Research Article

Azimuthally Anisotropic 3D Velocity Continuation

Figure 3

(a) Fault map from Northwest Scotland [36] used to model diffraction data. (b) Synthetic post-stack diffraction data modeled using (1) and a 3D model based on the fault map in (a). (c) Diffractions from (b) migrated using an isotropic velocity model. (d) Diffractions from (b) migrated by anisotropic 3D velocity continuation.
484653.fig.003a
(a) Fault map
484653.fig.003b
(b) Fault diffractions
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(c) Isotropic velocity continution
484653.fig.003d
(d) Anisotropic continuation