Post-seismic motions after the 2006–2007 Simushir earthquakes at different stages of the seismic cycle
- Authors: 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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Affiliations:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- Issue: Vol 473, No 1 (2017)
- Pages: 375-379
- Section: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189565
- DOI: https://doi.org/10.1134/S1028334X17030266
- ID: 189565
Cite item
Abstract
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.
About the authors
L. I. Lobkovsky
Shirshov Institute of Oceanology
Author for correspondence.
Email: llobkovsky@ocean.ru
Russian Federation, Moscow, 117218
I. S. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Russian Federation, Obninsk
V. V. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Russian Federation, Obninsk
I. A. Garagash
Schmidt Institute of Physics of the Earth
Email: llobkovsky@ocean.ru
Russian Federation, Moscow, 123242
B. V. Baranov
Shirshov Institute of Oceanology
Email: llobkovsky@ocean.ru
Russian Federation, Moscow, 117218
G. M. Steblov
Geophysical Survey of the Russian Academy of Sciences
Email: llobkovsky@ocean.ru
Russian Federation, Obninsk
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