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A continuum dislocation model of formation of grains whose boundaries have anon-vanishing thickness is proposed. For a single crystal deforming in simpleshear the lamellar structure of grains with thin layers containing dislocationsas the geometrically necessary boundaries turns out to be energeticallypreferable. The thickness and the energy of this type of grain boundary arecomputed as functions of the misorientation angle.

Formation of grains and dislocation structure of geometrically necessary boundaries