Application of Reverse Time Migration to Faults Imaging in Rakhine Basin, Myanmar

Figure 5

(a) Example velocity analysis for creating a velocity model from the conventional stack image showing the velocity spectrum, the stacking velocity for each maximum semblance, the interval velocities, and an NMO corrected supergather. (b) Smoothed velocity model in depth–distance domain with the velocities ranging from 1487 m/s to 5100 m/s over the survey geometry. The velocity model is based on the NMO velocities. Note that the depth scale is vertically exaggerated.

(a)

(b)