{"created":"2021-03-01T06:50:43.195861+00:00","id":32086,"links":{},"metadata":{"_buckets":{"deposit":"2e536619-0fab-42ad-941b-3e70767472ab"},"_deposit":{"id":"32086","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32086"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032086","sets":["80:4411:4421:4431","9:504:4413:4423:4432"]},"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Seismic Activity in Western Part of the Kii Peninsula : Relation between Magnitude and  Frequency of Earthquake Occurrence"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1973-03","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"5","bibliographicPageEnd":"5","bibliographicPageStart":"1","bibliographicVolumeNumber":"10","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":"The seismic activity in western part of Kii peninsula is relatively high. The relation between magnitude and frequency of earthquake occurrence in this area can be represented by so called Gutenberg-Richter's equation 'log N=a-bM'. The value of coefficients 'a'and 'b'is shown in Table 1.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"71224","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Nakamura, Masao"}]},{"nameIdentifiers":[{"nameIdentifier":"71225","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Kotani, Keiko"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/00032077","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":"中村, 正夫"}],"nameIdentifiers":[{"nameIdentifier":"71222","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"小谷, 啓子"}],"nameIdentifiers":[{"nameIdentifier":"71223","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":"jis0105001.pdf","filesize":[{"value":"154.8 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"jis0105001.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32086/files/jis0105001.pdf"},"version_id":"25277cec-20df-48da-89eb-f27322cfadf6"}]},"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":"紀伊半島西部の極浅発地震の活動 : マグニチュードと頻度の関係","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"紀伊半島西部の極浅発地震の活動 : マグニチュードと頻度の関係"}]},"item_type_id":"4","owner":"1","path":["4431","4432"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-12-22"},"publish_date":"2010-12-22","publish_status":"0","recid":"32086","relation_version_is_last":true,"title":["紀伊半島西部の極浅発地震の活動 : マグニチュードと頻度の関係"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T04:37:28.256096+00:00"}