{"created":"2021-03-01T06:18:13.118961+00:00","id":11334,"links":{},"metadata":{"_buckets":{"deposit":"8a18dbeb-58c9-42c5-bede-7003115f9ec4"},"_deposit":{"created_by":17,"id":"11334","owners":[17],"pid":{"revision_id":0,"type":"depid","value":"11334"},"status":"published"},"_oai":{"id":"oai:nagoya.repo.nii.ac.jp:00011334","sets":["879:1183:1184:1221"]},"author_link":["79544","79545","79546","79547","79548","79549","79550","79551","79552","79553"],"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":"Northwest Pacific Deep Water Ventilation Rate During the Past 35,000 years with the AMS <14>^C Foraminifera Ages","subitem_alternative_title_language":"en"}]},"item_9_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1992-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"121","bibliographicPageStart":"114","bibliographicVolumeNumber":"3","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":"P4 core, which is composed mainly of olive grayish mud with well-developed biogenic structures, was raised from the lower continental slope basin off Shikoku at lat. 32°09'N, log. 133°54'E from a depth of 2700m. Each of samples for ^<14>C dating analysis was taken from 19 horizons throughout the core. And we have done the measurement of ^<14>C age differences between benthic and planktonic foraminifera to determine deep ocean ventilation times, using accelerator mass spectrometry. The results suggest that there are clearly two main mode patterns of paleo-circulation here at about 13,000 y.B.P., which may be called glacial and post glacial type. The formar has a slow mode which are difference ages about 1,000 yr, the latter has complicated puls patterns from 2,000 yr to 1,000 years.","subitem_description_language":"en","subitem_description_type":"Abstract"}]},"item_9_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.18999/sumrua.3.114","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/110000475803/","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":"村山, 雅史","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79544","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Murayama, Masafumi","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79545","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"平, 朝彦","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79546","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Taira, Asahiko","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79547","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"岩倉, 央和","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79548","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Iwakura, Hirokazu","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79549","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"松本, 英二","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79550","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Mastumoto, Eiji","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79551","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"中村, 俊夫","creatorNameLang":"ja"}],"nameIdentifiers":[{"nameIdentifier":"79552","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Nakamura, Toshio","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"79553","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":"KJ00000187538.pdf","filesize":[{"value":"367.7 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00000187538.pdf","objectType":"fulltext","url":"https://nagoya.repo.nii.ac.jp/record/11334/files/KJ00000187538.pdf"},"version_id":"246fadc1-fd88-4c5d-bbb7-1184594b6db3"}]},"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":"AMS法による有孔虫<14>^C年代と海洋深層水循環","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"AMS法による有孔虫<14>^C年代と海洋深層水循環","subitem_title_language":"ja"}]},"item_type_id":"9","owner":"17","path":["1221"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2010-04-27"},"publish_date":"2010-04-27","publish_status":"0","recid":"11334","relation_version_is_last":true,"title":["AMS法による有孔虫<14>^C年代と海洋深層水循環"],"weko_creator_id":"17","weko_shared_id":-1},"updated":"2023-11-16T00:22:01.306443+00:00"}