Variability of clay-mineral composition on Carolina Slope (NW Atlantic) during marine isotope stages 1-3 and its paleoceanographic significance

Marine Geology

Volumn 189, Issue 1-2, 2002, Pages 163-174

  Cagatay M N ^a   Keigwin, L D ^b   Okay, N ^a   San, E ^c   Algan, O ^c  

^a ISTANBUL TECHNICAL UNIVERSITY   (Turkey)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c ISTANBUL UNIVERSITY   (Turkey)

Author keywords

Carolina Slope; Clay mineralogy; NW Atlantic Ocean; Paleoceanography; Stages 1 3

Indexed keywords

AMPLITUDE VARIATIONS;

CLAY; ISOTOPES; SEDIMENTATION; SEDIMENTS; SILT;

CLAY MINERALS;

CLAY MINERAL; HEINRICH EVENT; HOLOCENE; MARINE ISOTOPE STAGE; OCEAN DRILLING PROGRAM; PALEOCEANOGRAPHY;

ATLANTIC OCEAN;

EID: 0037106631     PISSN: 00253227     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0025-3227(02)00330-4     Document Type: Article

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