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

Lara F. Pérez; Tove Nielsen

doi:10.34194/geusb.v38.4416

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

Department of Geophysics and Sedimentary Basins

Research output: Contribution to journal › Article › Research › peer-review

2 Citations (Scopus)

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
Pages (from-to)	61-64
Number of pages	4
Journal	Geological Survey of Denmark and Greenland Bulletin
Volume	38
DOIs	https://doi.org/10.34194/geusb.v38.4416
Publication status	Published - 31 Jul 2017

Programme Area

Programme Area 3: Energy Resources

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

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10.34194/geusb.v38.4416Licence: CC BY

Cite this

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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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AU - Pérez, Lara F.

AU - Nielsen, Tove

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N2 - 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.

AB - 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.

UR - https://www.scopus.com/pages/publications/85024088415

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DO - 10.34194/geusb.v38.4416

M3 - Article

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SN - 1904-4666

SN - 1604-8156

VL - 38

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EP - 64

JO - Geological Survey of Denmark and Greenland Bulletin

JF - Geological Survey of Denmark and Greenland Bulletin

ER -

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

Abstract

Programme Area

UN SDGs

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