Seismotectonic deformations related to the 2010 Maule earthquake at different stages of the seismic cycle from satellite geodetic observations


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Abstract

The interpretation of multiannual satellite geodetic observations after the 2010 Maule earthquake is given on the basis of the keyboard concept of the subduction region structure. It is shown that this concept, combined with the models of viscoelastic relaxation in the asthenosphere and nonstationary convection system in the upper mantle, completely explains the surface displacements observed.

About the authors

L. I. Lobkovsky

Shirshov Institute of Oceanology

Author for correspondence.
Email: llobkovsky@ocean.ru
Russian Federation, Moscow

I. S. Vladimirova

Geophysical Survey of the Russian Academy of Sciences

Author for correspondence.
Email: ir.s.vladimirova@yandex.ru
Russian Federation, Obninsk

Yu. V. Gabsatarov

Geophysical Survey of the Russian Academy of Sciences

Email: ir.s.vladimirova@yandex.ru
Russian Federation, Obninsk

B. V. Baranov

Shirshov Institute of Oceanology

Email: ir.s.vladimirova@yandex.ru
Russian Federation, Moscow

I. A. Garagash

Schmidt Institute of Physics of the Earth

Email: ir.s.vladimirova@yandex.ru
Russian Federation, Moscow

G. M. Steblov

Schmidt Institute of Physics of the Earth

Email: ir.s.vladimirova@yandex.ru
Russian Federation, Moscow

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