{"@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/1360574094196335488.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2000jb900060"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000JB900060"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000JB900060"}},{"identifier":{"@type":"NAID","@value":"80011738471"}}],"dc:title":[{"@value":"Full interseismic locking of the Nankai and Japan‐west Kurile subduction zones: An analysis of uniform elastic strain accumulation in Japan constrained by permanent GPS"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We analyze permanent Global Positioning System (GPS) data obtained over Japan between 1995 and 1997 to estimate the instantaneous interseismic coupling ratio of the seismogenic zones due to the subduction of the Pacific and Philippine Sea plates below the Japanese islands. We first derive the GPS strain rate fields that characterize the crustal deformation of southern and northern Japan and invert them to determine the effective subduction velocity along the central Nankai trough on one side and the Japan‐west Kurile trench on the other. These “reference free” velocities are close to those predicted by plate motion models with respect to Eurasia. We conclude that the Eurasian reference frame gives a good approximation to the subduction motion and that to first order, both subduction zones were fully locked during the period of measurements. We then test whether the coupling ratio shows local variations within the seismogenic zones. To do this, we divide the subduction interface into 35 km×30 km elements that we model by point source groups, and we invert the GPS velocity field referenced to Eurasia to derive the coupling ratio (between 0 and 1) on each fault element. The results are coherent over the 3 years and confirm that both the central Nankai and the Japan‐west Kurile seismogenic zones are homogeneously fully locked. Most of the coupling ratios are close to 1 and a few are close to 0; intermediate values are rare. The zones of decoupling correspond either to strong postseismic afterslip associated with the 1994 Sanriku‐Oki interplate earthquake (Japan trench) or to a small overestimation of the actual lower limit of the locked zone. We conclude that within the resolution of the GPS data and the model, (1) partial coupling did not exist during these 3 years along the Nankai and Japan‐west Kurile trenches; (2) the small seismic coupling ratio previously derived from earthquakes analysis for the Japan and Kurile trenches may indicate that a significant part of the elastic energy is dissipated silently through slow earthquakes and postseismic afterslip; and (3) the heterogeneous coseismic slip pattern observed for the large and great earthquakes that rupture both subduction zones is in great contrast to the homogeneous loading. Finally, we discuss the nonelastic residual deformation within the frame of the long‐term deformation of the Japanese islands.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380574094196335616","@type":"Researcher","foaf:name":[{"@value":"Stéphane Mazzotti"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574094196335488","@type":"Researcher","foaf:name":[{"@value":"Xavier Le Pichon"}]},{"@id":"https://cir.nii.ac.jp/crid/1380574094196335489","@type":"Researcher","foaf:name":[{"@value":"Pierre Henry"}]},{"@id":"https://cir.nii.ac.jp/crid/1380861291122592768","@type":"Researcher","foaf:name":[{"@value":"Shin‐Ichi Miyazaki"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2000-06-10","prism:volume":"105","prism:number":"B6","prism:startingPage":"13159","prism:endingPage":"13177"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000JB900060"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000JB900060"}],"createdAt":"2002-09-17","modifiedAt":"2024-12-07","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031479094656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"十勝沖の地震活動 : 1952年十勝沖地震以降51年間の地震活動の特徴"},{"@language":"en","@value":"Seismic Activity off Tokachi Region, Southeastern Hokkaido, Japan : The Features for 51 Years since the 1952 Tokachi-Oki Earthquake"},{"@language":"ja-Kana","@value":"トカチオキ ノ ジシン カツドウ 1952ネン トカチオキ ジシン イコウ 51ネンカン ノ ジシン カツドウ ノ トクチョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1050293710890939264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Azimuthal differences and changes in strain rate and stress of the Japanese Islands deduced from geophysical data"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506455806336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2003年十勝沖地震 : 1952年十勝沖地震からの地震活動･前震･本震･余震および誘発地震"},{"@language":"en","@value":"The 2003 Tokachi-oki Earthquake, off Southeastern Hokkaido, Japan : Seismic Activities from the Former 1952 Tokachi-oki Earthquake, Foreshock, Mainshock, Aftershocks, and Triggered Earthquakes"},{"@language":"ja-Kana","@value":"2003ネン トカチオキ ジシン 1952ネン トカチオキ ジシン カラ ノ ジシン カツドウ ゼンシン ホンシン ヨシン オヨビ ユウハツ ジシン"}]},{"@id":"https://cir.nii.ac.jp/crid/1050845762473522944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Interseismic deformation of the Nankai subduction zone, southwest Japan, inferred from three-dimensional crustal velocity fields"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229806477824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Near‐field observations of an offshore <i>M<sub>w</sub></i> 6.0 earthquake from an integrated seafloor and subseafloor monitoring network at the Nankai Trough, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232468335104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Single-grain feldspar luminescence chronology of historical extreme wave event deposits recorded in a coastal lowland, 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206497185664","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoseismology along the Southern Kuril Trench, Inferred from Diatom-based Sea-level Reconstructions"},{"@language":"ja","@value":"珪藻化石群集を用いた海水準変動の復元と千島海溝南部の古地震およびテクトニクス"},{"@language":"ja-Kana","@value":"ケイソウ カセキ グンシュウ オ モチイタ カイスイジュン ヘンドウ ノ フクゲン ト チシマ カイコウ ナンブ ノ コジシン オヨビ テクトニクス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511842048","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coseismic and postseismic crustal deformation after the M<SUB>ω</SUB> 8 Tokachi-oki earthquake in Japan"},{"@value":"Coseismic and postseismic crustal deformation after the Mw 8 Tokachi-oki earthquake in Japan"},{"@value":"Post seismic crustal deformation from the Mw 8 Tokachi-oki earthquake on September 26, 2003 in Japan"},{"@value":"Co-seismic and 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Trough"},{"@value":"南海トラフにおける間隙水挙動に関する研究の現状と間隙水圧観測の意義"},{"@language":"ja-Kana","@value":"ナンカイ トラフ ニ オケル カンゲキスイ キョドウ ニ カンスル ケンキュウ ノ ゲンジョウ ト カンゲキ スイアツ カンソク ノ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279798144","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Long-term Earthquake Forecast and Tsunami Disaster Management in Japan Related to the 2011 off the Pacific Coast of Tohoku Earthquake"},{"@language":"ja","@value":"東北地方太平洋沖地震に関連した地震発生長期予測と津波防災対策"},{"@language":"ja-Kana","@value":"トウホク チホウ タイヘイヨウオキ ジシン ニ カンレン シタ ジシン ハッセイ チョウキ ヨソク ト ツナミ ボウサイ タイサク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679280382080","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spatial Variation of Slip Deficit Rate at the Nankai Trough, Southwest Japan Inferred from Three-Dimensional GPS Crustal Velocity Fields"},{"@value":"3次元GPS速度場から推定した南海トラフのすべり欠損分布"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679282008960","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"非地震性すべりの時空間変化と大地震の発生予測"},{"@language":"en","@value":"Spatial and Temporal Changes of Aseismic Slip and Its Role on Earthquake Forecasting"},{"@value":"総合報告 非地震性すべりの時空間変化と大地震の発生予測--三陸沖における近年の進展を中心に"},{"@language":"ja-Kana","@value":"ソウゴウ ホウコク ヒジシンセイスベリ ノ ジクウカン ヘンカ ト ダイジシン ノ ハッセイ ヨソク サンリクオキ ニ オケル キンネン ノ シンテン オ チュウシン ニ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488758912","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Investigation of the earthquake sequence off Miyagi prefecture with historical seismograms"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489147648","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A decade of GEONET: 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