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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Amplitude-variation-with-offset and prestack-waveform inversion: A direct comparison using a real data example from the Rock Springs Uplift, Wyoming, USA
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Amplitude-variation-with-offset and prestack-waveform inversion: A direct comparison using a real data example from the Rock Springs Uplift, Wyoming, USA

机译:偏移幅度变化和叠前波形反演:使用来自美国怀俄明州Rock Springs Uplift的真实数据示例进行的直接比较

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摘要

Recent advances in seismic data acquisition and processing allow routine extraction of offset-/angle-dependent reflection amplitudes from prestack seismic data for quantifying subsurface lithologic and fluid properties. Amplitude-variation-with-offset (AVO) inversion is the most commonly used practice for such quantification. Although quite successful, AVO has a few shortcomings primarily due to the simplicity in its inherent assumptions, and for any quantitative estimation of reservoir properties, they are generally interpreted in combination with other information. In recent years, waveform-based inversions have gained popularity in reservoir characterization and depth imaging. Going beyond the simple assumptions of AVO and using wave equation solutions, these methods have been effective in accurately predicting the subsurface properties. Developments of these waveform inversions have so far been along two lines: (1) the methods that use a locally 1D model of the subsurface for each common midpoint and use an analytical solution to the wave equation for forward modeling and (2) the methods that do not make any 1D assumption but use an approximate numerical solution to the wave equation in 2D or 3D for forward modeling. Routine applications of these inversions are, however, still computationally demanding. We described a multilevel parallelization of elastic-waveform inversion methodology under a 1D assumption that allowed its application in a reasonable time frame. Applying AVO and waveform inversion on a single data set from the Rock Springs Uplift, Wyoming, USA, and comparing them with one another, we also determined that the waveform-based method was capable of obtaining a much superior description of subsurface properties compared withAVO. We concluded that the waveform inversions should be the method of choice for reservoir property estimation as high-performance computers become commonly available.
机译:地震数据采集和处理的最新进展允许常规地从叠前地震数据中提取与偏移/角度有关的反射振幅,以量化地下岩性和流体性质。偏移幅度变化(AVO)反演是这种量化最常用的方法。尽管非常成功,但AVO仍然存在一些缺点,这主要是由于其固有假设的简单性,并且对于储层性质的任何定量估计,通常将它们与其他信息结合起来进行解释。近年来,基于波形的反演在储层表征和深度成像中越来越受欢迎。这些方法超越了AVO的简单假设并使用波动方程解,已经在准确预测地下属性方面有效。迄今为止,这些波形反演的发展主要有两方面:(1)对每个公共中点使用地下局部一维模型,并对波方程使用解析解进行正向建模的方法,以及(2)不要做任何一维假设,而是对2D或3D中的波动方程使用近似数值解进行正向建模。然而,这些反演的常规应用仍然在计算上要求很高。我们描述了一维假设下的弹性波形反演方法的多级并行化,该方法允许其在合理的时间范围内应用。将AVO和波形反演应用于来自美国怀俄明州Rock Springs Uplift的单个数据集,并将它们彼此进行比较,我们还确定,与AVO相比,基于波形的方法能够获得更好的地下特性描述。我们得出结论,随着高性能计算机的普及,波形反演应该成为油藏属性估算的一种选择方法。

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