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An investigation of the γ-Fe2O3+H2O system heated under high pressure

✍ Scribed by F. Mathieu; A. Rousset


Publisher
Springer
Year
1989
Tongue
English
Weight
203 KB
Volume
8
Category
Article
ISSN
0261-8028

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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