{"created":"2023-06-19T12:45:04.548961+00:00","id":4754,"links":{},"metadata":{"_buckets":{"deposit":"f244d4b2-57ae-428a-860f-01caa2089053"},"_deposit":{"created_by":3,"id":"4754","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"4754"},"status":"published"},"_oai":{"id":"oai:tokyo-metro-u.repo.nii.ac.jp:00004754","sets":["521:613:616:763:772"]},"author_link":["15940","15943","15947","15941","15944","15945","15946","15942"],"item_3_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"EVALUATING DISTRIBUTION OF SEISMIC INTENSITY IN SEISMIC MICROZONING : Part 2 : On the Comparison between Radiation Patterns of the Great Kanto Earthquake and the Distribution of Damage to wooden Structures"}]},"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1979-12","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"8","bibliographicPageEnd":"176","bibliographicPageStart":"165","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":"15944","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Miyano, Michio"}],"nameIdentifiers":[{"nameIdentifier":"15945","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Matsuda, Iware"}],"nameIdentifiers":[{"nameIdentifier":"15946","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Koizumi, Toshikazu"}],"nameIdentifiers":[{"nameIdentifier":"15947","nameIdentifierScheme":"WEKO"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"地震の強さとその分布を知る最も確かな方法は，いうまでもなく強震計の高密度分布による観測である。しかし，被害地震の歴史とその地域的広がりからみれば，その観測資料はあまりにも少ない。特に大地震の激震地の記録が欠けている。一方，大地震のインターバルは長いとはいえ，地震によって生じた現象や被害の記録は少なからず残されている。その1 (望月ほか，1978) にも述べてきたように，我が国各地に普遍的に分布する木造建物群の被害率は被害地震における地震動の強さの分布を推定するための簡易地震計の記録とみることができる。ところで，地震学の面における発震機構の研究は， 1960年代以降において特に著しく進展している。すなわち， 196O年以降震源の大きさ (断層面に沿ってのくいちがい変位量と断層面の大きさ)といった震源の物理的性質までが定量的に得られるようになってきた。かくして進展した断層震源理論 (近代的発震機構論)によればせん断型のくいちがいが数km/secの速度で断層面全体に広がっていく現象として地震を把えている。この研究では，サイスミック・マイクロゾーニングにおける入力地震動の強さの分布を評価する手法の確立の第一歩として金森・安藤 (1973)によって与えられている関東大地震の断層モデルからの実体波の生成と伝播を計算し，その結果を木造建物の被害分布と比較する。したがって，その対応性から地震断層理論の妥当性がチェックされ，かつ被害分布の面からも議論された結果，地震工学的にみて有意な震央位置が決定される。","subitem_description_type":"Abstract"},{"subitem_description":"For the purpose of evaluating areal distribution of seismic intensity，displacements of body waves deduced from the dynamic fault model of the Great Kanto Earthquake were analyzed by numerical integration for an infinite medium. The calculated patterns are very different between in the upthrown and downthrown blocks. The result，however，matches the areal distribution of damage to wooden structures caused by the earthquake. It means that distance from the fault trace is better explaining variable of distribution of seismic intensity than epicentral distance.","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":"宮野, 道雄"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"松田, 磐余"}],"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":"20024-008-013.pdf","filesize":[{"value":"595.9 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"20024-008-013.pdf","url":"https://tokyo-metro-u.repo.nii.ac.jp/record/4754/files/20024-008-013.pdf"},"version_id":"f6599b01-51c2-4b50-ad72-93b7ae66bffa"}]},"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2. 関東大地震の断層モデルによる実体波のRadiation Patternと被害分布の対応性","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2. 関東大地震の断層モデルによる実体波のRadiation Patternと被害分布の対応性"}]},"item_type_id":"3","owner":"3","path":["772"],"pubdate":{"attribute_name":"公開日","attribute_value":"2016-10-26"},"publish_date":"2016-10-26","publish_status":"0","recid":"4754","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2. 関東大地震の断層モデルによる実体波のRadiation Patternと被害分布の対応性"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-06-19T17:55:35.823457+00:00"}