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Figure 10
Rietveld refinement results for the Cumberland mudstone (∼41.1 h integration). The vertical lines near 7.4 and 10.1° 2θ represent the positions of split Pearson VII profiles used to model the ∼10 Å and ∼14 Å diffraction peaks from phyllosilicates. The differences near 22° 2θ are due to the 02l diffraction band from the phyllosilicates.

IUCrJ
Volume 1| Part 6| October 2014| Pages 514-522
ISSN: 2052-2525
doi:10.1107/S2052252514021150