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 language | English |
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Pages (from-to) | 61-64 |
Number of pages | 4 |
Journal | Geological Survey of Denmark and Greenland Bulletin |
Volume | 38 |
DOIs | |
Publication status | Published - 31 Jul 2017 |
Programme Area
- Programme Area 3: Energy Resources