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Prestack shot-gather depth migration by a rigid flow of Gaussian wave packets

机译:高斯波包的刚性流动引起的叠前炮集深度偏移

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摘要

We introduce a new method for prestack depth migration of seismic common-shot gathers. The computational procedure follows standard steps of the reverse-time migration, i.e., downward continuation of the source and the receiver wavefields, followed by application of an imaging condition (e.g. zero-lag cross-correlation of these fields). In our method we first find a sparse data representation with a small number of Gaussian wave packets. We then approximate the downward wavefield propagation (for the source and the receiver fields) by a rigid flow of these wave packets along seismic rays. In this case, the wave packets are simply translated and rotated according to the ray geometry. One advantage of using Gaussian wave packets is that analytic formulas can be used for translation, rotation, and the application of the cross-correlation imaging condition. Moreover, they allow more sparse representations than competing methods. Finally we formulate a computationally and memory efficient migration procedure, as only few rays have to be traced, and since it is cheap to compute the cross-correlation for the intersecting rays.
机译:我们介绍了一种新的地震普通散布地震道集深度偏移方法。计算程序遵循逆时偏移的标准步骤,即源和接收器波场的向下连续,然后应用成像条件(例如,这些场的零滞后互相关)。在我们的方法中,我们首先找到具有少量高斯波包的稀疏数据表示。然后,我们通过这些波包沿地震射线的刚性流动来近似向下波场传播(对于源场和接收器场)。在这种情况下,波包可以根据射线几何形状简单地平移和旋转。使用高斯波包的一个优点是可以将解析公式用于平移,旋转以及互相关成像条件的应用。而且,与竞争方法相比,它们允许更多的稀疏表示。最后,由于仅需追踪很少的光线,并且由于计算相交光线的互相关比较便宜,因此我们制定了一种计算和内存有效的迁移过程。

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