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Wavefield interpolation in 3D large-step Fourier wavefield extrapolation

机译:3D大步傅里叶波场外推中的波场内插

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Extrapolating wavefields and imaging at each depth during three-dimensional recursive wave-equation migration is a time-consuming endeavor. For efficiency, most commercial techniques extrapolate wavefields through thick slabs followed by wavefield interpolation within each thick slab. In this article, we develop this strategy by associating more efficient interpolators with a Fourier-transform-related wavefield extrapolation method. First, we formulate a three-dimensional first-order separation-of-variables screen propagator for large-step wavefield extrapolation, which allows for wide-angle propagations in highly contrasting media. This propagator significantly improves the performance of the split-step Fourier method in dealing with significant lateral heterogeneities at the cost of only one more fast Fourier transform in each thick slab. We then extend the two-dimensional Kirchhoff and Born-Kirchhoff local wavefield interpolators to three-dimensional cases for each slab. The three-dimensional Kirchhoff interpolator is based on the traditional Kirchhoff formula and applies to moderate lateral velocity variations, whereas the three-dimensional Born-Kirchhoff interpolator is derived from the Lippmann-Schwinger integral equation under the Born approximation and is adapted to highly laterally varying media. Numerical examples on the three-dimensional salt model of the Society of Exploration Geophysicists/European Association of Geoscientists demonstrate that three-dimensional first-order separation-of-variables screen propagator Born-Kirchhoff depth migration using thick-slab wavefield extrapolation plus thin-slab interpolation tolerates a considerable depth-step size of up to 72 ms, eventually resulting in an efficiency improvement of nearly 80% without obvious loss of imaging accuracy. Although the proposed three-dimensional interpolators are presented with one-way Fourier extrapolation methods, they can be extended for applications to general migration methods.
机译:在三维递归波方程迁移过程中,在每个深度外推波场和成像是一项费时的工作。为了提高效率,大多数商业技术通过厚板外推波场,然后在每个厚板内进行波场内插。在本文中,我们通过将更高效的插值器与傅立叶变换相关的波场外推方法相关联来开发此策略。首先,我们为大型波场外推公式化了三维一阶变量分离屏幕传播器,它允许在高对比度介质中进行广角传播。该传播器显着提高了分步傅里叶方法在处理明显的横向异质性方面的性能,其代价是每个厚板中仅需再进行一次快速傅里叶变换。然后,我们将二维Kirchhoff和Born-Kirchhoff局部波场内插器扩展到每个平板的三维情况。三维Kirchhoff插值器基于传统的Kirchhoff公式,适用于中等的横向速度变化,而三维Born-Kirchhoff插值器是在Born近似下从Lippmann-Schwinger积分方程派生的,适用于高度横向变化媒体。勘探地球物理学家协会/欧洲地球科学家协会的三维盐模型的数值示例表明,使用厚板波场外推法和薄板法进行的三维一阶变量分离筛分传播器Born-Kirchhoff深度迁移插值可忍受高达72 ms的相当大的深度步长,最终导致效率提高了近80%,而没有明显降低成像精度。尽管提出的三维插值器具有单向傅里叶外推方法,但可以将其扩展为适用于一般的偏移方法。

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