{"created":"2021-03-01T06:50:42.140484+00:00","id":32070,"links":{},"metadata":{"_buckets":{"deposit":"95b13b8f-5f59-47dd-b01e-ec87f7ae1196"},"_deposit":{"id":"32070","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32070"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032070","sets":["80:4411:4417","9:504:4413:4418"]},"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"On the P Wave Travel Time Residuals of the 1965 Rat Islands, Aleutian Earthquake"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1974-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"130","bibliographicPageStart":"121","bibliographicVolumeNumber":"12","bibliographic_titles":[{"bibliographic_title":"地震研究所研究速報"}]}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Statistical characteristics of the P wave travel time residuals have been studied by using the aftershocks of the 1965 Rat Islands, Aleutian Earthquake. There are not a few stations of which mean residuals are as large as several seconds. It will be necessary to adopt \"station corrections\" in order to get more precise locations of hypocenters. Variances for residuals noted with eP and P onsets are larger than the ones for iP onsets or total observations. Generally the mean values are 0.0, and the standard deviation are 1.1 seconds.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"71161","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Maki, Tadashi"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/00032061","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":"AN10165194","subitem_source_identifier_type":"NCID"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"051.1","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":"牧, 正"}],"nameIdentifiers":[{"nameIdentifier":"71160","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":"2017-06-12"}],"displaytype":"detail","filename":"jis0120009.pdf","filesize":[{"value":"428.7 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"jis0120009.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32070/files/jis0120009.pdf"},"version_id":"8b19ddf8-3bce-4b91-a73c-a600a9b1a6ef"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"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":"1965年アリューシャン余震のP波走時残差について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"1965年アリューシャン余震のP波走時残差について"}]},"item_type_id":"4","owner":"1","path":["4417","4418"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-12-22"},"publish_date":"2010-12-22","publish_status":"0","recid":"32070","relation_version_is_last":true,"title":["1965年アリューシャン余震のP波走時残差について"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T04:08:24.450727+00:00"}