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During the formation of persistent slip bands, cross slip bands between primary slip bands were often observed.
Dislocation slip bands can be observed.
In addition, slip bands inside the cells are also observed.
Consequently, GNB formation localizes deformation in specific slip bands.
The crack propagated along persistent slip bands within the grain.
It can be seen clearly that the slip bands aligned parallel to the (0001) basal plane intersect the slip bands propagating along the (10-11) planeidal plane.
Crack nucleation and propagation along slip bands were difficult in the grains with wavy or cross slip bands, and they were easy in the grains with straight slip bands.
Severe slip bands were observed in the Ag nanowires after the deformation.
The Ag NWs showed good ductility, and severe slip bands were observed after deformation.
The computation results demonstrate that the random and square distribution patterns of diamond particles lead to long-distance slip bands and stacking slip bands in the SiC matrix, respectively.
A number of microstructural changes were observed in the recovered pipe fragments: deformation of the soft alpha-ferrite grains, deformation of pearlite colonies, twin formation, bands of distorted pearlite colonies, slip bands, and cross-slip bands.
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