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We develop a dip-dependent residual moveout formulation and test it on a synthetic dataset with steep dips.
We perform the new residual moveout method as a phase shift in the Fourier domain,
and obtain more accurate curvature parameters than with traditional spatial residual moveout.
Although a 2-D example is tested in this paper, the method can easily be extended to 3-D.
Stanford Exploration Project
10/14/2003