Doklady Earth Sciences

, Volume 484, Issue 1, pp 92–96 | Cite as

Common Neoproterozoic–Early Paleozoic Evolution of Ore-Bearing Sedimentary Complexes in the Southern Siberian Craton

  • A. E. BudyakEmail author
  • S. Yu. Skuzovatov
  • Yu. I. Tarasova
  • Kuo-Lung Wang
  • N. A. Goryachev


A comparison of the lithological–geochemical parameters for the deposits of the Dalnetaiga series of the Bodaibo synclinorium (the Buzhuikhta and Khomolkho formations) and the Olokit structural-formational zone (the Itykit and Ondok formations), hosting polymetallic deposits (Kholodnin, Ioko-Rybach’e), along with the obtained geochronological LA-ICP-MS U–Pb age estimates of the Ondok Formation (~600 Ma), indicates their similar stratigraphic position in the Neoproterozoic in Southern Siberia. At the first stage of formation of polymetallic and gold-ore objects, the siderochalcophylic trend is considered to have appeared synchronously in the two structural zones, which could have been caused by the hydrothermal activity in the back-arc basin of the Olokit structure.



This work was carried out under state assignment Project IX.130.3.1. (0350-2016-0032) and was supported by the Russian Foundation for Basic Research (project no. 18-05-00081).


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Copyright information

© Pleiades Publishing, Ltd. 2019

Authors and Affiliations

  • A. E. Budyak
    • 1
    • 2
    Email author
  • S. Yu. Skuzovatov
    • 1
    • 3
  • Yu. I. Tarasova
    • 1
    • 5
  • Kuo-Lung Wang
    • 3
  • N. A. Goryachev
    • 1
    • 4
  1. 1.Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of SciencesIrkutskRussia
  2. 2.Irkutsk Science Center, Siberian Branch, Russian Academy of SciencesIrkutskRussia
  3. 3.Institute of Earth Sciences, Academia SinicaTaipeiTaiwan
  4. 4.Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch, Russian Academy of SciencesMagadanRussia
  5. 5.Irkutsk National Research Technical University IrkutskRussia

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