ABSTRACT
Riemannian wavefield extrapolation (RWE) is a generalization
of downward continuation to coordinate systems that closely
conform to the orientation of extrapolated wavefields.
If the coordinate system overturns, so does the computed
wavefield, despite being extrapolated with a one-way solution
to the acoustic wave-equation.
This allows for accurate imaging of structures of arbitrarily
steep dips with simple operators equivalent to standard extrapolators.
An obvious question for RWE is which is an optimal coordinate
system for a given velocity model.
One option is to compute ray coordinates as a solution
to the wide-band eikonal equation in a smoothed velocity model.
However, this solution ignores the natural variability and frequency
dependence of wavepaths in cases of complicated velocity models,
for example under salt bodies.
The solution advocated in this paper is a recursive bootstrap
procedure where a frequency-dependent coordinate system is computed
on-the-fly at every step from the gradient of the monochromatic
wavefield phase of the preceding few steps, coupled with standard RWE.
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