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dc.contributor.author入倉, 孝次郎ja
dc.contributor.author赤松, 純平ja
dc.contributor.author松波, 孝治ja
dc.contributor.alternativeIRIKURA, Kojiroen
dc.contributor.alternativeAKAMATSU, Junpeien
dc.contributor.alternativeMATSUNAMI, Kojien
dc.date.accessioned2009-01-30T05:07:52Z-
dc.date.available2009-01-30T05:07:52Z-
dc.date.issued1975-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70018-
dc.description.abstractMicrotremors were observed at the earthquake-observational points on the ground andthe rock and at several points in the vicinity of the observational points. The peak frequenciesand amplitudes of the spectra of the microtremors vary with the thickness of the depositlayers. However, the peak frequencies of microtremors are not consistent with those ofspectral ratios of S waves between the ground motions and the rock motions. This is partlydue to the difference of the length of time window for computation of spectra. Moreover, the difference of the nature of microtremors with that of earthquake motions should heconsidered in estimating amplification characteristics of ground motions.en
dc.format.mimetypeapplication/pdf-
dc.language.isojpn-
dc.publisher京都大学防災研究所ja
dc.publisher.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.subject.ndc453-
dc.subject.ndc511.27-
dc.title地盤による地震波の震動特性と雑微動特性の比較ja
dc.title.alternativeCOMPARISON OF EARTHQUAKE GROUND MOTIONS AND MICROTREMORSen
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN00027784-
dc.identifier.jtitle京都大学防災研究所年報. Bja
dc.identifier.volume18-
dc.identifier.issueB-
dc.identifier.spage1-
dc.identifier.epage9-
dc.textversionpublisher-
dc.sortkey01-
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html-
dcterms.accessRightsopen access-
dc.identifier.pissn0386-412X-
dc.identifier.jtitle-alternativeDisaster Prevention Research Institute Annuals. Ben
出現コレクション:No.18 B

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