The phase relations and thermodynamic properties of behoite, bertrandite, beryl, bromellite, chrysoberyl, euclase and phenakite have been quantitatively evaluated from a combination of new phase-equilibrium, solubility, calorimetric and volumetric measurements, and with data from the literature. The resulting thermodynamic model is consistent with natural low-variance assemblages and can be used to interpret many beryllium-mineral occurrences.-J.A.Z.
|Original language||English (US)|
|Number of pages||24|
|State||Published - 1986|
ASJC Scopus subject areas
- Geochemistry and Petrology