Bottom-current variability during the last glacial-deglacial transition, Northern Rockall Trough and Faroe Bank Channel, NE Atlantic
Two Sediment gravity cores and a multicore collected from contourite sediment drifts north and south of the Wyville Thomson Ridge provide a detailed textural record of bottom-current variability since the last glaciation. Four radiocarbon dates indicate that collectively the cores span the last c. 4...
Published in: | Scottish Journal of Geology |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2009
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Subjects: | |
Online Access: | https://pure.uhi.ac.uk/en/publications/596ffce6-2e02-4437-b912-46cc614d4f0b https://doi.org/10.1144/0036-9276/01-375 |