High-order kernels for Riemannian wavefield extrapolation

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Abstract

Riemannian wavefield extrapolation is a technique for one-way extrapolation of acoustic waves. Riemannian wavefield extrapolation generalizes wavefield extrapolation by downward continuation by considering coordinate systems different from conventional Cartesian ones. Coordinate systems can conform with the extrapolated wavefield, with the velocity model or with the acquisition geometry. When coordinate systems conform with the propagated wavefield, extrapolation can be done accurately using low-order kernels. However, in complex media or in cases where the coordinate systems do not conform with the propagating wavefields, low order kernels are not accurate enough and need to be replaced by more accurate, higher-order kernels. Since Riemannian wavefield extrapolation is based on factorization of an acoustic wave-equation, higher-order kernels can be constructed using methods analogous to the one employed for factorization of the acoustic wave-equation in Cartesian coordinates. Thus, we can construct space-domain finite-differences as well as mixed-domain techniques for extrapolation. High-order Riemannian wavefield extrapolation kernels improve the accuracy of extrapolation, particularly when the Riemannian coordinate systems does not closely match the general direction of wave propagation. © 2007 European Association of Geoscientists & Engineers.

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APA

Sava, P., & Fomel, S. (2008). High-order kernels for Riemannian wavefield extrapolation. Geophysical Prospecting, 56(1), 49–60. https://doi.org/10.1111/j.1365-2478.2007.00660.x

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