{"created":"2021-03-01T06:52:31.597984+00:00","id":33714,"links":{},"metadata":{"_buckets":{"deposit":"807b419d-cd78-4b3a-867c-a8699205da0a"},"_deposit":{"id":"33714","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"33714"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00033714","sets":["80:4535:4967:4971","9:504:4538:4969:4972"]},"author_link":["131668","131667"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"半円形の半島をおそつた津波の回折"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1963-09-30","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"594","bibliographicPageStart":"589","bibliographicVolumeNumber":"41","bibliographic_titles":[{"bibliographic_title":"東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]},"item_4_description_13":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"1960年のチリ津波が日本をおそつたとき,北海逆の襟裳岬,関東地方の犬吠岬で岬より少し根元に寄つたところで,津波の波高が最大値をとることを見た.筆者は,この現象を,津波の海岸線にそつての回折であると考え,これを定性的に説明せんとの考えのもとに,半円形の半島をおそった津波の回折を海岸線についてのみ計算した.そして回折波によつて,波高の最大点が実際に起り得ることを知つた.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"131668","nameIdentifierScheme":"WEKO"}],"names":[{"name":"桃井, 高夫"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000033714","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":"AN00162258","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00408972","subitem_source_identifier_type":"ISSN"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"453","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":"Momoi, Takao"}],"nameIdentifiers":[{"nameIdentifier":"131667","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":"2017-06-26"}],"displaytype":"detail","filename":"ji0413007.pdf","filesize":[{"value":"258.1 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0413007.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/33714/files/ji0413007.pdf"},"version_id":"1d2771e4-0abc-4b54-9859-7eb5612182b1"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"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":"Diffraction of Tsunami Invading a Semi-circular Peninsula","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Diffraction of Tsunami Invading a Semi-circular Peninsula","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["4971","4972"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"33714","relation_version_is_last":true,"title":["Diffraction of Tsunami Invading a Semi-circular Peninsula"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:55:07.307085+00:00"}