shows 2-D cross-sections through the simple 3-D
synthetic model used to test lateral velocity variations.
The velocity model consisted of a linear gradient of 0.85
s-1 dipping at 45![]() |
For the migration, we used 20 reference velocities, and truncated filter coefficients when they became 103 times smaller than the leading value, with a maximum of 20 points. Filters contained 8-10 coefficients for average frequencies.
Figure
shows the results of the migration.
The three dipping beds are well imaged in cross-section, and in the
depth-slice the effect of the velocity gradient is apparent
from the slight azimuthal anisotropy of the impulse response.