P-Cable 3D study of pockmarks and shallow fluid flow systems at the Snøhvit field in the SW Barents Sea
Successful collaboration between UiT and VBPR
Analysis of high-resolution 3D P-Cable seismic data from the Hammerfest Basin to describe likely fluid pathways leading to pockmark formation at the seabed. Also explaining the age and timescale of pockmark development, and conceptual model illustrating pockmark formation mechanisms.