Journal of Geological Research / 2012 / Article / Fig 5

Research Article

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.

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