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DISLOCATION CREEP [1 record]

Record 1 2000-12-14

English

Subject field(s)
  • Rheology
CONT

Crustal deformation is dominated by dislocation processes. Dislocations are line defects in a crystal (ex: line of missing atoms). Dislocations can move easily at high temperature (say 300°C for quartz). The motion of dislocations in a crystallographic plane is called dislocation glide. Dislocation glide allows deformation of crystals and results in crystallographic preferred orientation. A strong microfabric is typically interpreted as resulting from dislocation glide mechanisms because very few other processes would produce a crystallographic preferred orientation.

French

Domaine(s)
  • Rhéologie
DEF

Fluage caractérisé des mouvements intercristallins.

Spanish

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