Abstract
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) |
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Pages (from-to) | 277-300 |
Number of pages | 24 |
Journal | American Mineralogist |
Volume | 71 |
Issue number | 3-4 |
State | Published - Jan 1 1986 |
Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology