Migration Using a Transversely Isotropic Medium with Symmetry Normal to the Reflector Dip
Figure 6
Migrated section after a VTI migration with velocity of 2 km/s and of the TTI synthetic data in Figure 4. Again, the angle gathers obtained using an isotropic mapping at 8 km location are displayed on the right, and the top section shows a depth slice as a function of angle gather at depth 2 km.
