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|Title:||Footprints of past earthquakes revealed in the afterslip of the 2010 Mw 7.8 Mentawai tsunami earthquake||Authors:||Feng, Lujia
Natawidjaja, Danny H.
Hill, Emma Mary
|Issue Date:||2016||Source:||Feng, L., Barbot, S., Hill, E. M., Hermawan, I., Banerjee, P., & Natawidjaja, D. H. (2016). Footprints of past earthquakes revealed in the afterslip of the 2010 Mw 7.8 Mentawai tsunami earthquake. Geophysical Research Letters, 43(18), 9518-9526.||Series/Report no.:||Geophysical Research Letters||Abstract:||The 2010 Mw 7.8 Mentawai tsunami earthquake marks one of the first tsunami earthquakes to have postseismic deformation observed by geodetic instruments. The Sumatran GPS Array has recorded the postseismic deformation following this event continuously for >5 years. The spatiotemporal evolution of the postseismic deformation is well explained by velocity-strengthening frictional sliding on the Sunda megathrust. Our results show that the 2010 afterslip progressed downdip relative to the 2010 coseismic rupture. The southeastern portion of the afterslip region overlaps the area that slipped during the main shock and afterslip of the 2007 Mw 8.4 Bengkulu earthquake, while the northwestern portion slipped an area without recent large earthquakes. By incorporating pre-earthquake stress conditions into quasi-dynamic models, we demonstrate that the preceding cumulative slip from the 2007 sequence might have caused a ∼0.1 MPa difference in pre-earthquake Coulomb stress between the southeastern and northwestern portions of the afterslip region.||URI:||https://hdl.handle.net/10356/86282
|ISSN:||0094-8276||DOI:||10.1002/2016GL069870||Rights:||© 2016 American Geophysical Union. This is the author created version of a work that has been peer reviewed and accepted for publication by Geophysical Research Letters, American Geophysical Union. It incorporates referee’s comments but changes resulting from the publishing process, such as copyediting, structural formatting, may not be reflected in this document. The published version is available at: [http://dx.doi.org/10.1002/2016GL069870].||Fulltext Permission:||open||Fulltext Availability:||With Fulltext|
|Appears in Collections:||EOS Journal Articles|
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