中产生的足迹。我们通过使用NAZ采集几何图形的合成数据和现场数据证明了该方法的有效性。最后,我们讨论了它的一些局限性,并提出了进一步改进的想法。
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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