{"created":"2023-06-19T12:45:07.820706+00:00","id":4819,"links":{},"metadata":{"_buckets":{"deposit":"4e008849-7ff4-465f-b9d7-f5bc42378e1e"},"_deposit":{"created_by":3,"id":"4819","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"4819"},"status":"published"},"_oai":{"id":"oai:tokyo-metro-u.repo.nii.ac.jp:00004819","sets":["521:613:616:763:778"]},"author_link":["16151","16149","16147","16146","16150","16148","16145","16152"],"item_3_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"ON THE METHOD TO EVALUATE DISTRIBUTION OF SEISMIC INTENSITY FOR THE SEISMIC MICROZONING : Part 5 : Relationships among Hypocentral Distance，Landforms (Ground Conditions) and Seismic Intensity of the Fukui Earthquake"}]},"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1981","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"14","bibliographicPageEnd":"134","bibliographicPageStart":"121","bibliographic_titles":[{"bibliographic_title":"総合都市研究"}]}]},"item_3_creator_3":{"attribute_name":"著者別名","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Mochizuki, Toshio"}],"nameIdentifiers":[{"nameIdentifier":"16149","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Matsuda, Iware"}],"nameIdentifiers":[{"nameIdentifier":"16150","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Miyano, Michio"}],"nameIdentifiers":[{"nameIdentifier":"16151","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Koizumi, Toshikazu"}],"nameIdentifiers":[{"nameIdentifier":"16152","nameIdentifierScheme":"WEKO"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"筆者らは一連の研究で，地震の規模 (マグニチュー)，型 (海洋型，内陸直下型)などによる被害，震度分布の差異について，主として墓石および木造建物被害調査に基づく震度と震源距離・地形 (地盤)の関係に着目して検討を行ってきた。本報告は，それらの中でいまだ対象とされていなかった内陸型大地震の事例として，1948年福井地震を取り上げ，断層面が地表に対して一般にほぼ90°に近い角度をなすと考えられるこのタイプの地震における，適切な震源距離の測定方法を明らかにすべく，線震源，面震源の両面から，各種地形および地盤種毎の震源距離と震度の関係に若干の検討を加えたものである。さらに，断層との位置関係において被災地をブロック化し，地盤種別に各ブロックの震度と震源距離の関係を比較することにより，断層の破壊に伴う震度分布の方向性の有無についても考察した。","subitem_description_type":"Abstract"},{"subitem_description":"This paper investigates relationships among hypocentral distance，landforms (ground conditions) and seismic intensity of the Fukui Earthquake. The best way to measure the hypocentral distance for this earthquake，which is an example of one occurring inland，was considered. Distribution of radiation energy from the fault plane and radiation pattern of seismic intensity were also studied.","subitem_description_type":"Abstract"}]},"item_3_description_40":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"subitem_description":"postprint","subitem_description_type":"Other"}]},"item_3_publisher_33":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京都立大学都市研究センター"}]},"item_3_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00134354","subitem_source_identifier_type":"NCID"}]},"item_3_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03863506","subitem_source_identifier_type":"ISSN"}]},"item_3_version_type_16":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"望月, 利男"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"松田, 磐余"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"宮野, 道雄"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"小泉, 敏一"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-12"}],"displaytype":"detail","filename":"20024-014-011.pdf","filesize":[{"value":"643.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"20024-014-011.pdf","url":"https://tokyo-metro-u.repo.nii.ac.jp/record/4819/files/20024-014-011.pdf"},"version_id":"1700faf1-9ea0-45ff-b1f3-876cc03c324b"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"サイスミック・マイクロゾーニングにおける震度分布の評価手法について : その5，福井地震における震度と震源距離・地形 (地盤) の関係","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"サイスミック・マイクロゾーニングにおける震度分布の評価手法について : その5，福井地震における震度と震源距離・地形 (地盤) の関係"}]},"item_type_id":"3","owner":"3","path":["778"],"pubdate":{"attribute_name":"公開日","attribute_value":"2016-10-26"},"publish_date":"2016-10-26","publish_status":"0","recid":"4819","relation_version_is_last":true,"title":["サイスミック・マイクロゾーニングにおける震度分布の評価手法について : その5，福井地震における震度と震源距離・地形 (地盤) の関係"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-06-19T17:53:21.203658+00:00"}