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Limits on the areal extent of the Barents Sea ice sheet in Late Weichselian time

✍ Scribed by Kurt Lambeck


Book ID
116157919
Publisher
Elsevier Science
Year
1996
Tongue
English
Weight
966 KB
Volume
12
Category
Article
ISSN
0921-8181

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A fully integrated ice-sheet and glacio-isostatic numerical model was run in order to investigate the crustal response to ice loading during the Late Weichselian glaciation of the Barents Sea. The model was used to examine the hypothesis that relative reductions in water depth, caused by glacio-isos