Effect of crystal preferred orientations on the thermal diffusivity of quartz polycrystalline aggregates at high temperature

Tectonophysics

Volumn 465, Issue 1-4, 2009, Pages 150-163

  Gibert, Benoit ^a   Mainprice, David ^a  

^a UNIVERSITÉ MONTPELLIER 2   (France)

Author keywords

Anisotropy; Crystal preferred orientations; Lower crust; Quartz; Quartzite; Thermal diffusivity

Indexed keywords

AGGREGATE PROPERTIES; AMBIENT PRESSURES; CRYSTAL PREFERRED ORIENTATIONS; DIFFUSIVITY ANISOTROPIES; DIRECT MEASUREMENTS; ELECTRON BACK-SCATTERED DIFFRACTIONS; FABRIC STRENGTHS; GRANULITE FACIES; GREENSCHIST; HEAT TRANSPORTS; HIGH TEMPERATURES; LOWER CRUST; M METHODS; MYLONITE; NATURAL ROCKS; ORTHOGONAL DIRECTIONS; PETROPHYSICAL; POLYCRYSTALLINE AGGREGATES; PRESSURE AND TEMPERATURES; QUARTZITE; SINGLE-CRYSTAL PROPERTIES; VOLUME-AVERAGING;

AGGREGATES; ANISOTROPY; CRYSTALLINE ROCKS; CRYSTALLOGRAPHY; FABRICS; GARNETS; OXIDE MINERALS; PRESSURE EFFECTS; QUARTZ; SINGLE CRYSTALS; STRUCTURAL DESIGN; STRUCTURAL GEOLOGY; TENSORS; THERMAL DIFFUSION; THERMAL DIFFUSIVITY; THERMAL EFFECTS; THREE DIMENSIONAL; X RAY POWDER DIFFRACTION;

CRYSTAL ORIENTATION;

ANISOTROPY; CRYSTAL CHEMISTRY; DIFFUSIVITY; MICROSTRUCTURE; P-T CONDITIONS; PREFERRED ORIENTATION; QUARTZ; QUARTZITE;

EID: 60749112799     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2008.11.006     Document Type: Article

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