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Comparison of selected fragments and electron microprobe analytical data of Facies 2 (Unit 3, floor) sediment in the Dinaledi Chamber, and floor sediments in the Dragon's Back Chamber.
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A series of experimental samples with Cl contents ranging from 2 to 80 ppm that have been determined by SIMS (Dalou et al., 2012), were analyzed by electron microprobe using the analytical conditions described above.
This is usually done via electron microprobe analysis or, occasionally, other analytical approaches.
To determine the composition of the run products, hand-picked crystals of sufficient size were embedded in epoxy resin and analysed with a JEOL JXA-8100 electron microprobe in the wavelength-dispersive analytical mode.
The analytical spots for FTIR, Raman, and the electron microprobe were all at the same coordinates and identified by the sample textures.
Selected scale-fragments were further investigated by high spatial (temporal) resolution analytical techniques involving elemental mapping using the wavelength-dispersive analytical mode (WDX) and back-scattered electron imaging (BSE) using a JEOL JXA-8200 electron microprobe (EPMA).
The most common analytical procedure is to quantify the major elemental composition of the sample via an electron microprobe (EMP).
The primary instrument used is the electron microprobe.
An electron microprobe functions in much the same manner.
The electron microprobe is widely used for analyzing the composition of the component minerals.
The chemical analysis of minerals is undertaken with the electron microprobe (see above).
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