Temperature survey of zircon from the granitoids of the Subpolar Urals

Now significant experience of use of zircon as geothermometer was accumulated. This allows applying different methodologies to determine a more accurate temperature mode of formation of the given rocks. The study results of accessory granitoids zircon of the Subpolar Urals (the Badjaju, Yarot, Kozhim and Nikolaihsor massifs) are presented in this paper. The temperatures of crystallization of the mineral using thermometry of zircon saturation and the classic evolutionary - morphological analysis were determined. the comparison of data, obtained in different ways, was carriedout. the temperatures of formation of the studied massifs of the Subpolar Urals were specified.