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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.
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Editors Adam A. Garde and Ole Bennike
The 17 contributions in this Review of Survey activities reflect the wide range of activities currently performed by the Geological Survey of Denmark and Greenland, commonly in collaboration with external partners.
Topics in and around Denmark include the important Danish potential for geothermal energy, a shale gas [...]
