{"@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/1050845760653604352.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"HDL","@value":"http://hdl.handle.net/2433/147266"}},{"identifier":{"@type":"DOI","@value":"10.1029/2011gl048800"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048800"}},{"identifier":{"@type":"URI","@value":"http://www.agu.org/journals/gl/gl1117/2011GL048800/2011GL048800.pdf"}},{"identifier":{"@type":"NAID","@value":"80022178291"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@language":"en","@value":"Near-surface weakening in Japan after the 2011 Tohoku-Oki earthquake"}],"dc:language":"en","description":[{"notation":[{"@value":"[1] The magnitude (MW) 9.0 Tohoku-Oki earthquake on 11 March 2011 was one of the largest in recent history. Ground motion caused by the seismicity around the time of the main shock was recorded by KiK-net, the strong-motion network that covers most of Japan. By deconvolving waveforms generated by earthquakes that are recorded at the surface and in a borehole at KiK-net station FKSH18, we detect a reduction of shear-wave velocity in the upper 100 m of about 10%, and a subsequent healing that varies logarithmically with time. Using all available borehole and surface records of more than 300 earthquakes that occurred between 1 January 2011 and 26 May 2011, we observe a reduction in the shear-wave velocity of about 5% in the upper few hundred meters after the Tohoku-Oki earthquake throughout northeastern Japan. The area of the velocity reduction is about 1,200 km wide, which is much wider than earlier studies reporting velocity reductions following other larger earthquakes. The reduction of the shear-wave velocity is an indication that the shear modulus, and hence the shear strength, is reduced over a large part of Japan."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1030862623798958592","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000017396882"}],"foaf:name":[{"@language":"en","@value":"Nakata, N."},{"@language":"ja","@value":"仲田, 典弘"}]},{"@id":"https://cir.nii.ac.jp/crid/1070845760653604352","@type":"Researcher","foaf:name":[{"@language":"en","@value":"Snieder, R."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"},{"@type":"NCID","@value":"AA00657102"}],"prism:publicationName":[{"@language":"en","@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union"}],"prism:publicationDate":"2011-09-02","prism:volume":"38","prism:number":"17","prism:startingPage":"n/a","prism:endingPage":"n/a"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["©2011. American Geophysical Union.","This is not the published version. Please cite only the published version.","この論文は出版社版でありません。引用の際には出版社版をご確認ご利用ください。"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011GL048800"},{"@id":"http://www.agu.org/journals/gl/gl1117/2011GL048800/2011GL048800.pdf"},{"@id":"http://hdl.handle.net/2433/147266"}],"foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=KiK-net","dc:title":"KiK-net"},{"@id":"https://cir.nii.ac.jp/all?q=near%20surface","dc:title":"near surface"},{"@id":"https://cir.nii.ac.jp/all?q=seismic%20interferometry","dc:title":"seismic interferometry"},{"@id":"https://cir.nii.ac.jp/all?q=shear-wave%20velocity","dc:title":"shear-wave velocity"}],"dcterms:subject":[{"subjectScheme":"Other","notation":[{"@language":"en","@value":"KiK-net"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"near surface"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"seismic interferometry"}]},{"subjectScheme":"Other","notation":[{"@language":"en","@value":"shear-wave velocity"}]}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257464854272","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"10J05857"},{"@type":"JGN","@value":"JP10J05857"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-10J05857/"}],"notation":[{"@language":"ja","@value":"地震波干渉法を用いたHi-netデータによる三次元構造解析と時間差調査手法開発"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202178012032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temporal changes of subsurface velocities during strong shaking as seen from seismic interferometry"}]},{"@id":"https://cir.nii.ac.jp/crid/1050001202726471680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional structure of V_p, V_s, and V_p/V_s beneath northeastern Japan: Implications for arc magmatism and 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low-frequency earthquakes in the Nankai subduction zone and application to the 2016<i>M</i>w 5.9 off-Kii Peninsula earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050856995323429760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evidence of Dynamic Crustal Deformation in Tohoku, Japan, From Time‐Varying Receiver Functions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709047552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimating near‐surface shear wave velocities in Japan by applying seismic interferometry to KiK‐net data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216709540480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temporal change in shear velocity and polarization anisotropy related to the 2011 M9.0 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Japan"},{"@language":"ja","@value":"2011年4月11日福島県いわき市付近で発生した地震（M7）の余震に伴う地下水位変動"},{"@language":"ja-Kana","@value":"2011ネン 4ガツ 11ニチ フクシマケン イワキシ フキン デ ハッセイ シタ ジシン(M7)ノ ヨシン ニ トモナウ チカ スイイ ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206495136512","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地震波干渉法を用いた近地自然地震Pコーダ波による地殻構造探査"},{"@language":"en","@value":"Subsurface exploration with P-coda of local earthquakes using seismic interferometry"},{"@language":"ja-Kana","@value":"ジシンハ カンショウホウ オ モチイタ キン チ シゼン ジシン Pコーダハ ニ ヨル チカク コウゾウ タンサ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512426624","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent progress of seismic observation networks in Japan"},{"@value":"Recent progress of seismic observation networks in Japan--Hi-net, F-net, K-NET and KiK-net"},{"@value":"Recent progress of seismic observation networks in Japan —Hi-net, F-net, K-NET 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