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Having rotated the data, we can now stack to produce an estimate
of the source wavelets for use in deconvolution. We would like to
deconvolve in order to sharpen the SV event and (hopefully) reveal
distinct SH events that have arrival times that differ only slightly
from the SV.
Figure 4 is a wiggle-trace display of a small window
of the P wave section after rotation (and NMO correction).
Trace balancing has also been performed to emphasize
variations in wavelet shape (rather than amplitude) from trace
to trace.
The window is centered around the P event.
The wavelet shape is quite consistent,
leading us to believe that we have
done a good job of rotation, and that the wavelet produced
by stacking will be meaningful.
We repeated the entire processing sequence using a window of data
containing the SV event. The picked arrival directions were
very similar to the P case.
Figure 5 shows the P and
SV wavelets produced by stacking. These have been used by Leonid
Vanyan (Vanyan, 1990) to deconvolve the data.
rotwin
Figure 4 A small portion of the P wave section after rotation and NMO correction.
The shape of the arrival is quite consistent.
wavelets
Figure 5 P (solid line) and SV (dotted line) wavelets obtained by stacking the data
after rotation. These wavelets can be used in deconvolution.
Next: Conclusions
Up: Cole & Karrenbach: Rotation
Previous: DATA ROTATION
Stanford Exploration Project
1/13/1998