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dc.contributor.author田中, 豊ja
dc.contributor.author林, 守孝ja
dc.contributor.author加藤, 正明ja
dc.contributor.author藤田, 和夫ja
dc.contributor.alternativeTANAKA, Yutakaen
dc.contributor.alternativeHAYASHI, Moritakaen
dc.contributor.alternativeKATO, Masaakien
dc.contributor.alternativeHUZITA, Kazuoen
dc.date.accessioned2009-01-30T04:59:06Z-
dc.date.available2009-01-30T04:59:06Z-
dc.date.issued1972-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/69849-
dc.description.abstractThe observations of ground tilts and strains at Rokko observation station were rewardedwith remarkable results as expected: Principal axis of compressional strain at both sides ofOotsuki fault are near the E-W direction. It coincides with the pattern of stress field in thenorthwestern part of Kinki district including the Rokko area. On the earth tidal observations, peculiar phenomena were found in amplitude and phase of M2-waves. The terms of tidalstrain by oceanic load are influenced by elasticity of individual rock on which extensometers areset, probably since the station is near coast and in fracture zones as a vertical layered structure.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.title六甲断層破砕帯における地殻変動の連続観測(第一報)ja
dc.title.alternativeCONTINUOUS OBSERVATION OF CRUSTAL DEFORMATIONS IN A FRACTURE ZONE OF ROKKO FAULT SYSTEM (FIRST REPORT)en
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.volume15-
dc.identifier.issueB-
dc.identifier.spage29-
dc.identifier.epage41-
dc.textversionpublisher-
dc.sortkey04-
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.15 B

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