THE NATURE OF RED LUMINESCENCE OF NATURAL BENITOITE BATISI3O9

dc.contributor.author	Gaft M.
dc.contributor.author	Nagli L.
dc.contributor.author	Waychunas G.
dc.contributor.author	Panczer G.
dc.date.accessioned	2023-12-16T06:35:06Z
dc.date.available	2023-12-16T06:35:06Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=27983307
dc.identifier.citation	Mineralogy and Petrology, 2005, 85, 1-2, 33-44
dc.identifier.issn	0930-0708
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/42339
dc.description.abstract	This work examines the red luminescence of benitoite studied by laser-induced time-resolved luminescence spectroscopy. This method allows the differentiation between luminescence centers of similar emission wavelengths, but different decay times. We have also examined the luminescence intensity and decay time as a function of temperature. We found that the red emission of benitoite consists of two individual bands and one line and suggest that the activators of luminescence in benitoite system are Ti3+ and a d3 element, namely Cr3+ or Mn4+. © Springer-Verlag/Wien 2005.
dc.subject	luminescence
dc.subject	benitoite
dc.title	THE NATURE OF RED LUMINESCENCE OF NATURAL BENITOITE BATISI3O9
dc.type	Статья
dc.identifier.doi	10.1007/s00710-005-0100-x

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