The Fe-Ni-S system at 725 degrees C was studied by means of dry syntheses in evacuated silica glass tubes and microprobe/textural analyses. Contrary to previous beliefs it is dominated by an extensive solid solution field of (Ni,Fe)(3+/-x)S-2 (up to 33 at % Fe) which coexists with sulphide melt; mss does not coexist with melt at this temperature.
|Journal||Neues Jahrbuch fuer Mineralogie. Monatshefte|
|Publication status||Published - 1995|