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Doklady Earth Sciences

, Volume 483, Issue 1, pp 1394–1398 | Cite as

The Paleomagnetic Pole of the Siberian Paleocontinent at the Late Ediacaran Stage of Evolution of the Active Continental Margin (South Yenisei Ridge)

  • P. I. Kadilnikov
  • A. E. Vernikovskaya
  • N. E. Mikhaltsov
  • V. A. VernikovskyEmail author
  • N. Yu. Matushkin
GEOLOGY
  • 21 Downloads

Abstract

The results of the first paleomagnetic study of a late Neoproterozoic magmatic complex on the Siberian paleocontinent (Siberia) using U–Pb geochronological data are presented. The igneous rocks of the Zimoveyniy massif (block) of the South Yenisei Ridge formed in an active continental margin setting and recorded the initial thermoremanent magnetization. Our calculations let us determine with reasonable certitude that in the late Ediacaran Siberia was located in the subequatorial latitudes.

Notes

ACKNOWLEDGMENTS

This study was supported by the Russian Foundation for Basic Research (project no. 18-05-00854) and the Russian Science Foundation (project 14-37-00030).

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Copyright information

© Pleiades Publishing, Ltd. 2018

Authors and Affiliations

  • P. I. Kadilnikov
    • 1
    • 2
  • A. E. Vernikovskaya
    • 1
    • 2
  • N. E. Mikhaltsov
    • 1
    • 2
  • V. A. Vernikovsky
    • 1
    • 2
    Email author
  • N. Yu. Matushkin
    • 1
    • 2
  1. 1.Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Science NovosibirskRussia
  2. 2.Novosibirsk State UniversityNovosibirskRussia

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