Abstract
Reversed experiments on andalusite + water = hydroxyl topaz were run between 600o-900oC and 650-2000 kbar. The thermodynamic calculations based on this data agree well with observations on natural assemblages. -K.A.R.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 956-974 |
| Number of pages | 19 |
| Journal | American Mineralogist |
| Volume | 67 |
| Issue number | 9-10 |
| State | Published - 1982 |
| Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology