{"created":"2021-03-01T06:53:22.959559+00:00","id":34482,"links":{},"metadata":{"_buckets":{"deposit":"88de1406-e271-488f-b7cf-9e5e995f0155"},"_deposit":{"id":"34482","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"34482"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00034482","sets":["80:4535:5167:5171","9:504:4538:5169:5172"]},"author_link":["133844","133845","133842","133843"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"33. 地殼内の不連續面に於ける境界波の生成(第2報)"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1939-09-20","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"547","bibliographicPageStart":"539","bibliographicVolumeNumber":"17","bibliographic_titles":[{"bibliographic_title":"東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University"}]}]},"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":"地殼内に密度又は彈性の不連續面があると，この面に沿うて英國のStoneleyの述べたやうな地震波炉傳播する．前囘の第1暇報に於てこのやうな波が如何に作られるかを2次元の彈性論を以て説明し，且つ，實際にあるやうな3次元のものは研究中といふ事にして置いたところが，英国のある人がある雜誌にこの3次元の方を一層期待するやうに述べてをるので，物理的の本質はあまり變らぬけれども，ともかくも3次元の問題を解いて出して置いた次第である．計算の方法も前囘と同様にSommerfeldの電磁波の解法に關係あるものを用ひたのであるから，第1報と異なるやうな特徴が殆どない．即ち前囘の研究の擴張を試みたといふのに過ぎないのである．","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"133844","nameIdentifierScheme":"WEKO"}],"names":[{"name":"妹澤, 克惟"}]},{"nameIdentifiers":[{"nameIdentifier":"133845","nameIdentifierScheme":"WEKO"}],"names":[{"name":"金井, 淸"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000034482","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京帝国大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00029699","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, Tokyo Imperial University"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Sezawa, Katsutada"}],"nameIdentifiers":[{"nameIdentifier":"133842","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Kanai, Kiyoshi"}],"nameIdentifiers":[{"nameIdentifier":"133843","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":"2017-06-27"}],"displaytype":"detail","filename":"ji0173002.pdf","filesize":[{"value":"342.3 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0173002.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/34482/files/ji0173002.pdf"},"version_id":"6536596d-7ed2-49f8-9c10-b90dacc04001"}]},"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":"33. The Formation of Boundary Waves at the Surface of a Discontinuity within the Earth's Crust.II","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"33. The Formation of Boundary Waves at the Surface of a Discontinuity within the Earth's Crust.II","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["5171","5172"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-06-06"},"publish_date":"2008-06-06","publish_status":"0","recid":"34482","relation_version_is_last":true,"title":["33. The Formation of Boundary Waves at the Surface of a Discontinuity within the Earth's Crust.II"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:09:33.327489+00:00"}