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The 2405 Ma doleritic dykes in the Karelian Craton: A fragment of a Paleoproterozoic large igneous province

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Abstract

New data on the age and composition of doleritic dykes of the Karelian Craton on the Fennoscandian Shield are reported. Based on the results of U–Pb dating of baddeleyite, a new age episode (2404 ± 5 Ma) in the formation of basic rocks on the Karelian Craton is established. Comparison of the composition of the studied dolerite with that of dykes of the same age from other Archean cratons worldwide shows their essential similarity and allows us to suggest their formation within a single large igneous province. The data obtained support the current models of supercontinental reconstructions for the period of 2400 Ma.

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References

  1. P. G. Eriksson and K. C. Condie, Gondwana Res. 25 (1), 30–47 (2014).

    Article  Google Scholar 

  2. K. Kullerud, K. P. Skjerlie, F. Corfu, and J. D. de la Rosa, Precambrian Res. 150 (3–4), 183–200 (2006).

    Article  Google Scholar 

  3. J. Vuollo and H. Huhma, in Precambrian Geology of Finland Key to the Evolution of the Fennoscandian Shield (Elsevier, Amsterdam, 2005), Vol. 14, pp. 195–236.

    Book  Google Scholar 

  4. J. H. F. L. Davies and L. M. Heaman, Precambrian Res. 249, 198–198 (2014).

    Article  Google Scholar 

  5. H. S. R. Hughes, I. McDonald, K. M. Goodenough, T. J. R. Ciborowski, A. C. Kerr, J. H. F. L. Davies, and D. Selby, Precambrian Res. 250, 126–126 (2014).

    Article  Google Scholar 

  6. T. J. R. Ciborowski, A. C. Kerr, I. Mcdonald, R. E. Ernst, H. S. R. Hughes, and M. J. Minifie, Precambrian Res. 250, 166–166 (2014).

    Article  Google Scholar 

  7. S. A. Pisarevsky, B. De Waele, S. Jones, U. Söderlund, and R. E. Ernst, Precambrian Res. 259, 231–231 (2015).

    Google Scholar 

  8. T. Bayanova, J. Ludden, and F. P. Mitrofanov, Geol. Soc. London, Spec. Publ. 323 (1), 165–198 (2009).

    Article  Google Scholar 

  9. A. V. Stepanova, E. B. Salnikova, A. V. Samsonov, S. V. Egorova, Y. O. Larionova, and V. S. Stepanov, Precambrian Res. 259, 57–57 (2015).

    Article  Google Scholar 

  10. U. Söderlund and L. Johansson, Geochem., Geophys., Geosyst. 3 (2), 1–7 (2002).

    Article  Google Scholar 

  11. T. E. Krogh, Geochim. Cosmochim. Acta 37 (3), 485–494 (1973).

    Article  Google Scholar 

  12. K. R. Ludwig, PbDat for MS-DOS. Ver. 1.21, U.S. Geological Survey Open-File Rep. No. 88-542 (1991).

  13. K. R. Ludwig, ISOPLOT/Ex. Ver. 2.06: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronological Center Special Publication No. 1a (Geochronol. Center, Berkeley, CA, 1999).

    Google Scholar 

  14. R. H. Steiger and E. Jäger, Earth Planet. Sci. Lett. 36 (3), 359–362 (1977).

    Article  Google Scholar 

  15. J. S. Stacey and J. D. Kramers, Earth Planet. Sci. Lett. 26 (2), 207–221 (1975).

    Article  Google Scholar 

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Correspondence to A. V. Stepanova.

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Original Russian Text © A.V. Stepanova, E.B. Salnikova, A.V. Samsonov, Yu.O. Larionova, S.V. Egorova, V.M. Savatenkov, 2017, published in Doklady Akademii Nauk, 2017, Vol. 472, No. 2, pp. 185–191.

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Stepanova, A.V., Salnikova, E.B., Samsonov, A.V. et al. The 2405 Ma doleritic dykes in the Karelian Craton: A fragment of a Paleoproterozoic large igneous province. Dokl. Earth Sc. 472, 72–77 (2017). https://doi.org/10.1134/S1028334X17010196

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  • DOI: https://doi.org/10.1134/S1028334X17010196

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