Effects of bottom water warming and sea level rise on Holocene hydrate dissociation and mass wasting along the Norwegian-Barents Continental Margin
Paleoceanography, Continental margins and sedimentary basins, Marine Geology and Geophysics, Numerical solutions, Tectonophysics, Marine sediments—processes and transport, General, Oceanography, Mathematical Geophysics, Modeling, gas‐hydrate stability, thermobaric model, Storegga slide