Synchronous Changes in Sediment Transport and Provenance at the Iceland-Faroe Ridge Linked to Millennial Climate Variability From 55 to 6 ka BP

Unique marine sediment cores retrieved from the southwestern slope of the Iceland-Faroe Ridge (IFR), close to the main axis of the Iceland-Scotland Overflow Water (ISOW), revealed prominent sedimentary cycles reflecting near-bottom current dynamics, sediment transport, and deposition, coincident wit...

Full description

Bibliographic Details
Main Authors: Mirzaloo, M., Nürnberg, D., Kienast, M., Van Der Lubbe, H. J. L.
Format: Text
Language:English
Published: FID GEO 2019
Subjects:
Greenland
Reykjanes
Fennoscandian
Iceland
Online Access:https://dx.doi.org/10.23689/fidgeo-4707
https://e-docs.geo-leo.de/handle/11858/9053

Similar Items