Figure F7. Isopach map of all sediment that lies above reflection surface PP-12 (post-late Miocene), with contours in milliseconds two-way traveltime (from Shipboard Scientific Party, 2001a). Sediment deposition is mostly concentrated in the Prydz Channel Fan. Elsewhere in Prydz Bay, post-PP-12 sediments are thin and have been highly eroded at various times.

Figure F7. Isopach map of all sediment that lies above reflection surface PP-12 (post-late Miocene), with contours in milliseconds two-way traveltime (from Shipboard Scientific Party, 2001a). Sediment deposition is mostly concentrated in the Prydz Channel Fan. Elsewhere in Prydz Bay, post-PP-12 sediments are thin and have been highly eroded at various times.