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Radon and tectonic activity of the faults at the Central Mongolia
- Authors: Seminsky K.Z.1, Bobrov A.A.1, Demberel S.2
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Affiliations:
- Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences
- Institute of Astronomy and Geophysics of Mongolian Academy of Sciences
- Issue: Vol 487, No 5 (2019)
- Pages: 538-542
- Section: Geology
- URL: https://journals.eco-vector.com/0869-5652/article/view/15901
- DOI: https://doi.org/10.31857/S0869-56524875538-542
- ID: 15901
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Abstract
The relationship between the radon and tectonic activity of the faults for two geodynamically active regions of Central Mongolia is shown. Radon fault activity grew with increased seismic activity and with an increase in the contribution of extension in the dynamic framework of their formation. It is higher in concentrated faults of late stages of development compared with wide zones of fractures in the early stages of the formation. The established patterns will help increase the effectiveness of the use of radon surveys in studies of the seismic hazard of faults of the Earth’s crust.
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About the authors
K. Z. Seminsky
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences
Author for correspondence.
Email: seminsky@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033
A. A. Bobrov
Institute of the Earth`s Crust of the Siberian Branch of the Russian Academy of Sciences
Email: seminsky@crust.irk.ru
Russian Federation, 128, Lermontova street, Irkutsk, 664033
S. Demberel
Institute of Astronomy and Geophysics of Mongolian Academy of Sciences
Email: seminsky@crust.irk.ru
Mongolia, 1, Amariin gudamj, Ulaanbaatar, 2010620
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