We investigate the magnetic polariton modes which propagate in metamagnet thin films, consisting of ferromagnetically ordered layers, with the intralayer ferromagnetic exchange interactions being much stronger than the weak antiferromagnetic interaction between adjacent layers. We consider also the presence of an external magnetic field H 0 applied perpendicular to the layers. We confine our discussion to the metamagnet materials FeCl 2 and FeBr 2 in which the magnetic anisotropy is sufficiently large compared with the weak antiferromagnetic coupling, so that there is no spin-flop phase intermediate between the AFM and FM phases. The dynamic response of a metamagnetic material is derived within the classical torque equation of motion model. Our theoretical results indicate that there is a larger frequency separation in FeBr 2, compared with FeCl 2 in the surface magnetic polariton spectra, which favor the former material for experimental studies.
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