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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Bibliographic Details
Main Authors: Moore, James Daniel Paul, Barbot, Sylvain, Iinuma, T., Ohta, Y., Iwamori, H., Muto, J.
Other Authors: Earth Observatory of Singapore
Format: Article
Language:English
Published: 2019
Subjects:
Online Access:https://hdl.handle.net/10356/81160
http://hdl.handle.net/10220/50073
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Institution: Nanyang Technological University
Language: English
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