Abstract
The crystal structure of the high-pressure phase-II of cristobalite has been solved by neutron diffraction (space group P21/c, a = 8.3780(11) Å, b = 4.6018(6) Å, c = 9.0568(13) Å, β = 124.949(7)°, at P = 3.5 GPa). This phase corresponds to a distortion of the high-temperature cubic β-phase, rather than of the ambient temperature and pressure tetragonal α-phase.
Original language | English |
---|---|
Pages (from-to) | 569-576 |
Number of pages | 8 |
Journal | Mineralogical Magazine |
Volume | 64 |
Issue number | 3 |
DOIs | |
State | Published - Jun 2000 |
Keywords
- Cristobalite
- High-pressure
- Neutron diffraction
- Phase transitions