All specimens studied by the authors of the original description contained somedjurleite.
Note: Many of the reported associations ofdigenite anddjurleite, identified by powder diffraction, could be anilite and djurleite, as anilite transforms to digenite during grinding (Goble, 1985). If heated, anilite decomposes to high digenite and covellite above 70 +- 3°C (Morimoto & Koto, 1970).
3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1) 1 : Sulphides etc. of Cu