Figure 11. Prestack depth-migrated seismic section east of Site 900, converted with the velocity model shown in Figure 6. The landward-tilted blocks are separated by normal faults stopping at the underlying reflector H, which is therefore interpreted as detachment fault subcropping near Site 900. Wedge-shaped sedimentary sequences thicken towards the block-bounding faults and can clearly be identified as syn- and/or prerift sediments as also indicated by the changes in velocity. Above, the postrift sequence shows regular and subparallel bedding.