{"created":"2023-05-15T10:00:57.637040+00:00","id":5434,"links":{},"metadata":{"_buckets":{"deposit":"9fbeb0f9-c3e8-49c8-99fb-3911baa02eb5"},"_deposit":{"created_by":5,"id":"5434","owner":"5","owners":[5],"pid":{"revision_id":0,"type":"depid","value":"5434"},"status":"published"},"_oai":{"id":"oai:miyazaki-u.repo.nii.ac.jp:00005434","sets":["73","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":[{"creatorAffiliations":[{"affiliationNameIdentifiers":[{"affiliationNameIdentifier":"","affiliationNameIdentifierScheme":"ISNI","affiliationNameIdentifierURI":"http://www.isni.org/isni/"}],"affiliationNames":[{"affiliationName":"","affiliationNameLang":"ja"}]}],"creatorNames":[{"creatorName":"Harada, Takanori","creatorNameLang":"en"},{"creatorName":"原田, 隆典","creatorNameLang":"ja"},{"creatorName":"ハラダ, タカノリ","creatorNameLang":"ja-Kana"}],"familyNames":[{"familyName":"Harada","familyNameLang":"en"},{"familyName":"原田","familyNameLang":"ja"},{"familyName":"ハラダ","familyNameLang":"ja-Kana"}],"givenNames":[{"givenName":"Takanori","givenNameLang":"en"},{"givenName":"隆典","givenNameLang":"ja"},{"givenName":"タカノリ","givenNameLang":"ja-Kana"}],"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/files/3-dimensional_2002_harada.pdf"},"version_id":"43bd38c3-0d9e-49d3-8fb9-6c537f7a4276"}]},"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":"5","path":["73","27"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2020-06-21"},"publish_date":"2020-06-21","publish_status":"0","recid":"5434","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":"5","weko_shared_id":2},"updated":"2023-09-03T07:04:51.820643+00:00"}