Rare-Earth Sublattice Canting in DyIG, ErIG, and YbIG

Abstract
Neutron diffraction data taken on DyIG, ErIG, and YbIG at show superlattice reflections at low temperatures that indicate a decomposition of the rare‐earth sublattice. The data are interpreted with a model in which rare‐earth spins tilt away from [111] in {110} planes, with a double conical arrangement, although this model is not unique.

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