{"created":"2021-03-01T06:53:23.629321+00:00","id":34492,"links":{},"metadata":{"_buckets":{"deposit":"104deb2b-f34e-4469-a14a-bb83ee804553"},"_deposit":{"id":"34492","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"34492"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00034492","sets":["80:4535:5167:5173","9:504:4538:5169:5174"]},"author_link":["133872","133873","133870","133871"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"16. レーレー型波が地殼の内部層に傳播する條件"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1939-06-30","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"189","bibliographicPageStart":"179","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":"十年程前にレーレー型波が地殼の内部層に傳播し得る事を述べた．今囘はその傳播についての正確なる條件を研究して見たのである．研究結果の要點は次の如くである．(1) 波動の速度は内部層の橫波と外部層の橫波との間にある．(2) 内部層の中間面について對稱なる振幅分布をなす波動の場合には各μ'/μに對して1つの分散曲線しかないが，斜對稱の振幅分布をなす場合には數多くの分散曲線がある．之等の曲線は互に異なる數の節平面が内部層中に存在する場合に相當するのである．換言すれば零次，一次，二次，……の振動を示す譯である．","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"133872","nameIdentifierScheme":"WEKO"}],"names":[{"name":"妹澤, 克惟"}]},{"nameIdentifiers":[{"nameIdentifier":"133873","nameIdentifierScheme":"WEKO"}],"names":[{"name":"金井, 淸"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000034492","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":"133870","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Kanai, Kiyoshi"}],"nameIdentifiers":[{"nameIdentifier":"133871","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":"ji0172001.pdf","filesize":[{"value":"634.6 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0172001.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/34492/files/ji0172001.pdf"},"version_id":"10fa9787-29d9-411e-bbe0-c6c636e63b22"}]},"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":"16. The Requisite Condition for Rayleigh-waves for Transmission through an Inner Stratum of the Earth","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"16. The Requisite Condition for Rayleigh-waves for Transmission through an Inner Stratum of the Earth","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["5173","5174"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-06-06"},"publish_date":"2008-06-06","publish_status":"0","recid":"34492","relation_version_is_last":true,"title":["16. The Requisite Condition for Rayleigh-waves for Transmission through an Inner Stratum of the Earth"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T05:29:44.115853+00:00"}