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Doklady Earth Sciences

, Volume 472, Issue 2, pp 159–162 | Cite as

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

  • V. A. Petrov
  • O. V. Andreeva
  • V. V. Poluektov
  • D. V. Kovalenko
Geology

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.

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Copyright information

© Pleiades Publishing, Ltd. 2017

Authors and Affiliations

  • V. A. Petrov
    • 1
  • O. V. Andreeva
    • 1
  • V. V. Poluektov
    • 1
  • D. V. Kovalenko
    • 1
  1. 1.Institute of Geology of Ore Deposits, Petrography, Mineralogy, and GeochemistryRussian Academy of SciencesMoscowRussia

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