{"created":"2023-07-25T11:00:54.579246+00:00","id":2827,"links":{},"metadata":{"_buckets":{"deposit":"f5228c51-6e65-4620-8e2c-5709ff4a839b"},"_deposit":{"created_by":4,"id":"2827","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"2827"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00002827","sets":["1259:1260:1265:414:423"]},"author_link":["3483","3484"],"item_1_alternative_title_5":{"attribute_name":"論文名よみ","attribute_value_mlt":[{"subitem_alternative_title":"EROSIONAL TOPOGRAPHY OBSERVED ON THE UPPER CONTINENTAL RISE, WILKES LAND, EAST ANTARCTICA"}]},"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1996-09","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"116","bibliographicPageStart":"109","bibliographicVolumeNumber":"9","bibliographic_titles":[{"bibliographic_title":"Proceedings of the NIPR Symposium on Antarctic Geosciences"}]}]},"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":[{"nameIdentifier":"3483","nameIdentifierScheme":"WEKO"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"KAGAMI, Hideo","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"3484","nameIdentifierScheme":"WEKO"}]}]},"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":"Erosional topography is recognized on the upper continental rise between 123°and 134°E off Wilkes Land, East Antarctica. Erosion of the upper continental rise up to roughly 500m is observed on seismic lines and is considered to be caused by down-slope density currents of cold shelf water or by thermohaline induced contour currents of Antarctic bottom water. Development of the abyssal channel systems is another bit of evidence that sediments are swept off the sea floor to create erosional depressions on the upper continental rise off Wilkes Land. Because these eroding currents are only active and effective at the continental margin around Antarctica, erosional depressions of the upper continental rise are responsible for formation of the Antarctic margin type.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00002827","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":"AA1072335X","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":"Faculty of Science, Josai University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1996-09-01"}],"displaytype":"detail","filename":"KJ00002409874.pdf","filesize":[{"value":"750.0 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00002409874","url":"https://nipr.repo.nii.ac.jp/record/2827/files/KJ00002409874.pdf"},"version_id":"0db0a85c-2514-4756-8496-f62d7bc5d2e9"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"erosional depressions","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"upper continental rise","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"off Wilkes Land","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Antarctic margin type","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Antarctic bottom water","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"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":"EROSIONAL TOPOGRAPHY OBSERVED ON THE UPPER CONTINENTAL RISE, WILKES LAND, EAST ANTARCTICA","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"EROSIONAL TOPOGRAPHY OBSERVED ON THE UPPER CONTINENTAL RISE, WILKES LAND, EAST ANTARCTICA"}]},"item_type_id":"1","owner":"4","path":["423"],"pubdate":{"attribute_name":"公開日","attribute_value":"1996-09-01"},"publish_date":"1996-09-01","publish_status":"0","recid":"2827","relation_version_is_last":true,"title":["EROSIONAL TOPOGRAPHY OBSERVED ON THE UPPER CONTINENTAL RISE, WILKES LAND, EAST ANTARCTICA"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:41:54.840595+00:00"}