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Mossbauer spectroscopy was used to study iron in the β-, δ-, δ'- and -iron tellurides in the temperature range from 300 to 1000 K. Mossbauer diffusional line broadening was observed in all phases except the -phase. The activation energies for iron diffusional jump frequencies in the β-, δ- and δ'-phases increased in this order with increasing tellurium concentrations. This fact may be explained...
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