Email this article Neoproterozoic granitoids on Wrangel Island
- Authors: Luchitskaya M.V.1, Sergeev S.A.2,3, Sokolov S.D.1, Tuchkova M.I.1
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Affiliations:
- Geological Institute
- Karpinskii Russian Geological Research Institute
- Institute of Earth Sciences
- Issue: Vol 469, No 1 (2016)
- Pages: 652-655
- Section: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188569
- DOI: https://doi.org/10.1134/S1028334X16070126
- ID: 188569
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Abstract
Based on geochronological U–Pb studies, the age of Wrangel Island granitoids was estimated as Neoproterozoic (Cryogenian). Some granitoids contain zircons with inherited cores with an estimated age of 1010, 1170, 1200, and >2600 Ma, assuming the presence of ancient (Neoarchean–Mesoproterozoic) rocks in the Wrangel Island foundation and their involvement in partial melting under granitoid magma formation.
About the authors
M. V. Luchitskaya
Geological Institute
Author for correspondence.
Email: luchitskaya@ginas.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 109017
S. A. Sergeev
Karpinskii Russian Geological Research Institute; Institute of Earth Sciences
Email: luchitskaya@ginas.ru
Russian Federation, Sredny pr. 74, St. Petersburg, 191126; Universitetskaya nab. 7–9, St. Petersburg, 199034
S. D. Sokolov
Geological Institute
Email: luchitskaya@ginas.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 109017
M. I. Tuchkova
Geological Institute
Email: luchitskaya@ginas.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 109017
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