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LEVELING SURVEY ON EAST ONGUL ISLAND, ANTARCTICA AND ITS IMPLICATIONS
https://doi.org/10.15094/00002840
https://doi.org/10.15094/000028401c0f1c44-3f6c-470f-be34-5fd14020752f
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002368113 (587.4 kB)
|
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 | LEVELING SURVEY ON EAST ONGUL ISLAND, ANTARCTICA AND ITS IMPLICATIONS | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | leveling survey | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | crustal uplift | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | oceanic tide | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | elevated beach | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | local earthquake | |||||
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 | 10.15094/00002840 | |||||
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 | LEVELING SURVEY ON EAST ONGUL ISLAND, ANTARCTICA AND ITS IMPLICATIONS | |||||
著者名よみ |
カミヌマ, カツタダ
× カミヌマ, カツタダ× キムラ, イサオ |
|||||
著者名(英) |
KAMINUMA, Katsutada
× KAMINUMA, Katsutada× KIMURA, Isao |
|||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
The Geographical Survey Institute | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | A route for a repeat leveling survey was established on East Ongul Island (69°S, 39°E), East Antarctica by the 20th Japanese Antarctic Research Expedition (JARE-20) in 1979 and JARE-23 in 1982. One of the purposes for establishing the leveling route is to detect crustal movement in Antarctica. The leveling measurements were repeated in 1992 and in 1996. Because of the time limitation, only 2.3km out of the total length of 5.3km route was surveyed. The mean square error every one kilometer is obtained as ±0.57mm. Bench Mark (BM) 1040 is taken as a reference point which is also the reference point for oceanic tide observations at Syowa Station and is located on the westernmost point of the route. The height change between measurements in 1982 and 1996 at the easternmost point BM 1026 is -0.2mm. No appreciable change of height at BM 1026 was observed for the last 14 years. This fact supports the idea of a block movement of crust which is explained as a process of crustal uplift after deglaciation. | |||||
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. 19-25, 発行日 1997-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |