Post-seismic motions after the 2006–2007 Simushir earthquakes at different stages of the seismic cycle
- Авторы: Lobkovsky L.I.1, Vladimirova I.S.2, Gabsatarov V.V.2, Garagash I.A.3, Baranov B.V.1, Steblov G.M.2
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Учреждения:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- Выпуск: Том 473, № 1 (2017)
- Страницы: 375-379
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189565
- DOI: https://doi.org/10.1134/S1028334X17030266
- ID: 189565
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Аннотация
We analyzed long-term satellite geodesic observations after the Simushir earthquakes of 2006–2007. Application of a key model of the structure of the island arc regions combined with a model of nonstationary convective system in the upper mantle allowed us to find a consistent explanation of the motion of the Earth’s surface and distinguish the segments of the island arc at different stages of the seismic cycle.
Об авторах
L. Lobkovsky
Shirshov Institute of Oceanology
Автор, ответственный за переписку.
Email: llobkovsky@ocean.ru
Россия, Moscow, 117218
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Россия, Obninsk
V. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Россия, Obninsk
I. Garagash
Schmidt Institute of Physics of the Earth
Email: llobkovsky@ocean.ru
Россия, Moscow, 123242
B. Baranov
Shirshov Institute of Oceanology
Email: llobkovsky@ocean.ru
Россия, Moscow, 117218
G. Steblov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Россия, Obninsk
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