Hydrolytic weakening of olivine at mantle pressure: Evidence of [100](010) slip system softening from single-crystal deformation experiments

Physics of the Earth and Planetary Interiors

Volumn 216, Issue , 2013, Pages 12-20

  Girard, Jennifer ^a   Chen, Jiuhua ^a   Raterron, Paul ^b   Holyoke, Caleb W ^c  

^a FLORIDA INTERNATIONAL UNIVERSITY   (United States)

^b UNIVERSITÉ LILLE 1   (France)

^c TEXAS A AND M UNIVERSITY   (United States)

Author keywords

High pressure; Olivine; Plasticity; Single crystal

Indexed keywords

ABSORBANCES; ACTIVATION VOLUME; CRYSTAL DEFORMATION; DIFFERENTIAL STRESS; DISLOCATION CLIMB; DISLOCATION GLIDE; DISLOCATION SLIP; FLOW LAW; FORSTERITES; FT-IR SPECTRUM; HIGH PRESSURE; HIGH TEMPERATURE; HYDROLYTIC WEAKENING; HYDROXYL CONTENT; LOW CONFINING PRESSURE; LOW WATER; RECOVERING PROCESS; REFERENCE FRAME; SEM AND TEM; SITU X-RAY DIFFRACTION; SLIP SYSTEM; TIME RESOLVED IMAGING; WATER FUGACITY; WAVE NUMBERS;

DEFORMATION; DISLOCATIONS (CRYSTALS); EXPERIMENTAL MINERALOGY; EXPERIMENTS; FOURIER TRANSFORM INFRARED SPECTROSCOPY; OLIVINE; PLASTICITY; RHEOLOGY; TALC; X RAY DIFFRACTION;

SINGLE CRYSTALS;

COMPRESSION; CONFINING PRESSURE; CRYSTAL STRUCTURE; CRYSTALLOGRAPHY; DEFORMATION MECHANISM; DEHYDRATION; DISLOCATION; EXPERIMENTAL MINERALOGY; FORSTERITE; FTIR SPECTROSCOPY; FUGACITY; MANTLE PROCESS; OLIVINE; P-T CONDITIONS; PRESSURE EFFECT; RHEOLOGY; STRAIN RATE; X-RAY DIFFRACTION;

EID: 84873151743     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2012.10.009     Document Type: Article

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