plastset deformatsiooni põhjustav kristallivõre jääv muutus (deformatsioon) kristallisisese libisemismehhanismi kohaselt (seotud paralleelsete kristallograafiatasandite libisemisega üle üksteise) (vt nihe)
a mechanism of deformation in which parallel crystallographic planes in a body remain parallel but are relatively displaced in a direction parallel to themselves with a tendency for adjacent planes to slide over each other (see: shear)
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