{"@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/1361699994109308544.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2007jb005361"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007JB005361"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007JB005361"}}],"dc:title":[{"@value":"Faulting processes controlled by the nonuniform thermal structure of the crust and uppermost mantle beneath the northeastern Japanese island arc"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We performed a finite element analysis, taking into account nonlinear viscoelasticity and plasticity, to construct a two‐dimensional model of the deformation and faulting processes that occur in the deeper parts of the seismogenic zone beneath northeastern Japan. Our finite element code was developed on the basis of the GeoFEM parallel finite element code using plug‐ins to adopt several nonlinear functions. An extensive onshore‐offshore wide‐angle seismic expedition conducted across northeastern Japan in 1997 revealed a detailed image of the deep crust and uppermost mantle structures. In modeling the deformation and faulting beneath the Ou Backbone Range and Dewa Hill, northeastern Japan, we consider a realistic crust and uppermost mantle structure revealed by the 1997 seismic expedition and the existence of the two hot regions revealed by geothermal observations in a compressional tectonic setting. The numerical results reveal that shortening deformation due to nonlinear viscous flow occurs in the hot region in the lower crust and the uppermost mantle, resulting in shear faulting in the upper crust. Our model reproduces three reverse fault zones that are consistent with those observed. We investigate the stress accumulation process over a period approximately corresponding to the earthquake recurrence interval by prohibiting plastic faulting and found that the stress is loaded along the fault zone at magnitudes much lower than the absolute stress level. The results indicate that the loading processes of large inland earthquakes in northeastern Japan are determined by the nonuniform thermal structure in the deeper crust and uppermost mantle.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994109308546","@type":"Researcher","foaf:name":[{"@value":"Bunichiro Shibazaki"}],"jpcoar:affiliationName":[{"@value":"International Institute for Seismology and Earthquake Engineering Building Research Institute  Tsukuba, Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994109308544","@type":"Researcher","foaf:name":[{"@value":"Kazuteru Garatani"}],"jpcoar:affiliationName":[{"@value":"ITOCHU Techno‐Solutions Corporation  Chiyoda‐ku, Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801200163968","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"70151719"},{"@type":"NRID","@value":"1000070151719"},{"@type":"NRID","@value":"9000254753796"},{"@type":"NRID","@value":"9000254262888"},{"@type":"NRID","@value":"9000254270741"},{"@type":"NRID","@value":"9000254741760"},{"@type":"NRID","@value":"9000004602253"},{"@type":"NRID","@value":"9000410904541"},{"@type":"NRID","@value":"9000413694882"},{"@type":"NRID","@value":"9000254753595"},{"@type":"NRID","@value":"9000410949604"},{"@type":"NRID","@value":"9000254270803"},{"@type":"NRID","@value":"9000400157697"},{"@type":"NRID","@value":"9000000774168"},{"@type":"NRID","@value":"9000391405458"},{"@type":"NRID","@value":"9000254753522"},{"@type":"NRID","@value":"9000254263101"},{"@type":"NRID","@value":"9000001755402"},{"@type":"NRID","@value":"9000254262834"},{"@type":"NRID","@value":"9000410949332"},{"@type":"NRID","@value":"9000403549786"},{"@type":"NRID","@value":"9000283228254"},{"@type":"NRID","@value":"9000391402104"},{"@type":"NRID","@value":"9000391405187"},{"@type":"NRID","@value":"9000410949812"},{"@type":"NRID","@value":"9000254753590"},{"@type":"NRID","@value":"9000403551953"},{"@type":"NRID","@value":"9000258411897"},{"@type":"NRID","@value":"9000254271201"},{"@type":"NRID","@value":"9000254741494"},{"@type":"NRID","@value":"9000017413614"},{"@type":"NRID","@value":"9000254753539"},{"@type":"NRID","@value":"9000254262969"},{"@type":"NRID","@value":"9000254270771"},{"@type":"NRID","@value":"9000410949853"},{"@type":"NRID","@value":"9000410948881"},{"@type":"NRID","@value":"9000254262818"},{"@type":"NRID","@value":"9000254270790"},{"@type":"NRID","@value":"9000258415648"},{"@type":"NRID","@value":"9000004598565"},{"@type":"NRID","@value":"9000254740635"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/iwasaki-t"}],"foaf:name":[{"@value":"Takaya Iwasaki"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute University of Tokyo  Bunkyo‐ku, Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994109308545","@type":"Researcher","foaf:name":[{"@value":"Akiko Tanaka"}],"jpcoar:affiliationName":[{"@value":"Geological Survey of Japan AIST  