{"created":"2021-03-01T06:53:49.588552+00:00","id":34879,"links":{},"metadata":{"_buckets":{"deposit":"4b3e30c3-35f2-45f0-bc9f-ebe7aa7e5654"},"_deposit":{"id":"34879","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"34879"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00034879","sets":["80:4535:5237:5241","9:504:4538:5239:5242"]},"author_link":["84391","84392"],"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1932-09-22","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"516","bibliographicPageStart":"499","bibliographicVolumeNumber":"10","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_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Some earthquakes in western Kwanto, which were believed very shallow seated, revealed two particular wave-groups U1 and U2 (Fig.2). Assuming a thin surface layer and these waves as P and S waves in the layer, we can find close connections between this and other two phenomena, the (P-P1) durations, which we discussed before, arid the anomaly of (P-S) duration observed in the case of the Ito swarm earthquakes in 1930.","subitem_description_type":"Abstract"}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000034879","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":"地震研究所"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Matuzawa, Takeo"}],"nameIdentifiers":[{"nameIdentifier":"84391","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Fukutomi, Takaharu"}],"nameIdentifiers":[{"nameIdentifier":"84392","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":"2017-06-13"}],"displaytype":"detail","filename":"ji0103001.pdf","filesize":[{"value":"5.0 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0103001.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/34879/files/ji0103001.pdf"},"version_id":"62787f90-3176-4996-92a2-eee1655e652c"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"deu"}]},"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":"Zwei merkwuerdige Wellengruppen bei einigen Erdbeben in Kwanto und die dritte Mitteilung uber den vorlaufenden Teil der Erdbebenbewegungen","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Zwei merkwuerdige Wellengruppen bei einigen Erdbeben in Kwanto und die dritte Mitteilung uber den vorlaufenden Teil der Erdbebenbewegungen","subitem_title_language":"de"}]},"item_type_id":"4","owner":"1","path":["5241","5242"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2017-02-07"},"publish_date":"2017-02-07","publish_status":"0","recid":"34879","relation_version_is_last":true,"title":["Zwei merkwuerdige Wellengruppen bei einigen Erdbeben in Kwanto und die dritte Mitteilung uber den vorlaufenden Teil der Erdbebenbewegungen"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:09:48.194641+00:00"}