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

Figure 8

Result of applying PSDM-RTM. (a) The result of the inner product of the wavefields shown in Figure 7. (b) Resulting image after summing all 1669 single image gathers. The right-hand side shows steep dips, folds, and complex stratigraphic sediments in the submarine canyon at distances between about 30–40 km, both at the surface and at a depth of around 2.1 km. Note that the depth scale is vertically exaggerate.

(a)

(b)