MODELLING OF POSTSEISMIC PROCESSES IN SUBDUCTION ZONES

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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Bibliographic Details
Main Author:	Irina S. Vladimirova
Format:	Article
Language:	English
Published:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2015-09-01
Series:	Геодинамика и тектонофизика
Subjects:	viscosity asthenosphere postseismic processes viscoelastic relaxation
Online Access:	https://www.gt-crust.ru/jour/article/view/159

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