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  1. Article

    Open Access

    New Evidence of the Independent Precambrian Tectonic History of the Faddey Terrane of the Central Taimyr Accretionary Belt

    New geostructural, petro-geochemical, U–Pb geochronological and paleomagnetic data for sills of metagabbro-dolerites of the Severobyrranga and Yasnenskiy complex specify the paleotectonic position of the Fadde...

    N. Yu. Matushkin, Corresponding member of the RAS D. V. Metelkin in Doklady Earth Sciences (2023)

  2. No Access

    Article

    Geodynamics of a Breakup of Western Part of the Karelian Craton: Data on 2.1 Ga Mafic Magmatism

    Mafic intraplate magmatism is the main source of information about the geodynamics of processes that lead to the breakup of continental blocks. The article discusses geodynamics of the breakup of the Archean s...

    A. V. Samsonov, A. V. Stepanova, E. B. Salnikova, Yu. O. Larionova in Petrology (2023)

  3. Article

    Open Access

    Erratum to: New Evidence of the Independent Precambrian Tectonic History of the Faddey Terrane of the Central Taimyr Accretionary Belt

    An Erratum to this paper has been published: https://doi.org/10.1134/S1028334X23070267

    N. Yu. Matushkin, Corresponding member of the RAS D. V. Metelkin in Doklady Earth Sciences (2024)

  4. No Access

    Article

    Age Limits for the Zaonega Formation of the Ludicovian Superhorizon and the Shunga Event in the Onega Basin: New U–Pb Zircon Data for the Konchezero Sill

    New U–Pb data for zircon from the Konchezero sill reliably determine the age of the Suisari Formation of the Ludicovian and the limit of the maximum age of the volcanogenic–sedimentary Zaonega Formation with i...

    A. V. Stepanova, Corresponding Member of the RAS A. V. Samsonov in Doklady Earth Sciences (2024)

  5. Article

    Open Access

    Paleoproterozoic Dacite Dikes of the Vorontsovka Terrane, Volga–Don Orogen: Geochemistry, Age, and Petrogenesis

    Metamorphosed dacitic porphyry dikes were first found in the western part of the Vorontsovka terrane, which is located in the Paleoproterozoic Volga–Don orogen at the margin of Archean Sarmatia and Volga–Ural ...

    K. A. Savko, A. V. Samsonov, E. Kh. Korish, N. S. Bazikov, A. N. Larionov in Petrology (2024)

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