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A similar trend is observed for dislocation density.
b The metachert shows microstructural evidence for dislocation creep.
First, we analyze the necessary stress for dislocation nucleation at surfaces versus that for dislocation penetration of twin boundaries, the latter being stress for yielding.
This approach simplifies and extends existing results for dislocation dynamics.
The stress exponent for dislocation creep is about 6.6.
Grain boundaries are introduced as obstacles for dislocation motion.
More than half (56%) showed impingement, including 94% of those removed for dislocation.
Two cups were revised (0.9%): one for dislocation and another for infection.
In principle, these codes can be extended to allow for dislocation modeling in finite bodies.
A thermostatistical model for dislocation evolution is employed to describe deformation twinning in martensite.
The analysis for dislocation and bond angles at different incidence angles is shown in Fig. 10.
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