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


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Аннотация

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.

Авторлар туралы

E. Rytsk

Institute of Precambrian Geology and Geochronology

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

S. Velikoslavinsky

Institute of Precambrian Geology and Geochronology

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

I. Alekseev

St. Petersburg State University

Хат алмасуға жауапты Автор.
Email: i.alekseev@spbu.ru
Ресей, St. Petersburg, 199034

E. Bogomolov

Institute of Precambrian Geology and Geochronology

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

V. Kovach

Institute of Precambrian Geology and Geochronology

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

V. Samorukov

RudKaralon Company

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

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