{"@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/1361699995273282432.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/95jb02842"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F95JB02842"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/95JB02842"}}],"dc:title":[{"@value":"Intraplate deformation in the Japanese Islands: A kinematic study of intraplate deformation at a convergent plate margin"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Relative motions within the deforming Japanese Islands with respect to the Sea of Japan are determined using earthquake records over the last 414 years, slip rates on Quaternary faults, and angular change rates obtained from triangulation in the last century. We use a least squares inversion method to match the strain rates on the surface of the Earth with continuous spline functions to recover the velocity gradient tensors. The directions of the principal strain axes obtained from seismic, geological, and geodetic data are in general agreement with each other, with the maximum shortening axis oriented in a WNW direction. Principal strain rate magnitudes obtained from the geodetic data are about 3–5 times larger than the principal strain rates obtained from the seismic and geological data. Intraplate deformation in southwestern Japan determined from the seismic data accommodates a velocity of5.5±2(l σ) mm/yr in a direction parallel to the Nankai trough, which is about 25% of the plate motion velocity component parallel to the Nankai trough between the Philippine Sea and Eurasian plates. In northern Honshu, the velocity vectors from the seismic data are nearly parallel to the plate motion vector at the Japan trench, and the intraplate deformation accommodates about 6% of the total Pacific‐Eurasian or North American plate motion velocity. The velocity vector at Kashima, northern Honshu, calculated from the geodetic data is about 9–12 mm/yr in a direction of N55°W‐N76°W, which is about half of the very long baseline interferometry velocity calculated in the Eurasian reference frame, suggesting that the Sea of Japan may not be rigidly attached to the assumed rigid Eurasian plate.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380579820231849344","@type":"Researcher","foaf:name":[{"@value":"B. Shen‐Tu"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995273282433","@type":"Researcher","foaf:name":[{"@value":"W. E. Holt"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995273282432","@type":"Researcher","foaf:name":[{"@value":"A. J. Haines"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1995-12-10","prism:volume":"100","prism:number":"B12","prism:startingPage":"24275","prism:endingPage":"24293"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F95JB02842"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/95JB02842"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050845763140670720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimate of the contraction rate of central Japan through the deformation of the Philippine Sea slab"}]},{"@id":"https://cir.nii.ac.jp/crid/1050848249756527488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coulomb stress change on inland faults during megathrust earthquake cycle in southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431099443584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical experiment toward simultaneous estimation of the spatiotemporal evolution of interseismic fault slips and block motions in southwest Japan"}]},{"@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/1360567182088900992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Persistent inelastic deformation in central Japan revealed by GPS observation before and after the Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861287035222144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic and Geological Deformation of the Island Arc in Northeast Japan Revealed by the 2011 Tohoku Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865816799207168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evaluation of earthquake potential using a kinematic crustal block motion model in Java, Indonesia, based on GNSS observation"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511644288","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Secular crustal deformation in central Japan, based on the wavelet analysis of GPS time-series data"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279780608","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismotectonics of the Japanese Islands Based on GPS Observation"},{"@language":"ja","@value":"GPS観測に基づく日本列島の地震テクトニクス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279790976","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Co -and post- seismic Deformation and Fault Model of the 2011 off the Pacific Coast of Tohoku Earthquake"},{"@language":"ja","@value":"2011年（平成23年）東北地方太平洋沖地震に伴う地震時および地震後の地殻変動と断層モデル"},{"@language":"ja-Kana","@value":"2011ネン(ヘイセイ 23ネン)トウホク チホウ タイヘイヨウオキ ジシン ニ トモナウ ジシンジ オヨビ ジシン ゴ ノ チカク ヘンドウ ト ダンソウ モデル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217064448","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Crustal deformation of northeastern Japan based on geodetic data for recent 120 years"},{"@language":"ja","@value":"測地観測データに基づく東北日本の最近120年間の地殻変動"},{"@language":"ja-Kana","@value":"ソクチ カンソク データ ニ モトズク トウホク ニホン ノ サイキン 120ネンカン ノ チカク ヘンドウ"},{"@value":"Crustal deformation of northeastern Japan based on geodetic data for recent 120 years [in Japanese with English abstract]"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489147648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A decade of GEONET: 1994-2003"},{"@value":"A decade of GEONET: 1994-2003--The continuous GPS observation in Japan and its impact on earthquake studies"},{"@language":"ja-Kana","@value":"decade of GEONET 1994 2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003 —The continuous GPS observation in Japan and its impact on earthquake studies—"},{"@value":"1994–2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observations in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observation in Japan and its impact on earthquake studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681490788224","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Elastic and inelastic strains in the Japanese Islands deduced from GPS dense array"}]},{"@id":"https://cir.nii.ac.jp/crid/1390290393637121408","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Updating “the laws of convergence rate of plates” by Otsuki (1989)"},{"@language":"ja","@value":"プレート収れん速度の法則（Otsuki, 1989）の更新"},{"@language":"ja-Kana","@value":"プレートシュウレンソクド ノ ホウソク(Otsuki, 1989)ノ 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