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Rapakivi Granites of the Kodar Complex (Aldan Shield): Age, Sources, and Tectonic Setting

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The paper reports geochemical, geochronological (ID–TIMS zircon U–Pb) and isotope–geochemical (Nd, Pb) study of granitoids of the Kodar complex developed in the western part of the Aldan shield. It has been established that these rocks can be classified as postcollisional A–type rapakivi granites, which together with the mafic–ultramafic rocks of the Chinei complex compose a single magmatic association formed within 1876 ± 4–1859 ± 2 Ma. The massifs of this association are a part of the giant South Siberian magmatic belt over 2500 km in length, which was formed at the final stage (1.88–1.84 Ga) of evolution of the Paleoproterozoic orogen. Globally, this belt is the largest stitching suture, which marks the formation of the Siberian craton and its entrance into the Paleoproterozoic Nuna supercontinent. The formation of the initial magmas of the Kodar granitoids was related to the mantle–crustal interaction during the mixing of primary mafic mantle magmas or their derivatives with anatectic melts derived through partial melting of the Archean lower continental crust of the region under the thermal influence of mafic magma. The crustal component in the source clearly predominates and has a heterogeneous nature. The mantle component is mainly represented by ancient enriched mantle, with the possible contribution of the OIB–type component.

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ACKNOWLEDGMENTS

We are grateful to V.V. Yarmolyuk and A.A. Tsygankov for valuable advices and constructive comments that significantly improved the manuscript. L.B. Makar’ev and A.N. Timashkov (VSEGEI) are thanked for kindly given geological materials and fruitful discussion of problems of granitoid magmatism of the Aldan shield.

Funding

The studies were supported by the Russian Foundation for Basic Research (project nos. 17-05-00659, 18-05-00403, 19-05-00647, 20-05-00401), Russian Science Foundation (project nos. 19-17-00205), the State Tasks IPGG RAS (project nos. 0153-2019-0002, 0153-2019-0001 and 0153-2019-0001) and the Government of the Russian Federation (project no. 075-15-2019-1883).

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Authors and Affiliations

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

    A. M. Larin, A. B. Kotov, V. P. Kovach, E. B. Sal’nikova, V. M. Savatenkov, S. D. Velikoslavinskii, N. G. Rizvanova & N. A. Sergeeva

  2. Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Science, 664033, Irkutsk, Russia

    D. P. Gladkochub & T. M. Skovitina

  3. Moscow State University, 119234, Moscow, Russia

    V. Yu. Vodovozov

  4. Geological Institute (GIN), Russian Academy of Sciences, 109017, Moscow, Russia

    V. Yu. Vodovozov

Authors
  1. A. M. Larin
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  2. A. B. Kotov
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  3. V. P. Kovach
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  4. E. B. Sal’nikova
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  5. D. P. Gladkochub
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  6. V. M. Savatenkov
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  7. S. D. Velikoslavinskii
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  8. T. M. Skovitina
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  9. N. G. Rizvanova
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  10. N. A. Sergeeva
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  11. V. Yu. Vodovozov
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Corresponding author

Correspondence to A. M. Larin.

Additional information

Translated by M. Bogina

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Larin, A.M., Kotov, A.B., Kovach, V.P. et al. Rapakivi Granites of the Kodar Complex (Aldan Shield): Age, Sources, and Tectonic Setting. Petrology 29, 277–299 (2021). https://doi.org/10.1134/S0869591121030036

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  • DOI: https://doi.org/10.1134/S0869591121030036

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