Deep velocity structure of the southern edge of the Siberian Craton and Baikal Rifting
- Authors: Mordvinova V.V.1, Кobelev М.М.1,2, Chritova М.А.1,2, Тurutanov Е.C.1, Коbeleva Е.А.1,2, Тrynkova D.S.1, Tsydypova L.R.3
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Affiliations:
- Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences
- Baikal Branch of the Federal Research Center "United Geophysical Service" of the Russian Academy of Sciences
- Geological Institute, Siberian Branch of the Russian Academy of Sciences
- Issue: Vol 484, No 1 (2019)
- Pages: 93-97
- Section: Geophysics
- URL: https://journals.eco-vector.com/0869-5652/article/view/12150
- DOI: https://doi.org/10.31857/S0869-5652484193-97
- ID: 12150
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Abstract
The velocity structure of the southern edge of the ancient Siberian craton has been modeled to an 80-km depth based on teleseismic records of a P-receiver function method (P–S). The correlation between the deep and the surface structure determined through modeling is indicative of the submeridional convergence of the south-western edge of the Siberian craton with the Central Asian mobile belt. A sublatitudinal crust extension in the contact zone caused by such convergence may initiate Baikal rifting at the craton’s southeastern edge.
About the authors
V. V. Mordvinova
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences
Author for correspondence.
Email: mordv@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033
М. М. Кobelev
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences; Baikal Branch of the Federal Research Center "United Geophysical Service" of the Russian Academy of Sciences
Email: mordv@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033; Irkutsk
М. А. Chritova
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences; Baikal Branch of the Federal Research Center "United Geophysical Service" of the Russian Academy of Sciences
Email: mordv@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033; Irkutsk
Е. Ch. Тurutanov
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences
Email: mordv@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033
Е. А. Коbeleva
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences; Baikal Branch of the Federal Research Center "United Geophysical Service" of the Russian Academy of Sciences
Email: mordv@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033; Irkutsk
D. S. Тrynkova
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences
Email: mordv@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033
L. R. Tsydypova
Geological Institute, Siberian Branch of the Russian Academy of Sciences
Email: mordv@crust.irk.ru
Russian Federation, 6A, Sakhyanova street, Ulan-Ude, 670047
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