{"created":"2023-05-15T10:00:59.284659+00:00","id":5468,"links":{},"metadata":{"_buckets":{"deposit":"4e83e1db-0272-4f62-9d3e-fa358f947297"},"_deposit":{"created_by":5,"id":"5468","owner":"5","owners":[5],"pid":{"revision_id":0,"type":"depid","value":"5468"},"status":"published"},"_oai":{"id":"oai:miyazaki-u.repo.nii.ac.jp:00005468","sets":["73","73:27"]},"author_link":["29405","13413","29401","29404","29402"],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2002-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"594","bibliographicPageStart":"587","bibliographicVolumeNumber":"48A","bibliographic_titles":[{"bibliographic_title":"構造工学論文集"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"In this paper, to develop a computer simulation method for the fault-ground system with laterally inhomogeneous layered media, a direct 3-dimensional boundary element method is combined with the seismic waves radiated from a extended rupturing fault based on a kinematic source model. By using the developed method, it is found that the seismic wave field on free field ground surface near a strike slip fault is like a vortex of sea water.It is also found that the characteristics of motions chang greatly in relating with the position of a valley shaped sedimental layered media and the 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"}]},{"creatorNames":[{"creatorName":"黒田, 拓氏"},{"creatorName":"クロダ, タクオ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"29401","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"山上, 武志"},{"creatorName":"ヤマガミ, タケシ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"29402","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Kuroda, Takuo","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"29404","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Yamagami, Takesi","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"29405","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":"3jigenntyokusetu_2018_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/5468/files/3jigenntyokusetu_2018_harada.pdf"},"version_id":"2e88e9ad-df94-4693-85ab-9d94405a6692"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"seismic ground motions, kinematic source model, boundary element method, 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":"3次元直接境界要素法による震源断層-不整形地盤系の応答解析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":"3次元直接境界要素法による震源断層-不整形地盤系の応答解析と震源断層近傍地震動の渦現象","subitem_title_language":"ja"},{"subitem_title":"A Direct 3 Dimensional Boundary Element Method of Analysis of Fault-Ground System with Laterally Inhomogeneous Layered Media and Vortex of Seismic Wave Field 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":"5468","relation_version_is_last":true,"title":["3次元直接境界要素法による震源断層-不整形地盤系の応答解析と震源断層近傍地震動の渦現象"],"weko_creator_id":"5","weko_shared_id":2},"updated":"2023-09-03T07:04:47.917830+00:00"}