Email this article Diagnostics of the stress state of the lithosphere in Mongolia based on seismic source data
- Authors: Klyuchevskii A.V.1, Demberel S.2, Dem’yanovich V.M.1, Bayaraa G.2
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Affiliations:
- Institute of the Earth’s Crust, Siberian Branch
- Institute of Astronomy and Geophysics
- Issue: Vol 473, No 2 (2017)
- Pages: 433-437
- Section: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/189665
- DOI: https://doi.org/10.1134/S1028334X17040018
- ID: 189665
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Abstract
The obtained results indicate that earthquakes of Mongolia form under the conditions of an alternating field of regional stresses, which is related to pulsed activations in the BRS and superimposed on the quasi-stationary field of global stresses of the Earth.
About the authors
A. V. Klyuchevskii
Institute of the Earth’s Crust, Siberian Branch
Author for correspondence.
Email: akluchev@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033
S. Demberel
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Mongolia, Ulaanbaatar
V. M. Dem’yanovich
Institute of the Earth’s Crust, Siberian Branch
Email: akluchev@crust.irk.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033
G. Bayaraa
Institute of Astronomy and Geophysics
Email: akluchev@crust.irk.ru
Mongolia, Ulaanbaatar
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