Journal of Geological Research / 2012 / Article / Fig 9

Research Article

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

Figure 9

Permafrost and GH response to surface forcing considering simple surface temperature history model constrained by present −20°C terrestrial conditions in the QEIG (as in Figure 3). No ice sheet insulation effect is considered.

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