
ANALYSIS OF THE CHEMICAL COMPOSITION OF CHAROITE ROCKS
Author(s) -
M. V. Marchuk,
Т. С. Соколова,
А. В. Левин
Publication year - 2017
Publication title -
geodinamika i tektonofizika
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.336
H-Index - 8
ISSN - 2078-502X
DOI - 10.5800/gt-2017-8-3-0277
Subject(s) - outcrop , massif , geology , eluvium , mineralization (soil science) , shield , geochemistry , geography , archaeology , paleontology , weathering , soil science , soil water
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]