Gas Hydrate Formation and Dissipation Histories in the Northern Margin of Canada: Beaufort-Mackenzie and the Sverdrup Basins

Figure 5

3 Myr history of surface temperature forcing (“cold” versus “warm” models), IBP and GH base depth variation—Case 1 model (entrapment by structural cap (GH formation was considered below 900 m only)) for the high 60% GH saturation assumed as maximum case.