{"created":"2023-07-25T10:59:16.110454+00:00","id":866,"links":{},"metadata":{"_buckets":{"deposit":"dc88b9de-e3f4-45b1-87b4-b14ade575f8c"},"_deposit":{"created_by":4,"id":"866","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"866"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00000866","sets":["1:356:361"]},"author_link":["555","570"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1978-01","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"234","bibliographicPageStart":"227","bibliographicVolumeNumber":"7","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Special issue"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Naruse, R.","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Shimizu, H.","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":"Flow lines of the ice sheet surface in Mizuho Plateau, East Antarctica were deduced from the results of observations of topographic features of the surface and measurements of surface flow of the ice sheet. This paper gives the distribution of paths of ice flow over Mizuho Plateau, and also the results of surface strains of the ice sheet measured by the square strain grids. Tensile strains whose directions were roughly parallel to the directions of the ice flow were predominant almost all over Mizuho Plateau. Considerably large compressive strains were observed in such regions with remarkable surface depressions as Mizuho Camp. The ice mass of 4.5×(10)^9 ton a year was estimated to pass across the vertical cross section along Route A (from A033 to S240), while 3×(10)^9 ton a year across Route S (from S124 to S240), both towards the Shirase Glacier.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733561","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":"The Institute of Low Temperature Science, Hokkaido University"},{"subitem_text_language":"en","subitem_text_value":"The Institute of Low Temperature Science, Hokkaido University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1978-01-01"}],"displaytype":"detail","filename":"KJ00000011840.pdf","filesize":[{"value":"884.9 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000011840","url":"https://nipr.repo.nii.ac.jp/record/866/files/KJ00000011840.pdf"},"version_id":"d4a01079-377a-4328-adbb-435886d24d8e"}]},"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":"Flow Line of the Ice Sheet over Mizuho Plateau","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Flow Line of the Ice Sheet over Mizuho Plateau","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["361"],"pubdate":{"attribute_name":"公開日","attribute_value":"1978-01-01"},"publish_date":"1978-01-01","publish_status":"0","recid":"866","relation_version_is_last":true,"title":["Flow Line of the Ice Sheet over Mizuho Plateau"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T14:05:27.222312+00:00"}