{"created":"2021-03-01T06:50:41.745657+00:00","id":32064,"links":{},"metadata":{"_buckets":{"deposit":"2722e595-53aa-48c2-b257-3a61113d359b"},"_deposit":{"id":"32064","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32064"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032064","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":"Preliminary Report on a Dipping Mohorovicic Discontinuity in the Kii Peninsula as Inferred from Teleseismic P Wave Propagations"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1974-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"56","bibliographicPageStart":"41","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":"It should be emphasized that when using an array to determine directly dT/dΔ for the study of the structure of the Earth's deep interior, the necessity for the correction for the near surface structures is inevitable, particularly in such a region as the Kii Peninsula where existence of a dipping Moho-discontinuity is expected. A teleseismic slowness vector analysis method given by Zengeni(1970) is applied for the study of the diwing Moho-discontinuity in the Kii Peninsula.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"71143","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Mizoue, Megumi"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/00032055","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":"溝上, 恵"}],"nameIdentifiers":[{"nameIdentifier":"71142","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":"jis0120003.pdf","filesize":[{"value":"854.6 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"jis0120003.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32064/files/jis0120003.pdf"},"version_id":"eb59d3bd-f0c0-48c8-8931-536385899de3"}]},"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":"遠地地震P波の伝播から推定される紀伊半島におけるMoho不連続面の傾斜について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"遠地地震P波の伝播から推定される紀伊半島におけるMoho不連続面の傾斜について"}]},"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":"32064","relation_version_is_last":true,"title":["遠地地震P波の伝播から推定される紀伊半島におけるMoho不連続面の傾斜について"],"weko_creator_id":"1","weko_shared_id":null},"updated":"2022-12-19T04:06:53.568581+00:00"}