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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| Format: | Article |
| Language: | English |
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Institute of the Earth's crust, Siberian Branch of RAS
2015-09-01
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| Series: | Geodinamika i Tektonofizika |
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| Online Access: | https://www.gt-crust.ru/jour/article/view/159 |