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INTERMITTENT MICRO-SEISMIC ACTIVITIES AROUND SYOWA STATION, EAST ANTARCTICA
https://doi.org/10.15094/00002681
https://doi.org/10.15094/000026810a67e7d7-0150-481e-9d44-96072f4b2739
名前 / ファイル | ライセンス | アクション |
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KJ00002368264 (1.8 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1991-09-01 | |||||
タイトル | ||||||
タイトル | INTERMITTENT MICRO-SEISMIC ACTIVITIES AROUND SYOWA STATION, EAST ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
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 | 10.15094/00002681 | |||||
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 | INTERMITTENT MICRO-SEISMIC ACTIVITIES AROUND SYOWA STATION, EAST ANTARCTICA | |||||
著者名よみ |
カミヌマ, カツタダ
× カミヌマ, カツタダ× アカマツ, ジュンペイ |
|||||
著者名(英) |
KAMINUMA, Katsutada
× KAMINUMA, Katsutada× AKAMATSU, Junpei |
|||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Disaster Prevention Research Institute, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Antarctica seems to be the only one aseismic continent on the earth. No large earthquakes of which magnitude is larger than 5 have been located in the Antarctic Continent, although, small and micro-earthquake activities are detected by the worldwide seismic network and some local networks in the Antarctic. A tripartite seismic array was established at Syowa Station (69°S, 39°E) in 1987 for studying the local seismicity. Ten micro-earthquakes were recorded by the tripartite array during 19 months from June 1987 to January 1989. These earthquakes are located in the geological and geophysical structural boundaries of the coastal area in the Antarctic Continent and offshore. Other four earthquakes were recorded during 9 months from February to October, 1989. The local earthquakes around Syowa Station occurred intermittently. There are many well-developed elevated beaches and marine terraces in the coastal ice-free area of the Antarctic Continent. These have been formed by the relative lowering of sea level, caused by the crustal uplift after the deglaciation. The local micro-earthquakes seem to have been caused by the tectonic stress which was accumulated by the slow-moving crustal uplift. As local earthquakes occur intermittently, it seems that the crustal uplift is not a linear movement but an intermittent one, and the local earthquakes occur corresponding with the intermittent crustal uplift. | |||||
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 5, p. 1-10, 発行日 1991-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |