{"created":"2021-03-01T06:50:41.276926+00:00","id":32057,"links":{},"metadata":{"_buckets":{"deposit":"3c3f6132-0447-49ab-9a15-65b2f06e2d2a"},"_deposit":{"id":"32057","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32057"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032057","sets":["80:4411:4415","9:504:4413:4416"]},"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Source Area of the Tsunami of the Nemuro Peninsula in 1973 and its Comparison with the Tsunami in 1894"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1974-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"76","bibliographicPageStart":"67","bibliographicVolumeNumber":"13","bibliographic_titles":[{"bibliographic_title":"地震研究所研究速報"}]}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Based on tide gauge records, the tsunamis accompanying the main shock (M=7.4) on June 17 and the largest aftershock (M=7.1) on June 24, 1973 off the Nemuro peninsula are investigated. The magnitudes of two tsunamis are m=1.5 and 0.5 respectively. The sea bottom of the tsunami source may be uplifted, judging from the initial motion of the tsunamis observed in the upward direction at the Hokkaido and Sanriku coasts. The source dimension is 130km long parallel to the Nemuro peninsula and the area is 7.2×103km2. The estimated source area of tsunami agrees well with the aftershock area and that of the second tsunami lies in the east side of the main source.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"71129","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Hatori, Tokutaro"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/00032048","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN10165194","subitem_source_identifier_type":"NCID"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"051.1","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"地震研究所"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"羽鳥, 徳太郎"}],"nameIdentifiers":[{"nameIdentifier":"71128","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-06-12"}],"displaytype":"detail","filename":"jis0130006.pdf","filesize":[{"value":"565.3 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"jis0130006.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32057/files/jis0130006.pdf"},"version_id":"c029af18-b55e-43c4-8248-a8de914def24"}]},"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":"1973年根室半島沖津波の波源域と1894年津波との比較","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"1973年根室半島沖津波の波源域と1894年津波との比較"}]},"item_type_id":"4","owner":"1","path":["4415","4416"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-12-22"},"publish_date":"2010-12-22","publish_status":"0","recid":"32057","relation_version_is_last":true,"title":["1973年根室半島沖津波の波源域と1894年津波との比較"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T04:08:23.766630+00:00"}