{"created":"2023-06-19T12:45:22.179214+00:00","id":5178,"links":{},"metadata":{"_buckets":{"deposit":"803b2c58-004c-4705-a3c1-2b1adf96c725"},"_deposit":{"created_by":3,"id":"5178","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"5178"},"status":"published"},"_oai":{"id":"oai:tokyo-metro-u.repo.nii.ac.jp:00005178","sets":["521:613:616:763:807"]},"author_link":["17357","17356"],"item_3_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Classification of Landforms and Deposits for Earthquake Damage Estimation"}]},"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1989","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"38","bibliographicPageEnd":"23","bibliographicPageStart":"13","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":"Matsuda, Iware"}],"nameIdentifiers":[{"nameIdentifier":"17357","nameIdentifierScheme":"WEKO"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"地震被害想定のための地形・地質の分類について，2つの方法を述べた。1つは，被害実態に基づくものであり， もう1つは地震工学的計算に基づくものである。被害実態に基づくものについては，関東地震の木造家屋の全壊率から，関東地方全域の震度(K)分布を求めた。さらに，震源断層面からの距離と震度との関係を地形毎に求め，広域の震度分布を予測する方法を示した。また，狭い範囲については，旧横浜市を例にとり，地形と沖積層の厚さと層序から，木造家屋の全壊率を説明した。地震工学的計算に基づくものについては，東京都で行われている被害想定を例に採りながら，地質学的地盤型から地震工学的地盤型を設定する手順を示し，サイスミック・マイクロゾーニングのための地盤分類について述べた。最後に，今後は，応答結果をデータベース化することが必要であることを示した。","subitem_description_type":"Abstract"},{"subitem_description":"Two methods of classificalion of landforms and deposits for the purpose of earthquake damage estimation are outlined. Method 1 is based on actual damage conditions，and method 2 relies on results of technical earthquake calculation Method 1 enables us to predict distribution of intensity (K) over a large area. In the example of a Kanto earthquake，first distribution of intensity (K) for the entire Kanto region is established from the percentage of totally destroyed wooden houses. Then，the relationship between the intensity (K) and the distance between the earthquake generated fault and the fault plane for each landform is determined. For smaller areas，e.g. Yokohama Old Town，the percentage of totally destroyed wooden houses can be explained from the landform and the depth and atratigraphy of recent deposits. Damage estimation in the Tokyo Metropolitan Area is an example of Method 2. The procedure for determining seismo-technological ground types from geological ground is explafned and ground classification for seismic micro zoning is outlined. Finally，I point out the need for storing response analysis results in data base form.","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":"松田, 磐余"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-12-26"}],"displaytype":"detail","filename":"20024-038-003.pdf","filesize":[{"value":"563.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"20024-038-003.pdf","url":"https://tokyo-metro-u.repo.nii.ac.jp/record/5178/files/20024-038-003.pdf"},"version_id":"26305c6f-5e97-4941-8dff-eea4761595bf"}]},"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":"地震被害想定のための地形・地質の分類","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"地震被害想定のための地形・地質の分類"}]},"item_type_id":"3","owner":"3","path":["807"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-01-10"},"publish_date":"2017-01-10","publish_status":"0","recid":"5178","relation_version_is_last":true,"title":["地震被害想定のための地形・地質の分類"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-06-19T17:46:29.021524+00:00"}