(Table 3) Peak intensity ratios in the <2 µm fraction and smectite crystallinity, ODP Hole 114-699A

DOI

For the calculation of the peak intensity ratio the peak height of the clay minerals was divided by the peak height of the internal standard of the same XRD trace.

Identifier
DOI https://doi.org/10.1594/PANGAEA.755277
Related Identifier https://doi.org/10.1594/PANGAEA.755279
Related Identifier https://doi.org/10.2973/odp.proc.sr.114.121.1991
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.755277
Provenance
Creator Monty, Claude L V; Westall, Francis; van der Gaast, Sjierk
Publisher PANGAEA
Publication Year 1991
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 14 data points
Discipline Earth System Research
Spatial Coverage (-30.677 LON, -51.542 LAT); South Atlantic Ocean
Temporal Coverage Begin 1987-03-20T10:45:00Z
Temporal Coverage End 1987-03-26T15:29:00Z