“…With increasing x , additional reflections (Figure 2b) indicate the presence of a secondary phase possibly isostructural to some stannite‐type tetragonal phases (
, i.e. Cu 2 M GeS 4 ( M =Fe, Co, Hg) and Cu 2 M SnS 4 ( M =Mn, Fe, Co, Zn, Cd, Hg)
[4–8] . From x =0.2, the content of the assumed tetragonal phase increases at the expense of the orthorhombic phase, the content of which significantly decreases in x =0.4 and x =0.5 samples.…”