S-ratios of sediment core PS69/288-3

DOI

IRM subsequently acquired in oppositely directed fields of 100 mT (IRM-100) and 300 mT (IRM-300) was measured in order to estimate the ratio of low- ([titano-]magnetite/maghemite) to high-coercive (hematite, goethite) magnetic minerals by calculation of S-100 = IRM-100/IRM700 and S-300 = IRM-300/IRM700 ratios (Liu et al., 2012)

Identifier
DOI https://doi.org/10.1594/PANGAEA.874150
Related Identifier https://doi.org/10.1594/PANGAEA.873755
Related Identifier https://doi.org/10.1038/NCOMMS15591
Related Identifier https://doi.org/10.1029/2012RG000393
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.874150
Provenance
Creator Kuhn, Gerhard ORCID logo; Hillenbrand, Claus-Dieter ORCID logo; Kasten, Sabine ORCID logo; Smith, James A ORCID logo; Nitsche, Frank-Oliver (ORCID: 0000-0002-4137-547X); Frederichs, Thomas ORCID logo; Wiers, Steffen ORCID logo; Ehrmann, Werner; Klages, Johann Philipp ORCID logo; Mogollón, José M ORCID logo
Publisher PANGAEA
Publication Year 2017
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 1104 data points
Discipline Earth System Research
Spatial Coverage (-102.991 LON, -74.416 LAT); Amundsen Sea