Asynchronous ice-sheet development along the central East Greenland margin: A GLANAM project contribution

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Abstract

The sedimentary record of the glaciated margins of the North Atlantic holds evidence of past ice-sheet activity, and reflects spatial and temporal variations in the ice–ocean–climate interaction as well as the influence of tectonic processes. Furthermore, the record of cross-shelf ice sheets provides a direct link between the continental ice cover and the deep ocean, a relevant issue in the context of climate research.
Original languageEnglish
Pages (from-to)61-64
Number of pages4
JournalGeological Survey of Denmark and Greenland Bulletin
Volume38
DOIs
Publication statusPublished - 31 Jul 2017

Programme Area

  • Programme Area 3: Energy Resources

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