{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360002216799083392.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/nature13778"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature13778.pdf"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature13778"}},{"identifier":{"@type":"PMID","@value":"25231864"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Prevalence of viscoelastic relaxation after the 2011 Tohoku-oki earthquake"}],"description":[{"notation":[{"@value":"After a large subduction earthquake, crustal deformation continues to occur, with a complex pattern of evolution. This postseismic deformation is due primarily to viscoelastic relaxation of stresses induced by the earthquake rupture and continuing slip (afterslip) or relocking of different parts of the fault. When postseismic geodetic observations are used to study Earth's rheology and fault behaviour, it is commonly assumed that short-term (a few years) deformation near the rupture zone is caused mainly by afterslip, and that viscoelasticity is important only for longer-term deformation. However, it is difficult to test the validity of this assumption against conventional geodetic data. Here we show that new seafloor GPS (Global Positioning System) observations immediately after the great Tohoku-oki earthquake provide unambiguous evidence for the dominant role of viscoelastic relaxation in short-term postseismic deformation. These data reveal fast landward motion of the trench area, opposing the seaward motion of GPS sites on land. Using numerical models of transient viscoelastic mantle rheology, we demonstrate that the landward motion is a consequence of relaxation of stresses induced by the asymmetric rupture of the thrust earthquake, a process previously unknown because of the lack of near-field observations. Our findings indicate that previous models assuming an elastic Earth will have substantially overestimated afterslip downdip of the rupture zone, and underestimated afterslip updip of the rupture zone; our knowledge of fault friction based on these estimates therefore needs to be revised."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380284919964705666","@type":"Researcher","foaf:name":[{"@value":"Tianhaozhe Sun"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705671","@type":"Researcher","foaf:name":[{"@value":"Kelin Wang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705536","@type":"Researcher","foaf:name":[{"@value":"Takeshi 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Hino"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705537","@type":"Researcher","foaf:name":[{"@value":"Jiangheng He"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705670","@type":"Researcher","foaf:name":[{"@value":"Hiromi Fujimoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705538","@type":"Researcher","foaf:name":[{"@value":"Motoyuki Kido"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705667","@type":"Researcher","foaf:name":[{"@value":"Yukihito Osada"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705664","@type":"Researcher","foaf:name":[{"@value":"Satoshi Miura"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801187362048","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50451513"},{"@type":"NRID","@value":"1000050451513"},{"@type":"ORCID","@value":"0000-0003-4818-477X"},{"@type":"NRID","@value":"9000001115953"},{"@type":"NRID","@value":"9000245917735"},{"@type":"NRID","@value":"9000413693966"},{"@type":"NRID","@value":"9000251867571"},{"@type":"NRID","@value":"9000014231935"},{"@type":"NRID","@value":"9000410904517"},{"@type":"NRID","@value":"9000255735949"},{"@type":"NRID","@value":"9000256898238"},{"@type":"NRID","@value":"9000406059252"},{"@type":"NRID","@value":"9000400196298"},{"@type":"NRID","@value":"9000254262597"},{"@type":"NRID","@value":"9000408783347"},{"@type":"NRID","@value":"9000326253268"},{"@type":"NRID","@value":"9000347362376"},{"@type":"NRID","@value":"9000379600347"},{"@type":"NRID","@value":"9000403163437"},{"@type":"NRID","@value":"9000403425837"},{"@type":"NRID","@value":"9000256137598"},{"@type":"NRID","@value":"9000016658722"},{"@type":"NRID","@value":"9000408484233"},{"@type":"NRID","@value":"9000317548895"},{"@type":"NRID","@value":"9000254263413"},{"@type":"NRID","@value":"9000396153769"},{"@type":"NRID","@value":"9000256137808"},{"@type":"NRID","@value":"9000296681351"},{"@type":"NRID","@value":"9000396153820"},{"@type":"NRID","@value":"9000263067862"},{"@type":"NRID","@value":"9000409285216"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0134552"}],"foaf:name":[{"@value":"Yusaku Ohta"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964705669","@type":"Researcher","foaf:name":[{"@value":"Yan Hu"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2014-09-17","prism:volume":"514","prism:number":"7520","prism:startingPage":"84","prism:endingPage":"87"},"reviewed":"false","invited":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/nature13778.pdf"},{"@id":"http://www.nature.com/articles/nature13778"}],"createdAt":"2014-09-16","modifiedAt":"2023-05-18","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782145807488","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23253003"},{"@type":"JGN","@value":"JP23253003"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23253003/"}],"notation":[{"@language":"ja","@value":"アラスカの地殻隆起・重力変動観測による粘弾性構造解明と地球環境変動モニタリング"},{"@language":"en","@value":"Study on viscoelastic structure and monitoring of global change by observation of uplifting and gravity in Alaska, US"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782277971584","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26000002"},{"@type":"JGN","@value":"JP26000002"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26000002/"}],"notation":[{"@language":"ja","@value":"深海調査で迫るプレート境界浅部すべりの謎～その過去・現在"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782279212416","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26109007"},{"@type":"JGN","@value":"JP26109007"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-26109007/"}],"notation":[{"@language":"ja","@value":"島弧地殻における変形・断層すべり過程のモデル構築"},{"@language":"en","@value":"Development of models for deformation and fault slip processes in the island arc crust"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338805918336","@type":"Article","resourceType":"学術雑誌論文(journal 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Earthquake With the High Azimuthal Coverage Tsunami Data From the S‐Net Wide and Dense Network: Implication for the Stress Regime in the Tohoku Overriding Plate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021390741906432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal distributions of afterslip and locking on the plate interface associated with the 2011 Tohoku-Oki earthquake using a 3-D temperature and strain rate-dependent heterogeneous viscosity model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021395469197056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Progress in modeling the Tohoku-oki megathrust earthquake cycle and associated crustal deformation processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022497406926848","@type":"Article","resourceType":"学術雑誌論文(journal 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method of the asthenosphere's viscosity and afterslip using a fast and scalable finite-element adjoint solver"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693415558272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Low Coseismic Friction on the Tohoku-Oki Fault Determined from Temperature Measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704780608512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First measurement of the displacement rate of the Pacific Plate near the Japan Trench after the 2011 Tohoku-Oki earthquake using GPS/acoustic technique"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704781222656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial distribution of the faulting types of small earthquakes around the 2011 Tohoku‐oki 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708445291520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710932846208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Imaging the distribution of transient viscosity after the 2016\n            <i>M</i>\n            <sub>w</sub>\n            7.1 Kumamoto earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286993150092288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evidence of Changes of Seismic Properties in the Entire Crust Beneath Japan After the <i>M</i><sub><i>w</i></sub> 9.0, 2011 Tohoku‐oki 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