Abstract
Heulandites from Rudno (Poland) and from Val Fassa (Italy) were studied by Mössbauer spectroscopy method. It was shown that iron can exist in different forms: as a magnetically, diluted hematite or as ions built into the framework of a zeolite or bound in its channels.
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Kraczka, J., Kulgawczuk, D.S., Hrynkiewicz, A.Z. et al. Mössbauer study of naturally occurring heulandites. Hyperfine Interact 29, 1129–1132 (1986). https://doi.org/10.1007/BF02399433
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DOI: https://doi.org/10.1007/BF02399433