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

<table>Steady-state profiles corresponding to Mallik-Richards I. area geothermal model for the range of surface temperatures varying from −10°C to 0°C which are possible in the preglacial, glacial, and interglacial periods.</table>

Journal of Geological Research

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Figure 4

Figure 4: Gas Hydrate Formation and Dissipation Histories in the Northern Margin of Canada: Beaufort-Mackenzie and the Sverdrup Basins 