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Deepwater circulation on Blake Outer Ridge (western North Atlantic) during the Holocene, Younger Dryas, and Last Glacial Maximum (2008)

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