Tsukuba, Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801209043968","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50159547"},{"@type":"NRID","@value":"1000050159547"},{"@type":"ORCID","@value":"0000-0003-0808-0757"},{"@type":"CINII_AUTHOR_ID","@value":"DA19070894"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA19070894#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA19070894"},{"@type":"NRID","@value":"9000391400827"},{"@type":"NRID","@value":"9000007771930"},{"@type":"NRID","@value":"9000266443229"},{"@type":"NRID","@value":"9000001755585"},{"@type":"NRID","@value":"9000237727344"},{"@type":"NRID","@value":"9000391406325"},{"@type":"NRID","@value":"9000254262874"},{"@type":"NRID","@value":"9000254262262"},{"@type":"NRID","@value":"9000254262275"},{"@type":"NRID","@value":"9000254741787"},{"@type":"NRID","@value":"9000405103777"},{"@type":"NRID","@value":"9000405521311"},{"@type":"NRID","@value":"9000014140037"},{"@type":"NRID","@value":"9000016835652"},{"@type":"NRID","@value":"9000024133117"},{"@type":"NRID","@value":"9000391400901"},{"@type":"NRID","@value":"9000254270909"},{"@type":"NRID","@value":"9000254262395"},{"@type":"NRID","@value":"9000411621709"},{"@type":"NRID","@value":"9000299513427"},{"@type":"NRID","@value":"9000000931512"},{"@type":"NRID","@value":"9000023738402"},{"@type":"NRID","@value":"9000413694875"},{"@type":"NRID","@value":"9000397969348"},{"@type":"NRID","@value":"9000391403778"},{"@type":"NRID","@value":"9000408484410"},{"@type":"NRID","@value":"9000006241187"},{"@type":"NRID","@value":"9000404679282"},{"@type":"NRID","@value":"9000254741736"},{"@type":"NRID","@value":"9000018493821"},{"@type":"NRID","@value":"9000009700397"},{"@type":"NRID","@value":"9000019055012"},{"@type":"NRID","@value":"9000023769998"},{"@type":"NRID","@value":"9000023618599"},{"@type":"NRID","@value":"9000406034850"},{"@type":"NRID","@value":"9000391403826"},{"@type":"NRID","@value":"9000391401435"},{"@type":"NRID","@value":"9000254754012"},{"@type":"NRID","@value":"9000254263027"},{"@type":"NRID","@value":"9000018621946"},{"@type":"NRID","@value":"9000000931355"},{"@type":"NRID","@value":"9000398128080"},{"@type":"NRID","@value":"9000370763591"},{"@type":"NRID","@value":"9000391401467"},{"@type":"NRID","@value":"9000254741488"},{"@type":"NRID","@value":"9000399763390"},{"@type":"NRID","@value":"9000241836780"},{"@type":"NRID","@value":"9000023757795"},{"@type":"NRID","@value":"9000329897341"},{"@type":"NRID","@value":"9000409470212"},{"@type":"NRID","@value":"9000409470230"},{"@type":"NRID","@value":"9000254262312"},{"@type":"NRID","@value":"9000410320304"},{"@type":"NRID","@value":"9000241208979"},{"@type":"NRID","@value":"9000016787972"},{"@type":"NRID","@value":"9000256898259"},{"@type":"NRID","@value":"9000023730730"},{"@type":"NRID","@value":"9000397969380"},{"@type":"NRID","@value":"9000391404680"},{"@type":"NRID","@value":"9000391403675"},{"@type":"NRID","@value":"9000254754141"},{"@type":"NRID","@value":"9000254262388"},{"@type":"NRID","@value":"9000391401353"},{"@type":"NRID","@value":"9000345427943"},{"@type":"NRID","@value":"9000254753991"},{"@type":"NRID","@value":"9000000767630"},{"@type":"NRID","@value":"9000000931412"},{"@type":"NRID","@value":"9000391401082"},{"@type":"NRID","@value":"9000391406207"},{"@type":"NRID","@value":"9000000093589"},{"@type":"NRID","@value":"9000006227892"},{"@type":"NRID","@value":"9000254262910"},{"@type":"NRID","@value":"9000254262865"},{"@type":"NRID","@value":"9000254741449"},{"@type":"NRID","@value":"9000399560486"},{"@type":"NRID","@value":"9000279888051"},{"@type":"NRID","@value":"9000382633918"},{"@type":"NRID","@value":"9000408575960"},{"@type":"NRID","@value":"9000397829049"},{"@type":"NRID","@value":"9000020942665"},{"@type":"NRID","@value":"9000397829028"},{"@type":"NRID","@value":"9000412040960"},{"@type":"NRID","@value":"9000376548183"},{"@type":"NRID","@value":"9000000767610"},{"@type":"NRID","@value":"9000000931373"},{"@type":"NRID","@value":"9000254263125"},{"@type":"NRID","@value":"9000344119288"},{"@type":"NRID","@value":"9000388508124"},{"@type":"NRID","@value":"9000292870776"},{"@type":"NRID","@value":"9000241821357"},{"@type":"NRID","@value":"9000256898265"},{"@type":"NRID","@value":"9000023944794"},{"@type":"NRID","@value":"9000391400861"},{"@type":"NRID","@value":"9000391403485"},{"@type":"NRID","@value":"9000409996417"},{"@type":"NRID","@value":"9000241830728"},{"@type":"NRID","@value":"9000375914881"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/iio"}],"foaf:name":[{"@value":"Yoshihisa Iio"}],"jpcoar:affiliationName":[{"@value":"Research Center for Earthquake Prediction, Disaster Prevention Research Institute Kyoto University  Uji, Kyoto 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":"2008-08","prism:volume":"113","prism:number":"B8","prism:startingPage":"B08415"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2007JB005361"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2007JB005361"}],"createdAt":"2008-08-26","modifiedAt":"2023-09-25","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004230122316544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Two‐dimensional viscosity structure of the northeastern Japan islands arc‐trench system"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523299840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological structure of northeastern Japan lithosphere based on geophysical observations and rock mechanics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711231218944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of late Cenozoic magmatism and the crust–mantle structure in the NE Japan Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179757965312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Heterogeneous stress state of island arc crust in northeastern Japan affected by hot mantle fingers"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180316129664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological Structure Beneath NE Japan Inferred from Coseismic Strain Anomalies Associated with the 2011 Tohoku-oki Earthquake (Mw9.