Blue zircon from Ratanakiri, Cambodia

Author(s)
Manuela Zeug, Lutz Nasdala, Bhuwadol Wanthanachaisaeng, Walter A. Balmer, Fernando Corfu, Manfred Wildner
Abstract

Zircon from Ratanakiri Province, north-eastern Cambodia, is well known in the gem trade for its vivid blue colour that results from heat treatment. The untreated brown material turns blue under reducing conditions at ~900-1,000°C. Ratanakiri zircon is characterised by remarkably low contents of trace elements. In particular, the actinides have low concentrations (e.g. approximately 120 ppm U and 95 ppm Th). Together with the very young age of the zircon ( < 1 million years [Ma]), this results in an extremely low self-irradiation dose, which in turn is in agreement with its non-radiation-damaged, nearly perfectly crystalline state. The heat treatment, therefore, does not result in detectable changes in the zircon's structural state. The cause of the blue colour, presumably related to a valence change upon heating in the reducing environment, is still under debate. The absorption of the treated Ratanakiri zircon is decidedly different from that of blue U

4+-doped and blue V

4+-doped synthetic ZrSiO

4. Absorption spectra show a strongly pleochroic band at 18,200- 13,000 cm

-1 (corresponding to ~550-770 nm wavelength) that is clearly responsible for the treated blue colour; however, its assignment remains unresolved.

Organisation(s)
Department of Mineralogy and Crystallography
External organisation(s)
Burapha University, University of Oslo, Chulalongkorn University
Journal
The Journal of Gemmology
Volume
36
Pages
112-132
No. of pages
21
ISSN
1355-4565
DOI
https://doi.org/10.15506/JoG.2018.36.2.112
Publication date
06-2018
Peer reviewed
Yes
Austrian Fields of Science 2012
104026 Spectroscopy, 105116 Mineralogy
Keywords
ASJC Scopus subject areas
Geochemistry and Petrology
Portal url
https://ucrisportal.univie.ac.at/en/publications/865ec945-f621-4c7b-b993-1e8db95c89b9