Dip and offset together

SHERWOOD'S DEVILISH

The migration process should be thought of as being interwoven with the velocity estimation process. J.W.C. Sherwood [1976] indicated how the two processes, migration and velocity estimation, should be interwoven. The moveout correction should be considered in two parts, one depending on offset, the NMO, and the other depending on dip. This latter process was conceptually new. Sherwood described the process as a kind of filtering, but he did not provide implementation details. He called his process Devilish, an acronym for ``dipping-event velocity inequalities licked.'' The process was later described more functionally by Yilmaz as prestack partial migration, and now the process is usually called dip moveout (DMO) although some call it MZO, migration to zero offset. We will first see Sherwood's results, then Rocca's conceptual model of the DMO process, and finally two conceptually distinct, quantitative specifications of the process.

Figure 8.16 contains a panel from a stacked section.

digicon
Figure 16. Conventional stacks with varying velocity. (distributed by Digicon, Inc.)

The panel is shown several times; each time the stacking velocity is different. It should be noted that at the low velocities, the horizontal events dominate, whereas at the high velocities, the steeply dipping events dominate. After the Devilish correction was applied, the data was restacked as before. Figure 8.17 shows that the stacking velocity no longer depends on the dip.

devlish
Figure 17. Devilish stacks with varying velocity. (distributed by Digicon, Inc.)

This means that after Devilish, the velocity may be determined without regard to dip. In other words, events with all dips contribute to the same consistent velocity rather than each dipping event predicting a different velocity. So the Devilish process should provide better velocities for data with conflicting dips. And we can expect a better final stack as well.

Dip and offset together