“…For example, LVMs of substitutional S, Be, Mg, and Ca in zinc-blende CdTe and ZnTe as well as S, Be, and Mg in wurtzite CdSe were already reported. [15][16][17][18] Oxygen possesses three stable isotopes-the predominant 16 O one (99.76%) and two other isotopes with very low natural abundances of 0.2% ( 18 O) and 0.04% ( 17 O), which provides the possibility for an unambiguous identification of oxygen-related defects via their isotopic LVM signatures.…”