Skip to main content
Log in

The First Discovery of Pseudotachylytes in the Paleoproterozoic Ladoga Zonal Metamorphosed Complex of Fennoscandia and Their 40Ar/39Ar Dating

  • GEOLOGY
  • Published:
Doklady Earth Sciences Aims and scope Submit manuscript

Abstract

The results of 40Ar/39Ar dating of pseudotachylytes, first identified in the Paleoproterozoic zonally metamorphosed (greenschist to granulite facies) Ladoga complex of svecofennides, are presented. A wide age range of the formation of pseudotachylytes in the Riphean (1.59–1.31 Ga), presumably caused by the exhumation of deep rocks during the Svecofennian tectonogenesis and the subsequent orogenesis and riftogenesis in southeastern Fennoscandia, has been established.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1.
Fig. 2.
Fig. 3.

Similar content being viewed by others

REFERENCES

  1. Yu. A. Morozov, et al., Dokl. Earth Sci. 484 (5), 129–134 (2019).

    Article  Google Scholar 

  2. J. D. Kirkpatrick and C. D. Rowe, J. Stuct. Geol. 52, 183–198 (2013).

    Google Scholar 

  3. Ladoga Paleoproterozoic Structure (Geological Institute of Karelian Scientific Center RAS, Petrozavodsk, 2020) [in Russian].

  4. D. A. Velikoslavinskii, Comparative Characteristic of Regional Moderate and Low Pressure Metamorphism (Nauka, Leningrad, 1972) [in Russian].

    Google Scholar 

  5. Yu. A. Morozov, et al., Petrologiya (2020) [in Press].

  6. V. A. Drits and A. G. Kossovskaya, Clay Minerals (Nauka, Moscow, 1991) [in Russian].

    Google Scholar 

  7. S. H. Haines and B. A. van der Pluijm, J. Struct. Geol. 43, 2–32 (2012).

    Article  Google Scholar 

  8. Yu. A. Morozov, et al., Izv., Phys. Solid Earth 54 (1), 1–22 (2018).

    Article  Google Scholar 

  9. A. V. Travin, D. S. Yudin, et al., Geochem. Int. 47 (11), 1107–1125 (2009).

    Article  Google Scholar 

  10. T. Torvela, I. Manttari, and T. Hermansson, Precambrian Res. 160, 277–298 (2008).

    Article  Google Scholar 

  11. Yu. V. Amelin, et al., Contrib. Mineral. Petrol. 127, 353–368 (1997).

    Article  Google Scholar 

  12. M. Vaasjoki, et al., Precambrian Res. 51, 227–243 (1991).

    Article  Google Scholar 

  13. A. M. Larin, Stratigr. Geol. Correl. 17 (3), 235–259 (2009).

    Article  Google Scholar 

  14. A. V. Amantov, Reg. Geol. Metallog., No. 58, 22–32 (2014).

Download references

ACKNOWLEDGMENTS

We are grateful to Professor R.V. Veselovskii (Moscow State University; Schmidt Institute of Physics of the Earth, Russian Academy of Sciences) for assistance in the performance of this work and discussion of results.

Funding

This work was performed within the state assignments of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, and the Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, and was supported in part by the Russian Foundation for Basic Research, project no. 19–05–00256 (synmetamorphic structure formation in the sedimentary cover–basement system).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Yu. A. Morozov.

Additional information

Translated by D. Voroshchuk

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Morozov, Y.A., Yudin, D.S., Travin, A.V. et al. The First Discovery of Pseudotachylytes in the Paleoproterozoic Ladoga Zonal Metamorphosed Complex of Fennoscandia and Their 40Ar/39Ar Dating. Dokl. Earth Sc. 493, 485–489 (2020). https://doi.org/10.1134/S1028334X20070119

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S1028334X20070119

Keywords:

Navigation