High-temperature ferroelastic strain below the I2/c-I1̄ transition in Ca1-xSrxAl2Si2O8 feldspars

Martin D. Mcguinn*, Simon A.T. Redfern

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

13 Citations (Scopus)

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 languageEnglish
Pages (from-to)1159-1172
Number of pages14
JournalEuropean Journal of Mineralogy
Volume9
Issue number6
DOIs
Publication statusPublished - 1997
Externally publishedYes

ASJC Scopus Subject Areas

  • Geochemistry and Petrology

Keywords

  • Ca-Sr feldspars
  • Ferroelasticity
  • High-temperature X-ray diffraction
  • Landau theory
  • Phase transition

Fingerprint

Dive into the research topics of 'High-temperature ferroelastic strain below the I2/c-I1̄ transition in Ca1-xSrxAl2Si2O8 feldspars'. Together they form a unique fingerprint.

Cite this