Sea-level fluctuations imply that the Younger Dryas ice-sheet expansion in western Norway commenced during the Allerød

Quaternary Science Reviews

Volumn 26, Issue 17-18, 2007, Pages 2128-2151

  Lohne, Øystein S ^a   Bondevik, Stein ^b   Mangerud, Jan ^a,c   Svendsen, John Inge ^a,c  

^a UNIVERSITY OF BERGEN   (Norway)

^b UNIVERSITY OF TROMSØ   (Norway)

^c BJERKNES CENTRE FOR CLIMATE RESEARCH   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

GEOCHRONOLOGY; GRAVITATIONAL EFFECTS; NORWAY;

DATING DEPOSITS; ICE-SHEETS; SEA-LEVEL FLUCTUATIONS; TRANSGRESSION;

SEA LEVEL;

ALLEROD; DEGLACIATION; HOLOCENE; ICE SHEET; LATE GLACIAL; SEA LEVEL CHANGE; TRANSGRESSION; YOUNGER DRYAS;

EURASIA; EUROPE; NORTHERN EUROPE; NORWAY; SCANDINAVIA;

EID: 35548935658     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2007.04.008     Document Type: Article

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