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Permafrost at the ice base of recent pleistocene glaciations–inferences from borehole temperature profiles
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Paleo-temperature reconstruction from precise depth (>2.0 km) well temperature logs can offer information on whether the bed of an ice sheet was frozen. Inversion or upward extrapolation of the >2-km-deep geothermal profile is the only method by which temperature evolution at the base of...
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