Seismotectonic deformations related to the 2010 Maule earthquake at different stages of the seismic cycle from satellite geodetic observations
- Autores: 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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Afiliações:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- Edição: Volume 477, Nº 2 (2017)
- Páginas: 1498-1503
- Seção: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/191813
- DOI: https://doi.org/10.1134/S1028334X17120261
- ID: 191813
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Resumo
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.
Sobre autores
L. Lobkovsky
Shirshov Institute of Oceanology
Autor responsável pela correspondência
Email: llobkovsky@ocean.ru
Rússia, Moscow
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Autor responsável pela correspondência
Email: ir.s.vladimirova@yandex.ru
Rússia, Obninsk
Yu. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: ir.s.vladimirova@yandex.ru
Rússia, Obninsk
B. Baranov
Shirshov Institute of Oceanology
Email: ir.s.vladimirova@yandex.ru
Rússia, Moscow
I. Garagash
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
Rússia, Moscow
G. Steblov
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
Rússia, Moscow
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