ANALYSIS OF THE CHEMICAL COMPOSITION OF CHAROITE ROCKS

• Published in: Geodynamics & Tectonophysics
• Main Authors: M. V. Marchuk, T. S. Sokolova, A. V. Levin
• Format: Article in Journal/Newspaper
• Language: English; Russian
• Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017
• Subjects: Science; Q; Aldan; Kamen’; Yakutia
• Online Access: https://doi.org/10.5800/GT-2017-8-3-0277; https://doaj.org/article/ec252a4a0a7e47bd994c33a552a398bf

The unique charoite mineralization, established on the Murun alkaline massif in the northwestern part of the Aldan shield on the border of the Irkutsk region and Yakutia, is still of great interest to some of researchers (geologists, crystallographers, geochemists, etc.). The outcrops of charoite-bearing rocks at the “Sirenevyi Kamen” deposit are noted both in the indigenous outcrops and in eluvial clatters [Bondarenko, 2009].