Tectonomagmatic cycles and geodynamic conditions of formation of the ore-bearing systems in the Southern Argun’ Region


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The evolution of the geological structure in the Southern Argun’ Region is studied in terms of changing geodynamic conditions of the Proterozoic, Caledonian, and Variscan Tectonomagmatic Cycles, which also under Mesozoic tectonomagmatic activation led to the formation of latite igneous rocks enriched in Au, Cu–Mo, Pb–Zn–Ag, volcanic and plutonic complexes of the caldera structures with Mo–U, Pb–Zn, and fluorite ores, and rare-metal granites with a Sn–W–Li–Ta spectrum.

作者简介

V. Petrov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: akimolan@igem.ru
俄罗斯联邦, Moscow, 119117

O. Andreeva

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

编辑信件的主要联系方式.
Email: akimolan@igem.ru
俄罗斯联邦, Moscow, 119117

V. Poluektov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: akimolan@igem.ru
俄罗斯联邦, Moscow, 119117

D. Kovalenko

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: akimolan@igem.ru
俄罗斯联邦, Moscow, 119117

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