Geochemical Evolution and Ore-Bearing Metasomatic Rocks of the Baga-Gazryn Multiphase Massif of Rare-Metal Li–F Granites (Mongolia)

This paper considers the geochemical evolution of igneous and metasomatic rocks in the Baga-Gazryn Massif on the basis of new precision analytical data. The Baga-Gazryn rocks are characterized by enrichment in F, which is concentrated in Li–F mica, topaz, and fluorite. Along with F, zwitters and mic...

Full description

Saved in:
Bibliographic Details
Published in:Doklady earth sciences 2018-12, Vol.483 (1), p.1468-1472
Main Authors: Antipin, V. S., Kuzmin, M. I., Odgerel, D., Kousch, L. V., Perepelov, A. B.
Format: Article
Language:English
Subjects:
Concentrates (ores)
Data processing
Earth and Environmental Science
Earth Sciences
Evolution
Fluorite
Geochemistry
Granite
Heavy metals
Lithium
Mica
Niobium
Rock
Rocks
Tantalum
Titanium
Topaz
Zinc
Zirconium
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:This paper considers the geochemical evolution of igneous and metasomatic rocks in the Baga-Gazryn Massif on the basis of new precision analytical data. The Baga-Gazryn rocks are characterized by enrichment in F, which is concentrated in Li–F mica, topaz, and fluorite. Along with F, zwitters and microclinites are enriched in Li, Rb, Cs, and ore elements Sn, W, Zn. High-charge elements (Zr, Hf, Nb, Ta, and Ti) and also Th and U are not very different in the Baga-Gazryn granites of various phases and metasomatic rocks.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X18110168