Migration Using a Transversely Isotropic Medium with Symmetry Normal to the Reflector Dip
Figure 7
Migrated section after DTI-based migration with velocity of 2 km/s and of the TTI synthetic data in Figure 4. The angle gathers obtained, now, using the VTI mapping at 2.5 km location are displayed on the right. The top section shows a depth slice as a function of angle gather at depth 2 km.
