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...

Full description

Bibliographic Details
Main Author: Kissel, Catherine
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