Relationship between Radon and the Tectonic Activity of Faults in Central Mongolia


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The relationship between radon and the tectonic activity of faults for two geodynamically active regions of Central Mongolia is shown with account for the influence of individual characteristics of the radon field. As a whole, the radon activity of the faults increases with an increasing contribution of extension to the dynamic environment of their formation, with increasing seismic activity, and near concentrated faults of the late stages of evolution in comparison with the wide zones of fractures at the early stages of the formation of the internal structure. The studied patterns should provide an increase in the efficiency of application of radon surveys in investigation of the seismic hazard of faults in the Earth’s crust.

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K. Seminsky

Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: seminsky@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033

A. Bobrov

Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences

Email: seminsky@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033

S. Demberel

Institute of Astronomy and Geophysics, Mongolian Academy of Sciences

Email: seminsky@crust.irk.ru
蒙古, Ulaanbaatar

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