Low field magnetic susceptibility in Holocene sediment core CH77-02 from the Gardar drift

Low field magnetic susceptibility normalized by the volume and measured on u-channels with a Bartington MS2C 45-mm diameter susceptibility bridge at 2 cm intervals with a resolution of about 4-5 cm.

Data and Resources

This dataset has no data

Cite this as

Kissel, Catherine (2019). Dataset: Low field magnetic susceptibility in Holocene sediment core CH77-02 from the Gardar drift. https://doi.org/10.1594/PANGAEA.899293

DOI retrieved: 2019

Additional Info

Field Value
Imported on November 29, 2024
Last update November 29, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.899293
Author Kissel, Catherine
Given Name Catherine
Family Name Kissel
Source Creation 2019
Publication Year 2019
Resource Type text/tab-separated-values - filename: CH77-02-SC_magnetic_susceptibility
Subject Areas
Name: Geophysics

Related Identifiers
Title: Variations in the strength of the North Atlantic bottom water during Holocene
Identifier: https://doi.org/10.1016/j.epsl.2013.03.042
Type: DOI
Relation: References
Year: 2013
Source: Earth and Planetary Science Letters
Authors: Kissel Catherine , Van Toer Aurélie , Laj Carlo E , Cortijo Elsa , Michel Elisabeth .