{"@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/1360004233288139392.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011gl047834"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL047834"}},{"identifier":{"@type":"URI","@value":"http://www.agu.org/journals/gl/gl1115/2011GL047834/2011GL047834.pdf"}},{"identifier":{"@type":"HANDLE","@value":"1912/4791"}},{"identifier":{"@type":"NAID","@value":"10030553653"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Widespread seismicity excitation throughout central Japan following the 2011 M=9.0 Tohoku earthquake and its interpretation by Coulomb stress transfer"}],"dcterms:alternative":[{"@value":"WIDESPREAD SEISMICITY AFTER TOHOKU QUAKE"}],"description":[{"notation":[{"@value":"[1] We report on a broad and unprecedented increase in seismicity rate following the M=9.0 Tohoku mainshock for M ≥ 2 earthquakes over inland Japan, parts of the Japan Sea and Izu islands, at distances of up to 425 km from the locus of high (≥15 m) seismic slip on the megathrust. Such an increase was not seen for the 2004 M=9.1 Sumatra or 2010 M=8.8 Chile earthquakes, but they lacked the seismic networks necessary to detect such small events. Here we explore the possibility that the rate changes are the product of static Coulomb stress transfer to small faults. We use the nodal planes of M ≥ 3.5 earthquakes as proxies for such small active faults, and find that of fifteen regions averaging ∼80 by 80 km in size, 11 show a positive association between calculated stress changes and the observed seismicity rate change, 3 show a negative correlation, and for one the changes are too small to assess. This work demonstrates that seismicity can turn on in the nominal stress shadow of a mainshock as long as small geometrically diverse active faults exist there, which is likely quite common."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420282801190373376","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"80313047"},{"@type":"NRID","@value":"1000080313047"},{"@type":"NRID","@value":"9000291605309"},{"@type":"NRID","@value":"9000019055002"},{"@type":"NRID","@value":"9000365088019"},{"@type":"NRID","@value":"9000347361372"},{"@type":"NRID","@value":"9000402807897"},{"@type":"NRID","@value":"9000018698297"},{"@type":"NRID","@value":"9000406193542"},{"@type":"NRID","@value":"9000399560505"},{"@type":"NRID","@value":"9000398156124"},{"@type":"NRID","@value":"9000391405368"},{"@type":"NRID","@value":"9000345299693"},{"@type":"NRID","@value":"9000412590801"},{"@type":"NRID","@value":"9000411245133"},{"@type":"NRID","@value":"9000018698292"},{"@type":"NRID","@value":"9000018698291"},{"@type":"NRID","@value":"9000018657133"},{"@type":"NRID","@value":"9000283342011"},{"@type":"NRID","@value":"9000414942953"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000004459"}],"foaf:name":[{"@value":"Shinji Toda"}],"jpcoar:affiliationName":[{"@value":"Disaster Prevention Research Institute; Kyoto University; Kyoto Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288139520","@type":"Researcher","foaf:name":[{"@value":"Ross S. Stein"}],"jpcoar:affiliationName":[{"@value":"U.S. Geological Survey; Menlo Park California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004233288139400","@type":"Researcher","foaf:name":[{"@value":"Jian Lin"}],"jpcoar:affiliationName":[{"@value":"Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA"}]}],"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%2F2011GL047834"},{"@id":"http://www.agu.org/journals/gl/gl1115/2011GL047834/2011GL047834.pdf"}],"createdAt":"2011-08-05","modifiedAt":"2024-04-09","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Central%20Japan","dc:title":"Central Japan"},{"@id":"https://cir.nii.ac.jp/all?q=Coulomb%20stress","dc:title":"Coulomb stress"},{"@id":"https://cir.nii.ac.jp/all?q=Seismicity%20excitation","dc:title":"Seismicity excitation"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257119887232","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23240039"},{"@type":"JGN","@value":"JP23240039"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23240039/"}],"notation":[{"@language":"ja","@value":"地震活動異常を診断する統計的時空間モデルと確率利得を上げる実効的予測の戦略的研究"},{"@language":"en","@value":"Strategic research of effective prediction to increase the probability gain statistical space-time model for diagnosing abnormal seismic activity"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202548410112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Remote triggering of seismicity at Japanese volcanoes following the 2016 M7.3 Kumamoto earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001339269691776","@type":"Article","resourceType":"学術雑誌論文(journal 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Japan, after the 2011 Off the Pacific Coast of Tohoku Earthquake"},{"@language":"ja","@value":"2011年東北地方太平洋沖地震の発生後に活発化した霞ヶ浦南端直下の正断層型地震活動"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305619072","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2011年3月15日静岡県東部地震（Mj6.4）の遅れ誘発過程に関する研究"},{"@language":"en","@value":"Delayed Triggering Process for the Mj6.4 Eastern Shizuoka Earthquake of 15 March 2011"},{"@language":"ja-Kana","@value":"2011ネン 3ガツ 15ニチ シズオカケン トウブ ジシン(Mj6.4)ノ オクレ ユウハツ カテイ ニ カンスル ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206240399104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Current issues and a prospective view to the next step for long-term crustal earthquake forecast in Japan"},{"@language":"ja","@value":"内陸地震の長期評価に関する課題と新たな視点"},{"@language":"ja-Kana","@value":"ナイリク ジシン ノ チョウキ ヒョウカ ニ カンスル カダイ ト アラタ ナ 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