Cyclic sedimentation on the Faeroe Drift 53-10 ka BP related to climatic variations

More than 15 sedimentary cycles dated to the last glacial period (53-10 ka BP) have been recognized in a contourite deposit on the Faeroe Drift in the southern part of the Norwegian Sea. Each cycle consists of a silty, basaltic lower part and a clayey, acidic (siliceous) upper part. The sedimentary...

Full description

Bibliographic Details
Published in:Geological Society, London, Special Publications
Main Authors: Rasmussen, Tine L., Thomsen, Erik, Van Weering, Tjeerd C. E.
Format: Book Part
Language:English
Published: Geological Society 1998
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/39504/
https://oceanrep.geomar.de/id/eprint/39504/1/Rasmussen.pdf
https://doi.org/10.1144/GSL.SP.1998.129.01.16