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EROSIONAL TOPOGRAPHY OBSERVED ON THE UPPER CONTINENTAL RISE, WILKES LAND, EAST ANTARCTICA
https://doi.org/10.15094/00002827
https://doi.org/10.15094/000028270f152f44-d54a-43d2-86da-7ee59f9f317b
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002409874 (750.0 kB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1996-09-01 | |||||
タイトル | ||||||
タイトル | EROSIONAL TOPOGRAPHY OBSERVED ON THE UPPER CONTINENTAL RISE, WILKES LAND, EAST ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | erosional depressions | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | upper continental rise | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | off Wilkes Land | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Antarctic margin type | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Antarctic bottom water | |||||
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 | 10.15094/00002827 | |||||
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 | EROSIONAL TOPOGRAPHY OBSERVED ON THE UPPER CONTINENTAL RISE, WILKES LAND, EAST ANTARCTICA | |||||
著者名よみ |
カガミ, ヒデオ
× カガミ, ヒデオ |
|||||
著者名(英) |
KAGAMI, Hideo
× KAGAMI, Hideo |
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著者所属(英) | ||||||
en | ||||||
Faculty of Science, Josai University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Erosional topography is recognized on the upper continental rise between 123°and 134°E off Wilkes Land, East Antarctica. Erosion of the upper continental rise up to roughly 500m is observed on seismic lines and is considered to be caused by down-slope density currents of cold shelf water or by thermohaline induced contour currents of Antarctic bottom water. Development of the abyssal channel systems is another bit of evidence that sediments are swept off the sea floor to create erosional depressions on the upper continental rise off Wilkes Land. Because these eroding currents are only active and effective at the continental margin around Antarctica, erosional depressions of the upper continental rise are responsible for formation of the Antarctic margin type. | |||||
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. 109-116, 発行日 1996-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |