{"@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/1362262945686501248.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2004jb003203"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JB003203"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JB003203"}},{"identifier":{"@type":"NAID","@value":"80019105557"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Interplate coupling beneath NE Japan inferred from three‐dimensional displacement field"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The northeastern Japan arc is located in a typical subduction zone and is a seismically active region where large interplate earthquakes have occurred repeatedly. The nationwide GPS network has made it possible to investigate the crustal deformation in unprecedented detail; however, vertical displacements are less accurate than the horizontal ones and have not been used to constrain interplate coupling models. In this study, GPS carrier phase data are analyzed in order to estimate three components of site displacements. The result indicates uplift along the Japan Sea coast and subsidence along the Pacific Ocean coast. Using the vertical site velocities together with the horizontal ones as the data for a geodetic inversion method, a new model of interplate coupling is constructed to explain both the horizontal and vertical velocities for the interseismic period from 1997 to 2001. The model demonstrates strong coupling in the area off Miyagi and in the area off Aomori through the area off Tokachi, including the areas of asperities. The downdip limit of the locked fault zone on the plate boundary has been estimated seismologically to be at a depth of 50–60 km in northeastern Japan, and the distribution of slip deficits derived in this study indicates that the transition zone extends down to a depth of about 100 km.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262945686501250","@type":"Researcher","foaf:name":[{"@value":"Yoko Suwa"}],"jpcoar:affiliationName":[{"@value":"Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945686501248","@type":"Researcher","foaf:name":[{"@value":"Satoshi Miura"}],"jpcoar:affiliationName":[{"@value":"Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945686501251","@type":"Researcher","foaf:name":[{"@value":"Akira Hasegawa"}],"jpcoar:affiliationName":[{"@value":"Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945686501249","@type":"Researcher","foaf:name":[{"@value":"Toshiya Sato"}],"jpcoar:affiliationName":[{"@value":"Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science Tohoku University  Sendai Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945686501252","@type":"Researcher","foaf:name":[{"@value":"Kenji Tachibana"}],"jpcoar:affiliationName":[{"@value":"Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science Tohoku University  Sendai Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2006-04","prism:volume":"111","prism:number":"B4","prism:startingPage":"1"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JB003203"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JB003203"}],"createdAt":"2006-04-04","modifiedAt":"2023-10-13","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000781801204224","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15204037"},{"@type":"JGN","@value":"JP15204037"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15204037/"}],"notation":[{"@language":"ja","@value":"プレート境界におけるアスペリティのマッピングとすべりの時空間分布の推定"},{"@language":"en","@value":"Mapping of asperities and estimation of spatiotemporal distribution of interplate slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000781804654080","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15340142"},{"@type":"JGN","@value":"JP15340142"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15340142/"}],"notation":[{"@language":"ja","@value":"海陸プレート境界近傍におけるプレート運動ゆらぎの測地学的検出の試み"},{"@language":"en","@value":"Investigation for geodetic detection of variation in crustal deformation near the subduction plate boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782433009920","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"17253003"},{"@type":"JGN","@value":"JP17253003"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-17253003/"}],"notation":[{"@language":"ja","@value":"米国アラスカ州南部における後氷期地殻隆起の総合測地観測と粘弾性構造の推定"},{"@language":"en","@value":"Study on viscoelastic structure beneath Southeastern Alaska, United States through geodetic observation of crustal uplift Caused by deglaciation"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001339269691776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneities in Stress and Strength in Tohoku and Its Relationship with Earthquake Sequences Triggered by the 2011 M9 Tohoku-Oki Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050006065615081472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stress release process along an intraplate fault analogous to the plate boundary: a case study of the 2017 M5.2 Akita-Daisen earthquake, NE Japan"}]},{"@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 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Plate"}]},{"@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/1360869855136930304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Elusive Role of Aseismic Slip Along a Seaward Dipping Normal Fault in the Indirect Triggering of a Normal Faulting Earthquake Sequence in Northeast Japan Following the 2011 Tohoku‐Oki Megathrust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855583860224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"GNSS-Acoustic positioning error in the vertical component considering the uncertainty of a reference sound speed 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シズミコミタイ ニ オケル ジシン ハッセイ ト カザン セイセイ ノ モデル"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204066296704","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Report of the Geodetic Works in Japan for the Period January 2003 to December 2006"},{"@value":"Reports to the IUGG: Report of the geodetic works in Japan for the period from January 2003 to December 2006"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204067406848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Introduction of 10 Hz GPS Receiver for the Improved Observation of Seafloor Crustal Movement"},{"@language":"ja","@value":"10 Hz GPS受信機導入による海底地殻変動観測高度化の試み"},{"@language":"ja-Kana","@value":"10 Hz GPS ジュシンキ ドウニュウ ニ ヨル カイテイ チカク ヘンドウ カンソク コウドカ ノ 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article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interplate Slip Distribution Inferred from Co- and Post-seismic Deformation Associated with the 2005 Miyagi-oki Earthquake (<I>M</I>7.2)"},{"@language":"ja","@value":"2005年宮城県沖地震(<I>M</I>7.2)に伴った地震時・地震後地殻変動から推定されたプレート境界面上のすべり分布"},{"@value":"2005年宮城県沖地震(M7.2)に伴った地震時・地震後地殻変動から推定されたプレート境界面上のすべり分布"},{"@language":"ja-Kana","@value":"2005ネン ミヤギケンオキ ジシン M7 2 ニ トモナッタ ジシンジ ジシンゴ チカク ヘンドウ カラ スイテイサレタ プレート キョウカイメンジョウ ノ スベリ ブンプ"},{"@value":"Interplate Slip Distribution Inferred from Co- and Post-seismic Deformation Associated with the 2005 Miyagi-oki Earthquake (M7.2)"},{"@value":"Interplate slip distribution inferred from co- and post-seismic deformation associated with the 2005 Miyagi-oki earthquake (N7.2)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303058688","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mechanisms for Variation 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