Summary
The thermoluminescence of α- and μ-cordierite samples has been recordedvs. temperature and wavelength. Arguments ascribing the observed emission to the easy ion exchanges characterizing cordierite lattices are advanced.
References
W. Schreyer andJ. F. Schairer:Z. Kristallogr., Kristallgeom., Kristallphys.,116, 60 (1961).
A. Betekhtin:A Course of Mineralogy (Peace Publishers, Moscow, 1961).
P. Brovetto, A. Delunas, V. Maxia, G. Spano andC. Cortese:Nuovo Cimento D,12, 331 (1990).
P. Brovetto, A. Delunas, V. Maxia, M. Salis, D. Mazza, M. Vallino andA. Delmastro:Nuovo Cimento D,13, 1379 (1991).
W. Schreyer andJ. F. Schairer:J. Petrol.,2, 349 (1961).
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Brovetto, P., Maxia, V., Salis, M. et al. Investigation of cordierite lattice defects by thermoluminescence experiments. Nouv Cim D 14, 655–660 (1992). https://doi.org/10.1007/BF02462352
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DOI: https://doi.org/10.1007/BF02462352