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) |
|---|---|
| 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