Spatial and temporal Arctic Ocean depositional regimes: a key to the evolution of ice drift and current patterns

Sediment physical properties measured in cores from all the major ridges and plateaus in the central Arctic Ocean were studied in order to analyze the spatial and temporal consistency of sediment depositional regimes during the Quaternary. In total, six physiographically distinct areas are outlined....

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Sellen, E., O'Regan, Matthew, Jakobsson, M.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2010
Subjects:
Online Access:https://orca.cardiff.ac.uk/id/eprint/7540/
https://doi.org/10.1016/j.quascirev.2010.06.005