Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison

The 3D geometrical evolution of the Barents Sea Ice Sheet (BSIS), particularly during its late-glacial retreat phase, remains largely ambiguous due to the paucity of direct marine- and terrestrial-based evidence constraining its horizontal and vertical extent and chronology. One way of validating th...

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Veröffentlicht in:	Quaternary science reviews 2016-09, Vol.147, p.122-135
Hauptverfasser:	Auriac, A., Whitehouse, P.L., Bentley, M.J., Patton, H., Lloyd, J.M., Hubbard, A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Barents Sea Geofag: 450 Geosciences: 450 Glacial isostatic adjustment modelling Ice sheet Matematikk og Naturvitenskap: 400 Mathematics and natural science: 400 Relative sea level VDP
Online-Zugang:	Volltext
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