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

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 enriche...

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Published inDoklady earth sciences Vol. 472; no. 2; pp. 159 - 162
Main Authors Petrov, V. A., Andreeva, O. V., Poluektov, V. V., Kovalenko, D. V.
Format Journal Article
LanguageEnglish
Published Moscow Pleiades Publishing 01.02.2017
Springer
Springer Nature B.V
Subjects
Calderas
Earth and Environmental Science
Earth Sciences
Geological structures
Geology
Igneous rocks
Magma
Mesozoic
Plate tectonics
Tectonics
Zinc compounds
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Summary: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.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
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ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X17020179