{"@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/1362262945923677440.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.20965/jdr.2013.p0878"}},{"identifier":{"@type":"URI","@value":"https://www.fujipress.jp/main/wp-content/themes/Fujipress/phyosetsu.php?ppno=DSSTR000800050004"}}],"dc:title":[{"@value":"A New Ground Motion Prediction Equation for Japan Applicable up to M9 Mega-Earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>In this study we suggest a new ground motion prediction equation applicable up to the moment magnitude 9 using the strong motion records from the 2011 Tohoku-oki earthquake. We determined a base model with moment magnitude and the shortest distance from the source fault as parameters. In order to avoid overestimating amplitude atmagnitude larger than 8, we examined two models – a quadratic magnitude term and a linear magnitude term with a complete amplitude saturation term at someMw. We then adopt additional correction terms corresponding to amplification by deep sediments or shallow soft soils, and anomalous seismic intensity distribution in order to improve prediction.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262945923677441","@type":"Researcher","foaf:name":[{"@value":"Nobuyuki Morikawa"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945923677440","@type":"Researcher","foaf:name":[{"@value":"Hiroyuki Fujiwara"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"18838030"},{"@type":"PISSN","@value":"18812473"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/18812473"}],"prism:publicationName":[{"@value":"Journal of Disaster Research"}],"dc:publisher":[{"@value":"Fuji Technology Press Ltd."}],"prism:publicationDate":"2013-10-01","prism:volume":"8","prism:number":"5","prism:startingPage":"878","prism:endingPage":"888"},"reviewed":"false","url":[{"@id":"https://www.fujipress.jp/main/wp-content/themes/Fujipress/phyosetsu.php?ppno=DSSTR000800050004"}],"createdAt":"2016-04-14","modifiedAt":"2023-08-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050869456405222272","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Ground motion prediction equation for the Kathmandu Valley, Nepal based on strong motion records during the 2015 Gorkha Nepal earthquake sequence"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168844207488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"An Evaluation of Strong-Motion Parameters at the S-net Ocean-Bottom Seismograph Sites Near the Kanto Basin for Earthquake Early 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