GRACE constraints on Earth rheology of the Barents Sea and Fennoscandia
<p>The Barents Sea is situated on a continental margin and was home to a large ice sheet at the Last Glacial Maximum. Studying the solid Earth response to the removal of this ice sheet (glacial isostatic adjustment; GIA) can give insight into the subsurface rheology of this region. However, be...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-03-01
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| Series: | Solid Earth |
| Online Access: | https://www.solid-earth.net/11/379/2020/se-11-379-2020.pdf |