The colour and luminescence of tugtupite (beryllosodalite) from Ilímaussaq

Authors

  • A.S Povarennykh
  • A.N Platonov
  • A.N Tarashchan
  • V.P Belichenko

DOI:

https://doi.org/10.34194/bullggu.v95.6636

Abstract

Tugtupite, Na4 [BeAlSi4O12] Cl, is a mineral with bright pink colour and yellow-orange UV-luminescence. The visible region of the spectral absorption curves and the luminescence spectrum of tugtupite from the Ilímaussaq alkaline massif (South Greenland) were studied. Calculated and experimental values of vibrational frequencies of different molecular ions were compared, and it was established that the luminescence of tugtupite is caused by S2 molecular ions occupying the position of Cl ions in the crystal structure. These ions are also the cause of the colour of tugtupite, probably in combination with other, thermically less stable, radiation centres.

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Published

1971-06-30

How to Cite

Povarennykh, A., Platonov, A., Tarashchan, A., & Belichenko, V. (1971). The colour and luminescence of tugtupite (beryllosodalite) from Ilímaussaq. Bulletin Grønlands Geologiske Undersøgelse, 95, 2–12. https://doi.org/10.34194/bullggu.v95.6636