Quantitative Mineralogical Analyses of Carbonate rich Sediments by X-ray Powder Diffraction

Author(s)
A. M. Mansour, Werner E. Piller, Christian Leopold Lengauer
Abstract

The quantitative analysis of carbonate rich materials is tested with conventional and Rietveld methods. In the case of artificial mixtures of aragonite, calcite, Mg-calcite and quartz the Rietveld method provides reliable results with a maximum deviation of ±5 wt %. In the natural samples, however, the conventional methods give more reliable results in comparison to chemical and sedimentological measurements. This is caused by the peak overlap of calcite/Mg-calcite, peak broadening of the Mg-calcite, and the difficulties in the refinement of minor amounts of feldspar phases.

Organisation(s)
Department of Mineralogy and Crystallography
External organisation(s)
South Valley University, Karl-Franzens-Universität Graz
Journal
Powder Diffraction
Volume
10
Pages
112-116
No. of pages
5
ISSN
0885-7156
DOI
https://doi.org/10.1017/S0885715600014469
Publication date
06-1995
Peer reviewed
Yes
Austrian Fields of Science 2012
105116 Mineralogy, 105113 Crystallography
Keywords
ASJC Scopus subject areas
Radiation, Materials Science(all), Instrumentation, Condensed Matter Physics
Portal url
https://ucrisportal.univie.ac.at/en/publications/quantitative-mineralogical-analyses-of-carbonate-rich-sediments-by-xray-powder-diffraction(10eefa37-ee9a-408b-b8ca-e8517ff506e8).html