Мақаланы E-mail арқылы жіберу Neoproterozoic granitoids on Wrangel Island
- Авторлар: Luchitskaya M.V.1, Sergeev S.A.2,3, Sokolov S.D.1, Tuchkova M.I.1
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Мекемелер:
- Geological Institute
- Karpinskii Russian Geological Research Institute
- Institute of Earth Sciences
- Шығарылым: Том 469, № 1 (2016)
- Беттер: 652-655
- Бөлім: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188569
- DOI: https://doi.org/10.1134/S1028334X16070126
- ID: 188569
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Аннотация
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.
Авторлар туралы
M. Luchitskaya
Geological Institute
Хат алмасуға жауапты Автор.
Email: luchitskaya@ginas.ru
Ресей, Pyzhevskii per. 7, Moscow, 109017
S. Sergeev
Karpinskii Russian Geological Research Institute; Institute of Earth Sciences
Email: luchitskaya@ginas.ru
Ресей, Sredny pr. 74, St. Petersburg, 191126; Universitetskaya nab. 7–9, St. Petersburg, 199034
S. Sokolov
Geological Institute
Email: luchitskaya@ginas.ru
Ресей, Pyzhevskii per. 7, Moscow, 109017
M. Tuchkova
Geological Institute
Email: luchitskaya@ginas.ru
Ресей, Pyzhevskii per. 7, Moscow, 109017
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