Neoproterozoic granitoids on Wrangel Island
- 作者: Luchitskaya M.V.1, Sergeev S.A.2,3, Sokolov S.D.1, Tuchkova M.I.1
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隶属关系:
- Geological Institute
- Karpinskii Russian Geological Research Institute
- Institute of Earth Sciences
- 期: 卷 469, 编号 1 (2016)
- 页面: 652-655
- 栏目: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188569
- DOI: https://doi.org/10.1134/S1028334X16070126
- ID: 188569
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详细
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.
作者简介
M. Luchitskaya
Geological Institute
编辑信件的主要联系方式.
Email: luchitskaya@ginas.ru
俄罗斯联邦, Pyzhevskii per. 7, Moscow, 109017
S. Sergeev
Karpinskii Russian Geological Research Institute; Institute of Earth Sciences
Email: luchitskaya@ginas.ru
俄罗斯联邦, Sredny pr. 74, St. Petersburg, 191126; Universitetskaya nab. 7–9, St. Petersburg, 199034
S. Sokolov
Geological Institute
Email: luchitskaya@ginas.ru
俄罗斯联邦, Pyzhevskii per. 7, Moscow, 109017
M. Tuchkova
Geological Institute
Email: luchitskaya@ginas.ru
俄罗斯联邦, Pyzhevskii per. 7, Moscow, 109017
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