Evidence for an 12/a to Imab phase transition in the silica polymorph moganite at ∼570 K

P. J. Heaney, J. E. Post

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Abstract

Rietveld analysis of synchrotron X-ray powder diffraction data for the silica mineral moganite from 100 K to 1354 K has revealed a reversible phase transition from space group 12/a to Imab at approximately 570 K. The thermal expansion behavior of the lattice parameters alters sharply at the transition point, and the monoclinic β angle decreases to 90°. The displacive transition from α- to β- moganite is effected by the rotation of apparently rigid tetrahedra about the [010] axis, and the linear temperature dependence of the volume strain and of the non-symmetry-breaking e11 and e22 strains indicates that the character of the transition is second-order. The continuous increase in the b axis over the entire temperature range reveals a concomitant rotation of tetrahedra about [100] that does not affect the overall symmetry. In addition, we present a refinement without structural constraints for α-moganite at room temperature using time-of-flight neutron diffraction data.

Original languageEnglish (US)
Pages (from-to)1358-1366
Number of pages9
JournalAmerican Mineralogist
Volume86
Issue number11-12
DOIs
StatePublished - Jan 1 2001

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology

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