{"created":"2023-07-25T11:01:35.457467+00:00","id":3648,"links":{},"metadata":{"_buckets":{"deposit":"a5902214-8eb9-48e4-8e48-eba623198590"},"_deposit":{"created_by":4,"id":"3648","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"3648"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00003648","sets":["1259:1260:1262:524:528"]},"author_link":["5302","5304","5305","5303"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"VARIATION OF NATURAL LEVEES OF SUBMARINE CANYONS AROUND ANTARCTICA : AN INDICATOR OF ANTARCTIC CONTOUR-CURRENT"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1991-05","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"118","bibliographicPageStart":"108","bibliographicVolumeNumber":"4","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology"}]}]},"item_1_creator_7":{"attribute_name":"著者名よみ","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"カガミ, ヒデオ"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"イワサキ, テツヤ"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"KAGAMI, Hideo","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"IWASAKI, Tetsuya","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"Natural levees developing at the western side of the submarine canyons on the continental rise around the Antarctic continent are for the first time described quantitatively. It is found that they apparently involve in large benthic flow.The observations presented here suggest that the benthic flow may be caused by a combination of bottom-trapped Rossby waves, the background mean current which most probably consists of Antarctic Bottom Water, and high-frequency tidal flow.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00003648","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA10756213","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Department of Geology, Faculty of Science, Kochi University:(Present address) Faculty of Science, Josai University"},{"subitem_text_language":"en","subitem_text_value":"Department of Geology, Faculty of Science, Kochi University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1991-05-01"}],"displaytype":"detail","filename":"KJ00000767851.pdf","filesize":[{"value":"1.7 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000767851","url":"https://nipr.repo.nii.ac.jp/record/3648/files/KJ00000767851.pdf"},"version_id":"ee22c55e-7311-48bd-b327-cb3384bb2fc7"}]},"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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"VARIATION OF NATURAL LEVEES OF SUBMARINE CANYONS AROUND ANTARCTICA : AN INDICATOR OF ANTARCTIC CONTOUR-CURRENT","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"VARIATION OF NATURAL LEVEES OF SUBMARINE CANYONS AROUND ANTARCTICA : AN INDICATOR OF ANTARCTIC CONTOUR-CURRENT"}]},"item_type_id":"1","owner":"4","path":["528"],"pubdate":{"attribute_name":"公開日","attribute_value":"1991-05-01"},"publish_date":"1991-05-01","publish_status":"0","recid":"3648","relation_version_is_last":true,"title":["VARIATION OF NATURAL LEVEES OF SUBMARINE CANYONS AROUND ANTARCTICA : AN INDICATOR OF ANTARCTIC CONTOUR-CURRENT"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:31:00.325191+00:00"}