Abstract
Lattice parameters of feldspars of composition Ca1-xSrxAl2Si2O8, (x = 0.85, 0.80, and 0.75) have been measured as a function of temperature (T) from room-T to 950°C. At room-T each is triclinic (I1̄), undergoing a continuous ferroelastic displacive transition to a monoclinic phase (I2/c) on heating. The observed critical temperature (Tc) increases as Ca content increases. The thermodynamic character of the transition also changes, from near-second-order at x = 0.85, approaching tricritical as Ca content increases. Curvature of the transition line through composition (X)-T space suggests the importance of high-order coupling between X and the order parameter. Strain-tails in α and γ close to Tc are interpreted in terms of inhomogeneity of the M-cation distribution, related to tweed microstructures noted in previous investigations. A Landau model is derived which describes the observed transition-related phenomena in the system Ca1-xSrxAl2Si2O8 as a function of T and X.
Original language | English |
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Pages (from-to) | 1159-1172 |
Number of pages | 14 |
Journal | European Journal of Mineralogy |
Volume | 9 |
Issue number | 6 |
DOIs | |
Publication status | Published - 1997 |
Externally published | Yes |
ASJC Scopus Subject Areas
- Geochemistry and Petrology
Keywords
- Ca-Sr feldspars
- Ferroelasticity
- High-temperature X-ray diffraction
- Landau theory
- Phase transition