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Polychronous zirconology of syenites from the Avashla intrusion in the Kurgass anticline (Southern Urals)

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Abstract

Zircons were separated from syenites of the Avashla intrusion in the Kurgass anticline of the Bashkir megaanticlinorium in the Southern Urals. The obtained samples were dated using the U–Pb procedure by means of a SHRIMP II ion microprobe. The integrated mineralogical, geochemical, and isotope studies of zircons resulted in primary data on the origin and current conditions of zircons in syenites of the Avashla intrusion. The relics of early zircon generations (1320–1340 Ma) allowed us to specify the geological position of syenites along with the stratigraphic location of the enclosing sedimentary rocks. The time of the transformation (metamorphism) of the zircons at the Middle–Upper Riphean boundary is represented by a dating of 1097±20 Ma, which is of importance for specifying the boundary age and for revealing a geological event that started a new development stage of the stratoregion in the Upper Riphean.

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Authors and Affiliations

  1. Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Yekaterinburg, 620016, Russia

    A. A. Krasnobaev, V. N. Puchkov & S. V. Busharina

  2. Institute of Geology, Ufa Scientific Center, Russian Academy of Sciences, Ufa, 450077, Russia

    A. A. Krasnobaev, V. N. Puchkov & N. D. Sergeeva

  3. Karpinsky Russian Geological Research Institute, St. Petersburg, 199106, Russia

    S. P. Shokalski

Authors
  1. A. A. Krasnobaev
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  2. V. N. Puchkov
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  3. N. D. Sergeeva
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  4. S. P. Shokalski
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  5. S. V. Busharina
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Correspondence to V. N. Puchkov.

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Original Russian Text © A.A. Krasnobaev, V.N. Puchkov, N.D. Sergeeva, S.P. Shokalski, S.V. Busharina, 2017, published in Doklady Akademii Nauk, 2017, Vol. 473, No. 2, pp. 195–200.

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Krasnobaev, A.A., Puchkov, V.N., Sergeeva, N.D. et al. Polychronous zirconology of syenites from the Avashla intrusion in the Kurgass anticline (Southern Urals). Dokl. Earth Sc. 473, 323–328 (2017). https://doi.org/10.1134/S1028334X1703014X

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  • DOI: https://doi.org/10.1134/S1028334X1703014X

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