Skip to main content
Log in

Geological structure and isotopic—geochronologic study of rocks from the Strel’na segment of the Terskii Greenstone belt, Kola Peninsula

  • Published:
Stratigraphy and Geological Correlation Aims and scope Submit manuscript

Abstract

The geological structure, age, and genesis of sedimentary—volcanogenic, metamorphic, and metasomatic rocks from the Terskii greenstone belt fringing the southern Imandra—Varzuga structure in the southeastern Kola Peninsula are discussed with defining main stages in endogenic activity of the region in the Late Archean and Early Proterozoic. The U-Pb method (SHRIMP-II, ID-TIMS, and Pb-LS techniques) was used to determine the age of volcano-sedimentary rocks of the Imandra Group as well as that of magmatic and superimposed metamorphic and metasomatic processes. The basic—intermediate metavolcanics of the Imandra Group are dated at 2.67 Ga, which corresponds to the Lopingian Gimol’skii Superhorizon (Late Archean). The Archean metavolcanics were subjected to Early Proterozoic regional metamorphism 2.1 Ga ago and metasomatic processes in the period of 1.85 to 1.77 Ga ago. The obtained data indicate multistage evolution of rock formation in the Terskii greenstone belt located in the southern flank of the Imandra—Varzuga structure in the Kola Peninsula.

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.

Similar content being viewed by others

References

  1. B. Yu. Astaf’ev, O. A. Voinova, A S. Voinov, and D. I. Matukov, “Geological Structure, Petrological Properties, and Age of the Upper Archean Imandra Group (Kola Peninsula). Archean Geology and Geodynamics,” in Materials of the 1st Russian Conference on Problems of Precambrian Geology and Geodynamics (Center of the Information Culture, St. Petersburg, 2005) [in Russian].

    Google Scholar 

  2. T. B. Bayanova, Age of Reference Geological Complexes in the Kola Region and Duration of Magmatism (Nauka, St. Petersburg, 2004) [in Russian].

    Google Scholar 

  3. R. G. Berman and L. Y. Aranovich., “Optimized Standard State and Solution Properties of Minerals,” Contrib. Mineral. Petrol. 126(1–2), 1–24 (1996).

    Article  Google Scholar 

  4. L. P Black, S. L. Kamo, C. M. Allen, et al., “TEMORA 1: A New Zircon Standard for U—Pb Geochronology,” Chem. Geol. 200, 155–170 (2003).

    Article  Google Scholar 

  5. J. S. Daly, V V Balaganskii, M. Ya, Timmerman, et al., “First Isotopic Data on Early Proterozoic Supracrustal Rocks of the Terskii Area, Kola Peninsula,” in Abstracts of the 3 rd All-Russian Meeting “General Problems of Precambrian Subdivision” (KNTs RAN, Apatity, 2000), pp. 86–89 [in Russian].

  6. J. S. Daly, V V Balaganskii, M. Ya, Timmerman, et al., “Ion Microprobe U—Pb Zircon Geochronology and Isotopic Evidence Supporting a Tanscrustal Suture in the Lapland—Kola Orogen, Northern Fennoscandian Shield,” Precambr. Res. 105(2–4), 289–314 (2001).

    Article  Google Scholar 

  7. V I. Fonarev, A. A. Grafchikov, and A. N. Konilov, “The system of Concordant Mineralogical Thermometers for Metamorphic Complexes,” in Physicochemical Analysis of Mineral Formation (Nauka, Moscow, 1989), pp. 96—126 [in Russian].

    Google Scholar 

  8. R. Frei and B. S. Kamber, “Single Mineral Pb-Pb Dating,” Earth Planet. Sci. Lett. 129, 261–268 (1995).

    Article  Google Scholar 

  9. Geology of Ore Areas of the Murmansk Region. Appendix 3. Catalog of Geochronologic Data on the Northeastern Baltic Shield, Ed. By F.P. Mitrofanov (KNTs RAN, Apatity, 2002), pp. 16–52 [in Russian].

    Google Scholar 

  10. T. E. Krogh, “A Low-contamination Method for Hydrothermal Decomposition of Zircon and Extraction of U and Pb for Isotopic Age Determinations,” Geochim. Cosmochim Acta 37, 485–494 (1973).

    Article  Google Scholar 

  11. V. K. Kuz’min, M. N. Naumov, N. G. Berezhnaya, and E. N. Lepikhina, “Geological Structure, Composition, and Age of the Ondomozero Massif, Northeastern Baltic Shield,” Dokl. Akad. Nauk 401(6) 1–5 (2005) [Doklady Earth Sciences 401, 386–390 (2005).

    Google Scholar 

  12. K. R. Ludwig, “PbDat for MS-DOS. Version 1.21,” Geol. Survey Open-File Rept. 8-542 1–35 (1991).

    Google Scholar 

  13. K. R. Ludwig, “User’s Manual for Isoplo/Ex, Version 2.10. A Geochronological Toolkit for Microsoft Excel,” Berkeley Geochronology Center Spec. Publ., No. la, 1–120 (1999a).

    Google Scholar 

  14. K. R. Ludwig, “ISOPLOT/Ex. Version 2.06. A Geochronological Toolkit for Microsoft Excel,” Berkeley Geochronology Center Spec. Publ., No. la, 1–49 (1999b).

    Google Scholar 

  15. K. R. Ludwig, “SQUID 1.00, A User’s Manual,” Berkeley Geochronology Center Spec. Publ., No. 2, 1–120 (2000).

    Google Scholar 

  16. Precambrian Geology of the USSR, Ed. by D.V Rundquist and F.P. Mitrofanov (Nauka, Leningrad, 1988) [in Russian].

    Google Scholar 

  17. The Early Precambrian of the Baltic Shield, Ed. by V. A. Glebovitskii Nauka, St. Petersburg, 2005) [in Russian].

    Google Scholar 

  18. The State Geological Map of the Russian Federation. Scale 1: 1000000 (New Series). Sheet Q-(35)-37 (“Kirovsk”+. Explanatory Notes and Set of Maps, Ed. by Yu.B. Bogdanov (VSEGEI, St. Petersburg, 2004) [in Russian].

    Google Scholar 

  19. I. S. Williams, U—Th—Pb Geochronology by Ionic Microprobe,” Rev. Econ Geol., No. 7, 1–35 (1998).

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to B. Yu. Astaf’ev.

Additional information

Original Russian Text © B.Yu. Astaf’ev, O.A. Levchenkov, N.G. Rizvanova, O.A. Voinova, A.S. Voinov, L.K. Levskii, A.F. Makeev, K.I. Lokhov, 2010, published in Stratigrafiya. Geologicheskaya Korrelyatsiya, 2010, Vol. 18, No. 1, pp. 3–17.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Astaf’ev, B.Y., Levchenkov, O.A., Rizvanova, N.G. et al. Geological structure and isotopic—geochronologic study of rocks from the Strel’na segment of the Terskii Greenstone belt, Kola Peninsula. Stratigr. Geol. Correl. 18, 1–15 (2010). https://doi.org/10.1134/S0869593810010016

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S0869593810010016

Key words

Navigation