Deglaciation of a marine-based ice sheet: Late Weichselian palaeo-ice dynamics and retreat in the southern Barents Sea reconstructed from onshore and offshore glacial geomorphology

Quaternary Science Reviews

Volumn 29, Issue 3-4, 2010, Pages 424-442

  Winsborrow, Monica C M ^a   Andreassen, Karin ^a   Corner, Geoffrey D ^a   Laberg, Jan Sverre ^a  

^a UNIVERSITY OF TROMSØ   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

3D SEISMIC; BARENTS SEA; CONFIGURATION AND DYNAMICS; CONTINENTAL MARGIN; DATA SETS; DEGLACIATIONS; DEVELOPED SERIES; EUSTATIC SEA LEVEL; FENNOSCANDIA; GLACIAL GEOMORPHOLOGY; GROUNDING LINE; GROUNDING-ZONE WEDGES; HIGH VARIABILITY; ICE DYNAMICS; ICE SHEET; ICE STREAMS; KOLA PENINSULA; REMOTE SENSING DATA; SEA FLOOR; SOURCE AREA; SPATIAL AND TEMPORAL VARIATION; SWATH BATHYMETRY;

DYNAMICS; GEOMORPHOLOGY; GLACIAL GEOLOGY; GLACIERS; HYDRAULICS; LANDFORMS; REMOTE SENSING; SEA ICE; SEA LEVEL; THREE DIMENSIONAL;

GEOCHRONOLOGY;

DEGLACIATION; EUSTACY; GEOMORPHOLOGY; GLACIAL ENVIRONMENT; GLACIER RETREAT; ICE SHEET; LAST GLACIAL MAXIMUM; REMOTE SENSING; SEA ICE; SPATIOTEMPORAL ANALYSIS; SWATH BATHYMETRY; WEICHSELIAN;

ARCTIC OCEAN; BARENTS SEA; FENNOSCANDIA; KOLA PENINSULA; MURMANSK [RUSSIAN FEDERATION]; RUSSIAN FEDERATION;

EID: 74649086905     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2009.10.001     Document Type: Article

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