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

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Abstract

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.

Original languageEnglish
Pages (from-to)1394-1398
Number of pages5
JournalDoklady Earth Sciences
Volume483
Issue number1
DOIs
Publication statusPublished - 1 Dec 2018

Keywords

  • MAGMATISM
  • CRATON

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