• DOI:10.3749/CANMIN.49.6.1687
Corpus ID: 56429488

A REVISION OF PHASE RELATIONS IN THE SYSTEM Fe–Ni–S FROM 650° TO 450°C

@article{Kitakaze2011ARO,
  title={A REVISION OF PHASE RELATIONS IN THE SYSTEM Fe–Ni–S FROM 650° TO 450°C},
  author={A. Kitakaze and A. Sugaki and H. Itoh and R. Komatsu},
  journal={Canadian Mineralogist},
  year={2011},
  volume={49},
  pages={1687-1710}
}

• A. Kitakaze, A. Sugaki, +1 author R. Komatsu
• Published 2011
• Geology
• Canadian Mineralogist

An elongate field of high-form pentlandite solid-solution, Fe 5.65 Ni 3.35 S 7.85 , β 2 (Ni 4± x S 3 ), occurs in the system Fe–Ni–S at 650°C. This solid solution coexists with monosulfide solid-solution, β 1 (Ni,Fe) 3± x S 2 and γ (Fe,Ni). Pentlandite with a composition Fe 5.60 Ni 3.40 S 7.82 first appears as a stable phase at 625°C owing to the phase transition of the most Fe-rich high-form pentlandite with the same composition. It grows as a limited solid-solution, from Fe 5.64 Ni 3.36 S 7… Expand

View via Publisher

msoc.eng.yamaguchi-u.ac.jp

Save to Library

Create Alert

Cite

Launch Research Feed