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303055616","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Process by Which Intraplate Earthquakes Are Generated"},{"@language":"ja","@value":"内陸地震の発生過程"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238343808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geologic structure and late Cenozoic evolution of the Hokuriku and Shin’etsu regions, north-central Japan"},{"@language":"ja","@value":"北陸および信越地域における後期新生代の地質構造発達史"},{"@language":"ja-Kana","@value":"ホクリク オヨビ シンエツチイキ ニ オケル コウキ シンセイダイ ノ チシツ コウゾウ ハッタツシ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240339712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rheological profile across the northeastern Japan lithosphere toward precise modeling of the 2011 Tohoku Oki Earthquake"},{"@language":"ja","@value":"東日本太平洋沖地震後の余効変動解析へ向けた東北日本弧レオロジー断面"},{"@language":"ja-Kana","@value":"ヒガシニホン タイヘイヨウオキ ジシン ゴ ノ ヨコウヘンドウ カイセキ エ ムケタ トウホク ニホン コ レオロジー ダンメン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240400128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Modeling of crustal deformation and fault development in the Ou Backbone range and the midNiigata region: Toward an understanding of the mechanisms of large inland earthquakes"},{"@language":"ja","@value":"奥羽脊梁山脈周辺および中越地域における地殻の変形と断層形成過程のモデル化: 内陸大地震発生過程解明に向けて"},{"@language":"ja-Kana","@value":"オウウ セキリョウ サンミャク シュウヘン オヨビ チュウエツ チイキ ニ オケル チカク ノ ヘンケイ ト ダンソウ ケイセイ カテイ ノ モデルカ : ナイリク ダイジシン ハッセイ カテイ カイメイ ニ ムケテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001277392978688","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Modeling Deformation and Stress States in the Island-arc Crust Considering Heterogeneous Rheological Structure"},{"@language":"ja","@value":"不均質レオロジー構造を考慮した島弧地殻における変形と応力場のモデル化"},{"@language":"ja-Kana","@value":"フキンシツ レオロジー コウゾウ オ コウリョ シタ トウコ チカク ニ オケル ヘンケイ ト オウリョクジョウ ノ モデルカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390294045393167872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strain-rate Field of Japan Estimated from GNSS Data and Its Interpretation Based on Inter- and Intra-arc Deformation"},{"@language":"ja","@value":"GNSSデータに基づく日本列島の歪み速度場と島弧間および島弧内変動"},{"@language":"ja-Kana","@value":"GNSS データ ニ モトズク ニホン レットウ ノ ヒズミ ソクドジョウ ト トウコ カン オヨビ トウコ ナイ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390567172584432256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Cenozoic Igneous Activity and Crustal Structure in the NE Japan Arc: Background of Inland Earthquake Activity"},{"@language":"ja","@value":"東北日本弧における後期新生代の火成活動と地殻構造"},{"@value":"東北日本弧における後期新生代の火成活動と地殻構造 : 内陸地震活動の背景"},{"@language":"ja-Kana","@value":"トウホク ニホン コ ニ オケル コウキ シンセイダイ ノ カセイカツドウ ト チカク コウゾウ : ナイリク ジシン カツドウ ノ ハイケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942184938624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic evidence of viscoelastic relaxation after the 2008 Iwate-Miyagi Nairiku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417117561472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"(U–Th)/He thermochronometric mapping across the northeast Japan Arc : towards understanding mountain building in an island-arc setting"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317034586368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Consistent estimation of strain-rate fields from GNSS velocity data using basis function expansion with ABIC"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2007jb005361"},{"@type":"OPENAIRE","@value":"doi_dedup___::af09d03b77d3c4f42130a7d14411e4ed"},{"@type":"CROSSREF","@value":"10.1002/grl.50906_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.5047/eps.2012.04.001_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2011.03.002_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.5575/geosoc.116.624_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0026_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.5026/jgeography.131.479_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.1002/2015jb012664_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.1007/1345_2015_135_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.5026/jgeography.128.813_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.529_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01474-5_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2011.0007_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.365_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01151-z_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"},{"@type":"CROSSREF","@value":"10.1144/sp385.15_references_DOI_KkfmtIo7MG4U00ZHf2h6MlHm50f"}]}