Post-seismic motions after the 2006–2007 Simushir earthquakes at different stages of the seismic cycle
- 作者: 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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隶属关系:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- 期: 卷 473, 编号 1 (2017)
- 页面: 375-379
- 栏目: Geophysics
- URL: https://journal-vniispk.ru/1028-334X/article/view/189565
- DOI: https://doi.org/10.1134/S1028334X17030266
- ID: 189565
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详细
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.
作者简介
L. Lobkovsky
Shirshov Institute of Oceanology
编辑信件的主要联系方式.
Email: llobkovsky@ocean.ru
俄罗斯联邦, Moscow, 117218
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
俄罗斯联邦, Obninsk
V. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
俄罗斯联邦, Obninsk
I. Garagash
Schmidt Institute of Physics of the Earth
Email: llobkovsky@ocean.ru
俄罗斯联邦, Moscow, 123242
B. Baranov
Shirshov Institute of Oceanology
Email: llobkovsky@ocean.ru
俄罗斯联邦, Moscow, 117218
G. Steblov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
俄罗斯联邦, Obninsk
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