Crystallographic preferred orientation in wüstite (FeO) through the cubic-to-rhombohedral phase transition

Physics and Chemistry of Minerals

Volumn 39, Issue 8, 2012, Pages 613-626

  Kaercher, P ^a   Speziale, S ^b   Miyagi, L ^c   Kanitpanyacharoen, W ^a   Wenk, H R ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^c UNIVERSITY OF UTAH   (United States)

Author keywords

Diamond anvil cell; Phase transition; Preferred orientation; W stite

Indexed keywords

ADVANCED LIGHT SOURCE; COMPRESSION DIRECTIONS; CRYSTALLOGRAPHIC PREFERRED ORIENTATIONS; CUBIC PHASE; DIAMOND-ANVIL CELL; IN-SITU; POLYCRYSTAL PLASTICITY; PREFERRED ORIENTATIONS; RADIAL GEOMETRIES; RHOMBOHEDRAL PHASE; TEXTURE PATTERNS; UNIAXIAL STRESS; VARIANT SELECTION;

LIGHT SOURCES; PHASE TRANSITIONS; TEXTURES; X RAY DIFFRACTION;

IRON OXIDES;

COMPRESSION; CRYSTAL STRUCTURE; CRYSTALLOGRAPHY; DEFORMATION; DIAMOND ANVIL CELL; MAGNESIOWUSTITE; ORIENTATION; PHASE TRANSITION; PLASTICITY; TEMPERATURE EFFECT; TEXTURE;

EID: 84865783922     PISSN: 03421791     EISSN: 14322021     Source Type: Journal    
DOI: 10.1007/s00269-012-0516-x     Document Type: Article

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