{"created":"2021-03-01T06:27:29.963616+00:00","id":19961,"links":{},"metadata":{"_buckets":{"deposit":"d032b067-c899-4ef7-89b5-f6e696973ce1"},"_deposit":{"id":"19961","owners":[],"pid":{"revision_id":0,"type":"depid","value":"19961"},"status":"published"},"_oai":{"id":"oai:nagoya.repo.nii.ac.jp:00019961","sets":["879:1183:1184:1735"]},"author_link":["84172","84173","84174","84175","84176","84177","84178","84179","84180","84181","84182","84183","84184","84185","84186","84187","84188","84189","84190","84191","84192","84193","84194","84195","84196","84197"],"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":"Geological and diatomological studies of a 60m core (AZK-101) by boring machine and 13m peat cores (ATP-1～3) by Thomas-type hand-operated sampler from the upper Pleistocene to the Holocene, in the Azuma River Area in Hokkaido, Japan, : 2014 Geological researches of the Alluvial Deposits in the Azuma River Area (Part 1)","subitem_alternative_title_language":"en"}]},"item_9_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2015-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"72","bibliographicPageStart":"67","bibliographicVolumeNumber":"26","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":"Five drilling cores (AZK-101, AZK-2, AZK-3, AZK-4 and AZK-5) in the area Hamaatsuma to Kamiatsuma and four hand-operated drilling peat cores in the area Tomisato to Poronai along Azuma River, southern Hokkaido, were investigated based on lithologic observation, pollen analysis, diatom analysis, tephrochronology and AMS 14C dating. Consequently the authors revealed the existence of buried valley, and explained the vegetation and salinity change of the Upper Pleistocene to the Holocene deposits in the Azuma River area.","subitem_description_language":"en","subitem_description_type":"Abstract"}]},"item_9_description_5":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"名古屋大学年代測定総合研究センターシンポジウム報告","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.26.67","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","subitem_publisher_language":"ja"}]},"item_9_select_15":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"open 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