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Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake
The deformation transient following large subduction zone earthquakes is thought to originate from the interaction of viscoelastic flow in the asthenospheric mantle and slip on the megathrust that are both accelerated by the sudden coseismic stress change. Here, we show that combining insight from l...
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| 出版年: | Nat Commun |
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| 主要な著者: | , , , , , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group UK
2019
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6435688/ https://ncbi.nlm.nih.gov/pubmed/30914636 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-08984-7 |
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