Magnetic susceptibility of sediment core LV76-21

DOI

The sediment magnetic susceptibility (MS) was measured onboard using a Satis Geo KM-7 kappameter at a resolution of 1 cm. Within 2 h after coring, the sediment core was split, and one half of core was used for the MS measurements. Values of the sediment MS are determined by concentration of terrigenous ferromagnetic material and of volcanogenic material as well.

Identifier
DOI https://doi.pangaea.de/10.1594/PANGAEA.954779
Related Identifier https://doi.pangaea.de/10.1594/PANGAEA.954780
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.954779
Provenance
Creator Gorbarenko, Sergey A ORCID logo; Kirichenko, Ivan S; Psheneva, Olga; Bosin, Aleksandr A ORCID logo
Publisher PANGAEA
Publication Year 2024
Rights Creative Commons Attribution 4.0 International; Data access is restricted (moratorium, sensitive data, license constraints); https://creativecommons.org/licenses/by/4.0/
OpenAccess false
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 548 data points
Discipline Earth System Research
Spatial Coverage (167.262 LON, 51.567 LAT)