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Figure 1
Part of the measured high-resolution X-ray diffraction spectrum of powdered geological aragonite (open circles) superimposed on the best-fit calculated Rietveld refinement profile (solid line) and their difference (solid line at the bottom). Upper, middle and lower rows of tick marks represent Bragg positions of aragonite, α-quartz and calcite reflections, respectively. The insert shows two closely related diffraction peaks, 200 (on the right) and 102 (on the left), the latter missing in the JCPDS file 41–1475.

Journal logoSTRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS
ISSN: 2052-5206
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