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オーストラリア西岸沖の大陸斜面における堆積層構造について
https://doi.org/10.15094/00007542
https://doi.org/10.15094/0000754222683266-2930-4f5a-bfb7-d3672bd980b6
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002476464 (5.0 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 1969-03-01 | |||||
タイトル | ||||||
タイトル | オーストラリア西岸沖の大陸斜面における堆積層構造について | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | SEISMIC REFLECTION PROFILING ON THE CONTINENTAL SLOPE OF THE WESTERN AUSTRALIA | |||||
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 | 10.15094/00007542 | |||||
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 | オーストラリア セイガン オキ ノ タイリク シャメン ニ オケル タイセキソウ コウゾウ ニ ツイテ | |||||
著者名(日) |
堀田, 宏
× 堀田, 宏 |
|||||
著者名(英) |
HOTTA, Hiroshi
× HOTTA, Hiroshi |
|||||
著者所属(日) | ||||||
北海道大学理学部地球物理学教室 | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geophysics, Faculty of Science, Hokkaido University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The continuous seismic reflection profiling was made in 1965-1966 during the 7th Japanese Antarctic Research Expedition This paper reports on the structure of sediments on the continental slope along the west coast of the Australian continent, as a part of the results The pneumatic gun of Lament Geological Observatory type was used as the sound source The ship's track is given in Fig 1 Photographic records are presented in Figs 3, 4, 6 and 8. Line drawings from these photographic records are presented in Figs 5, 7, 9 and 10 In these pictures, horizontal distances are given in terms of the ship's navigation time One hour navigation of the ship gives approximately 22km of distance, as the ship ran at a rate of 12 kt during the observation Depths of the sea bottom and each reflector are given in two way reflection travel time in seconds. The whole area of observation is divided into three regions depending on the character of structure of sediments Each region is numbered from the north to the south. Schematic illustrations of Fig. 11 show the character of structure of sediments in each region This division may not have practically any geological significance, since there is only one profile running parallel to the continental slope of the Australian continent | |||||
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 34, p. 23-34, 発行日 1969-03 |
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国際十進分類法 | ||||||
主題Scheme | UDC | |||||
主題 | 551.1/.4:552 | |||||
出版者 | ||||||
出版者 | 国立極地研究所 |