Abstract
A representative series of feldspars of composition Ca1-xSrxAl2Si2O8 has been synthesized. The cell parameters have been measured as a function of composition, and a continuous ferroelastic transition from monoclinic to triclinic observed at Ca0.09Sr0.91Al2Si2O8 on increasing Ca content. Ferroelastic and coelastic strains arise in the triclinic phase and indicate that the transition may be modeled in terms of coupled order parameters (primary ferroelastic and secondary coelastic) within the framework of Landau theory. The primary order parameter suggests behavior according to a second-order model. -Authors
Original language | English |
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Pages (from-to) | 24-30 |
Number of pages | 7 |
Journal | American Mineralogist |
Volume | 79 |
Issue number | 1-2 |
Publication status | Published - 1994 |
Externally published | Yes |
ASJC Scopus Subject Areas
- Geophysics
- Geochemistry and Petrology