Early island-arc granitoids of the Shchuchinskaya zone of the Polar Urals: U–Pb (SIMS) zircon isotope data
- Authors: Sobolev I.D.1, Shadrin A.N.2, Rastorguev V.A.2, Kozyreva D.A.3
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Affiliations:
- Department of Geology
- NAO Siberian Scientific-Analytical Center
- Institute of Physics of the Earth
- Issue: Vol 72, No 2 (2017)
- Pages: 115-125
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174402
- DOI: https://doi.org/10.3103/S0145875217020065
- ID: 174402
Cite item
Abstract
Granitoids of the Rechnoy and Yalya-Pe paleovolcanoes, which were ascribed to the Silurian Khoimpe complex during a geological mapping, and granitoids of the Nganotsky-1 and Nganotsky-2 plutons that were ascribed to the Early Devonian Yunyaga complex were studied in the Shchuchinskaya zone of the Polar Urals. It was established that according to the mineral and chemical compositions the rocks of the plutons studied correspond to island-arc granitoids of I-type. Zircons from granitoids of the Rechnoy and Yalya-Pe paleovolcanoes and the Nganotsky-1 pluton yielded concordant U–Pb (SIMS) isotope ages of 456 ± 6, 454 ± 4, and 463 ± 3 Ma, respectively, which indicates the existence of an island arc within the Shchuchinskaya zone starting from the Middle–Late Ordovician. Based on the obtained zircon ages of granitoids, the country volcanics were ascribed to the Syaday Formation; the upper stratigraphic boundary of their formation was specified as the Middle–Upper Ordovician.
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About the authors
I. D. Sobolev
Department of Geology
Author for correspondence.
Email: sobolev_id@mail.ru
Russian Federation, Moscow
A. N. Shadrin
NAO Siberian Scientific-Analytical Center
Email: sobolev_id@mail.ru
Russian Federation, Tyumen, 625016
V. A. Rastorguev
NAO Siberian Scientific-Analytical Center
Email: sobolev_id@mail.ru
Russian Federation, Tyumen, 625016
D. A. Kozyreva
Institute of Physics of the Earth
Email: sobolev_id@mail.ru
Russian Federation, Moscow, 123995