WEKO3
アイテム
{"_buckets": {"deposit": "972cdfff-3c8a-4614-b09e-55813b1f2a0c"}, "_deposit": {"created_by": 4, "id": "2598", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "2598"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00002598", "sets": ["417"]}, "author_link": ["2402", "2403"], "item_1_alternative_title_5": {"attribute_name": "論文名よみ", "attribute_value_mlt": [{"subitem_alternative_title": "COASTAL GEOMORPHOLOGY OF SEYMOUR ISLAND (MARAMBIO ISLAND), ANTARCTIC PENINSULA REGION"}]}, "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1989-09", "bibliographicIssueDateType": "Issued"}, "bibliographicPageStart": "145", "bibliographicVolumeNumber": "3", "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": "オモト, クニオ"}], "nameIdentifiers": [{"nameIdentifier": "2402", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "OMOTO, Kunio", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "2403", "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": "On the northern coast of Marambio Island (Seymour Island), there develop periglacial landforms such as frost domes, ice-wedges, ice-wedge casts, gelifluction terraces and lobes. There also develop raised beach topography at several levels. In order to estimate formative ages of them, five algae samples and three fine marine sediments were collected from the coast. The radiocarbon ages of them revealed that the frost domes and the lower raised beaches were formed during the late Holocene.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00002598", "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": "Department of Geography, College of Humanities and Sciences, Nihon University"}]}, "item_1_text_3": {"attribute_name": "記事種別(英)", "attribute_value_mlt": [{"subitem_text_language": "en", "subitem_text_value": "ABSTRACT"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1989-09-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00002368188.pdf", "filesize": [{"value": "48.7 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 48700.0, "url": {"label": "KJ00002368188", "url": "https://nipr.repo.nii.ac.jp/record/2598/files/KJ00002368188.pdf"}, "version_id": "d80f248e-4d8a-45f3-9783-ca2c16bf0a03"}]}, "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": "COASTAL GEOMORPHOLOGY OF SEYMOUR ISLAND (MARAMBIO ISLAND), ANTARCTIC PENINSULA REGION", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "COASTAL GEOMORPHOLOGY OF SEYMOUR ISLAND (MARAMBIO ISLAND), ANTARCTIC PENINSULA REGION"}]}, "item_type_id": "1", "owner": "4", "path": ["417"], "permalink_uri": "https://doi.org/10.15094/00002598", "pubdate": {"attribute_name": "公開日", "attribute_value": "1989-09-01"}, "publish_date": "1989-09-01", "publish_status": "0", "recid": "2598", "relation": {}, "relation_version_is_last": true, "title": ["COASTAL GEOMORPHOLOGY OF SEYMOUR ISLAND (MARAMBIO ISLAND), ANTARCTIC PENINSULA REGION"], "weko_shared_id": 4}
COASTAL GEOMORPHOLOGY OF SEYMOUR ISLAND (MARAMBIO ISLAND), ANTARCTIC PENINSULA REGION
https://doi.org/10.15094/00002598
https://doi.org/10.15094/000025985120257d-008f-4b43-8cc5-4be9f4546cb9
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002368188 (48.7 kB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1989-09-01 | |||||
タイトル | ||||||
タイトル | COASTAL GEOMORPHOLOGY OF SEYMOUR ISLAND (MARAMBIO ISLAND), ANTARCTIC PENINSULA REGION | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00002598 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
記事種別(英) | ||||||
en | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | COASTAL GEOMORPHOLOGY OF SEYMOUR ISLAND (MARAMBIO ISLAND), ANTARCTIC PENINSULA REGION | |||||
著者名よみ |
オモト, クニオ
× オモト, クニオ |
|||||
著者名(英) |
OMOTO, Kunio
× OMOTO, Kunio |
|||||
著者所属(英) | ||||||
en | ||||||
Department of Geography, College of Humanities and Sciences, Nihon University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | On the northern coast of Marambio Island (Seymour Island), there develop periglacial landforms such as frost domes, ice-wedges, ice-wedge casts, gelifluction terraces and lobes. There also develop raised beach topography at several levels. In order to estimate formative ages of them, five algae samples and three fine marine sediments were collected from the coast. The radiocarbon ages of them revealed that the frost domes and the lower raised beaches were formed during the late Holocene. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 3, p. 145, 発行日 1989-09 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |