Clay mineral determination of sediment core GeoB13823-2

DOI

Device: PANalytical EMPYREAN; CuK[Alpha] radiation (40 kV, 40 mA)Method: Each sample was analyzed between 2.5° and 29° 2 Theta, with a step size of 0.013° in the air-dried state and after ethylene glycol solvation. X-ray diffraction measurements were performed on organic and carbonate-free, preferentially oriented clay-size filer cakes (< 2 µm) with molybdenite as an internal standard. Further details of sample preparation techniques are described in Petschick et al. [1996] and Diekmann and Kuhn [1999]. Diffractograms were evaluated using the "MacDiff 4.2.5" software [Petschick et al., 1996] without using a weighted average smoothing but applying a molybdenite (006) peak correction.

Identifier
DOI https://doi.org/10.1594/PANGAEA.874944
Related Identifier https://doi.org/10.1594/PANGAEA.874957
Related Identifier https://doi.org/10.1002/2016PA003079
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.874944
Provenance
Creator Warratz, Grit ORCID logo; Henrich, Rüdiger; Voigt, Ines ORCID logo; Chiessi, Cristiano Mazur ORCID logo; Kuhn, Gerhard ORCID logo; Lantzsch, Hendrik ORCID logo
Publisher PANGAEA
Publication Year 2017
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 252 data points
Discipline Earth System Research
Spatial Coverage (-53.344 LON, -38.145 LAT)