Resumé
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.
| Originalsprog | Engelsk |
|---|---|
| Sider (fra-til) | 61-64 |
| Antal sider | 4 |
| Tidsskrift | Geological Survey of Denmark and Greenland Bulletin |
| Vol/bind | 38 |
| DOI | |
| Status | Udgivet - 31 jul. 2017 |
Programområde
- Programområde 3: Energiressourcer