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dc.contributor.author井元, 政二郎ja
dc.contributor.author岸本, 兆方ja
dc.contributor.alternativeIMOTO, Masajiroen
dc.contributor.alternativeKISHIMOTO, Yoshimichien
dc.date.accessioned2009-02-10T01:43:19Z-
dc.date.available2009-02-10T01:43:19Z-
dc.date.issued1977-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70133-
dc.description.abstractIn this paper, we discuss the difference in distributions between larger and smaller after-shocks that followed some large earthquakes with magnitude larger than 7 at trenches of thePacific Ocean. By a method similar to the t-test, it seems probable that the epicenters ofthe smaller shocks are located slightly landward in comparison with those of the larger shocks, especially in South Kuril and Philippine.On the statistic basis mentioned above, epicenters of the main shocks are compared withthose of their aftershocks. It is ascertained that most of epicenters of the main shocks withreversal dip-slip fault are situated iandward, except the events in New Britain Trench andNew Hebrides.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.ndc453.3-
dc.subject.ndc452.8-
dc.title海溝周辺に発生する地震の余震分布に関する一つの検討ja
dc.title.alternativeON A BIAS OF AFTERSHOCK EPICENTERS AT TRENCHES OF THE PACIFIC OCEANen
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.volume20-
dc.identifier.issueB-1-
dc.identifier.spage59-
dc.identifier.epage67-
dc.textversionpublisher-
dc.sortkey07-
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.20 B-1

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