The solubility of carbon in iron-nickel sulfide melts at 1673 K was studied in the entire range of compositions of the Fe-FeS-N3S2-Ni tetragon. The boundaries of the stratification area were determined in this system upon its being saturated with carbon. Lines of carbon isosolubility are plotted in the tetragon field outside the stratification area.
机构:
Univ Complutense Madrid, Fac Ciencias Geol, Dept Mineral & Petrol, C Jose Antonio Novais,12,Ciudad Univ, Madrid 28040, SpainCSIC, Inst Andaluz Ciencias Tierra, Avda Palmeras 4, Granada 18100, Spain