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

Authors

  • Lara F. Pérez Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark
  • Tove Nielsen Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark

DOI:

https://doi.org/10.34194/geusb.v38.4416

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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Volume 38 GEUS Bulletin front cover

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Published

31-07-2017

How to Cite

Pérez, L. F., & Nielsen, T. (2017). Asynchronous ice-sheet development along the central East Greenland margin: a GLANAM project contribution. GEUS Bulletin, 38, 61–64. https://doi.org/10.34194/geusb.v38.4416

Issue

Vol. 38 (2017): Review of Survey activities 2016

Section

RESEARCH ARTICLE | SHORT

License

GEUS Bulletin is an open-access, peer-reviewed journal published by the Geological Survey of Denmark and Greenland (GEUS). This article is distributed under a CC-BY 4.0 licence, permitting free redistribution and reproduction for any purpose, even commercial, provided proper citation of the original work. Author(s) retain copyright over the article contents. Read the full open access policy.