Modelling the influence of glacial isost
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Daniel Howell; Martin J. Siegert; Julian A. Dowdeswell
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Article
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2000
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John Wiley and Sons
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English
โ 509 KB
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