The North American Late Wisconsin ice sheet and mantle viscosity from glacial rebound analyses
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文摘
New constraints on the deglaciation of the North American ice sheet. Importance of palaeo-gradients of pro-glacial lakes in glacial rebound inversions. North American ice sheet multi-domed from at least 18–17 ka BP onwards. Mantle viscosity under North America higher than for continental margins and oceans.
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