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dc.contributor.author渡辺, 邦彦ja
dc.contributor.author尾池, 和夫ja
dc.contributor.alternativeWATANABE, Kunihikoen
dc.contributor.alternativeOIKE, Kazuoen
dc.date.accessioned2009-03-02T07:53:35Z-
dc.date.available2009-03-02T07:53:35Z-
dc.date.issued1985-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70742-
dc.description.abstractOn May 30th, 1984, an earthquake of M5.6 occurred at the Yamasaki fault. Concerningto this earthquake, precursors, co- and post seismic phenomena of various kinds were observed.Among these, crustal deformations observed by extensometers and tiltmeters were analized.Both the strain and tilt steps were observed. Aftereffects of the ground strain were also recog-nized too.We concluded that these are compound phenomena consisting of both the strain originatedat the hypocentral region and the peculiar local strain effects around the observation site.Besides, it can be regarded that fault zones or fractured zones are "windows for earthquakeprediction", where the signals related to earthquakes frequently appear.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.ndc455.8-
dc.subject.ndc454.4-
dc.title安富観測坑で記録された山崎断層の地震(1984年5月30日, M5.6)にかかわる地殻変動ja
dc.title.alternativeCRUSTAL DEFORMATIONS RELATED TO THE YAMASAKI FAULT EARTHQUAKE ON MAY 30TH, 1984, M5.6, OBSERVED AT THE YASUTOMI OBSERVATION TUNNELen
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.volume28-
dc.identifier.issueB-1-
dc.identifier.spage99-
dc.identifier.epage109-
dc.textversionpublisher-
dc.sortkey11-
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.28 B-1

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