LUMINESCENCE SPECTROSCOPIC STUDY OF CR3+ IN BRAZILIAN TOPAZES FROM OURO PRETO

dc.contributor.authorTarashchan A.N.
dc.contributor.authorTaran M.N.
dc.contributor.authorRager H.
dc.contributor.authorIwanuch W.
dc.date.accessioned2025-03-15T04:58:53Z
dc.date.available2025-03-15T04:58:53Z
dc.date.issued2006
dc.description.abstractIn this paper, the results of investigation of luminescent properties of topazes from Ouro Preto, Brazil are presented. It is established that all photoluminescence characteristics of variously colored topazes are due to three structurally non-equivalent Cr3+ centers isomorphically substituting Al3+ in the topaz structure and forming [CrO4F2]7-, [CrO4OH,F]7-, and [CrO4(OH)2]7- complexes. Kinetics of thermal annealing indicates different thermal stability of these centers. Less stable [CrO4OH, F]7-- and [CrO4(OH)2]7- complexes diminish in temperature range 950-1,100°C, accompanied by appearance of corundum phase. The most stable [CrO4F2]7- centers completely decay at 1,250°C and luminescence spectrum of product obtained becomes identical to that of Cr3+ in mullite indicating that topaz completely transforms to mullite. © Springer-Verlag 2005.
dc.identifierhttps://elibrary.ru/item.asp?id=27832918
dc.identifier.citationPhysics and Chemistry of Minerals, 2006, 32, 10, 679-690
dc.identifier.doi10.1007/s00269-005-0042-1
dc.identifier.issn0342-1791
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/48540
dc.subjectCHROMIUM
dc.subjectLUMINESCENCE
dc.subjectPHASE-TRANSITIONS
dc.subjectTOPAZ
dc.titleLUMINESCENCE SPECTROSCOPIC STUDY OF CR3+ IN BRAZILIAN TOPAZES FROM OURO PRETO
dc.typeСтатья

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