Abstract
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.
| Original language | English |
|---|---|
| Journal | Neues Jahrbuch fuer Mineralogie. Monatshefte |
| Volume | 1 |
| Pages (from-to) | 1-10 |
| ISSN | 0028-3649 |
| Publication status | Published - 1995 |