Enviar artigo por via de e-mail Origin of the Elikanskii granite–gneiss swell in the West Stanovoi terrane of the Central Asian Fold Belt: Results of structural studies
- Autores: Mazukabzov A.M.1, Kotov A.B.2, Skovitina T.M.1, Sklyarov E.V.1,3, Larin A.M.2
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Afiliações:
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Precambrian Geology and Geochronology
- Far East Federal University
- Edição: Volume 467, Nº 1 (2016)
- Páginas: 224-227
- Seção: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188122
- DOI: https://doi.org/10.1134/S1028334X16030119
- ID: 188122
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Resumo
Structural studies showed that the Elikanskii granite–gneiss swell is similar to the Late Mesozoic Cordilleran-type metamorphic core complexes distinguished in the southern part of the Eravninskii terrane and in the northeastern part of the Argun–Idermeg superterrane of this belt.
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Sobre autores
A. Mazukabzov
Institute of the Earth’s Crust, Siberian Branch
Autor responsável pela correspondência
Email: mazuk@crust.irk.ru
Rússia, ul. Lermontova 128, Irkutsk, 664033
A. Kotov
Institute of Precambrian Geology and Geochronology
Email: mazuk@crust.irk.ru
Rússia, nab. Makarova 2, St. Petersburg, 199034
T. Skovitina
Institute of the Earth’s Crust, Siberian Branch
Email: mazuk@crust.irk.ru
Rússia, ul. Lermontova 128, Irkutsk, 664033
E. Sklyarov
Institute of the Earth’s Crust, Siberian Branch; Far East Federal University
Email: mazuk@crust.irk.ru
Rússia, ul. Lermontova 128, Irkutsk, 664033; Vladivostok
A. Larin
Institute of Precambrian Geology and Geochronology
Email: mazuk@crust.irk.ru
Rússia, nab. Makarova 2, St. Petersburg, 199034
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