Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (2008)
Attributed to:
DEEP WESTERN BOUNDARY CURRENT VARIABILITY IN THE SUBTROPICAL NORTHWEST ATLANTIC OCEAN DURING THE PAST 450 KYR
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2007gc001771
Publication URI: http://dx.doi.org/10.1029/2007gc001771
Type: Journal Article/Review
Parent Publication: Geochemistry, Geophysics, Geosystems
Issue: 3