Seismotectonic deformations related to the 2010 Maule earthquake at different stages of the seismic cycle from satellite geodetic observations
- Authors: Lobkovsky L.I.1, Vladimirova I.S.2, Gabsatarov Y.V.2, Baranov B.V.1, Garagash I.A.3, Steblov G.M.3
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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 477, No 2 (2017)
- Pages: 1498-1503
- Section: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/191813
- DOI: https://doi.org/10.1134/S1028334X17120261
- ID: 191813
Cite item
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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