Tectonomagmatic cycles and geodynamic conditions of formation of the ore-bearing systems in the Southern Argun’ Region
- Authors: Petrov V.A.1, Andreeva O.V.1, Poluektov V.V.1, Kovalenko D.V.1
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Affiliations:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Issue: Vol 472, No 2 (2017)
- Pages: 159-162
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/189268
- DOI: https://doi.org/10.1134/S1028334X17020179
- ID: 189268
Cite item
Abstract
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.
About the authors
V. A. Petrov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: akimolan@igem.ru
Russian Federation, Moscow, 119117
O. V. Andreeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Author for correspondence.
Email: akimolan@igem.ru
Russian Federation, Moscow, 119117
V. V. Poluektov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: akimolan@igem.ru
Russian Federation, Moscow, 119117
D. V. Kovalenko
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: akimolan@igem.ru
Russian Federation, Moscow, 119117