{"created":"2021-03-01T06:18:13.627569+00:00","id":11342,"links":{},"metadata":{"_buckets":{"deposit":"aa30ed9d-0a08-478e-ad53-a9b18ef7dbad"},"_deposit":{"created_by":17,"id":"11342","owners":[17],"pid":{"revision_id":0,"type":"depid","value":"11342"},"status":"published"},"_oai":{"id":"oai:nagoya.repo.nii.ac.jp:00011342","sets":["879:1183:1184:1223"]},"author_link":["79703","79704","79705","79706","79707","79708"],"item_1615768549627":{"attribute_name":"出版タイプ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_9_alternative_title_19":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Estimation of paleoseismicity and seismic potential of the active fault along the eastern boundary of the Shonai plain, northeast Japan","subitem_alternative_title_language":"en"}]},"item_9_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1993-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"25","bibliographicPageStart":"19","bibliographicVolumeNumber":"4","bibliographic_titles":[{"bibliographic_title":"名古屋大学加速器質量分析計業績報告書","bibliographic_titleLang":"ja"}]}]},"item_9_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Estimation of earthquake recurrence times and characterization of fault behavior provide important data for risk analysis. Inland earthquakes which produced by slip on active faults have recurrence times of more than thousand of years. Historical records of destructive earthquakes is insufficient to characterize the seismicity. Assessment of the seismic potential of an active fault is therefore often difficult. Only geological and geomorphological methods enable to estimate the recurrence times. Analyses of the stratigraphy and Carbon-14 ages of the two boreholes which arranged close to a fault have revealed the last two earthquakes produced by the fault in this study. The last earthquake occurred after 2,500 years before present (yBP), and the penultimate one occurred between 5,300yBP and 4,300yBP. The last one is likely to be correlated with the historical earthquake of 850 A.D.. On this assumption recurrence time is probably estimated to be 3,200〜4,200 years.","subitem_description_language":"en","subitem_description_type":"Abstract"}]},"item_9_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"タンデトロン加速器質量分析計業境報告 Summaries of Researches Using AMS","subitem_description_language":"ja","subitem_description_type":"Other"}]},"item_9_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.18999/sumrua.4.19","subitem_identifier_reg_type":"JaLC"}]},"item_9_publisher_32":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会","subitem_publisher_language":"ja"}]},"item_9_relation_43":{"attribute_name":"関連情報","attribute_value_mlt":[{"subitem_relation_type":"isVersionOf","subitem_relation_type_id":{"subitem_relation_type_id_text":"http://ci.nii.ac.jp/naid/110000475818/","subitem_relation_type_select":"URI"}}]},"item_9_rights_12":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会","subitem_rights_language":"ja"},{"subitem_rights":"本文データは学協会の許諾に基づきCiNiiから複製したものである","subitem_rights_language":"ja"}]},"item_9_select_15":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_9_text_14":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_text_value":"application/pdf"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"open access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_abf2"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"鈴木, 康弘","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79703","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Suzuki, Yasuhiro","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79704","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"堀, 正和","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79705","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Hori, Masakazu","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79706","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"松尾, 稔","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79707","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Matsuo, Minoru","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79708","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":"2018-02-20"}],"displaytype":"detail","filename":"KJ00000187559.pdf","filesize":[{"value":"402.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00000187559.pdf","objectType":"fulltext","url":"https://nagoya.repo.nii.ac.jp/record/11342/files/KJ00000187559.pdf"},"version_id":"b364fd51-c8d6-4099-bf43-4a17f52df73c"}]},"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":"ボーリング調査による地震履歴の推定 : 山形県庄内平野東縁活断層調査","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"ボーリング調査による地震履歴の推定 : 山形県庄内平野東縁活断層調査","subitem_title_language":"ja"}]},"item_type_id":"9","owner":"17","path":["1223"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2010-04-28"},"publish_date":"2010-04-28","publish_status":"0","recid":"11342","relation_version_is_last":true,"title":["ボーリング調査による地震履歴の推定 : 山形県庄内平野東縁活断層調査"],"weko_creator_id":"17","weko_shared_id":-1},"updated":"2023-11-16T00:22:21.068482+00:00"}