Permafrost at the ice base of recent pleistocene glaciations–inferences from borehole temperature profiles
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 long-...
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Format: | Other/Unknown Material |
Language: | English |
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2012
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Online Access: | https://era.library.ualberta.ca/items/d320cec2-16aa-4d80-ac8c-73a18636cb8f https://doi.org/10.7939/R3WS8HQ5X |