WEKO3
アイテム
南極昭和基地附近の海洋地質学展望(極地海洋学シンポジウム)
https://doi.org/10.15094/00007423
https://doi.org/10.15094/0000742302404e21-9e20-4737-8f68-a48ea8d113f5
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002476345 (4.1 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||||||
---|---|---|---|---|---|---|---|---|---|---|
公開日 | 1966-12-01 | |||||||||
タイトル | ||||||||||
タイトル | 南極昭和基地附近の海洋地質学展望(極地海洋学シンポジウム) | |||||||||
タイトル | ||||||||||
言語 | en | |||||||||
タイトル | CRITICAL REVIEW OF THE MARINE GEOLOGICAL RESULTS AROUND THE SYOWA STATION OBTAINED DURING THE FIRST SERIES OF THE JAPANESE ANTARCTIC RESEARCH EXPEDITIONS (1956-1962) (Reports read at the Symposium on Polar Oceanography) | |||||||||
言語 | ||||||||||
言語 | jpn | |||||||||
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 | 10.15094/00007423 | |||||||||
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 | ナンキョク ショウワ キチ フキン ノ カイヨウ チシツガク テンボウ キョクチ カイヨウガク シンポジウム | |||||||||
著者名(日) |
内尾, 高保
× 内尾, 高保
|
|||||||||
著者名(英) |
UCHIO, Takayasu
× UCHIO, Takayasu
|
|||||||||
著者所属(日) | ||||||||||
東京大学工学部資源開発工学教室 | ||||||||||
著者所属(英) | ||||||||||
en | ||||||||||
Petroleum Engineering Institute, the University of Tokyo | ||||||||||
抄録(英) | ||||||||||
内容記述タイプ | Other | |||||||||
内容記述 | The first series of the Japanese Antarctic Research Expeditions was completed in 1962, and the second series started in 1965 This is a critical review of all papers on marine geology so far published by Japanese scientists, and also of some papers by American and Soviet scientists related to the Japanese works It is the writer's desire that the review, pointing out the problems to be solved, might be of some use for the second series of the expeditions Conflicting interpretations of the results among the scientists are discussed They are, (1) origin of very deep continental shelf (What is the cause of very deep continental shelf around the Antarctica ? Fault or isostatic subsidence due to very thick continental ice cap, or else?), (2) glacial basins or submarine canyons (Are the depressions in Amundsen and Lutzow-Holm Bays glacial basins or submarine canyons formed by subaerial erosion or faulting?), (3) Tertiary ice-rafted gravels (If the gravels are Tertiary in age, they are very important to the geological history of Antarctica), (4) Quaternary marine sediments on the East Ongul Island (Are they really raised beach deposits or sediments deposited at depth of about 100m?) The other topics here included are (1) grain size, heavy mineral, clay mineral, and organic material distributions of the sediments, (2) total carbonate and organic production, and (3) oceanographic interpretation of Foraminifera distribution | |||||||||
雑誌書誌ID | ||||||||||
収録物識別子タイプ | NCID | |||||||||
収録物識別子 | AN00181831 | |||||||||
ISSN | ||||||||||
収録物識別子タイプ | ISSN | |||||||||
収録物識別子 | 00857289 | |||||||||
書誌情報 |
南極資料 巻 27, p. 2186-2195, 発行日 1966-12 |
|||||||||
国際十進分類法 | ||||||||||
主題Scheme | UDC | |||||||||
主題 | 551.46 | |||||||||
出版者 | ||||||||||
出版者 | 国立極地研究所 |