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MODELLING OF POSTSEISMIC PROCESSES IN SUBDUCTION ZONES

Large intraplate subduction earthquakes are generally accompanied by prolonged and intense postseismic anomalies. In the present work, viscoelastic relaxation in the upper mantle and the asthenosphere is considered as a main mechanism responsible for the occurrence of such postseismic effects. The s...

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Detalles Bibliográficos
Autor Principal: Irina S. Vladimirova
Formato: Artigo
Idioma:Inglês
Publicado: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2015-09-01
Series:Геодинамика и тектонофизика
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Acceso en liña:https://www.gt-crust.ru/jour/article/view/159
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