{"@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/1361137044189686272.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.tecto.2005.06.013"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195105005731?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195105005731?httpAccept=text/plain"}}],"dc:title":[{"@value":"Repeating earthquake activities associated with the Philippine Sea plate subduction in the Kanto district, central Japan: A new plate configuration revealed by interplate aseismic slips"}],"description":[{"notation":[{"@value":"Abstract   We detect repeating earthquakes associated with the Philippine Sea plate subduction to reveal the plate configuration. In the Kanto district, we find 140 repeating earthquake groups with 428 events by waveform similarity analysis. Most repeating earthquakes in the eastern part of the Kanto district occur with a regular time interval. They have thrust-type focal mechanisms and are distributed near the upper surface of the Philippine Sea plate. These observations indicate that the repeating earthquakes there occur as a repetition of ruptures on the isolated patches distributed on the plate boundary owing to the concentration of stress caused by aseismic slips in the surrounding areas. This shows that the distributions of repeating earthquakes suggest the aseismic slips in the surrounding areas of small patches. We determine spatial distributions of repeating earthquakes in the eastern part of the Kanto district and find that they correspond to the upper boundary of the Philippine Sea plate, that is, the upper boundary of the oceanic crust layer of the Philippine Sea plate. The plate geometry around Choshi is newly constrained by repeating earthquake data and a rather flat geometry in the eastern part of the Kanto district is revealed. The obtained geometry suggests uplift of the Philippine Sea plate due to the collision with the Pacific plate beneath Choshi.  Repeating earthquakes in the western part of the Kanto district have extremely shorter recurrence times, and their focal mechanisms are not of the thrust types. These repeating earthquakes are classified as “burst type” activity and likely to occur on the preexistent fault planes which are distributed around the “collision zone” between the Philippine Sea plate and the inland plate. The variation among the repeating earthquake activities in the Kanto district indicates that regular repetition of repeating earthquakes is possible only on the plate boundary with a smooth and simple geometry."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137044189686275","@type":"Researcher","foaf:name":[{"@value":"Hisanori Kimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044189686273","@type":"Researcher","foaf:name":[{"@value":"Keiji Kasahara"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044189686274","@type":"Researcher","foaf:name":[{"@value":"Toshihiro Igarashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044189686272","@type":"Researcher","foaf:name":[{"@value":"Naoshi Hirata"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2006-04","prism:volume":"417","prism:number":"1-2","prism:startingPage":"101","prism:endingPage":"118"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0040195105005731?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195105005731?httpAccept=text/plain"}],"createdAt":"2006-01-05","modifiedAt":"2023-05-06","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050856995322727808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Configuration and structure of the Philippine Sea Plate off Boso, Japan: constraints on the shallow subduction kinematics, seismicity, and slow slip events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229801884928","@type":"Article","resourceType":"学術雑誌論文(journal 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rate"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708262632832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Supraslab earthquake clusters above the subduction plate boundary offshore Sanriku, northeastern Japan: Seismogenesis in a graveyard of detached seamounts?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285711273633920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Repeating Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298341430855936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic reflection imaging of deep crustal structures using local earthquakes in the Kanto region, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565164302412416","@type":"Article","resourceType":"学術雑誌論文(journal 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spatial variations of seismic reflection intensity of the upper surface of the Philippine Sea plate off the Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654732797568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in seismicity and stress loading on subduction faults in the Kanto region, Japan, 2011–2014"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657254682240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Complex slab structure and arc magmatism beneath the Japanese Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204304147456","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Three-Dimensional Velocity Structure and Configuration of the Philippine Sea Slab beneath Kanto District, Central Japan, Estimated by Double-Difference Tomography"},{"@language":"ja","@value":"Double-Difference Tomography法による関東地方の3次元地震波速度構造およびフィリピン海プレートの形状の推定"},{"@language":"ja-Kana","@value":"Double Difference Tomographyホウ ニ ヨル カントウ チホウ ノ 3ジゲン ジシンハ ソクド コウゾウ オヨビ フィリピンカイ プレート ノ ケイジョウ ノ スイテイ"}]},{"@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 Changes?"},{"@language":"ja","@value":"地震活動変化から何を読み解くか？"},{"@value":"地震活動変化から何を読み解くか?--プレート境界地震のアスペリティの特定"},{"@language":"ja-Kana","@value":"ジシン カツドウ ヘンカ カラ ナニ オ ヨミ トク カ プレート キョウカイ ジシン ノ アスペリティ ノ 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