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Although the large coseismic slip of the 2011 Tohoku-Oki earthquake was limited to the middle segment, the observed negative residual gravity anomaly area in the southern segment corresponds to the postseismic slip area of the Tohoku-Oki earthquake. A density distribution model can explain the different slip behaviours of the two segments by considering their structural differences. The model indicates that the plate interface in the south was covered with a thick channel layer, as indicated by seismic survey imaging, and this layer resulted in a residual gravity anomaly. Numerical simulations which assumed evident frictional heterogeneity caused by the layer in the south efficiently reproduced M9 earthquakes recurring only in the middle, followed by evident postseismic slips in the south. This study proposes that although the layer makes the megathrust less compliant to seismic slip, it promotes aseismic slips following the growth of seismic slips on the fault in an adjacent region.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380290617865614722","@type":"Researcher","foaf:name":[{"@value":"Ryoko Nakata"}]},{"@id":"https://cir.nii.ac.jp/crid/1380290617865614725","@type":"Researcher","foaf:name":[{"@value":"Takane Hori"}]},{"@id":"https://cir.nii.ac.jp/crid/1380290617865614992","@type":"Researcher","foaf:name":[{"@value":"Seiichi 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Hino"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20452322"}],"prism:publicationName":[{"@value":"Scientific Reports"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2021-03-19","prism:volume":"11","prism:number":"1","prism:startingPage":"6480"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://www.nature.com/articles/s41598-021-86020-9.pdf"},{"@id":"https://www.nature.com/articles/s41598-021-86020-9"}],"createdAt":"2021-03-19","modifiedAt":"2023-10-23","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Science","dc:title":"Science"},{"@id":"https://cir.nii.ac.jp/all?q=Q","dc:title":"Q"},{"@id":"https://cir.nii.ac.jp/all?q=R","dc:title":"R"},{"@id":"https://cir.nii.ac.jp/all?q=Medicine","dc:title":"Medicine"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040566775626660096","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"19H05596"},{"@type":"JGN","@value":"JP19H05596"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-19H05596/"}],"notation":[{"@language":"ja","@value":"巨大地震の裏側～巨大化させないメカニズム"},{"@language":"en","@value":"Head and tail of massive earthquakes: Mechanism arresting growth of interpolate earthquakes"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050013474495795840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A review on slow earthquakes in the Japan Trench"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916334976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Documenting large earthquakes similar to the 2011 Tohoku-oki earthquake from sediments deposited in the Japan Trench over the past 1500 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216802652928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Seafloor observations indicate spatial separation of coseismic and postseismic slips in the 2011 Tohoku 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