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Post-seismic motions after the 2006–2007 Simushir earthquakes at different stages of the seismic cycle


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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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