ONTOGENESIS OF CORUNDUM DEPOSITS OF THE RAY-IZ MASSIF, THE POLAR URALS

Ontogenetic studies of a collection of corundum-bearing plagioclasites and glimmtrites from Rubinovy Log occurrence in the Ray-Iz massif, Polar Urals, indicate a magmatic model of formation of mineralization. The main morphological of feature is eutectic structure of rock-forming plagioclase, phlogo...

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Bibliographic Details
Main Authors: V.A. Popov, V.M. Vasilyev, I.A. Blinov, V.I. Popova
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2019-09-01
Series:Минералогия
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Online Access:https://journal.mineralogy.ru/wp-content/uploads/2019/11/2019-3-6.pdf
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