Isostatic uplift in the late Weichselian Barents Sea: implications for ice-sheet growth

Isostatic uplift in the late Weichselian Barents Sea: implications for ice-sheet growth

Results from a recent time-dependent ice-sheet modelling study of the late Weichselian Svalbard—Barents Sea ice sheet suggest that, under environmental conditions representative of those during the late Weichselian, ice derived solely from Svalbard may have occupied only the relatively shallow (

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Veröffentlicht in:Annals of glaciology 1996, Vol.23, p.352-358
Hauptverfasser: Siegert, M. J., Fjeldskaar, W.
Format: Artikel
Sprache:eng
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Zusammenfassung:Results from a recent time-dependent ice-sheet modelling study of the late Weichselian Svalbard—Barents Sea ice sheet suggest that, under environmental conditions representative of those during the late Weichselian, ice derived solely from Svalbard may have occupied only the relatively shallow (
ISSN:0260-3055
1727-5644
DOI:10.3189/S026030550001363X