Figure 5

Comparison of conventional CMP and relatively new CRS time-migrated depth sections of the main profile. It shows differences in seismic sections due to differences in processing approach (see text for processing details). (a) No prominent reflection bands are observed in the seismic section, (b) The Moho is bright and continuous in CRS section (after Mandal et al.21). Prominent NE dipping reflection bands are observed at the beginning and end of the seismic section.