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First Age Data of the Deposits of the Kondoma Iron Field, Gornaya Shoriya: Results of U–Pb (ID-TIMS) Dating of Garnet

  • GEOLOGY OF ORE DEPOSITS
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Abstract

The results of U‒Pb (ID-TIMS) geochronological studies of garnet from iron-bearing skarns of the Shalym deposit (Kondoma ore field, Gornaya Shoriya) are presented. Our data are the first direct estimation of the age of the formation of the iron deposit of the Kondoma ore field (499 ± 1 Ma). The formation of this deposit is related to the Middle to Late Cambrian subalkaline magmatism, which hasn’t previously been recognized within the Gornaya Shoriya fold areas (the western part of the Altai–Sayan fold area).

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Funding

This geochronological study was supported by the Russian Science Foundation, project no. 22-17-00211, and the geological studies were supported by a state contract of the Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, project no. FMUW-2022-0003.

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Authors and Affiliations

  1. Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, 199034, St. Petersburg, Russia

    M. V. Stifeeva, E. B. Salnikova &  A. B. Kotov

  2. Moscow State University, 119991, Moscow, Russia

    Yu. D. Gritsenko

  3. Fersman Mineralogical Museum, Russian Academy of Sciences, 119071, Moscow, Russia

    Yu. D. Gritsenko

Authors
  1. M. V. Stifeeva
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  2. E. B. Salnikova
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  3. A. B. Kotov
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  4. Yu. D. Gritsenko
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Corresponding author

Correspondence to M. V. Stifeeva.

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Translated by I. Melekestseva

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Stifeeva, M.V., Salnikova, E.B., Kotov, A.B. et al. First Age Data of the Deposits of the Kondoma Iron Field, Gornaya Shoriya: Results of U–Pb (ID-TIMS) Dating of Garnet. Dokl. Earth Sc. (2024). https://doi.org/10.1134/S1028334X23602845

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  • DOI: https://doi.org/10.1134/S1028334X23602845

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