Geology of the Karalon Gold Ore Field in the Mid-Vitim Highlands


Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

Abstract

The paper present new data on the geology of the Karalon gold ore field in northern Buryatia, including its regional position and a brief description of the mineralization, gold–sulfide and gold–quartz–low-sulfide ore objects, host rocks, and complexes, which are components that make up juvenile Late Neoproterozoic Earth’s crust formed in the course of rifting. Paleozoic dike series are characterized, as well as the ore-controlling complex of beresite–listvenite metasomatic rocks. Regularities in the emplacement of gold objects and their control are generalized. Veins and veinlets of gold–quartz mineralization are hosted in gently and steeply dipping structures in the ore field, which formed prior to the intrusive Dogaldyn massif of subalkaline rocks 252 Ma ago.

About the authors

E. Yu. Rytsk

Institute of Precambrian Geology and Geochronology

Email: i.alekseev@spbu.ru
Russian Federation, St. Petersburg, 199034

S. D. Velikoslavinsky

Institute of Precambrian Geology and Geochronology

Email: i.alekseev@spbu.ru
Russian Federation, St. Petersburg, 199034

I. A. Alekseev

St. Petersburg State University

Author for correspondence.
Email: i.alekseev@spbu.ru
Russian Federation, St. Petersburg, 199034

E. S. Bogomolov

Institute of Precambrian Geology and Geochronology

Email: i.alekseev@spbu.ru
Russian Federation, St. Petersburg, 199034

V. P. Kovach

Institute of Precambrian Geology and Geochronology

Email: i.alekseev@spbu.ru
Russian Federation, St. Petersburg, 199034

V. I. Samorukov

RudKaralon Company

Email: i.alekseev@spbu.ru
Russian Federation, Muya District, Republic of Buryatia, 671710

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2018 Pleiades Publishing, Ltd.