Journal of Geological Research / 2012 / Article / Fig 11

Research Article

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

Figure 11

The depth migration of the base of the GH stability zone responding to ice sheet buildup (from 0 km to 2 km thickness) for the QEIG geothermal and climate model. It was assumed that the pressure increase is a hydrostatic one and that the effect of 1 km thick ice sheet corresponds to 1 km of a water column.

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