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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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Auriac, A., Whitehouse, P.L., Bentley, M.J., Patton, H., Lloyd, J.M., Hubbard, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 2016
Subjects:
Online Access:http://dro.dur.ac.uk/19436/
http://dro.dur.ac.uk/19436/1/19436.pdf
https://doi.org/10.1016/j.quascirev.2016.02.011