Post-seismic motions after the 2006–2007 Simushir earthquakes at different stages of the seismic cycle
- Авторлар: 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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Мекемелер:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- Шығарылым: Том 473, № 1 (2017)
- Беттер: 375-379
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189565
- DOI: https://doi.org/10.1134/S1028334X17030266
- ID: 189565
Дәйексөз келтіру
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.
Авторлар туралы
L. Lobkovsky
Shirshov Institute of Oceanology
Хат алмасуға жауапты Автор.
Email: llobkovsky@ocean.ru
Ресей, Moscow, 117218
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Ресей, Obninsk
V. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Ресей, Obninsk
I. Garagash
Schmidt Institute of Physics of the Earth
Email: llobkovsky@ocean.ru
Ресей, Moscow, 123242
B. Baranov
Shirshov Institute of Oceanology
Email: llobkovsky@ocean.ru
Ресей, Moscow, 117218
G. Steblov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Ресей, Obninsk
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