{"@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/1360292621189464320.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2014gl059425"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2014GL059425"}}],"dc:title":[{"@value":"Long-period seismic amplification in the Kanto Basin from the ambient seismic field"}],"description":[{"notation":[{"@value":"Tokyo, like many seismically threatened cities, is situated atop a sedimentary basin that has the potential to trap and amplify seismic waves from earthquakes. We study amplification in the Kanto Basin by exploiting the information carried by the ambient seismic field. We use 375 seismic stations from the high sensitivity seismograph network across central Honshu as virtual sources and 296 seismic stations of the Metropolitan Seismic Observation network shallow borehole seismometers within the basin as receivers to map the basin response. We find a linear relationship between ground motion and basin depth at periods of 2–10 s that could be used to represent 3-D basin effects in ground motion prediction equations. We also find that the strength of basin seismic amplification depends strongly on the direction of illumination by seismic waves."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380292621189464321","@type":"Researcher","foaf:name":[{"@value":"Marine A. Denolle"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics; Stanford University; Stanford California USA"},{"@value":"Scripps Institute of Oceanography; UCSD; San Diego California USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292621189464324","@type":"Researcher","foaf:name":[{"@value":"Hiroe Miyake"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute; University of Tokyo; Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292621189464322","@type":"Researcher","foaf:name":[{"@value":"Shigeki Nakagawa"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute; University of Tokyo; Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292621189464320","@type":"Researcher","foaf:name":[{"@value":"Naoshi Hirata"}],"jpcoar:affiliationName":[{"@value":"Earthquake Research Institute; University of Tokyo; Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380292621189464323","@type":"Researcher","foaf:name":[{"@value":"Gregory C. Beroza"}],"jpcoar:affiliationName":[{"@value":"Department of Geophysics; Stanford University; Stanford California USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2014-04-04","prism:volume":"41","prism:number":"7","prism:startingPage":"2319","prism:endingPage":"2325"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://doi.wiley.com/10.1002/tdm_license_1.1"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2014GL059425"}],"createdAt":"2014-03-21","modifiedAt":"2023-07-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335849396864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Surface wave group velocity in the Osaka sedimentary basin, Japan, estimated using ambient noise cross-correlation functions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565167509920512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Beyond basin resonance: characterizing wave propagation using a dense array and the ambient seismic field"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580232138931968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Multimodal Rayleigh and Love Wave Joint Inversion for S‐Wave Velocity Structures in Kanto Basin, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654738589952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismic wavefield imaging of long‐period ground motion in the Tokyo metropolitan area, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390010292494410624","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"PROPAGATION CHARACTERISTIC OF THE BASIN EDGE INDUCED WAVE AT THE WESTERN EDGE OF THE KANTO BASIN OBSERVED FROM THE CONTINUOUS RECORD OF MeSO-net"},{"@language":"ja","@value":"MeSO-net連続地震観測記録にみられる関東平野西端部による盆地端部生成波の伝播特性"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/2014gl059425"},{"@type":"OPENAIRE","@value":"doi_dedup___::4eef343ebaa6640df3c3519ce3cb59f5"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0694-3_references_DOI_Rse2YXMJl4AQIjdVAOgm3BZV6fB"},{"@type":"CROSSREF","@value":"10.1093/gji/ggw205_references_DOI_Rse2YXMJl4AQIjdVAOgm3BZV6fB"},{"@type":"CROSSREF","@value":"10.1029/2022jb025017_references_DOI_AKWqDbKqKfBERcTdaaPSdq09eo3"},{"@type":"CROSSREF","@value":"10.1002/2017jb014276_references_DOI_Rse2YXMJl4AQIjdVAOgm3BZV6fB"},{"@type":"CROSSREF","@value":"10.3130/aijs.87.251_references_DOI_Rse2YXMJl4AQIjdVAOgm3BZV6fB"}]}