{"@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/1363388844295300736.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2001gl014632"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2001GL014632"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001GL014632"}}],"dc:title":[{"@value":"Characteristic small‐earthquake sequence off Sanriku, northeastern Honshu, Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We found eight similar earthquakes of <jats:italic>M</jats:italic>4.8 regularly occurring from 1957 to 1995 on the plate boundary off Sanriku, northeastern Japan. The mean recurrence interval of the events is 5.35 years and its standard deviation is only 0.53 years. These events have the same focal mechanisms of low‐angle thrust fault type and their source sizes are estimated to be around 1 km. The slip of each event is comparable to the cumulative amount of relative plate motion in the inter‐seismic period. Thus, these events are probably caused by repeating slip at a small but strong asperity surrounded by creeping zone on the plate boundary. The next event was expected to occur by the end of November 2001 with 99% probability and actually <jats:italic>M</jats:italic>4.7 event occurred on November 13, 2001.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844295300736","@type":"Researcher","foaf:name":[{"@value":"Toru Matsuzawa"}],"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/1380579818731519232","@type":"Researcher","foaf:name":[{"@value":"Toshihiro Igarashi"}],"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/1380579818731519233","@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"}]}],"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":"2002-06","prism:volume":"29","prism:number":"11","prism:startingPage":"1543"},"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%2F2001GL014632"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2001GL014632"}],"createdAt":"2002-10-27","modifiedAt":"2023-10-31","relatedProduct":[{"@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 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Africa"},{"@language":"ja-Kana","@value":"ミナミアフリカ ダイシンド キンコウザン デ ノ ビショウ ハカイ カンソク ニ ヨル シンゲン ノ ブツリ ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390003825203695104","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repeating Earthquakes Along the Colombian Subduction Zone"},{"@value":"Repeating earthquakes. Along the Colombia subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390006750773490176","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cause of Successive Occurrences of Earthquakes in a Short Time off the Eastern Coast of Osumi Peninsula, Southwestern Japan"},{"@language":"ja","@value":"大隅半島東方沖の一部領域で短時間に地震が連発する原因の考察"},{"@language":"ja-Kana","@value":"オオスミ ハントウ トウホウオキ ノ イチブ リョウイキ デ タンジカン ニ ジシン ガ レンパツ スル ゲンイン ノ コウサツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279701888","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Probabilistic Predictions of Recurrent Earthquakes and Aftershocks"},{"@language":"ja","@value":"繰り返し地震および余震の確率予測"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279703808","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"What Can We Read in Seismic Activity 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ケンショウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489243392","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Introduction to EPS special section for the M7.1 and M6.4 earthquakes in northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390302867852485248","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Repeating Earthquakes in the Continental Crust and Subducting Slabs, and Seismological and Tectonic Implications: Proposal for an Extended Fault-valve Model"},{"@language":"ja","@value":"内陸地殻およびスラブ内の繰り返し地震とその地震学的およびテクトニクス的意義"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845712984151168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"Matched Filter法を用いた2011年東北地方太平洋沖地震直後の小地震の検出"},{"@language":"en","@value":"Detection of Small Earthquakes Using the Matched Filter Method 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