Abstract
An investigation using TEM, high temperature X-ray powder diffraction and high temperature single-crystal X-ray diffraction revealed previously unreported microstructures and phase transitions in natural kaliophilite. Measurements of unit cell dimensions from room temperature to 895°C indicate the existence of a displacive phase transition at ~725°C between two hexagonal phases with the same unit cell. A symmetry change of P6322 ⇄ P63 is tentatively suggested with the concomitant development of merohedral twins. The thermal evolution of kaliophilite is sufficiently different from that of kalsilite to indicate that it has a different framework topology and is not a true stuffed tridymite structure. -from Authors
Original language | English (US) |
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Pages (from-to) | 1209-1220 |
Number of pages | 12 |
Journal | European Journal of Mineralogy |
Volume | 4 |
Issue number | 6 |
DOIs | |
State | Published - 1992 |
All Science Journal Classification (ASJC) codes
- Geochemistry and Petrology