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...
保存先:
| 第一著者: | |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2015-09-01
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| シリーズ: | Геодинамика и тектонофизика |
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| オンライン・アクセス: | https://www.gt-crust.ru/jour/article/view/159 |
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