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New Data on the Age of Neoproterozoic Volcanic Rocks of the Isakovka Terrane, Sayan–Yenisei Accretion Belt (U–Pb, Zircon)

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Abstract

A Late Neoproterozoic U–Pb zircon age is established for the first time for arc metadacites (691 ± 8.8 Ma) and basalts (572 ± 6.5 Ma) from the Kiselikha Formation of the Kutukas Series. The manifestation of basaltic volcanism is associated with rifting processes. Our studies specify the Late Precambrian stratigraphy of the Yenisei Range and the evolutionary features of the Sayan–Yenisei accretion belt at the Neoproterozoic stage of its history. The fold-and-thrust structures of the junction zone between the Yenisei Range and the West Siberian Plate may be favorable in terms of the search for unconventional oil and gas traps.

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Funding

The studies were supported by the Russian Science Foundation, project no. 16–17–10201.

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Authors and Affiliations

  1. Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, 620022, Yekaterinburg, Russia

    P. S. Kozlov & K. S. Ivanov

  2. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, 630090, Novosibirsk, Russia

    I. I. Likhanov, A. D. Nozhkin & S. V. Zinoviev

  3. Novosibirsk State University, 630090, Novosibirsk, Russia

    S. V. Zinoviev

Authors
  1. P. S. Kozlov
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  2. I. I. Likhanov
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  3. K. S. Ivanov
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  4. A. D. Nozhkin
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  5. S. V. Zinoviev
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Corresponding author

Correspondence to I. I. Likhanov.

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Translated by N. Astafiev

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Kozlov, P.S., Likhanov, I.I., Ivanov, K.S. et al. New Data on the Age of Neoproterozoic Volcanic Rocks of the Isakovka Terrane, Sayan–Yenisei Accretion Belt (U–Pb, Zircon). Dokl. Earth Sc. 488, 1196–1199 (2019). https://doi.org/10.1134/S1028334X19100131

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  • DOI: https://doi.org/10.1134/S1028334X19100131

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