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A number of different techniques, including optical, fluorescence and scanning electron microscopy, quantitative colour analysis, and x-ray diffraction analysis are used routinely to determine the provenance of rock and sediment particles and powders, and to assess differences and/or similarities between samples. In the case of samples containing gravel particles, different particle types can often be distinguished on the basis of simple properties such as overall shape, texture and colour. More detailed analysis involving examination of thin sections and various forms of mineralogical and chemical analysis, may be required to fully characterise each particle type. Samples which contain predominantly sand and coarse silt are normally examined using a combination of microscopic techniques including scanning electron microscopy. Elemental analysis of individual particles is undertaken by electron microprobe analysis or x-ray microanalysis in the SEM. The bulk mineralogical composition of sands, silts and clays is most commonly determined by x-ray powder diffraction.
Publications Pye, K. (2007). Geological and Soil Evidence: Forensic Applications. CRC Press, Boca Raton, 335 pp. |
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