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Clay mineral signature of the NW Atlantic Boundary Undercurrent

✍ Scribed by N. Fagel; C. Robert; C. Hillaire-Marcel

Book ID
103261596
Publisher
Elsevier Science
Year
1996
Tongue
English
Weight
907 KB
Volume
130
Category
Article
ISSN
0025-3227

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Variability of clay-mineral composition
Variability of clay-mineral composition on Carolina Slope (NW Atlantic) during marine isotope stages 1–3 and its paleoceanographic significance
✍ M.N Γ‡ağatay; L.D Keigwin; N Okay; E SarΔ±; O Algan πŸ“‚ Article πŸ“… 2002 πŸ› Elsevier Science 🌐 English βš– 542 KB

The clay-mineral composition of marine isotope stages 1^3 sediments at the Ocean Drilling program (ODP) Site 1055 on the Carolina Slope consists mainly of illite, kaolinite, chlorite and smectite. Clay-mineral variability is marked by a distinct increase in the relative amounts of kaolinite and smec