Тип публикации: статья из журнала
Год издания: 2014
Идентификатор DOI: 10.1134/S1028334X1407006X
Ключевые слова: Bifurcation (mathematics), Hysteresis, Attractor structure, Large earthquakes, Magnitude distribution, Nonlinear resonance, Riftogenesis, Spatial temporals, Time-periods, Earthquakes, bifurcation, earthquake magnitude, Baikal Region, Russian Federation
Аннотация: The hypothesis that large earthquakes in the Baikal region are a response to bifurcations in nonlinear resonance hysteresis in a system consisting of three oscillators, attractor structures of riftogenesis, is substantiated. The hypothesis is confirmed by the spatial-temporal and magnitude distribution of large earthquakes: all the pairs of earthquakes with magnitude M-LH > 5.5 that took place in the region within a small time period but were remote from one another show fair agreement with the main theoretical conclusions.
Издание
Журнал: DOKLADY EARTH SCIENCES
Выпуск журнала: Vol. 457, Is. 1
Номера страниц: 845-849
ISSN журнала: 1028334X
Место издания: NEW YORK
Издатель: MAIK NAUKA/INTERPERIODICA/SPRINGER
Персоны
- Klyuchevskii A.V. (Institute of Biophysics, Siberian Branch, Russian Academy of Sciences; Krasnoyarsk Research Center, Siberian Branch, Russian Academy of Sciences; Siberian Federal University; Institute of the Earth's Crust, Siberian Branch, Russian Academy of Sciences )
- Khlebopros R.G. (Institute of Biophysics, Siberian Branch, Russian Academy of Sciences; Krasnoyarsk Research Center, Siberian Branch, Russian Academy of Sciences; Siberian Federal University; Institute of the Earth's Crust, Siberian Branch, Russian Academy of Sciences, ul. Lermontova 128, Irkutsk 664033, Russian Federation)
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