Neoproterozoic granitoids on Wrangel Island
- Autores: Luchitskaya M.V.1, Sergeev S.A.2,3, Sokolov S.D.1, Tuchkova M.I.1
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Afiliações:
- Geological Institute
- Karpinskii Russian Geological Research Institute
- Institute of Earth Sciences
- Edição: Volume 469, Nº 1 (2016)
- Páginas: 652-655
- Seção: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188569
- DOI: https://doi.org/10.1134/S1028334X16070126
- ID: 188569
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Resumo
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.
Sobre autores
M. Luchitskaya
Geological Institute
Autor responsável pela correspondência
Email: luchitskaya@ginas.ru
Rússia, Pyzhevskii per. 7, Moscow, 109017
S. Sergeev
Karpinskii Russian Geological Research Institute; Institute of Earth Sciences
Email: luchitskaya@ginas.ru
Rússia, Sredny pr. 74, St. Petersburg, 191126; Universitetskaya nab. 7–9, St. Petersburg, 199034
S. Sokolov
Geological Institute
Email: luchitskaya@ginas.ru
Rússia, Pyzhevskii per. 7, Moscow, 109017
M. Tuchkova
Geological Institute
Email: luchitskaya@ginas.ru
Rússia, Pyzhevskii per. 7, Moscow, 109017
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