Seismotectonic deformations related to the 2010 Maule earthquake at different stages of the seismic cycle from satellite geodetic observations
- Авторлар: 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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Мекемелер:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- Шығарылым: Том 477, № 2 (2017)
- Беттер: 1498-1503
- Бөлім: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/191813
- DOI: https://doi.org/10.1134/S1028334X17120261
- ID: 191813
Дәйексөз келтіру
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.
Авторлар туралы
L. Lobkovsky
Shirshov Institute of Oceanology
Хат алмасуға жауапты Автор.
Email: llobkovsky@ocean.ru
Ресей, Moscow
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: ir.s.vladimirova@yandex.ru
Ресей, Obninsk
Yu. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: ir.s.vladimirova@yandex.ru
Ресей, Obninsk
B. Baranov
Shirshov Institute of Oceanology
Email: ir.s.vladimirova@yandex.ru
Ресей, Moscow
I. Garagash
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
Ресей, Moscow
G. Steblov
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
Ресей, Moscow
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