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Integral DMO with raytracing

Describe here algorithm for DMO to real data

One common objection to an exact PSPM is the presence of blind zones when lateral velocity gradients are large (Deregowski, 1986; Hale, 1988). A simple remedy of this problem that we would like to investigate is using PSPM for transforming data not to zero-offset, but to a sufficiently large offset without blind zones, or, if needed, to two different offsets.


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Next: References Up: Popovici and Biondi: PSPM Previous: PSPM IMPULSE RESPONSE IN
Stanford Exploration Project
1/13/1998