I. Hassan, DIRECT OBSERVATION OF PHASE-TRANSITIONS IN ALUMINATE SODALITE, CA-8[AL12O24](CRO4)(2), The American mineralogist, 81(11-12), 1996, pp. 1375-1379
Transmission electron microscopy (TEM) was used to study the structura
l changes that occur in aluminate sodalite, Ca-8[Al12O24](CrO4)(2), wh
en it is heated with the electron beam. Initially, a twinned orthorhom
bic crystal was heated, and it transformed to tetragonal and then to c
ubic symmetry. The cubic phase contains two-dimensional periodic antip
hase boundaries (APBs) along the {110} planes. The APBs are about 54 A
ngstrom apart. Structural modulations also occurred during the transfo
rmations. The transition from tetragonal to orthorhombic symmetry is a
lso associated with random transformation twins on a {110} plane; this
plane is both the composition and twin plane.