Dip-moveout correction in practice

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Seismic Data Analysis
Seismic-data-analysis.jpg
Series Investigations in Geophysics
Author Öz Yilmaz
DOI http://dx.doi.org/10.1190/1.9781560801580
ISBN ISBN 978-1-56080-094-1
Store SEG Online Store


Results of the previous section suggest the general DMO processing sequence shown in Figure 5.2-1.

  1. Perform velocity analysis at sparse intervals and pick just a few velocity functions with minimal dip effects.
  2. Apply NMO correction using the these flat-event velocities.
  3. Sort data to common-offset sections, apply DMO correction and sort back to CMP gathers.
  4. Apply inverse NMO correction using the flat-event velocities from step (a).
  5. Perform velocity analysis at frequent intervals as needed to derive an optimum stacking velocity field.
  6. Apply NMO correction using the optimum stacking velocity field.
  7. Stack the data and migrate using an edited and appropriately smoothed version of the optimum stacking velocity field.

Note that this processing sequence is similar to the sequence for residual statics corrections described in Figure 3.3-12. Both residual statics and DMO corrections are followed by a revision of velocities so as to get the most out of these corrections during stacking. In this section, we shall apply the sequence outlined above to two common cases of conflicting dips with different stacking velocities — salt flanks and fault planes.

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Dip-moveout correction in practice
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