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Volumn 29, Issue 2, 2010, Pages 176-197

Clay mineral cycles identified by diffuse spectral reflectance in Quaternary sediments from the Northwind Ridge: implications for glacial-interglacial sedimentation patterns in the Arctic Ocean

Author keywords

Arctic Ocean Quaternary palaeoclimate; Arctic Oscillation; Clay mineral provenance; Diffuse spectral reflectance; Glacial interglacial cycles; R mode factor analysis

Indexed keywords

AIR-SEA INTERACTION; CLAY MINERAL; CLIMATE OSCILLATION; CLIMATE VARIATION; FACTOR ANALYSIS; FINE GRAINED SEDIMENT; GLACIAL-INTERGLACIAL CYCLE; ICE COVER; ICE SHEET; MARINE SEDIMENT; PALEOCLIMATE; PROVENANCE; QUATERNARY; SEA ICE; SEA LEVEL CHANGE; SEDIMENT CORE; SEDIMENTATION; SPECTRAL REFLECTANCE;

EID: 77955085211     PISSN: 08000395     EISSN: 17518369     Source Type: Journal    
DOI: 10.1111/j.1751-8369.2010.00160.x     Document Type: Article
Times cited : (23)

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