A new determination of the equilibrium reaction: 2 Mg2[SiOt] @ 3 H~O ~ 1 Mgs[(OH)41 Si~05] ~-1 Mg(OH)~ forsterite serpentine brucite yielded equilibrium temperatures which lie (at identical H20-pressures ) about 60~ lower than all previously published data ( BowEN and TV~TLE, 1949;YODER, 1952; t~TAg
An experimental investigation of the thermal decomposition of brucite by thermosonimetry
β Scribed by Knut Lonvik
- Publisher
- Elsevier Science
- Year
- 1978
- Tongue
- English
- Weight
- 632 KB
- Volume
- 27
- Category
- Article
- ISSN
- 0040-6031
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