{"@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/1361699993854604032.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.tecto.2006.04.017"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195106002368?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195106002368?httpAccept=text/plain"}}],"dc:title":[{"@value":"A model with rigid rotations and slip deficits for the GPS-derived velocity field in Southwest Japan"}],"description":[{"notation":[{"@value":"Abstract   We interpret the GPS-derived velocity field in southwest Japan by a superposition of the elastic deformation caused by fault interactions (slips or slip deficits) on the rigid motion of tectonic blocks (or plates). Based on the strain rate field and crustal seismicity, we apply a model with three blocks (Inner Arc, Outer Arc, and the northern Ryukyu block) and slip deficits along the block boundaries.  Several characteristics of the synthesized contributions are found:  (1)   Westward motion of the outer arc relative to the Amurian plate and the inner arc,   (2)   southeastward motion of the northern Ryukyu block relative to the Amurian plate,   (3)   2−4 mm/yr deficits of left lateral slip rates along the boundary at 32°N in southern Kyushu,   (4)   0−8 mm/yr deficits of right lateral slip rates along the Median Tectonic Line and the Beppu-Shimabara Graben,   (5)   slip deficit rates on the plate interface smaller than those in the case without any consideration for rigid block motions,   (6)   clockwise deflection of slip deficit rate vector on the plate interface from that estimated when not taking rigid block motions into consideration."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699993854604032","@type":"Researcher","foaf:name":[{"@value":"Sou Nishimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993854604033","@type":"Researcher","foaf:name":[{"@value":"Manabu Hashimoto"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2006-08","prism:volume":"421","prism:number":"3-4","prism:startingPage":"187","prism:endingPage":"207"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0040195106002368?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195106002368?httpAccept=text/plain"}],"createdAt":"2006-06-23","modifiedAt":"2023-05-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810809480960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial heterogeneities in tectonic stress in Kyushu, Japan and their relation to a major shear zone Seismology"},{"@value":"Spatial heterogeneities in tectonic stress in Kyushu, Japan and their relation to a major shear zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564285794446208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inelastic strain rate in the seismogenic layer of Kyushu Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981430736000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismicity controlled by resistivity structure : the 2016 Kumamoto earthquakes, Kyushu Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216708861824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"3D modeling of the cycle of a great Tohoku-oki earthquake, considering frictional behavior at low to high slip velocities"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709545856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Small repeating earthquake activity, interplate quasi‐static slip, and interplate coupling in the Hyuga‐nada, southwestern Japan subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710979665536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strain partitioning and interplate coupling along the northern margin of the Philippine Sea plate, estimated from Global Navigation Satellite System and Global Positioning System-Acoustic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476777984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interseismic stress accumulation at the locked zone of Nankai Trough seismogenic fault off Kii Peninsula"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476823680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquake doublet in an active shear zone, southwest Japan: Constraints from geophysical and geochemical findings"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869459052787584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coseismic Slip and Early Afterslip of the 2024 Hyuganada Earthquake Modulated by a Subducted Seamount"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518711821056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleotsunami research along the Nankai Trough and Ryukyu Trench subduction zones – Current achievements and future 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