{"created":"2021-03-01T06:53:26.395453+00:00","id":34533,"links":{},"metadata":{"_buckets":{"deposit":"4333eb64-25ac-40ac-8095-90ea46216ccc"},"_deposit":{"id":"34533","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"34533"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00034533","sets":["80:4535:5177:5181","9:504:4538:5179:5182"]},"author_link":["133952","133953","133950","133951"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"38. 地殼内の不連續面に於ける境界波の生成(第1報)"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1938-09-20","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"526","bibliographicPageStart":"504","bibliographicVolumeNumber":"16","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":"2種の固體が平面で密管連續してをるとき，この境界層に沿うてRayleigh型の彈性波が傅播し得るけれどもLove型の彈性波は傳播し得ぬ事をStoneleyが述べてゐる．この論文では最初に傳はる固體波が夫々縱波，鉛直横波，水平である場合について前述の境界波が如何にして生成するか，又，反射，屈折の固體波は如何なるものであるかを數理的に取扱つて見たのである．地殼の中には水平な不連續面が幾つもある事は極く明かであるが，その結果として，水平横波が最初に傳はるときには結局境界波が現れ得ぬことになるのである．之に反して縱波や鉛直横波が最初に傳はるときは，境界波が生成するから，多くの不連續面に於て通過し反射する毎に固體波の波動勢力が境界波のそれに變化するのである．從て水平横波の振幅が比較的に減衰しない事實と一致する物理的性質をあらはす．","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"133952","nameIdentifierScheme":"WEKO"}],"names":[{"name":"妹澤, 克惟"}]},{"nameIdentifiers":[{"nameIdentifier":"133953","nameIdentifierScheme":"WEKO"}],"names":[{"name":"金井, 淸"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000034533","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":"133950","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Kanai, Kiyoshi"}],"nameIdentifiers":[{"nameIdentifier":"133951","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":"ji0163002.pdf","filesize":[{"value":"977.9 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0163002.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/34533/files/ji0163002.pdf"},"version_id":"3fefe6f9-d991-435e-9e11-05ab119d0a2c"}]},"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":"38. The Formation of Boundary Waves at the Surface of a Discontinuity within the Earth's Crust.I","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"38. The Formation of Boundary Waves at the Surface of a Discontinuity within the Earth's Crust.I","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["5181","5182"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-06-06"},"publish_date":"2008-06-06","publish_status":"0","recid":"34533","relation_version_is_last":true,"title":["38. The Formation of Boundary Waves at the Surface of a Discontinuity within the Earth's Crust.I"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:58:44.036581+00:00"}