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The Equilibrium FeO + H 2 = Fe + H 2 O at Temperatures up to the Melting Point of Iron

✍ Scribed by Chipman, John; Marshall, Shadburn


Book ID
126878701
Publisher
American Chemical Society
Year
1940
Tongue
English
Weight
709 KB
Volume
62
Category
Article
ISSN
0002-7863

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Stability of almandine in the system FeO
✍ I. Keesmann; S. Matthes; W. Schreyer; F. Seifert πŸ“‚ Article πŸ“… 1971 πŸ› Springer 🌐 English βš– 816 KB

Almandine, although decomposing in the presence of metallic iron into the anhydrous subsolidus assemblage fayalite + ferrocordierite + hereynite solid solution at low pressures, melts incongruently to hercynitess -~ quartz + liquid at 10 kb. At pressures between about 12 and 20 kb the products of in