{"@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/1362825895360905088.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03352767"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03352767.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03352767/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03352767"}}],"dc:title":[{"@value":"Crustal deformation associated with the Noto Hanto Earthquake in 2007 in Japan"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n          <jats:p>The Global Positioning System (GPS) network in Japan detected coseismic deformation from the 2007 Noto Hanto earthquake (<jats:italic>M</jats:italic>\n            <jats:sub>w</jats:sub> = 6.9). The result indicates a 21-cm southwestward displacement and a 7-cm upheaval at the GPS site near the epicenter. Synthetic Aperture Interferometry (InSAR) shows an approximately 50-cm movement toward the “Daichi” satellite, in ascending orbit, near the epicenter. The estimated fault slip distribution based on GPS and InSAR results shows a large slip area ranging up to 2 m near and northeast of the hypocenter. The slip area beneath the Sea of Japan southwest of the hypocenter also shows large slippage of around 2 m. Aftershocks are distributed in the asperity area and its vicinity, demonstrating that the asperity hypothesis clearly does not hold completely for this earthquake. Computed vertical displacements using the model are consistent with the geomorphological evidence of long-term uplift.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380006696611325440","@type":"Researcher","foaf:name":[{"@value":"Shinzaburo Ozawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895360905216","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Yarai"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895360905090","@type":"Researcher","foaf:name":[{"@value":"Mikio Tobita"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895360905088","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Une"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895360905091","@type":"Researcher","foaf:name":[{"@value":"Takuya Nishimura"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18805981"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/13438832"}],"prism:publicationName":[{"@value":"Earth, Planets and Space"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2008-02","prism:volume":"60","prism:number":"2","prism:startingPage":"95","prism:endingPage":"98"},"reviewed":"false","dc:rights":["https://creativecommons.org/licenses/by/4.0/","https://creativecommons.org/licenses/by/4.0/"],"url":[{"@id":"https://link.springer.com/content/pdf/10.1186/BF03352767.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03352767/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03352767"}],"createdAt":"2014-08-15","modifiedAt":"2021-09-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050859447951759616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Episodic transient deformation revealed by the analysis of multiple GNSS networks in the Noto Peninsula, central 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aperture radar interferograms"},{"@language":"ja","@value":"ＳＡＲ干渉画像を用いた能登半島地震及び中越沖地震に伴う地表変動の解析"},{"@language":"ja-Kana","@value":"SAR カンショウ ガゾウ オ モチイタ ノト ハントウ ジシン オヨビ チュウエツオキ ジシン ニ トモナウ チヒョウ ヘンドウ ノ カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241022208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic geomorphology and outcrops of the Atotsugawa fault system"},{"@language":"ja","@value":"跡津川断層系の変動地形と断層露頭"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001277365899264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic Landforms and Co-Seismic Uplift in the Southwestern Coastal Area of the Noto Peninsula, Central Japan"},{"@language":"ja","@value":"能登半島南西岸変動地形と地震性隆起"},{"@language":"ja-Kana","@value":"ノト ハントウ ミナミセイガン ヘンドウ チケイ ト ジシンセイ 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