Age and sources of the metasedimrntary rocks of the Tokur terrane in the Mongol-Okhotsk fold belt: results of the U–Pb geoсhronological and Lu–Hf isotope studies

Cover Page

Cite item

Full Text

Abstract

This paper presents the results of U–Pb (LA–ICP–MS) and Lu–Hf ­isotope studies of detrital zircons from metasedimentary rocks of the Tokur Terrane. It has been shown that metasedimentary rocks of the Tokur and Ekimchan formations are characterized by similar age peaks of detrital zircons, which indicates a close (or same) age of these formations. The lower age of the sedimentation is determined by the age of the youngest zircons of 326–323 Ma. The upper age boundary is determined of 254–251 Ma, based on the intruded of the Late Permian granitoids. The main sources of zircons in the metasedimentary rocks of the Tokur Terrane are the igneous and metamorphic complexes of the southeast framing of the North Asia Craton. The Tokur Terrane can be considered as a fragment of the Paleozoic accretionary complex, the formation in front of the southeastern margin of the North Asia Craton.

About the authors

V. A. Zaika

Institute of Geology and Natural Management of Far Eastern Branch of Russian Academy of Sciences

Email: sorokin@ascnet.ru
Russian Federation, 1, Relochniy lane, Blagoveshchensk, 675000

A. A. Sorokin

Institute of Geology and Natural Management of Far Eastern Branch of Russian Academy of Sciences

Author for correspondence.
Email: sorokin@ascnet.ru
Russian Federation, 1, Relochniy lane, Blagoveshchensk, 675000

A. P. Sorokin

Institute of Geology and Natural Management of Far Eastern Branch of Russian Academy of Sciences

Email: sorokin@ascnet.ru

Corresponding Member of the Russian Academy of Sciences

 

Russian Federation, 1, Relochniy lane, Blagoveshchensk, 675000

References

  1. Забродин В.Ю., Гурьянов В.А., Кисляков С.Г. и др. Государственная геологическая карта Российской Федерации 1: 1000000. Сер. Дальневосточная. Лист N 53. Третье поколение. СПб.: ВСЕГЕИ, 2007.
  2. Парфенов Л.М., Попеко Л.И., Томуртогоо О. // Тихоокеан. геология. 1999. Т. 18. № 5. С. 24-43.
  3. Агафоненко С.Г., Сережников А.Н., Яшнов А.Л. Государственная геологическая карта Российской Федерации 1:200 000. 2-е изд. Сер. Тугурская. Лист N 53-XXV (Экимчан) / под ред. А.В. Махинина. СПб.: ВСЕГЕИ, 2002.
  4. Ludwig K.R. User’s Manual for a Geochronological Toolkit for Microsoft Excel // Berkeley Geochronol. Center Spec. Publ. 2008. P. 1-75.
  5. Söderlund U., Patchett P.J., Vervoort J.D., et al. // Earth and Planet. Sci. Lett. 2004. V. 219. P. 311-324.
  6. Blichert-Toft J., Albarede F. // Earth and Planet. Sci. Lett. 1997. V. 148. P. 243-258.
  7. Vervoort J.D., Patchett P.J. // Geochim. et Cosmochim. Acta. 1996. V. 60. P. 3717-3723.
  8. Griffin W.L., Belousova E.A., Shee S.R., et al. // Precambr. Res. 2004. V. 131. P. 231-282.
  9. Великославинский С.Д., Котов А.Б., Сальникова Е.Б. и др. // ДАН. 2011. Т. 438. № . 3. С. 355-359.
  10. Великославинский С.Д., Котов А.Б., Ковач В.П. и др. // Геотектоника. 2017. № 4. С. 3-16.
  11. Великославинский С.Д., Котов А.Б., Ковач В.П. и др. // ДАН. 2016. Т. 468. № 4. С. 425-428.
  12. Kelty T.K., Yin A., Dash B., et al. // Tectonophysics. 2008. V. 451. P. 290-311.
  13. Bussien D., Gombojav N., Winkler W., Quadt A. // Tectonophysics. 2011. V. 510. P. 132-150.
  14. Сорокин А.А., Колесников А.А., Котов А.Б., Ковач В.П. // ДАН. 2014. Т. 454. № 6. C. 706-709.
  15. Сорокин А.А., Колесников А.А., Котов А.Б. и др. // ДАН. 2015. Т. 462. № 5. С. 590-594.

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2019 Russian academy of sciences

This website uses cookies

You consent to our cookies if you continue to use our website.

About Cookies