Отправить статью по E-mail Infrasonic Signals from Earthquakes of December 5, 2014, in the Water Area of Lake Hovsgol, Northern Mongolia
- Авторы: Sorokin A.G.1, Klyuchevskii A.V.2
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Учреждения:
- Institute of Solar-Terrestrial Physics, Siberian Branch, Russian Academy of Sciences
- Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences
- Выпуск: Том 484, № 2 (2019)
- Страницы: 198-202
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/194628
- DOI: https://doi.org/10.1134/S1028334X1902017X
- ID: 194628
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Аннотация
A comprehensive analysis of waveforms of seismic and infrasonic vibrations from the earthquake that occurred on December 5, 2014, in the water area of Lake Hovsgol was performed. The analysis showed that the infrasonic signal recorded at the Tory station (Geophysical Observatory of the Institute of Solar-Terrestrial Physics, Russian Academy of Sciences) was formed by the sources of three generation types: local, secondary, and epicentral. The obtained results gave support to the model of epicentral infrasonic signal generation by flexural waves from an elastic ice membrane on the surface of Lake Hovsgol.
Об авторах
A. Sorokin
Institute of Solar-Terrestrial Physics, Siberian Branch, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: sor@iszf.irk.ru
Россия, Irkutsk, 664033
A. Klyuchevskii
Institute of the Earth’s Crust, Siberian Branch,Russian Academy of Sciences
Email: sor@iszf.irk.ru
Россия, Irkutsk, 664033
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