Clay mineralogy of sdiment core PS2179-3 in the Arctic Ocean

DOI

Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay fraction consists only of clay minerals

Identifier
DOI https://doi.org/10.1594/PANGAEA.695338
Related Identifier https://doi.org/10.1594/PANGAEA.695350
Related Identifier https://doi.org/10.1016/j.margeo.2008.01.006
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.695338
Provenance
Creator Vogt, Christoph ORCID logo; Knies, Jochen
Publisher PANGAEA
Publication Year 2008
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 45 data points
Discipline Earth System Research
Spatial Coverage (138.029 LON, 87.746 LAT); Lomonosov Ridge, Arctic Ocean