In Chapter
, I present a formal development
of wave-equation datuming
operators based on the concept of adjoint operators. I compare
Kirchhoff, phase shift, and finite difference formulations both
mathematically and by means of synthetic examples.
In this development I present a generalized framework that
links all three of the wave-equation datuming formulations.
This allows me to compare their individual strengths and weaknesses, and
provides an understanding of exactly how wave-equation datuming transforms data
and how it differs from migration.
The synthetic examples demonstrate the utility of datuming in unraveling
topographic distortions and provide a practical comparison of how
the different methods behave in terms of dip resolution, artifacts, and
efficiency.
I conclude that Kirchhoff datuming is the best suited method for my applications because it offers the most efficient and accurate method of performing large extrapolation steps in variable velocity media. It is also readily extendible to three-dimensional applications.