{"created":"2023-06-20T15:40:21.567304+00:00","id":458,"links":{},"metadata":{"_buckets":{"deposit":"296b0f5e-67e1-4a61-a19d-5b7703269511"},"_deposit":{"created_by":17,"id":"458","owners":[17],"pid":{"revision_id":0,"type":"depid","value":"458"},"status":"published"},"_oai":{"id":"oai:nagano-nct.repo.nii.ac.jp:00000458","sets":["3:36"]},"author_link":["1074","1073","1075"],"item_2_alternative_title_1":{"attribute_name":"その他（別言語等）のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"The Directivity of Particle Motion of Microtremors in the Nagano-basin."}]},"item_2_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1991-12-27","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"45","bibliographicPageStart":"39","bibliographicVolumeNumber":"24","bibliographic_titles":[{"bibliographic_title":"長野工業高等専門学校紀要"}]}]},"item_2_description_19":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application","subitem_description_type":"Other"}]},"item_2_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The observations of microtremors were made in the Nagano-basin, where 192 locations were taken at the mesh of intervals of about 1 km. Wave motions in NS, EW, and UD components were compared between records due to the period of 2 sec. and 10 sec. seismometers. Particle orbits of surface motion were depicted from NS and EW components of microtremors. The predominant movement showing the directivity of the northeast-southwest or the northwest-southeast was rather clear in long period records than short period records. It seems to be attrilbuted to the underground structure in the Nagano-basin.","subitem_description_type":"Abstract"}]},"item_2_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"長野工業高等専門学校"}]},"item_2_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00179170","subitem_source_identifier_type":"NCID"}]},"item_2_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0286-1909","subitem_source_identifier_type":"ISSN"}]},"item_2_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":"服部, 秀人"}],"nameIdentifiers":[{"nameIdentifier":"1073","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"国井, 隆弘"}],"nameIdentifiers":[{"nameIdentifier":"1074","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"島, 坦"}],"nameIdentifiers":[{"nameIdentifier":"1075","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":"2013-02-19"}],"displaytype":"detail","filename":"nagano_nct-24-06.pdf","filesize":[{"value":"380.6 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"nagano_nct-24-06.pdf","url":"https://nagano-nct.repo.nii.ac.jp/record/458/files/nagano_nct-24-06.pdf"},"version_id":"d2f8a0d9-63af-439e-906c-0198bed1c8a5"}]},"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":"長野盆地の地盤構造と常時微動の方向性について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"長野盆地の地盤構造と常時微動の方向性について"}]},"item_type_id":"2","owner":"17","path":["36"],"pubdate":{"attribute_name":"公開日","attribute_value":"2013-02-19"},"publish_date":"2013-02-19","publish_status":"0","recid":"458","relation_version_is_last":true,"title":["長野盆地の地盤構造と常時微動の方向性について"],"weko_creator_id":"17","weko_shared_id":-1},"updated":"2023-06-20T16:07:15.863415+00:00"}