“…In heavy rare earth iron garnets, there exists a compensation temperature (T comp ) or inversion temperature (T I ) (Herpin, 1968) at which the bulk ferrite magnetization vanishes. For TbIG, T comp is equal to (243.5 ± 0.5 K) and (249.0 ± 0.5 K) for the single crystal and powder samples respectively (Lahoubi et al, 1985;Lahoubi, 1986). In the vicinity of T comp, the magnetic behavior is equivalent to that observed in the antiferromagnet compounds with the existence of the so-called field induced phase transitions which have been studied previously theoretically and experimentally (Zvezdin, 1995).…”