Pressure-induced slip-system transition in forsterite: Single-crystal rheological properties at mantle pressure and temperature

American Mineralogist

Volumn 92, Issue 8-9, 2007, Pages 1436-1445

  Raterron, Paul ^a   Chen, Jiuhua ^b   Li, Li ^a,b   Weidner, Donald ^a,b   Cordier, Patrick ^a  

^a UNIV LILLE   (France)

^b STONY BROOK UNIVERSITY   (United States)

Author keywords

High pressure; Olivine; Rheological law; Seismic anisotropy; Slip systems; Subduction zone; Upper mantle

Indexed keywords

ANISOTROPY; CREEP; CRYSTALLOGRAPHY; HIGH PRESSURE ENGINEERING; HIGH RESOLUTION TRANSMISSION ELECTRON MICROSCOPY; MAGNESIUM COMPOUNDS; SEISMOLOGY; SILICON COMPOUNDS; SINGLE CRYSTALS; STRAIN RATE; STRUCTURAL GEOLOGY; X RAY RADIOGRAPHY;

HIGH PRESSURE; RHEOLOGICAL LAW; SEISMIC ANISOTROPY; SLIP SYSTEM; SUBDUCTION ZONES; UPPER MANTLE;

OLIVINE;

CRYSTALLOGRAPHY; DEFORMATION; DISLOCATION; EXPERIMENTAL MINERALOGY; FORSTERITE; HIGH PRESSURE; HIGH TEMPERATURE; LATTICE DYNAMICS; PREFERRED ORIENTATION; PRESSURE EFFECT; RADIOGRAPHY; RHEOLOGY; SEISMIC ANISOTROPY; SEISMIC ATTENUATION; STRAIN RATE; SUBDUCTION ZONE; TRANSMISSION ELECTRON MICROSCOPY; UPPER MANTLE; X-RAY DIFFRACTION;

EID: 38849169762     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2007.2474     Document Type: Article

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