Abstract
Dislocation cathodoluminescence exhibiting certain peculiarities in anisotropy of polarization localized in sheets parallel to octahedral planes in a mosaic, semiconducting natural diamond is interpreted as a macroscopic manifestation of microscopic interactions between glide dislocations on these octahedral slip planes and the dislocations of the mosaic, whereby passage of fresh glide dislocations through low-angle boundaries and forest dislocations of the mosaic has produced jogs which have persisted since the deformation.

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