Post-seismic motions after the 2006–2007 Simushir earthquakes at different stages of the seismic cycle
- Autores: 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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Afiliações:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- Edição: Volume 473, Nº 1 (2017)
- Páginas: 375-379
- Seção: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189565
- DOI: https://doi.org/10.1134/S1028334X17030266
- ID: 189565
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Resumo
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.
Sobre autores
L. Lobkovsky
Shirshov Institute of Oceanology
Autor responsável pela correspondência
Email: llobkovsky@ocean.ru
Rússia, Moscow, 117218
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Rússia, Obninsk
V. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Rússia, Obninsk
I. Garagash
Schmidt Institute of Physics of the Earth
Email: llobkovsky@ocean.ru
Rússia, Moscow, 123242
B. Baranov
Shirshov Institute of Oceanology
Email: llobkovsky@ocean.ru
Rússia, Moscow, 117218
G. Steblov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Rússia, Obninsk
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