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 - 1986 |
| Externally published | Yes |
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ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics
Cite this
Phase equilibria and thermodynamic properties of minerals in the BeO-Al2O3-SiO2-H2O (BASH) system, with petrologic applications. / Barton, Mark D.
In: American Mineralogist, Vol. 71, No. 3-4, 1986, p. 277-300.Research output: Contribution to journal › Article
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TY - JOUR
T1 - Phase equilibria and thermodynamic properties of minerals in the BeO-Al2O3-SiO2-H2O (BASH) system, with petrologic applications.
AU - Barton, Mark D
PY - 1986
Y1 - 1986
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=0022834391&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0022834391&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0022834391
VL - 71
SP - 277
EP - 300
JO - American Mineralogist
JF - American Mineralogist
SN - 0003-004X
IS - 3-4
ER -