{"@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/1361981471344295552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/jgrb.50265"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjgrb.50265"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/jgrb.50265"}}],"dc:title":[{"@value":"Coseismic slip distribution for the <i>M<sub>w</sub></i> 9 2011 Tohoku‐Oki earthquake derived from 3‐D FE modeling"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The coseismic slip distribution of the <jats:italic>M<jats:sub>w</jats:sub></jats:italic> 9.0 2011 Tohoku‐Oki earthquake has been estimated by inverting near‐field onshore and offshore geodetic data, using Green's function calculated with a 3‐D finite element (FE) model. The FE model simulates several geophysical features of the subduction zone that hosted the rupture surface of the event. These features include a 3‐D geometric configuration and distribution of material properties of the tectonic system, a precise geometric configuration of the irregular rupture surface, and an irregular free surface according to the topography and bathymetry. A model that simulates rupture along the interface between the relatively weak overriding Okhotsk plate and stiff subducting slab of the Pacific Plate requires less slip to produce the observed surface deformation, compared to a model having uniform material properties across the rupture interface. Furthermore, the estimated slip of the heterogeneous model is more widely distributed over the shallow portion of the plate boundary, whereas the estimated slip of the homogeneous model is more focused updip of the epicenter. This demonstrates the sensitivity of inverse analyses of geodetic data for the 2011 Tohoku‐Oki earthquake to the simulated domain geometry and configuration of material properties.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004231402358405","@type":"Researcher","foaf:name":[{"@value":"C. Kyriakopoulos"}],"jpcoar:affiliationName":[{"@value":"School of Earth and Atmospheric Sciences Georgia Institute of Technology  Atlanta Georgia USA"},{"@value":"National Earthquake Center Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471344295556","@type":"Researcher","foaf:name":[{"@value":"T. Masterlark"}],"jpcoar:affiliationName":[{"@value":"Geology and Geological Engineering South Dakota School of Mines and Technology  Rapid City South Dakota USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471344295552","@type":"Researcher","foaf:name":[{"@value":"S. Stramondo"}],"jpcoar:affiliationName":[{"@value":"National Earthquake Center Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471344295555","@type":"Researcher","foaf:name":[{"@value":"M. Chini"}],"jpcoar:affiliationName":[{"@value":"National Earthquake Center Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"},{"@value":"Département Environnement et Agro‐biotechnologies (EVA) Centre de Recherché Public ‐ Gabriel Lippmann  Belvaux Luxembourg"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471344295553","@type":"Researcher","foaf:name":[{"@value":"C. Bignami"}],"jpcoar:affiliationName":[{"@value":"National Earthquake Center Istituto Nazionale di Geofisica e Vulcanologia  Rome Italy"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"21699313"},{"@type":"EISSN","@value":"21699356"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2013-07","prism:volume":"118","prism:number":"7","prism:startingPage":"3837","prism:endingPage":"3847"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjgrb.50265"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/jgrb.50265"}],"createdAt":"2013-06-27","modifiedAt":"2023-09-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002217556488960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An elastic/viscoelastic finite element analysis method for crustal deformation using a 3-D island-scale high-fidelity model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231402358528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detectability analysis of interplate fault slips in the Nankai subduction thrust using seafloor observation instruments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004236002955136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Learning from crustal deformation associated with the M9 2011 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142423994240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Decade of Lessons Learned from the 2011 Tohoku‐Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142451550720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low-Order Finite Element Solver with Small Matrix-Matrix Multiplication Accelerated by AI-Specific Hardware for Crustal Deformation Computation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286994500115200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Introduction of covariance components in slip inversion of geodetic data following a non-uniform spatial distribution and application to slip deficit rate estimation in the Nankai Trough subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892104447744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Real-time automatic uncertainty estimation of coseismic single rectangular fault model using GNSS data"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792008793216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-fidelity elastic Green’s functions for subduction zone models consistent with the global standard geodetic reference system"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/jgrb.50265"},{"@type":"CROSSREF","@value":"10.1093/gji/ggw123_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"},{"@type":"CROSSREF","@value":"10.1007/s11001-019-09380-y_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"},{"@type":"CROSSREF","@value":"10.1130/ges01531.1_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"},{"@type":"CROSSREF","@value":"10.1029/2020rg000713_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"},{"@type":"CROSSREF","@value":"10.1145/3394277.3401860_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01425-0_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"},{"@type":"CROSSREF","@value":"10.1093/gji/ggaa116_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01370-y_references_DOI_nLqD9eToa6G25ph1MUpNOzR7Vw"}]}