Crustal Heterogeneity of Antarctica Signals Spatially Variable Radiogenic Heat Production

Abstract Geothermal heat flow (GHF) is a key basal boundary condition for Antarctic ice‐sheet flow. Large‐scale variations are resolved by several recent models but knowledge of the smaller‐scale variations, crucial for ice sheet dynamics, is limited by unresolved variations in crustal radiogenic he...

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Bibliographic Details
Main Authors: L. Li, A. R. A. Aitken
Format: Article
Language:English
Published: Wiley 2024-01-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1029/2023GL106201
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