Seismotectonic deformations related to the 2010 Maule earthquake at different stages of the seismic cycle from satellite geodetic observations
- Авторы: 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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Учреждения:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- Выпуск: Том 477, № 2 (2017)
- Страницы: 1498-1503
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/191813
- DOI: https://doi.org/10.1134/S1028334X17120261
- ID: 191813
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Аннотация
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.
Об авторах
L. Lobkovsky
Shirshov Institute of Oceanology
Автор, ответственный за переписку.
Email: llobkovsky@ocean.ru
Россия, Moscow
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Автор, ответственный за переписку.
Email: ir.s.vladimirova@yandex.ru
Россия, Obninsk
Yu. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: ir.s.vladimirova@yandex.ru
Россия, Obninsk
B. Baranov
Shirshov Institute of Oceanology
Email: ir.s.vladimirova@yandex.ru
Россия, Moscow
I. Garagash
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
Россия, Moscow
G. Steblov
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
Россия, Moscow
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