Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/81160
Full metadata record
DC FieldValueLanguage
dc.contributor.authorMoore, James Daniel Paulen
dc.contributor.authorBarbot, Sylvainen
dc.contributor.authorIinuma, T.en
dc.contributor.authorOhta, Y.en
dc.contributor.authorIwamori, H.en
dc.contributor.authorMuto, J.en
dc.date.accessioned2019-10-02T03:55:08Zen
dc.date.accessioned2019-12-06T14:22:42Z-
dc.date.available2019-10-02T03:55:08Zen
dc.date.available2019-12-06T14:22:42Z-
dc.date.issued2019en
dc.identifier.citationMuto, J., Moore, J. D. P., Barbot, S., Iinuma, T., Ohta, Y., & Iwamori, H. (2019). Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake. Science Advances, 5(9), eaaw1164-. doi:10.1126/sciadv.aaw1164en
dc.identifier.urihttps://hdl.handle.net/10356/81160-
dc.identifier.urihttp://hdl.handle.net/10220/50073en
dc.description.abstractModeling 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 period. We explore the role of afterslip and viscoelastic relaxation and their interaction in the aftermath of the 2011 Mw (moment magnitude) 9.0 Tohoku earthquake based on a detailed model analysis of the postseismic deformation with laterally varying, experimentally constrained, rock rheology. Mechanical coupling between viscoelastic relaxation and afterslip notably modifies both the afterslip distribution and surface deformation. Thus, we highlight the importance of addressing mechanical coupling for long-term studies of postseismic relaxation, especially in the context of the geodynamics of the Japan trench across the seismic cycle.en
dc.description.sponsorshipNRF (Natl Research Foundation, S’pore)en
dc.format.extent8 p.en
dc.language.isoenen
dc.relation.ispartofseriesScience Advancesen
dc.rights© 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S.Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).en
dc.subjectPostseismic Deformationen
dc.subjectViscoelastic Flowen
dc.subjectScience::Geologyen
dc.titleCoupled afterslip and transient mantle flow after the 2011 Tohoku earthquakeen
dc.typeJournal Articleen
dc.contributor.researchEarth Observatory of Singaporeen
dc.identifier.doi10.1126/sciadv.aaw1164en
dc.description.versionPublished versionen
item.fulltextWith Fulltext-
item.grantfulltextopen-
Appears in Collections:EOS Journal Articles
Files in This Item:
File Description SizeFormat 
Coupled afterslip and transient mantle flow after the 2011 Tohoku earthquake.pdf5.05 MBAdobe PDFThumbnail
View/Open

Google ScholarTM

Check

Altmetric

Items in DR-NTU are protected by copyright, with all rights reserved, unless otherwise indicated.