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We now provide, as an example, an image gather obtained for a real dataset.
Figure 17 represents an offset ray-parameter gather at a
particular horizontal location. According to the theory, in the absence
of weighting,
the amplitude at high ph needs to be decreased, while
the amplitude at low ph needs to be increased.
The left panel shows the gather computed without the Jacobian
weighting factor, while the right panel shows the gather after amplitude
compensation.
As expected, the Jacobian weighting attenuates most of the energy at high
ph, and enhances the amplitude of the reflections at lower ph.
kja10.5
Figure 17 Real data example. The bottom panels are
offset ray-parameter gathers computed with compensated (left) and
uncompensated (right) amplitudes.
The top panels show the amplitude variation with
offset ray parameter for an event at about 1.75 km depth.
The amplitude decrease at small incidence angles is caused by the
absence of innermost offsets from the recorded data.
Next: Conclusions
Up: Sava and Biondi: Amplitude-preserved
Previous: Variable-velocity Jacobians
Stanford Exploration Project
4/30/2001