Gas Hydrate Formation and Dissipation Histories in the Northern Margin of Canada: Beaufort-Mackenzie and the Sverdrup Basins
Figure 15
IBP and GH bases variations in the last 100 ka according to the three versions of the ground surface temperature history. For all three versions, the history of the last 6 Myr was considered and is the same for the first 5.1 Myr. It differs in the last 0.9 Myr during the 9 large 100 ka glacial cycles. The differences are shown in this figure, where each version has its own color, the same for temperature, IBP, and GH.