A postseismic process in the area of the Simushir 11/2006 Earthquake recovered by the GRACE data


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The GRACE data make it possible to detect the areas where the earthquakes initiate postseismic creep in regions much larger than the focal area. This information is important for estimation of the seismic potential and position of the locked segments in the subduction zones.

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V. Mikhailov

Schmidt Institute of Physics of the Earth; Institut de Physique du Globe de Paris

编辑信件的主要联系方式.
Email: mikh@ifz.ru
俄罗斯联邦, ul. Bolshaya Gruzinskaya 10, Moscow, 123995; Paris

E. Timoshkina

Schmidt Institute of Physics of the Earth

Email: mikh@ifz.ru
俄罗斯联邦, ul. Bolshaya Gruzinskaya 10, Moscow, 123995

M. Diament

Institut de Physique du Globe de Paris

Email: mikh@ifz.ru
法国, Paris

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