Clay mineralogy of sdiment core PS2186-3 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.695342
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.695342
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
Resource Type Dataset
Format text/tab-separated-values
Size 54 data points
Discipline Earth System Research
Spatial Coverage (139.907 LON, 88.512 LAT); Lomonosov Ridge, Arctic Ocean