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Högbomite is a closest-packed polysomatic mineral composed of spinel, T 2 M 4 O 8 , and nolanitelike, TM 4 O 7 (OH), modules where T stands for tetrahedrally and M for octahedrally coordinated cations. The modules are stacked in an ordered fashion in various ratios. Single-crystal X-ray diffraction for a 24R and a 10T polysome and structure modeling for a 12H and 14T polysome have been applied to characterize different stacking variants.

Polysomatism in högbomite: The crystal structures of 10T, 12H, 14T, and 24R polysomes