Clay mineralogy of sdiment core PS2172-1 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. Smectite, illite, kaolinite and chlorite by area, kaolinite/chlorite by intensity

Identifier
DOI https://doi.org/10.1594/PANGAEA.695333
Related Identifier IsPartOf https://doi.org/10.1594/PANGAEA.695350
Related Identifier References 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.695333
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 90 data points
Discipline Earth System Research
Spatial Coverage (68.377 LON, 87.257 LAT); Amundsen Basin