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Figure 4
Illustration of the variant crossing phenomenon. (a) The crystallographic distance (in degrees) to the Bain OR. Frequently reported KS and NW ORs are at 11.07° and 9.74°, respectively. The map exhibits a much broader scatter. The black boundaries delineate different Bain groups. (b) A spatial map colored according to the value of θ. This panel shows that the orientation may cross multiple variants of a given OR in a single Bain group while preserving a spatial continuity at this scale (i.e. θ varies much more than 7.54°, which is the smallest Δθ separating two variants in the cited ORs).

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 57| Part 5| October 2024| Pages 1598-1608
https://doi.org/10.1107/S1600576724008392
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