WEKO3
アイテム
{"_buckets": {"deposit": "f11cd40c-a881-4fd2-91da-016af79e5979"}, "_deposit": {"created_by": 4, "id": "2842", "owners": [4], "pid": {"revision_id": 0, "type": "depid", "value": "2842"}, "status": "published"}, "_oai": {"id": "oai:nipr.repo.nii.ac.jp:00002842", "sets": ["424"]}, "author_link": ["3558", "3556", "3561", "3554", "3563", "3557", "3559", "3562", "3555", "3560"], "item_1_alternative_title_5": {"attribute_name": "論文名よみ", "attribute_value_mlt": [{"subitem_alternative_title": "PRELIMINARY REPORT OF THE TH95 GEOLOGICAL AND GEOPHYSICAL SURVEY RESULTS IN THE ROSS SEA AND DUMONT D\u0027URVILLE SEA"}]}, "item_1_biblio_info_14": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1997-09", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "58", "bibliographicPageStart": "36", "bibliographicVolumeNumber": "10", "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": "タナハシ, マナブ"}], "nameIdentifiers": [{"nameIdentifier": "3554", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "イシハラ, タケミ"}], "nameIdentifiers": [{"nameIdentifier": "3555", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ユアサ, マコト"}], "nameIdentifiers": [{"nameIdentifier": "3556", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ムラカミ, フミトシ"}], "nameIdentifiers": [{"nameIdentifier": "3557", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ニシムラ, アキラ"}], "nameIdentifiers": [{"nameIdentifier": "3558", "nameIdentifierScheme": "WEKO"}]}]}, "item_1_creator_8": {"attribute_name": "著者名(英)", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "TANAHASHI, Manabu", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "3559", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "ISHIHARA, Takemi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "3560", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "YUASA, Makoto", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "3561", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "MURAKAMI, Fumitoshi", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "3562", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "NISHIMURA, Akira", "creatorNameLang": "en"}], "nameIdentifiers": [{"nameIdentifier": "3563", "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": "Geophysical and geological surveys of the TH95 cruise on the R/V HAKUREI-MARU, in the abyssal basin and the continental rise area of Dumont d\u0027Urville Sea (DDS) offshore of Adelie and Wilkes Land, and Victoria Land Basin (VLB) in the western part of the Ross Sea continental shelf, were carried out in the 1995-96 austral summer season. The deformed very thick sedimentary sequences, which are interpreted to have been deposited in the pre-rift and rifting stage, are revealed under thick post-break-up pelagic sedimentary sequences in DDS. There are several basement highs of (1) the igneous basement, including ultra-mafic rocks, which was uplifted in associated with the fracture zone, (2) the uplifted oceanic basement which is deformed by the normal fault, (3) the structural high with anomalous basement, which is interpreted as a piece of micro-continent, in DDS. These phenomena suggest the wide area of DDS is underlain by the characteristic intermediate type of crust between oceanic and continental. Even the deep structure of most of the Ross Sea continental shelf is not clear by the strong sea bottom multiples, more than 7km of thick sedimentary sequences in VLB is confirmed with MCS and OBS survey. The sequences are deformed by the extensional normal faults along the western margin and the Terror Rift. Geological samples which were recovered in the VLB gave important evidence of the late Ross Ice Shelf advance and retreat history.", "subitem_description_type": "Other"}]}, "item_1_identifier_registration": {"attribute_name": "ID登録", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15094/00002842", "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": "Technology Research Center, Japan National Oil Corporation"}, {"subitem_text_language": "en", "subitem_text_value": "Geological Survey of Japan"}, {"subitem_text_language": "en", "subitem_text_value": "Geological Survey of Japan"}, {"subitem_text_language": "en", "subitem_text_value": "Geological Survey of Japan"}, {"subitem_text_language": "en", "subitem_text_value": "Geological Survey of Japan"}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "1997-09-01"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "KJ00002368115.pdf", "filesize": [{"value": "2.8 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_6", "mimetype": "application/pdf", "size": 