1. Structure and twinning of tetragonal [Ca.sub.3][Mn.sub.2][Ge.sub.3][O.sub.12] garnet
- Author
-
HEINEMANN, STEFAN and MILETICH, RONALD
- Subjects
Garnet -- Environmental aspects ,Twinning (Crystallography) -- Research ,Earth sciences - Abstract
Single crystals of tetragonal [Ca.sub.3][Mn.sub.2][Ge.sub.3][O.sub.12] garnet (space group symmetry [14.sub.1]/a, a = 12.3098(7) [Angstrom], c = 12.3277(9) [Angstrom]) were characterized by X-ray diffraction and transmission electron microscopy. Their structure is topologically isosymmetric to tetragonal high-pressure garnets such as majorite, displaying the same two distinct types of macroscopic twin mechanisms. Twinning occurs as pseudomerohedral ferroelastic twin lamellae with preferred orientation of the twin-domain boundaries parallel to [{101}.sub.tet], whereas merohedral ferrobielastic twin domains occur without any orientational preference. The crystal structure was determined from single-crystal X-ray diffraction data of a crystal fragment completely free of pseudo-merohedral twin domains. It shows two different Jahn-Teller distorted Mn[O.sub.6] octahedra, with a different orientation of the axis of polyhedral elongation. The ordering scheme of these Jahn-Teller distorted octahedra follows in an alternating pattern the densest rod packing, and the cooperative effect of the electronically induced octahedral distortion was found to be responsible for the cubic-to-tetragonal symmetry breaking in [Ca.sub.3][Mn.sub.2][Ge.sub.3][O.sub.12] garnet. The extent of polyhedral distortion indicates a partially dynamic character of the Jahn-Teller effect. The distortion of the tetrahedral T2 sites controls the cooperative effect of the lattice strain induced by the Jahn-Teller distortion of the [Mn.sup.3+] octahedra and thus is responsible for the overall lower symmetry.
- Published
- 2000