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

Lara F. Pérez, Tove Nielsen

Afdeling for Geofysik og Sedimentære Bassiner

Publikation: Bidrag til tidsskrift › Artikel › Forskning › peer review

2 Citationer (Scopus)

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	https://doi.org/10.34194/geusb.v38.4416
Status	Udgivet - 31 jul. 2017

Programområde

Programområde 3: Energiressourcer

FN’s Verdensmål

Dette resultat bidrager til følgende verdensmål

Adgang til dokumentet

10.34194/geusb.v38.4416Licens: CC BY

Citationsformater

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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.",

author = "P{\'e}rez, {Lara F.} and Tove Nielsen",

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doi = "10.34194/geusb.v38.4416",

language = "English",

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publisher = "De Nationale Geologiske Unders{\o}gelser for Danmark og Gr{\o}nland",

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T1 - Asynchronous ice-sheet development along the central East Greenland margin: A GLANAM project contribution

AU - Pérez, Lara F.

AU - Nielsen, Tove

PY - 2017/7/31

Y1 - 2017/7/31

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 - http://www.scopus.com/inward/record.url?scp=85024088415&partnerID=8YFLogxK

U2 - 10.34194/geusb.v38.4416

DO - 10.34194/geusb.v38.4416

M3 - Article

SN - 2597-2154

SN - 1904-4666

SN - 1604-8156

VL - 38

SP - 61

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

Resumé

Programområde

FN’s Verdensmål

Adgang til dokumentet

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Citationsformater