1. Comparison between seafloor bathymetry derived from a P-Cable 3D seismic survey (b) and multibeam bathymetry (a) in an area dominated by iceberg plough marks.
Comparison between seafloor bathymetry derived from a P-Cable 3D seismic survey (b) and multibeam bathymetry (a) in an area dominated by iceberg plough marks. Figure courtesy of Stefan Buenz, UiT, the Arctic University of Norway.
M. Jakobsson et al. Geological Society, London, Memoirs 2016;46:17-40
© 2016 The Author(s). Published by The Geological Society of London