“…DBI and DBII develop due to a gradual increase of lattice rotations and therefore they often appear together, in conjugate orientations related to each other, and are Philosophical Magazine 273 observed in a broad range of orientations including single and double slip crystals [14,24,25]. Veins, cells and dislocation wall structures are the most common patterns in the h111i region of orientations and they appear in the order of increasing strain amplitude [25,26]. Finally, the so-called labyrinth structure composed of two sets of mutually perpendicular dislocation walls (rungs) on {001} planes, with one wall family always formed perpendicular to the stress axis, is a characteristic dislocation arrangement for single crystals with the orientation of the tensile axis in the neighborhood of h100i [11,25,27,28].…”