Due to very bad weather we were able to run only one line crossing the ABFZ. The line AB01M was processed up to the stack and time migration. Fig.25 shows part of the neartrace (channel 22, offset 425 m from source) profile. The valley is filled by sediments which appear to be folded and displaced by strong currents flowing along the two walls.
The data seems to have a good potential also for deeper reflections.
figure
