The magnetic properties of iron-containing ETS-IO zeolite and its calc
ined variety have been studied by magnetic measurements, The results a
re consistent with the presence of paramagnetic ions and superparamagn
etic clusters. Calcination results in a shift of the blocking temperat
ures, although their frequency dependence cannot be ascribed to non-in
teracting clusters. The hypothesis of cluster-glass like behaviour is
discussed.