WEKO3
アイテム
{"_buckets": {"deposit": "0d5ea689-0275-4086-bbf5-f56178c2bc77"}, "_deposit": {"created_by": 4, "id": "3053", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "3053"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00003053", "sets": ["437"]}, "author_link": ["4411", "43382", "43385", "43384", "43383"], "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1999-10", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "226", "bibliographicPageStart": "215", "bibliographicVolumeNumber": "12", "bibliographic_titles": [{"bibliographic_title": "Polar geoscience"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Nishimura,Akira", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "4411", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Tanahashi,Manabu", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "43382", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Tokuhashi,Shuichi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "43383", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Oda,Hirokuni", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "43384", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Nakasone,Toru", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "43385", "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": "Sediment core samples are described from the area adjacent to Anvers Island north of the Antarctic Peninsula. The sequence is divided into three lithologic units, siliceous mud, alternation sandy silt and siliceous mud, and sandy silt with gravel, in descending order. These units suggest sedimentary environmental changes from under the ice sheet, to marine with highly influenced by fluctuation of the ice sheet, and finally to open marine. These major environmental changes are dated to ca. 16 ka BP and ca. 11.5 ka BP, respectively, based on uncorrected radiocarbon ages of organic carbon.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00003053", "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": "AA1130866X", "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": "Geological Survey of Japan/Geological Survey of Japan/Geological Survey of Japan/Geological Survey of Japan/awasaki Geological Engineering Co., Ltd."}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1999-10-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00000044170.pdf", "filesize": [{"value": "1.3 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 1300000.0, "url": {"label": "KJ00000044170", "url": "https://nipr.repo.nii.ac.jp/record/3053/files/KJ00000044170.pdf"}, "version_id": "65676208-88b4-4019-8479-8a79c9bf696a"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "late Quaternary", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "AMS radiocarbon ages", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "sea bottom sediments", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Antarctic Peninsula", "subitem_subject_language": "en", "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": "Marine sediment cores from the continental shelf around Anvers Island, Antarctic Peninsula region", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Marine sediment cores from the continental shelf around Anvers Island, Antarctic Peninsula region"}]}, "item_type_id": "1", "owner": "4", "path": ["437"], "permalink_uri": "https://doi.org/10.15094/00003053", "pubdate": {"attribute_name": "公開日", "attribute_value": "1999-10-01"}, "publish_date": "1999-10-01", "publish_status": "0", "recid": "3053", "relation": {}, "relation_version_is_last": true, "title": ["Marine sediment cores from the continental shelf around Anvers Island, Antarctic Peninsula region"], "weko_shared_id": 4}
Marine sediment cores from the continental shelf around Anvers Island, Antarctic Peninsula region
https://doi.org/10.15094/00003053
https://doi.org/10.15094/00003053bdd90e0e-0998-4d37-bdba-1503fb894b39
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000044170 (1.3 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1999-10-01 | |||||
タイトル | ||||||
タイトル | Marine sediment cores from the continental shelf around Anvers Island, Antarctic Peninsula region | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | late Quaternary | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | AMS radiocarbon ages | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | sea bottom sediments | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Antarctic Peninsula | |||||
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 | 10.15094/00003053 | |||||
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) | |||||
著者名(英) |
Nishimura,Akira
× Nishimura,Akira× Tanahashi,Manabu× Tokuhashi,Shuichi× Oda,Hirokuni× Nakasone,Toru |
|||||
著者所属(英) | ||||||
en | ||||||
Geological Survey of Japan/Geological Survey of Japan/Geological Survey of Japan/Geological Survey of Japan/awasaki Geological Engineering Co., Ltd. | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Sediment core samples are described from the area adjacent to Anvers Island north of the Antarctic Peninsula. The sequence is divided into three lithologic units, siliceous mud, alternation sandy silt and siliceous mud, and sandy silt with gravel, in descending order. These units suggest sedimentary environmental changes from under the ice sheet, to marine with highly influenced by fluctuation of the ice sheet, and finally to open marine. These major environmental changes are dated to ca. 16 ka BP and ca. 11.5 ka BP, respectively, based on uncorrected radiocarbon ages of organic carbon. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 12, p. 215-226, 発行日 1999-10 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |