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

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 TS...

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Published inDoklady earth sciences Vol. 464; no. 2; pp. 997 - 1000
Main Authors Ershova, V. B., Prokopiev, A. V., Khudoley, A. K., Shneider, G. V., Andersen, T., Kullerud, K., Makar’ev, A. A., Maslov, A. V., Kolchanov, D. A.
Format Journal Article
LanguageEnglish
Published Moscow Pleiades Publishing 01.10.2015
Springer
Springer Nature B.V
Subjects
Archipelagoes
Basins
Basins (Geology)
Cambrian
Earth and Environmental Science
Earth Sciences
Fossils
Geology
Islands
Ordovician
Zirconium
Kara Sea
PNE, Russia, Arkhangel'skaya, Severnaya Zemlya
Angular Unconformity
Cambrian
Ordovician
DOKLADY Earth Science
Detrital Zircon
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Summary: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.
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ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X15100013