{"created":"2023-06-19T12:45:05.934986+00:00","id":4786,"links":{},"metadata":{"_buckets":{"deposit":"618a27dc-3bac-47e8-a892-48a5b4ad4ae0"},"_deposit":{"created_by":3,"id":"4786","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"4786"},"status":"published"},"_oai":{"id":"oai:tokyo-metro-u.repo.nii.ac.jp:00004786","sets":["521:613:616:763:775"]},"author_link":["16065","16063","16062","16061","16064","16060"],"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 DISTRIBUTON OF SEISMIC INTENSITY IN THE SEISMIC MICROZONING : Part 3 : Relationships among Hypocentral Distance・Radiaton Pattern・Landforms and Seismic Intensity of the Great Kanto Earthquake"}]},"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1980-12","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"11","bibliographicPageEnd":"139","bibliographicPageStart":"127","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":"16063","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Matsuda, Iware"}],"nameIdentifiers":[{"nameIdentifier":"16064","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Miyano, Michio"}],"nameIdentifiers":[{"nameIdentifier":"16065","nameIdentifierScheme":"WEKO"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"広域地震防災の立場からある地方の地震危険度を考える場合，対象となる地震はある個性をもった幾つかに限定され，ある程度決定論的に議論ができると思われる。すなわち，南関東を対象とした場合，最も影響力の大きい地震は相模トラフ沿いの活断層，つまり関東大地震型の断層活動によるものであろう。さらに，一般にこのようなプレート間地震はreturn periodが短い。したがって，かつてこの断層が活動した時の地震動の強さの分布を可能な限り詳細に明らかにしておくことは重要な課題である。このような観点から，本報告では1923年関東大地震に際して活動したといわれている断層を有限な面震源と考え，その面からの最短距離・地形と被害，震度との関係を検討し，さらに断層の破壊の進行方向の効果による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 report investigates the relationships among hypocentral distance，landform，damage to wooden buildings and seismie intensity of the 1923 Great Kanto Earthquake. Moreover，the radiation pattern of seismic intensity following the effect of fault rupture is considered. In this report，hypocentral distance is defined as the shortest distance from the fault plane to each town (village).","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":[{}]}]},"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":"20024-011-012.pdf","filesize":[{"value":"613.2 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"20024-011-012.pdf","url":"https://tokyo-metro-u.repo.nii.ac.jp/record/4786/files/20024-011-012.pdf"},"version_id":"2e92698d-326f-4e42-8bef-e34781abe3d8"}]},"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3. 関東大地震における震度と震源距離・方向性・地形の関係","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3. 関東大地震における震度と震源距離・方向性・地形の関係"}]},"item_type_id":"3","owner":"3","path":["775"],"pubdate":{"attribute_name":"公開日","attribute_value":"2016-10-26"},"publish_date":"2016-10-26","publish_status":"0","recid":"4786","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3. 関東大地震における震度と震源距離・方向性・地形の関係"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-06-19T17:54:33.261943+00:00"}