(Table 3) Mineral composition of clay fraction from bottom sediments of the Sea of Okhotsk


0 = traces; + = kaolinite is inferred from resolution of reflection doublets of chlorite (004) and kaolinite (002) in diffractograms; empty digital cells = questionable data.

DOI https://doi.org/10.1594/PANGAEA.785141
Related Identifier https://doi.org/10.1594/PANGAEA.785142
Related Identifier https://doi.org/10.1023/B:LIMI.0000027612.41153.6c
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.785141
Creator Volokhin, Yu G; Astakhov, Anatolii S; Vashchenkova, N G
Publisher PANGAEA
Publication Year 2004
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 481 data points
Discipline Earth System Research
Spatial Coverage (144.732W, 46.973S, 153.623E, 58.583N); Sea of Okhotsk