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...

Full description

Bibliographic Details
Published in:Scottish Journal of Geology
Main Authors: McIntyre, Kate, Howe, John
Format: Article in Journal/Newspaper
Language:English
Published: 2009
Subjects:
SEA
Online Access:https://pure.uhi.ac.uk/en/publications/596ffce6-2e02-4437-b912-46cc614d4f0b
https://doi.org/10.1144/0036-9276/01-375