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...
Published in: | Geological Society, London, Special Publications |
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Main Authors: | , , |
Format: | Book Part |
Language: | English |
Published: |
Geological Society
1998
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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 |