An Early Neogene—Early Quaternary Contourite Drift System on the SW Barents Sea Continental Margin, Norwegian Arctic

An Early Neogene—Early Quaternary Contourite Drift System on the SW Barents Sea Continental Margin, Norwegian Arctic

Abstract The onset and evolution of the middle to late Cenozoic “icehouse” world was influenced by the development of the global ocean circulation linking the Norwegian–Greenland Sea‐Arctic Ocean to the Atlantic Ocean. The evolution of the early Neogene to early Quaternary Bjørnøyrenna Drift, locate...

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Bibliographic Details
Main Authors: T. A. Rydningen, G. V. Høgseth, A. P. E. Lasabuda, J. S. Laberg, P. A. Safronova, M. Forwick
Format: Article
Language:English
Published: Wiley 2020-11-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
contourite drift
Mid Miocene Climatic Optimum
high‐latitude ocean circulation
sedimentation rate
submarine slide
Barents Sea
Online Access:https://doi.org/10.1029/2020GC009142

Internet

https://doi.org/10.1029/2020GC009142

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