{"created":"2023-07-27T06:44:42.315260+00:00","id":35023,"links":{},"metadata":{"_buckets":{"deposit":"3e445865-42c0-476e-937a-7db5cfffce73"},"_deposit":{"created_by":3,"id":"35023","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"35023"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00035023","sets":["2812:2857:2858:2862"]},"author_link":["58447"],"item_9_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2006-08-01","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"98","bibliographicPageStart":"96","bibliographic_titles":[{"bibliographic_title":"2006名古屋大学・金沢大学22世紀COEプログラム合同地球環境学サマースクール資料"}]}]},"item_9_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Abstract - Lake sediments yield records of information about climatic and tectonic conditions in the past with local to global scales. Dating of sediments is the first step to extract quantitative information from the record. The magneto- and bio- stratigraphy is always a powerful tool. An orbital tuning of successive data on physical and chemical properties of sediments also could provide timescale. Radiometric dating techniques can provide stand-alone numerical values, though each methodology could be applied to restricted samples and time-spans. This paper reviews several radiometric dating methodologies which could be applied to lake sediments, addressing advantages and requirements of each methodology.","subitem_description_type":"Abstract"}]},"item_9_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"京都府立大学　農学研究科","subitem_description_type":"Other"}]},"item_9_publisher_17":{"attribute_name":"公開者","attribute_value_mlt":[{"subitem_publisher":"金沢大学２１世紀COEプログラム環日本海域の環境計測と長期・短期変動予測"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-10-05"}],"displaytype":"detail","filename":"TE-COE-TAKAHARA-H-2.pdf","filesize":[{"value":"31.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"TE-COE-TAKAHARA-H-2.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/35023/files/TE-COE-TAKAHARA-H-2.pdf"},"version_id":"5ef2c32d-f889-40c2-affc-356912e95eb6"}]},"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":"research report","resourceuri":"http://purl.org/coar/resource_type/c_18ws"}]},"item_title":"Vegetational differences between the coastal areas of the Japan Sea and the Pacific Ocean since the last interglacial (isotope stage 5e) in western Japan","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Vegetational differences between the coastal areas of the Japan Sea and the Pacific Ocean since the last interglacial (isotope stage 5e) in western Japan"}]},"item_type_id":"9","owner":"3","path":["2862"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-10-05"},"publish_date":"2017-10-05","publish_status":"0","recid":"35023","relation_version_is_last":true,"title":["Vegetational differences between the coastal areas of the Japan Sea and the Pacific Ocean since the last interglacial (isotope stage 5e) in western Japan"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-07-27T19:11:30.448124+00:00"}