{"created":"2023-07-25T11:04:15.676332+00:00","id":7332,"links":{},"metadata":{"_buckets":{"deposit":"9a65b8e1-770e-4b13-ba13-ddaba0624abc"},"_deposit":{"created_by":4,"id":"7332","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"7332"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00007332","sets":["1259:906:927"]},"author_link":["29","11358"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"PRINCE OLAV COAST オヨビ PRINCE Harald COAST フキン ノ カイテイ チケイ ト テイシツ ニツイテ"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1964-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"1787","bibliographicPageStart":"1777","bibliographicVolumeNumber":"21","bibliographic_titles":[{"bibliographic_title":"南極資料"}]}]},"item_1_creator_6":{"attribute_name":"著者名(日)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"佐藤, 任弘"},{"creatorName":"サトウ, タカヒロ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"SATO, Takahiro","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_11":{"attribute_name":"抄録(日)","attribute_value_mlt":[{"subitem_description":"南極大陸とアフリカ大陸との間には,中央大西洋海嶺の廷長とみられる西南西方向の海嶺があり,大洋底は南北2区に分けられる.北部は水深5,000～5,200mでやや凹凸に富むが,南部は5,200～5,300mで平坦である.南極周縁の大陸棚は,300～400mの外縁深度を有し,幅は60～70km以上に達する.陸棚斜面は4,000m以深で緩傾斜になる.第5次航海で得られた11地点の資料についてみると,大陸棚上の底質はかなり砂質で礫も伴うが,Prince Olav CoastやAmundsen Bay付近沖の陸棚斜面上部の底質は泥質である.しかし,これらの泥質堆積物は半遠洋性粘土の特徴を呈し,SiO_2に富み,CaCO_3・Fe_2O_3・Al_2O_3・P_2O_5などに乏しい.このことは,陸源性砕屑物の供給がかなり多いことを示すものであろう.","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"The deep sea floor between Africa and Antarctica is divided into two provinces by the continuation of Mid-Atlantic Ridge. The bottom sediments on the continental slope around Prince Olav Coast and Amundsen Bay are hemipelagic clays which are rich in SiO_2 and poor in CaCO_3, Fe_2O_3, Al_2O_3 and P_2O_5.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00007332","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"国立極地研究所"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00181831","subitem_source_identifier_type":"NCID"}]},"item_1_source_id_20":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00857289","subitem_source_identifier_type":"ISSN"}]},"item_1_subject_21":{"attribute_name":"国際十進分類法","attribute_value_mlt":[{"subitem_subject":"551.4：551.77/.79","subitem_subject_scheme":"UDC"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"The Hydrographic Office"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_value":"海上保安庁水路部"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1964-03-01"}],"displaytype":"detail","filename":"KJ00002476254.pdf","filesize":[{"value":"1.3 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002476254","url":"https://nipr.repo.nii.ac.jp/record/7332/files/KJ00002476254.pdf"},"version_id":"b31d6c33-b1ce-4344-9553-f25a6c08143d"}]},"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":"Prince Olav CoastおよびPrince Harald Coast付近の海底地形と底質について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Prince Olav CoastおよびPrince Harald Coast付近の海底地形と底質について"},{"subitem_title":"Submarine Topography and Several Bottom Sediments around Prince Olav and Prince Harald Coasts, Antarctica","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["927"],"pubdate":{"attribute_name":"公開日","attribute_value":"1964-03-01"},"publish_date":"1964-03-01","publish_status":"0","recid":"7332","relation_version_is_last":true,"title":["Prince Olav CoastおよびPrince Harald Coast付近の海底地形と底質について"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T11:56:48.009953+00:00"}