Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4

Journal of Quaternary Science

Volumn 27, Issue 5, 2012, Pages 475-484

  Andrews, J T ^a   Barber, D C ^b   Jennings, A E ^a   Eberl, D D ^c   Maclean, B ^d   Kirby, M E ^e   Stoner, J S ^f  

^a UNIVERSITY OF COLORADO   (United States)

^b BRYN MAWR COLLEGE   (United States)

^c U S GEOLOGICAL SURVEY   (United States)

^d GEOLOGICAL SURVEY OF CANADA   (Canada)

^e CALIFORNIA STATE UNIVERSITY   (United States)

^f OREGON STATE UNIVERSITY   (United States)

Author keywords

Baffin Bay; Detrital carbonate (DC ) events; Heinrich events; Labrador Sea; Laurentide Ice Sheet

Indexed keywords

CRETACEOUS; DETRITAL DEPOSIT; HEINRICH EVENT; LAURENTIDE ICE SHEET; PROVENANCE; SEDIMENT ANALYSIS; WATER DEPTH;

ATLANTIC OCEAN; BAFFIN BAY [LAGUNA MADRE]; BAFFIN ISLAND; CANADA; CUMBERLAND SOUND; HUDSON STRAIT; LABRADOR SEA; LAGUNA MADRE [TEXAS]; NUNAVUT; TEXAS; UNITED STATES;

EID: 84863597164     PISSN: 02678179     EISSN: 10991417     Source Type: Journal    
DOI: 10.1002/jqs.2535     Document Type: Article

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