Changes in the Western Boundary Undercurrent Outflow since the Last Glacial Maximum, from smectite/illite ratios in deep Labrador Sea sediments

Paleoceanography

Volumn 12, Issue 1, 1997, Pages 79-96

  Fagel, Nathalie ^a   Hillaire Marcel, Claude ^a   Robert, Christian ^b  

^a UNIVERSITÉ DU QUÉBEC À MONTRÉAL   (Canada)

^b STATION MARINE D ENDOUME   (France)

Author keywords

[No Author keywords available]

Indexed keywords

CLAY MINERALOGY; CLAY MINERALS; GYRE; LAST GLACIAL MAXIMUM; OUTFLOW; PALAEOCEANOGRAPHY; WESTERN BOUNDARY UNDERCURRENTS;

LABRADOR SEA;

EID: 0030961657     PISSN: 08838305     EISSN: 19449186     Source Type: Journal    
DOI: 10.1029/96PA02877     Document Type: Article

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