Baddeleyite segregations in zircon of the Azov zirconium-rare-earth deposit (Ukrainian Shield)
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Jul 31, 2014
About this article
Published Online: Jul 31, 2014
Page range: 125 - 131
DOI: https://doi.org/10.2478/mipo-2013-0009
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© by Dmytro K. Voznyak
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.
Baddeleyite as inclusions in zircon crystals is described for the first time from the ore zone of the Azov zirconium-rare-earth deposit in the Volodarsky (Pivdennokalchytsky) syenite Massif in the Ukrainian Shield. The main admixture in the zircon containing baddeleyite is hafnium (0.68 wt%). The baddeleyite occurs in a substance that fills cracks and that probably corresponds to glass. The chemical compositions of four baddeleyite segregations, and of the hosting glass, are presented. The baddeleyite formed as a result of interaction between zircon and silicate melt with a low SiO2 content. The silicate melt formed under the influence of highthermobaric CO2-fluid flows on the rock.