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The structure of the title compound is described as a cubic close-packed arrangement of O atoms containing Cu+/Cu2+ ions in a tetra­hedral coordination. Slabs of edge-sharing CrO6 octa­hedra and isolated CuO4 and GeO4 tetra­hedra are aligned parallel to the bc plane and are separated from each other by GeO4 tetra­hedra along a.

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The crystal structure of Ca2Ge7O16 has been redetermined in tetra­gonal symmetry and some comparison is made with Cd2Ge7O16 and AB4O9 structures having A = Sr, P and Ba, and B = Ge.

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The structural topology of the new synthetic material Ca3GeO4Cl2 is described and compared with the olivine-type Ca2GeO4 and norbergite-type Mg3SiO4F2.

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The structure and absolute configuration of tetra­gonal Y2Ge2O7 was determined from X-ray diffraction data. A comparison is made with related lanthanide pyrogermanates of the series R2Ge2O7 (R = Eu and Tb-Lu).
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