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SEDIMENTOLOGICAL STUDY OF THE SEA BOTTOM SEDIMENTS IN AND AROUND THE ROSS SEA CONTINENTAL SHELF, ANTARCTICA
https://doi.org/10.15094/00002828
https://doi.org/10.15094/000028283f83e15d-6cdb-4ae3-a65e-0fc13461080c
名前 / ファイル | ライセンス | アクション |
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KJ00002409875 (1.1 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1996-09-01 | |||||
タイトル | ||||||
タイトル | SEDIMENTOLOGICAL STUDY OF THE SEA BOTTOM SEDIMENTS IN AND AROUND THE ROSS SEA CONTINENTAL SHELF, ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Ross Sea | |||||
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 | Late Quaternary | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | sea bottom sediments | |||||
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 | 10.15094/00002828 | |||||
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 | SEDIMENTOLOGICAL STUDY OF THE SEA BOTTOM SEDIMENTS IN AND AROUND THE ROSS SEA CONTINENTAL SHELF, ANTARCTICA | |||||
著者名よみ |
ニシムラ, アキラ
× ニシムラ, アキラ× ユアサ, マコト× ナカソネ, トオル× ナカハラ, マサキ× イオカ, ノボル |
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著者名(英) |
NISHIMURA, Akira
× NISHIMURA, Akira× YUASA, Makoto× NAKASONE, Toru× NAKAHARA, Masaki× IOKA, Noboru |
|||||
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 | ||||||
Kawasaki Chishitsu Co. Ltd. | ||||||
著者所属(英) | ||||||
en | ||||||
Kawasaki Chishitsu Co. Ltd. | ||||||
著者所属(英) | ||||||
en | ||||||
Kansai Environmental Engineering Center Co. Ltd. | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Sediment cores collected in and around the Ross Sea, Antarctica, are described and discussed based on sedimentological data, such as visual descriptions, sedimentary structures, magnetic susceptibility, sand contents, and water content. On the Ross Sea Continental Shelf, the core sequences contain two lithologic units, soft diatomaceous mud in the upper and compound glacio-marine sediments in the lower. The lower lithologic unit suggests that highly ice-sheet influenced sedimentation existed in glacial times in the Ross Sea. The core sequences on the continental slope and deep-sea basins off the Ross Sea comprise foraminiferal ooze, siliceous mud, and terrigenous mud, sometimes with laminated parts. The laminated parts of the core sequences suggest that strengthened bottom water influenced sedimentation, probably in glacial times. The sedimentary environment in the Late Quaternary is reconstructed based on the core data. | |||||
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 9, p. 117-126, 発行日 1996-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |