Abstract
The domain structure in (011) crystalline garnet ferrite plates is studied with allowance for induced uniaxial anisotropy and two-constant cubic anisotropy. It is shown that the inclusion of the second constant of cubic anisotropy greatly affects the orientational phase diagram and also the topology of magnetic inhomogeneities in a given magnet. It is found, in particular, that 180°non-Bloch domain walls may appear in a certain range of combined anisotropy constants, causing a continuous change in the wall orientation.
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