Seismotectonic deformations related to the 2010 Maule earthquake at different stages of the seismic cycle from satellite geodetic observations
- 作者: 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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隶属关系:
- Shirshov Institute of Oceanology
- Geophysical Survey of the Russian Academy of Sciences
- Schmidt Institute of Physics of the Earth
- 期: 卷 477, 编号 2 (2017)
- 页面: 1498-1503
- 栏目: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/191813
- DOI: https://doi.org/10.1134/S1028334X17120261
- ID: 191813
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详细
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.
作者简介
L. Lobkovsky
Shirshov Institute of Oceanology
编辑信件的主要联系方式.
Email: llobkovsky@ocean.ru
俄罗斯联邦, Moscow
I. Vladimirova
Geophysical Survey of the Russian Academy of Sciences
编辑信件的主要联系方式.
Email: ir.s.vladimirova@yandex.ru
俄罗斯联邦, Obninsk
Yu. Gabsatarov
Geophysical Survey of the Russian Academy of Sciences
Email: ir.s.vladimirova@yandex.ru
俄罗斯联邦, Obninsk
B. Baranov
Shirshov Institute of Oceanology
Email: ir.s.vladimirova@yandex.ru
俄罗斯联邦, Moscow
I. Garagash
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
俄罗斯联邦, Moscow
G. Steblov
Schmidt Institute of Physics of the Earth
Email: ir.s.vladimirova@yandex.ru
俄罗斯联邦, Moscow
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