WEKO3
アイテム
{"_buckets": {"deposit": "c286d740-5af9-4810-ac0f-8327c9218f12"}, "_deposit": {"created_by": 4, "id": "852", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "852"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00000852", "sets": ["361"]}, "author_link": ["557"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1978-01", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "36", "bibliographicPageStart": "26", "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": "Yokoyama, K.", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "557", "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": "Among the structural phenomena on the ice sheet, the structures with the dimensions of (10)^1-(10)^4m are called here \"surface structures\". The data of the surface structures obtained in Mizuro Plateau up to date were compiled and refined. The surface structures were classified into five major groups, according to their physical characteristics, A) flat surface, B) undulation (isolated), C) undulation (grouped), D) crevasse and crack, E) moraine and muddy band. These structures are made mostly by deformation of ice caused by movement of an ice sheet. Thus the distribution of the surface structures would be a reflection of stress condition of the ice sheet; stress condition is controlled by ice thickness, flow velocity and bedrock topography. Referring to steepness and frequency of surface structures, Mizuho Plateau was divided into four subdivisional regions, coastal region, transitional region, inland region and mountainous region. The surface structures in the coastal region and in the vicinity of exposed land are steeper and more frequent than those of inland. Such variation of the feature of the surface structures is well explained by the distribution of the above-mentioned three factors which control the stress condition of the ice sheet. This paper is an approach to a study on dynamics of the ice sheet.", "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": "Disaster Prevention Research Institute, Kyoto 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", "download_preview_message": "", "file_order": 0, "filename": "KJ00000011826.pdf", "filesize": [{"value": "1.1 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1100000.0, "url": {"url": "https://nipr.repo.nii.ac.jp/record/852/files/KJ00000011826.pdf"}, "version_id": "32d03826-5759-46e3-be57-adc7e9555820"}]}, "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": "Distribution of Surface Structures of the Ice Sheet in Mizuho Plateau", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Distribution of Surface Structures of the Ice Sheet in Mizuho Plateau", "subitem_title_language": "en"}]}, "item_type_id": "1", "owner": "4", "path": ["361"], "permalink_uri": "https://nipr.repo.nii.ac.jp/records/852", "pubdate": {"attribute_name": "公開日", "attribute_value": "1978-01-01"}, "publish_date": "1978-01-01", "publish_status": "0", "recid": "852", "relation": {}, "relation_version_is_last": true, "title": ["Distribution of Surface Structures of the Ice Sheet in Mizuho Plateau"], "weko_shared_id": 4}
Distribution of Surface Structures of the Ice Sheet in Mizuho Plateau
https://nipr.repo.nii.ac.jp/records/852
https://nipr.repo.nii.ac.jp/records/852534e3bc6-f3c7-420f-b1b6-01a820141f19
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000011826.pdf (1.1 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1978-01-01 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Distribution of Surface Structures of the Ice Sheet in Mizuho Plateau | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Yokoyama, K.
× Yokoyama, K. |
|||||
著者所属(英) | ||||||
en | ||||||
Disaster Prevention Research Institute, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Among the structural phenomena on the ice sheet, the structures with the dimensions of (10)^1-(10)^4m are called here "surface structures". The data of the surface structures obtained in Mizuro Plateau up to date were compiled and refined. The surface structures were classified into five major groups, according to their physical characteristics, A) flat surface, B) undulation (isolated), C) undulation (grouped), D) crevasse and crack, E) moraine and muddy band. These structures are made mostly by deformation of ice caused by movement of an ice sheet. Thus the distribution of the surface structures would be a reflection of stress condition of the ice sheet; stress condition is controlled by ice thickness, flow velocity and bedrock topography. Referring to steepness and frequency of surface structures, Mizuho Plateau was divided into four subdivisional regions, coastal region, transitional region, inland region and mountainous region. The surface structures in the coastal region and in the vicinity of exposed land are steeper and more frequent than those of inland. Such variation of the feature of the surface structures is well explained by the distribution of the above-mentioned three factors which control the stress condition of the ice sheet. This paper is an approach to a study on dynamics of the ice sheet. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00733561 | |||||
書誌情報 |
Memoirs of National Institute of Polar Research. Special issue 巻 7, p. 26-36, 発行日 1978-01 |