{"created":"2023-05-15T10:21:36.161539+00:00","links":{},"metadata":{"_buckets":{"deposit":"8511a92c-80a5-4735-8012-bb91579208a0"},"_deposit":{"id":"5457.1","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"5457.1"},"status":"published"},"_oai":{"id":"oai:miyazaki-u.repo.nii.ac.jp:00005457.1","sets":["73:27"]},"author_link":["13413","29310","29312"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2000-08","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"576","bibliographicPageStart":"569","bibliographicVolumeNumber":"3","bibliographic_titles":[{"bibliographic_title":"応用力学論文集"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The earthquake ground motions are efficiently simulated using a discrete three fold Fourier transform of the analytical forms of seismic wave field in frequency wavenumber domain. They are derived by a stiffness matrices based formulation of the physical processes of propagation of seismic waves, which are radiated from a kinematic rupturing fault model. It is found from a numerical example that the seismic wave field on free field ground surface near a strike slip fault is like a vortex of sea water.","subitem_description_type":"Abstract"}]},"item_10001_version_type_20":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"原田, 隆典"},{"creatorName":"ハラダ, タカノリ","creatorNameLang":"ja-Kana"},{"creatorName":"Harada, Takanori","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"13413","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"山下, 肇"},{"creatorName":"ヤマシタ, ハジメ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"29310","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Yamashita, Hajime","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"29312","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":"2020-06-21"}],"displaytype":"detail","filename":"stiffnes_2000_harada.pdf","filesize":[{"value":"6.2 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"本文","url":"https://miyazaki-u.repo.nii.ac.jp/record/5457.1/files/stiffnes_2000_harada.pdf"},"version_id":"e7f27d69-1806-4018-a7fc-6bf66cf708dd"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":":stiffness matrix, seismic ground motion, kinematic source model, seismic waves, vortex","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"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":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"剛性マトリックスに基づく地震動の波形合成法と震源断層近傍地震動の渦現象","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"剛性マトリックスに基づく地震動の波形合成法と震源断層近傍地震動の渦現象","subitem_title_language":"ja"},{"subitem_title":"Stiffness Matrices Based Simulation of Ground Motion and Vortex of Seismic Wave Field Near A Faul","subitem_title_language":"en"}]},"item_type_id":"10001","owner":"2","path":["27"],"pubdate":{"attribute_name":"公開日","attribute_value":"2020-06-21"},"publish_date":"2020-06-21","publish_status":"0","recid":"5457.1","relation_version_is_last":true,"title":["剛性マトリックスに基づく地震動の波形合成法と震源断層近傍地震動の渦現象"],"weko_creator_id":"2","weko_shared_id":2},"updated":"2023-07-24T05:59:17.787394+00:00"}