{"@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/1360004233288308864.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011gl049729"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL049729"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011GL049729"}},{"identifier":{"@type":"NAID","@value":"20000996015"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Stress before and after the 2011 great Tohoku‐oki earthquake and induced earthquakes in inland areas of eastern Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Stress fields in inland areas of eastern Japan before and after the Tohoku‐oki earthquake were estimated by inverting focal mechanism data. Before the earthquake,<jats:italic>σ</jats:italic><jats:sub>1</jats:sub>axis was oriented EW in Tohoku but NW‐SE in Kanto‐Chubu. The stress fields changed after the earthquake in northern Tohoku and in southeastern Tohoku near Iwaki city, where the orientations of the principal stresses became approximately the same as the orientations of the static stress change associated with the earthquake. This indicates that differential stress magnitudes in these areas before the earthquake were smaller than 1 MPa. The stress field did not change in central Tohoku, even though the stresses loaded after the earthquake had nearly reversed orientations, which indicates that the differential stress magnitudes there were significantly larger than 1 MPa. In Kanto‐Chubu, stresses having nearly the same orientations as the background stresses were loaded after the earthquake, and the stress fields did not change as expected. This may have caused very high induced seismicities in Kanto‐Chubu.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004233288308740","@type":"Researcher","foaf:name":[{"@value":"Keisuke Yoshida"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288308873","@type":"Researcher","foaf:name":[{"@value":"Akira Hasegawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326219191680","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"30281968"},{"@type":"NRID","@value":"1000030281968"},{"@type":"ORCID","@value":"0000-0002-0334-279X"},{"@type":"NRID","@value":"9000020970954"},{"@type":"NRID","@value":"9000254262646"},{"@type":"NRID","@value":"9000254262652"},{"@type":"NRID","@value":"9000284268603"},{"@type":"NRID","@value":"9000254741781"},{"@type":"NRID","@value":"9000254262900"},{"@type":"NRID","@value":"9000254262643"},{"@type":"NRID","@value":"9000410904518"},{"@type":"NRID","@value":"9000410320352"},{"@type":"NRID","@value":"9000000119743"},{"@type":"NRID","@value":"9000001212862"},{"@type":"NRID","@value":"9000408484407"},{"@type":"NRID","@value":"9000005191168"},{"@type":"NRID","@value":"9000254741743"},{"@type":"NRID","@value":"9000001212872"},{"@type":"NRID","@value":"9000023611239"},{"@type":"NRID","@value":"9000409470223"},{"@type":"NRID","@value":"9000258414494"},{"@type":"NRID","@value":"9000018699101"},{"@type":"NRID","@value":"9000388538969"},{"@type":"NRID","@value":"9000008300536"},{"@type":"NRID","@value":"9000018369126"},{"@type":"NRID","@value":"9000238038283"},{"@type":"NRID","@value":"9000254741829"},{"@type":"NRID","@value":"9000279888034"},{"@type":"NRID","@value":"9000254741756"},{"@type":"NRID","@value":"9000254708737"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0211901"}],"foaf:name":[{"@value":"Tomomi Okada"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288308868","@type":"Researcher","foaf:name":[{"@value":"Takeshi Iinuma"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288308866","@type":"Researcher","foaf:name":[{"@value":"Yoshihiro Ito"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288308741","@type":"Researcher","foaf:name":[{"@value":"Youichi Asano"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2012-02","prism:volume":"39","prism:number":"3","prism:startingPage":"L03302"},"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%2F2011GL049729"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011GL049729"}],"createdAt":"2012-01-06","modifiedAt":"2023-10-30","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257039539456","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21109002"},{"@type":"JGN","@value":"JP21109002"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PLANNED-21109002/"}],"notation":[{"@language":"ja","@value":"地震波で診る地殻流体"},{"@language":"en","@value":"Geofluid investigated from seismic waves"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335851749248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Experimental and numerical investigation of the temperature response to stress changes of rocks"}]},{"@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 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