Within each cubic phase, increasing pressure decreases , so decreases and Bragg's law moves a given reflection to higher . Near , peaks of the rock salt structure disappear as those of the CsCl structure appear, potentially with a coexistence interval. The former has an FCC translation selection rule, with all even or all odd; mixed-parity reflections vanish kinematically. The latter has primitive-cubic translations and basis factor , so it has no FCC extinction rule. Odd-sum reflections may nevertheless be weak because the two ionic scattering factors are similar. Peak spacings, relative intensities and the cell volume per formula unit change discontinuously. A simple uniform shift of the entire original pattern cannot describe the structural transition.

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