Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake

Modeling of postseismic deformation following great earthquakes has revealed the viscous structure of the mantle and the frictional properties of the fault interface. However, for giant megathrust events, viscoelastic flow and afterslip mechanically interplay with each other during the postseismic p...

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Detaylı Bibliyografya
Yayımlandı:Sci Adv
Asıl Yazarlar: Muto, J., Moore, J. D. P., Barbot, S., Iinuma, T., Ohta, Y., Iwamori, H.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: American Association for the Advancement of Science 2019
Konular:
Research Articles
Online Erişim:https://ncbi.nlm.nih.gov/pmc/articles/PMC6760927/
https://ncbi.nlm.nih.gov/pubmed/31579819
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aaw1164
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