Seismotectonic deformations related to the 2010 Maule earthquake at different stages of the seismic cycle from satellite geodetic observations


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

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

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2017