creep mechanisms

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The mechanisms by which materials deform at the Earth's surface or, more commonly, at depth. These can be: (a) cataclastic, in which individual grains or fragments physically rotate or glide past one another; (b) dislocational, by a gliding motion along crystalline dislocations; (c) grain-boundary sliding; (d) recrystallization; and (e) the diffusion of individual atoms. Each process is dependent on the degree, temperature, and duration of the stress.

Subjects: Ecology and Conservation — Earth Sciences and Geography.

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