2800000.0, "url": {"label": "KJ00002368115", "url": "https://nipr.repo.nii.ac.jp/record/2842/files/KJ00002368115.pdf"}, "version_id": "671fc6a9-e227-42f0-a978-66a239f06228"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "Wilkes Land margin", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Dumont d\u0027Urville Sea", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Victoria Land Basin", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "marine geological and geophysical surveys", "subitem_subject_language": "en", "subitem_subject_scheme": "Other"}, {"subitem_subject": "sedimentary sequences", "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": "PRELIMINARY REPORT OF THE TH95 GEOLOGICAL AND GEOPHYSICAL SURVEY RESULTS IN THE ROSS SEA AND DUMONT D\u0027URVILLE SEA", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "PRELIMINARY REPORT OF THE TH95 GEOLOGICAL AND GEOPHYSICAL SURVEY RESULTS IN THE ROSS SEA AND DUMONT D\u0027URVILLE SEA"}]}, "item_type_id": "1", "owner": "4", "path": ["424"], "permalink_uri": "https://doi.org/10.15094/00002842", "pubdate": {"attribute_name": "公開日", "attribute_value": "1997-09-01"}, "publish_date": "1997-09-01", "publish_status": "0", "recid": "2842", "relation": {}, "relation_version_is_last": true, "title": ["PRELIMINARY REPORT OF THE TH95 GEOLOGICAL AND GEOPHYSICAL SURVEY RESULTS IN THE ROSS SEA AND DUMONT D\u0027URVILLE SEA"], "weko_shared_id": 4}
PRELIMINARY REPORT OF THE TH95 GEOLOGICAL AND GEOPHYSICAL SURVEY RESULTS IN THE ROSS SEA AND DUMONT D'URVILLE SEA
https://doi.org/10.15094/00002842
https://doi.org/10.15094/000028423be63980-6f8d-4a92-9229-e378cff43b9a
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002368115 (2.8 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1997-09-01 | |||||
タイトル | ||||||
タイトル | PRELIMINARY REPORT OF THE TH95 GEOLOGICAL AND GEOPHYSICAL SURVEY RESULTS IN THE ROSS SEA AND DUMONT D'URVILLE SEA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Wilkes Land margin | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Dumont d'Urville Sea | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Victoria Land Basin | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | marine geological and geophysical surveys | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | sedimentary sequences | |||||
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 | 10.15094/00002842 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | PRELIMINARY REPORT OF THE TH95 GEOLOGICAL AND GEOPHYSICAL SURVEY RESULTS IN THE ROSS SEA AND DUMONT D'URVILLE SEA | |||||
著者名よみ |
タナハシ, マナブ
× タナハシ, マナブ× イシハラ, タケミ× ユアサ, マコト× ムラカミ, フミトシ× ニシムラ, アキラ |
|||||
著者名(英) |
TANAHASHI, Manabu
× TANAHASHI, Manabu× ISHIHARA, Takemi× YUASA, Makoto× MURAKAMI, Fumitoshi× NISHIMURA, Akira |
|||||
著者所属(英) | ||||||
en | ||||||
Technology Research Center, Japan National Oil Corporation | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey of Japan | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey of Japan | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey of Japan | ||||||
著者所属(英) | ||||||
en | ||||||
Geological Survey of Japan | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Geophysical and geological surveys of the TH95 cruise on the R/V HAKUREI-MARU, in the abyssal basin and the continental rise area of Dumont d'Urville Sea (DDS) offshore of Adelie and Wilkes Land, and Victoria Land Basin (VLB) in the western part of the Ross Sea continental shelf, were carried out in the 1995-96 austral summer season. The deformed very thick sedimentary sequences, which are interpreted to have been deposited in the pre-rift and rifting stage, are revealed under thick post-break-up pelagic sedimentary sequences in DDS. There are several basement highs of (1) the igneous basement, including ultra-mafic rocks, which was uplifted in associated with the fracture zone, (2) the uplifted oceanic basement which is deformed by the normal fault, (3) the structural high with anomalous basement, which is interpreted as a piece of micro-continent, in DDS. These phenomena suggest the wide area of DDS is underlain by the characteristic intermediate type of crust between oceanic and continental. Even the deep structure of most of the Ross Sea continental shelf is not clear by the strong sea bottom multiples, more than 7km of thick sedimentary sequences in VLB is confirmed with MCS and OBS survey. The sequences are deformed by the extensional normal faults along the western margin and the Terror Rift. Geological samples which were recovered in the VLB gave important evidence of the late Ross Ice Shelf advance and retreat history. | |||||
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 10, p. 36-58, 発行日 1997-09 |
|||||
出版者 | ||||||
出版者 | National Institute of Polar Research |