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Local earthquake activity corroborates the crustal uplift, and it is an intermittent phenomenon. Sea level falling of 4.5mm/y was found using data in 1975-1992. This falling rate is consistent with geomorphological data. If the crustal uplift of 5mm/y continues for 10 years, the total uplift obtained will be 5cm. The total amount of the vertical crustal uplift would produce a change of about 15 μGal in gravity. Repeated measurements of absolute gravity over many years might detect absolute value of vertical crustal movement. Absolute gravity measurements at Syowa Station were made to establish one of the IAGBN (International Absolute Gravity Basestation Network) stations. Continuous observation by a SCG (Superconducting Gravimeter) was also started at Syowa Station. The SCG observation is believed to provide the highest sensitivity and highest resolution data for study of vertical crustal movement. 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ON THE POSSIBILITY OF DETECTING ABSOLUTE CRUSTAL UPLIFT AT SYOWA STATION, ANTARCTICA
https://doi.org/10.15094/00002820
https://doi.org/10.15094/00002820abbe69fe-8264-4bb2-b0da-b26b932c1514
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00002409867 (684.9 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 | ON THE POSSIBILITY OF DETECTING ABSOLUTE CRUSTAL UPLIFT AT SYOWA STATION, ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | local earthquake | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | raised beach | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | sea level change | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | gravity change | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | superconducting gravimeter | |||||
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 | 10.15094/00002820 | |||||
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 | ON THE POSSIBILITY OF DETECTING ABSOLUTE CRUSTAL UPLIFT AT SYOWA STATION, ANTARCTICA | |||||
著者名よみ |
カミヌマ, カツタダ
× カミヌマ, カツタダ |
|||||
著者名(英) |
KAMINUMA, Katsutada
× KAMINUMA, Katsutada |
|||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | There is a great deal of evidence concerning crustal uplift, after deglaciation, in the vicinity of Syowa Station (69.0°S, 39.6°E) from tide gauge data, seismic evidence, raised beaches, marine terraces, etc. The geomorphological and tide gauge data show that crustal uplift is going on around Syowa Station. Local earthquake activity corroborates the crustal uplift, and it is an intermittent phenomenon. Sea level falling of 4.5mm/y was found using data in 1975-1992. This falling rate is consistent with geomorphological data. If the crustal uplift of 5mm/y continues for 10 years, the total uplift obtained will be 5cm. The total amount of the vertical crustal uplift would produce a change of about 15 μGal in gravity. Repeated measurements of absolute gravity over many years might detect absolute value of vertical crustal movement. Absolute gravity measurements at Syowa Station were made to establish one of the IAGBN (International Absolute Gravity Basestation Network) stations. Continuous observation by a SCG (Superconducting Gravimeter) was also started at Syowa Station. The SCG observation is believed to provide the highest sensitivity and highest resolution data for study of vertical crustal movement. Using the absolute gravimeter together with the SCG will provide significant insight into the absolute elevation change. | |||||
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. 16-23, 発行日 1996-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |