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Tyrrellite, Cu(Co,Ni)2Se4, is a normal spinel containing Cu in a tetra­hedral coordination.

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Isokite, ideally CaMg(PO4)F, is isomorphous with C2/c titanite and consists of PO4, MgO4F2, and CaO6F polyhedra.

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This study presents the first structural report of kolbeckite, with the ideal formula ScPO4·2H2O (scandium phosphate dihydrate), based on single-crystal X-ray diffraction data. Kolbeckite belongs to the metavariscite mineral group, in which each PO4 tetra­hedron shares four vertices with four ScO4(H2O)2 octa­hedra and vice versa, forming a three-dimensional network of polyhedra.

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Iranite is isomorphous with hemihedrite, ZnPb10(CrO4)6(SiO4)2F2. The SiO4 and CrO4 tetra­hedra and CuO4(OH)2 octa­hedra form layers parallel to (120) that are held together by Pb2+ cations.
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