Electrical conductivity anisotropy of deformed talc rocks and serpentinites at 3GPa

Physics of the Earth and Planetary Interiors

Volumn 188, Issue 1-2, 2011, Pages 69-81

  Guo, Xinzhuan ^a   Yoshino, Takashi ^a   Katayama, Ikuo ^b  

^a OKAYAMA UNIVERSITY   (Japan)

^b HIROSHIMA UNIVERSITY   (Japan)

Author keywords

Anisotropy; Electrical conductivity; Orientation; Serpentinite; Subduction zone; Talc

Indexed keywords

ACTIVATION ENTHALPIES; COLD SUBDUCTION; CONDUCTION MECHANISM; CONDUCTION PATHS; ELECTRICAL CONDUCTIVITY; ELECTRICAL CONDUCTORS; FERRIC IRON; FREQUENCY RANGES; GRAIN INTERIORS; HYDROGEN CONCENTRATION; HYDROGEN MOBILITY; HYDROUS MINERAL; IMPEDANCE ANALYZER; IMPEDANCE SPECTRUM; MULTI-ANVIL PRESS; ORDERS OF MAGNITUDE; OXYGEN FUGACITY; PROTON MIGRATION; ROCK TYPES; SERPENTINITE; SUBDUCTION ZONES; TEMPERATURE RANGE; WELL-ALIGNED; Z-DIRECTIONS;

ANISOTROPY; CRYSTAL ORIENTATION; ENTHALPY; GRAIN BOUNDARIES; HYDROGEN; OXYGEN; ROCKS; STRUCTURAL GEOLOGY; TALC; TECTONICS;

ELECTRIC CONDUCTIVITY;

DEFORMATION; ELECTRICAL CONDUCTIVITY; ENTHALPY; FOLIATION; FUGACITY; GRAIN BOUNDARY; LINEATION; SERPENTINITE; SUBDUCTION ZONE; TALC; TEMPERATURE;

EID: 80053310182     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2011.06.012     Document Type: Article

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