Table of Contents
MIGRATION BY DOWNWARD CONTINUATION
Huygens secondary point source
Migration derived from downward continuation
Continuation of a dipping plane wave.
Downward continuation with Fourier transform
Linking Snell waves to Fourier transforms
Pseudocode to working code
Kirchhoff versus phase-shift migration
Damped square root
Adjointness and ordinary differential equations
Vertical exaggeration example
Vertical and horizontal resolution
Field data migration
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Stanford Exploration Project