Abstract
That leucite transforms from a tetragonal to a cubic polymorph with increasing temperature has been accepted for nearly a century, but the precise nature of this transition has provoked some disagreement. X-ray diffraction experiments suggest that leucite inverts directly from space group I41/a to Ia3d; however, two distinct absorption events appear in most calorimetric experiments, raising the possibility that leucite passes through an intermediate phase with space group I41/acd. The transition between low and high leucite was examined in situ during heating experiments with a transmission electron microscope. Dark-field imaging with the 420 diffracted beam revealed pseudomerohedral and merohedral twin types in the low-temperature polymorph, and with increasing temperature the contrast among both sets of twins steadily diminished. We conclude that leucite can indeed occur as a distinct intermediate phase with space group I41/acd that is metrically but not symmetrically cubic within the error of our measurements. -from Authors
Original language | English (US) |
---|---|
Pages (from-to) | 464-476 |
Number of pages | 13 |
Journal | American Mineralogist |
Volume | 75 |
Issue number | 5-6 |
State | Published - Jan 1 1990 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Geochemistry and Petrology