Neoproterozoic granitoids on Wrangel Island


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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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