{"created":"2023-06-19T12:43:36.886552+00:00","id":2968,"links":{},"metadata":{"_buckets":{"deposit":"c691d96c-4aae-4167-aa11-51189710c22c"},"_deposit":{"created_by":3,"id":"2968","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"2968"},"status":"published"},"_oai":{"id":"oai:tokyo-metro-u.repo.nii.ac.jp:00002968","sets":["521:522:524:525:558"]},"author_link":["8230","8227","8226","8228","8233","8229","8231","8232"],"item_3_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2000","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"35","bibliographicPageEnd":"49","bibliographicPageStart":"41","bibliographic_titles":[{"bibliographic_title":"Geographical Reports of Tokyo Metropolitan University"}]}]},"item_3_creator_2":{"attribute_name":"著者(ヨミ)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"ヒラカワ, カズオミ"}],"nameIdentifiers":[{"nameIdentifier":"8230","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"ノガミ, ミチオ"}],"nameIdentifiers":[{"nameIdentifier":"8231","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"イマイズミ, トシフミ"}],"nameIdentifiers":[{"nameIdentifier":"8232","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"オカダ, アツマサ"}],"nameIdentifiers":[{"nameIdentifier":"8233","nameIdentifierScheme":"WEKO"}]}]},"item_3_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Significant eight figures on the Quaternary glaciation in the Chilean Lake District are presented. They are maps showing the former ice margins of four different glaciations, stratigraphies of tephras and paleosoils, and cross sections of glacial landforms. Development of coalescent piedmont glaciers during each glaciation is clearly indicated in these figures. Description on tephra-stratigraphy and red soil must be significant to examine the chronology of these glaciations. The longitudinal profiles of outwash plains along the major rivers during the Last Glaciation can be prominent evidence to discuss the chronology in relation to the lowering of the sea level. On the basis of these profiles, the largest glacier advance during the Last Glaciation probably occurred during the isotope Stage 4.","subitem_description_type":"Abstract"}]},"item_3_publisher_33":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Department of Geography, Tokyo Metropolitan University"}]},"item_3_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AA00200173","subitem_source_identifier_type":"NCID"}]},"item_3_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03868710","subitem_source_identifier_type":"ISSN"}]},"item_3_version_type_16":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Hirakawa, Kazuomi"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Nogami, Michio"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Imaizumi, Toshifumi"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Okada, Atumasa"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-08-04"}],"displaytype":"detail","filename":"20005-35-005.pdf","filesize":[{"value":"354.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"20005-35-005.pdf","url":"https://tokyo-metro-u.repo.nii.ac.jp/record/2968/files/20005-35-005.pdf"},"version_id":"63cbd94f-dcc6-4845-8aad-f74227ea694f"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"glaciation","subitem_subject_scheme":"Other"},{"subitem_subject":"piedmont glacier","subitem_subject_scheme":"Other"},{"subitem_subject":"paleosoil","subitem_subject_scheme":"Other"},{"subitem_subject":"tephra","subitem_subject_scheme":"Other"},{"subitem_subject":"Chilean Lake District","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":"Some basic data on the quaternary glaciation in the chilean lake district","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Some basic data on the quaternary glaciation in the chilean lake district"}]},"item_type_id":"3","owner":"3","path":["558"],"pubdate":{"attribute_name":"公開日","attribute_value":"2010-11-30"},"publish_date":"2010-11-30","publish_status":"0","recid":"2968","relation_version_is_last":true,"title":["Some basic data on the quaternary glaciation in the chilean lake district"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-06-19T18:23:49.883929+00:00"}