Changes in the strength of the Iceland-Scotland Overflow Water in the last 200,000 years: Evidence from magnetic anisotropy analysis of core SU90-33

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Keywords: North Atlantic Deep Water; anisotropy; magnetite; paleoclimatology; smectite

Document Type: Research Article


Affiliations: Centre des Faibles Radioactivites, Laboratoire mixte CNRS-CEA, Avenue de la Terrasse 91198, Gif-sur-Yvette, France

Publication date: November 1, 1997

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