{"created":"2023-07-25T10:59:05.647606+00:00","id":616,"links":{},"metadata":{"_buckets":{"deposit":"775971de-5cc4-43e5-a699-4fc7ad40466c"},"_deposit":{"created_by":4,"id":"616","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"616"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00000616","sets":["1:314:320"]},"author_link":["437"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1983-02","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"83","bibliographicPageStart":"1","bibliographicVolumeNumber":"13","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Ser. C, Earth sciences"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"YOSHIDA, Yoshio","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":"The author describes the physiography of the Prince Olav and the Prince Harald Coasts and discusses the geomorphic development of the coastal and the inland icefree areas of the region based mainly on field surveys arid air-photograph interpretation. The Yamato Mountains are situated inland about 300 km away from the coast and consist of seven small massifs and some 20 nunataks with maximum elevation of 2490 m above sea level. They were once covered completely with the former ice sheet. The fall of the ice level revealed the glaciated topography including at least two cirques which had been formed by mountain glaciation prior to inundation of the former ice sheet. The trace of erosion by the wet-based ice sheet is found on a part of the bedrock. In the retreat of the ice from the highest to the present levels, three stages can be recognized ; the Yamato, the Fukushima, and the Meteorite Glacial Stages for the maximum, intermediate, and near past to present standstills of the ice sheet. During the ice retreat outlet glaciers and detached ice masses fed partly by drifted snow modified the topography of the presently ice-free areas. In the coastal region, the ice sheet retreated from the edge of the continental shelf prior to 30000 years before, leaving the glaciated ice-free areas on the present coast. Areal scouring of the former ice sheet produced the undulating surfaces with subsequent features controlled by geologic structures on the preglacially existed subdued topography. Selective linear erosion also cut the surface to produce precipitous cliffs and U-shaped valleys both in the ice-free areas and on the sea floor. Crooked glacial grooves and related minor topography suggest the erosion by the wet-based former ice sheet. Raised marine features after glaciation and radiocarbon dates give the information of crustal movement in time sequence.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733470","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":"National Institute of Polar Research"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1983-02-01"}],"displaytype":"detail","filename":"KJ00000011302.pdf","filesize":[{"value":"9.5 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000011302","url":"https://nipr.repo.nii.ac.jp/record/616/files/KJ00000011302.pdf"},"version_id":"e1f5a302-016b-4286-899a-5264b2f840e6"}]},"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":"Physiography of the Prince Olav and the Prince Harald Coasts, East Antarctica (Earth Sciences)","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Physiography of the Prince Olav and the Prince Harald Coasts, East Antarctica (Earth Sciences)","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["320"],"pubdate":{"attribute_name":"公開日","attribute_value":"1983-02-01"},"publish_date":"1983-02-01","publish_status":"0","recid":"616","relation_version_is_last":true,"title":["Physiography of the Prince Olav and the Prince Harald Coasts, East Antarctica (Earth Sciences)"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T15:08:56.829508+00:00"}