Email this article Origin of the Elikanskii granite–gneiss swell in the West Stanovoi terrane of the Central Asian Fold Belt: Results of structural studies
- Authors: 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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Affiliations:
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Precambrian Geology and Geochronology
- Far East Federal University
- Issue: Vol 467, No 1 (2016)
- Pages: 224-227
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188122
- DOI: https://doi.org/10.1134/S1028334X16030119
- ID: 188122
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Abstract
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.
About the authors
A. M. Mazukabzov
Institute of the Earth’s Crust, Siberian Branch
Author for correspondence.
Email: mazuk@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033
A. B. Kotov
Institute of Precambrian Geology and Geochronology
Email: mazuk@crust.irk.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034
T. M. Skovitina
Institute of the Earth’s Crust, Siberian Branch
Email: mazuk@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033
E. V. Sklyarov
Institute of the Earth’s Crust, Siberian Branch; Far East Federal University
Email: mazuk@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033; Vladivostok
A. M. Larin
Institute of Precambrian Geology and Geochronology
Email: mazuk@crust.irk.ru
Russian Federation, nab. Makarova 2, St. Petersburg, 199034
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