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Divergence correction, coherent noise suppression, and CMP sorting were
applied to the data before 2-D prestack depth migration.
In order to compensate for spherical divergence, we scaled the data
in the time axis using a function trace(t)= trace(t)*t.
Coherent noise suppression was also applied to eliminate the P-wave and S-wave
first arrivals. To eliminate the P-wave first arrival, we applied a linear
outer
mute to the data. The S-wave arrival was suppressed by applying a 2-D dip
filter.
Finally, the data was windowed to extract the CMPs with maximum offset
coverage and sorted by CMP location.
Figure 3 shows the zero-offset section of the resulting data.
zero-off
Figure 3 Zero-offset section of the
resulting synthetic data. Left: model 1, Right: model 2
Next: Prestack migration
Up: Elastic Modeling
Previous: Synthetic seismograms
Stanford Exploration Project
4/28/2000