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Figure 12
(a) A Williamson–Hall-type plot for the unprepared calcite rock sample. The Miller indices of each diffraction peak are shown on the plot and the error bars are as reported by the peak-fitting routine. The dotted line shows a straight-line fit through the points. (b) The experimental integral breadths (IB) for the same sample are plotted against the fitted values resulting from the Stephens anisotropic strain model (see main text for full details). Vertical error bars are as in part (a) whereas the horizontal error bars are as reported by the Stephens model-fitting routine. The points in red were excluded from the fit. The solid line shows the 1:1 correspondence (it is not a fit through the points).

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ISSN: 2053-2733
Volume 73| Part 4| July 2017| Pages 293-311
https://doi.org/10.1107/S2053273317008592
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