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The Vp/Vs Kinematic Parameter in the Southern Segment of the Kamchatka Seismic Subduction Zone during the Precursory Period of the March 25, 2020, MW = 7.5 Earthquake and Its Aftershock Processстатья
- Авторы: Kuchai M.S., Slavina L.B.
- Журнал: Journal of Volcanology and Seismology
- Том: 16
- Номер: 5
- Год издания: 2022
- Издательство: Springer Verlag
- Местоположение издательства: Germany
- Первая страница: 365
- Последняя страница: 376
- Оригинальные версии: КИНЕМАТИЧЕСКИЙ ПАРАМЕТР Vp/Vs ЮЖНОГО СЕГМЕНТА КАМЧАТСКОЙ СЕЙСМОФОКАЛЬНОЙ ЗОНЫ ПРИ ПОДГОТОВКЕ ЗЕМЛЕТРЯСЕНИЯ 25 МАРТА 2020 г., MW = 7.5 И РАЗВИТИИ ЕГО АФТЕРШОКОВОГО ПРОЦЕССА
- DOI: 10.1134/S0742046322050062
- Аннотация: The Vp/Vs kinematic parameter for the Kamchatka seismic subduction zone has been long monitored on a regular basis. This has allowed estimating the behavior of the parameter and revealing its features during the precursory period and actual rupturing of the March 25, 2020 earthquake which occurred in thePacific plate at the contact between the Pacific plate and the continental slope of Kamchatka. The March 25, 2020 earthquake with its high magnitude (ML = 7.6, MW = 7.5) is a rare enough event to occur in the Pacific plate. Knowledge of earth structure in the source region of the earthquake was updated based on the results of deep seismic sounding and continuous seismic profiling which was carried out in the area in the past. It was shown that the earthquake source area is at an inflection in the descending Pacific plate. The source area lies in the layer at the boundary between the asthenosphere and the crust and mantle. The layer is at depths of 30‒60 km and has lower Vp and Vs velocities. The inflection region along Kamchatka shows lower Vp/Vs values, which is a sign of extension along the plate. The source area is in the contact between the Pacific plate, which is subducting under the southern end of Kamchatka, and the North Kuril Islands, as well as the Seaof-Okhotsk plate. The region shows a distinct change in the anomalous values of the parameter from lower to higher, with the latter being typical for compression. Our study has allowed estimating possible regions of tension and compression in the geological medium.
- Добавил в систему: Кучай Марк Соломонович