Lattice-preferred orientations in post-perovskite-type MgGeO3 formed by transformations from different pre-phases

Physics of the Earth and Planetary Interiors

Volumn 180, Issue 3-4, 2010, Pages 195-202

  Okada, T ^a   Yagi, T ^a   Niwa, K ^a   Kikegawa, T ^b  

^a UNIVERSITY OF TOKYO   (Japan)

^b INSTITUTE OF MATERIALS STRUCTURE SCIENCE   (Japan)

Author keywords

D anisotropy; Lattice preferred orientation; MgGeO3; Plastic deformation; Post perovskite; Topotactic transformation

Indexed keywords

COMPRESSION AXIS; DEGREE OF DEFORMATIONS; DIAMOND-ANVIL CELL; DIFFRACTION PEAKS; DOMINANT SLIP SYSTEM; LASER-HEATED DIAMOND-ANVIL CELL; LATTICE PREFERRED ORIENTATION; ORTHOPYROXENE; POST-PEROVSKITE; RELATIVE INTENSITY; ROOM TEMPERATURE; SLIP PLANE; TOPOTACTIC TRANSFORMATION; WAVE POLARIZATIONS; X-RAY DIFFRACTION TECHNIQUES;

ANISOTROPY; DIAMONDS; GASKETS; HOLOGRAPHIC INTERFEROMETRY; OXIDE MINERALS; PEROVSKITE; PLASTIC DEFORMATION; SILICATES; SINGLE CRYSTALS; TOOLS; X RAY DIFFRACTION; X RAY POWDER DIFFRACTION;

PLASTICS;

ANISOTROPY; CRYSTAL CHEMISTRY; DIAMOND ANVIL CELL; LATTICE DYNAMICS; MICROSTRUCTURE; ORTHOPYROXENE; PEROVSKITE; PLASTIC DEFORMATION; POLARIZATION; PREFERRED ORIENTATION; TRANSFORMATION; X-RAY DIFFRACTION;

EID: 77953231376     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2009.08.002     Document Type: Article

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