Research Article

Migration Using a Transversely Isotropic Medium with Symmetry Normal to the Reflector Dip

Figure 5

Migrated section after an isotropic migration with velocity of 2 km/s of the TTI syntheticdata in Figure 4. The angle gathers obtained using an isotropic mapping at 2.5 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.
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