The system Pd-Fe-Ni-S was studied at 900 and 725 degrees C by means of
dry condensed charges. At both temperatures it is dominated by the ph
ase relationships involving sulphide melt. Pd-Fe-Ni alloys with broad
miscibility primarily coexist with the melt; they are relatively enric
hed in Pd, whereas the associated melt is enriched in Ni. With decreas
ing temperature the melt recedes from Fe-rich regions. The incompatibi
lity of PdS (extensive solid solution with Ni) and mss at 900 degrees
C is replaced by their co-crystallization (+/- disulphide(s) of Ni,Fe
or +/- sulphide melt) at 725 degrees C. The Ni/Fe ratio in the melt ch
anges regularly against that in mss with increasing S fugacity and Pd
contents in these two phases. (Ni,Fe)(3+/-x)S-2 and Pd4S play importan
t roles at 725 degrees C. The data offer an array of distribution coef
ficients and solubility values suitable for geological interpretations
.