Magnetic properties and sortable silt data from marine sedimentsfrom the Gardar drift and the Charlie-Gibbs fracture zone as tracers for bottom current dynamic
Magnetic properties coupled with sortable silt are investigated for Holocene marine sedimentary sequences located in the subpolar North Altantic, in the Charlie– Gibbs fracture zone (53°N) and in central (57°N) and southern Gardar drift (59°N). All the cores are located at water depths bathed by the...
Main Author: | |
---|---|
Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2019
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.899300 https://doi.org/10.1594/PANGAEA.899300 |