E.s.r., phosphorescence, and thermal studies of the synthetic zeolites mordenite and faujasite indicate that the Fe3+ impurity ions occupy tetrahedral Si4+ or Al3+ positions in the framework.
B. D. McNicol and G. T. Pott, J. Chem. Soc. D, 1970, 438 DOI: 10.1039/C29700000438
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