{"@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/1360004233288177792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011gl048432"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048432"}},{"identifier":{"@type":"URI","@value":"http://www.agu.org/journals/gl/gl1116/2011GL048432/2011GL048432.pdf"}},{"identifier":{"@type":"DOI","@value":"10.1029/2011gl048754"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048754"}},{"identifier":{"@type":"URI","@value":"http://www.agu.org/journals/gl/gl1116/2011GL048754/2011GL048754.pdf"}},{"identifier":{"@type":"NAID","@value":"20000546933"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Seismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquake"}],"dcterms:alternative":[{"@value":"HYDRATED FAULT AND INTRASLAB EARTHQUAKES"}],"description":[{"notation":[{"@value":"[1] We determine the focal mechanisms of earthquakes within the Philippine Sea slab beneath the Tokyo metropolitan area, and perform stress tensor inversions to investigate the detailed stress field within the slab. The results show a characteristic spatial variation in earthquake-generating stress. Slab stress in northeastern part of the PHS slab is characterized by down-dip tension (DDT), except for the uppermost tip of the seismic portion of the slab where down-dip compression (DDC) stress is dominant. We interpret that DDT is caused by the net slab pull and DDC is attributable to local resistance to subduction at the tip of the slab. In southwestern part of the PHS slab, σ1 and σ3 are generally rotated oblique to the dip of the slab, suggesting that earthquakes occur under stress conditions of neither DDC nor DDT. The rotations in σ1 and σ3 may be related to stress accumulation by the slip deficit along the asperity of the 1923 Kanto earthquake (M7.9)."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420845751160606592","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30361067"},{"@type":"NRID","@value":"1000030361067"},{"@type":"NRID","@value":"9000002427899"},{"@type":"NRID","@value":"9000254262653"},{"@type":"NRID","@value":"9000257916804"},{"@type":"NRID","@value":"9000331096686"},{"@type":"NRID","@value":"9000018699099"},{"@type":"NRID","@value":"9000254263590"},{"@type":"NRID","@value":"9000238038282"},{"@type":"NRID","@value":"9000001756845"},{"@type":"NRID","@value":"9000279888035"},{"@type":"NRID","@value":"9000254741159"},{"@type":"NRID","@value":"9000002108619"},{"@type":"NRID","@value":"9000014235008"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0200817"}],"foaf:name":[{"@value":"Junichi Nakajima"}],"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/1380004233288177800","@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/1420845751158693376","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"10543449"},{"@type":"NRID","@value":"1000010543449"},{"@type":"NRID","@value":"9000001674541"},{"@type":"NRID","@value":"9000019055168"},{"@type":"NRID","@value":"9000303163725"},{"@type":"NRID","@value":"9000361706721"},{"@type":"NRID","@value":"9000238038280"},{"@type":"NRID","@value":"9000256898263"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0154961"}],"foaf:name":[{"@value":"Saeko Kita"}],"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":"00948276"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2011-04","prism:volume":"38","prism:number":"7","prism:startingPage":"n/a","prism:endingPage":"n/a"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048432"},{"@id":"http://www.agu.org/journals/gl/gl1116/2011GL048432/2011GL048432.pdf"},{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048754"},{"@id":"http://www.agu.org/journals/gl/gl1116/2011GL048754/2011GL048754.pdf"}],"createdAt":"2011-08-08","modifiedAt":"2021-07-21","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782109827200","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22340126"},{"@type":"JGN","@value":"JP22340126"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22340126/"}],"notation":[{"@language":"ja","@value":"スラブ沈み込みに伴う日本列島下の温度分布・物質循環と地震学的微細構造の関連性"},{"@language":"en","@value":"Relationship between temperature distributions and material circulation associated with subduction of oceanic plates and seismological detailed structures beneath the Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782182428032","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23740329"},{"@type":"JGN","@value":"JP23740329"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23740329/"}],"notation":[{"@language":"ja","@value":"北海道下における島弧衝突過程とそれに伴う太平洋スラブの変形機構の解明"},{"@language":"en","@value":"Examination of the Arc-arc collision process and its relationship with deformation mechanism of the Pacific slab, beneath the 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