{"created":"2023-05-15T10:23:20.114010+00:00","links":{},"metadata":{"_buckets":{"deposit":"70dfac21-39b2-444e-931c-d020a3a15c2a"},"_deposit":{"id":"5434.1","owners":[2],"pid":{"revision_id":0,"type":"depid","value":"5434.1"},"status":"published"},"_oai":{"id":"oai:miyazaki-u.repo.nii.ac.jp:00005434.1","sets":["73:27"]},"author_link":["13413"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2002-01","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"72","bibliographicPageStart":"65","bibliographic_titles":[{"bibliographic_title":"Joint Workshop on US-Japan Cooperative Research in Urban Earthquake"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"To develop a computer simulation method of earthquake wave motions for the fault-ground system with laterally inhomogeneous media, a three dimensional direct boundary element method is combined with the seismic waves radiated from an extended rupturing fault based on a kinematic source model. By using the developed method, it is found that the seismic wave field on free surface near a strike slip fault exhibits the vortex nature like the movement of cloud during typhoon. It is also found that the spatial-temporal variation of the seismic wave field depends strongly on both the geometrical structure of the sedimentary valley and the position of the extended fault rupture.","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","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"13413","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":"3-dimensional_2002_harada.pdf","filesize":[{"value":"1.1 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"本文","url":"https://miyazaki-u.repo.nii.ac.jp/record/5434.1/files/3-dimensional_2002_harada.pdf"},"version_id":"25681919-db2e-49ff-b8d9-acfe08e16659"}]},"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":"3-Dimensional DBEM For Simulation Of Seismic Waves In Laterally Inhomogeneous Layered Media And Vortex Of Wave Motions Near A Fault","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"3-Dimensional DBEM For Simulation Of Seismic Waves In Laterally Inhomogeneous Layered Media And Vortex Of Wave Motions Near A Fault","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":"5434.1","relation_version_is_last":true,"title":["3-Dimensional DBEM For Simulation Of Seismic Waves In Laterally Inhomogeneous Layered Media And Vortex Of Wave Motions Near A Fault"],"weko_creator_id":"2","weko_shared_id":2},"updated":"2023-07-24T05:48:48.975842+00:00"}