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Doklady Earth Sciences

, Volume 464, Issue 2, pp 997–1000 | Cite as

Results of U–Pb (LA–ICPMS) dating of detrital zircons from metaterrigenous rocks of the basement of the North Kara basin

  • V. B. Ershova
  • A. V. Prokopiev
  • A. K. Khudoley
  • G. V. Shneider
  • T. Andersen
  • K. Kullerud
  • A. A. Makar’ev
  • A. V. Maslov
  • D. A. Kolchanov
Geology

Abstract

The U–Pb (LA–ICPMS) age was established for detrital zircons from the oldest, intensely deformed metasedimentary complexes without reliable fossils’ record, which represent the folded basement of the North Kara basin and are exposed on Bol’shevik and Troinoi islands (Severnaya Zemlya and Izvestii TSIK archipelagoes, respectively). Our data suggest the common evolution of the Cambrian–Ordovician sequences exposed on the islands of both archipelagoes.

Keywords

Cambrian Ordovician DOKLADY Earth Science Detrital Zircon Angular Unconformity 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Pleiades Publishing, Ltd. 2015

Authors and Affiliations

  • V. B. Ershova
    • 1
  • A. V. Prokopiev
    • 2
  • A. K. Khudoley
    • 1
  • G. V. Shneider
    • 3
  • T. Andersen
    • 4
  • K. Kullerud
    • 5
  • A. A. Makar’ev
    • 6
  • A. V. Maslov
    • 7
  • D. A. Kolchanov
    • 1
  1. 1.St. Petersburg State UniversitySt. PetersburgRussia
  2. 2.Diamond and Precious Metal Geology Institute, Siberian BranchRussian Academy of SciencesYakutskRussia
  3. 3.Karpinskii All-Russia Geological Research InstituteSt. PetersburgRussia
  4. 4.University of OsloBlindern, OsloNorway
  5. 5.University of TromsøTromsøNorway
  6. 6.Polar Marine Geosurvey ExpeditionSt. PetersburgRussia
  7. 7.Zavaritsky Institute of Geology and Geochemistry, Ural BranchRussian Academy of SciencesYekaterinburgRussia

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