Tectonomagmatic cycles and geodynamic conditions of formation of the ore-bearing systems in the Southern Argun’ Region
- Авторы: Petrov V.A.1, Andreeva O.V.1, Poluektov V.V.1, Kovalenko D.V.1
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Учреждения:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Выпуск: Том 472, № 2 (2017)
- Страницы: 159-162
- Раздел: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/189268
- DOI: https://doi.org/10.1134/S1028334X17020179
- ID: 189268
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Аннотация
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.
Об авторах
V. Petrov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: akimolan@igem.ru
Россия, Moscow, 119117
O. Andreeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Автор, ответственный за переписку.
Email: akimolan@igem.ru
Россия, Moscow, 119117
V. Poluektov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: akimolan@igem.ru
Россия, Moscow, 119117
D. Kovalenko
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: akimolan@igem.ru
Россия, Moscow, 119117
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