Formation of truscottite and xonotlite was studied at Ca/(Si + A~) = 0.6, 300-350Β°C and saturated steam pressures. Truscottite is favored by use of silicic acid rather than quartz, or of B-CzS rather than Ca(OH)2, and by the presence of small amounts of alkali. Partial replacement of Si by A~ has n
Equilibria and non-equilibria in the formation of xonotlite and truscottite
β Scribed by K. Luke; H.F.W. Taylor
- Publisher
- Elsevier Science
- Year
- 1984
- Tongue
- English
- Weight
- 421 KB
- Volume
- 14
- Category
- Article
- ISSN
- 0008-8846
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