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A revaluation of the seismicity in the Antarctic
https://doi.org/10.15094/00003071
https://doi.org/10.15094/000030714b38f760-aae9-4f24-9fad-c79e991ea0e1
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
KJ00000044188 (1.1 MB)
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| Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||||
|---|---|---|---|---|---|---|---|---|
| 公開日 | 2000-10-01 | |||||||
| タイトル | ||||||||
| タイトル | A revaluation of the seismicity in the Antarctic | |||||||
| 言語 | ||||||||
| 言語 | eng | |||||||
| キーワード | ||||||||
| 言語 | en | |||||||
| 主題Scheme | Other | |||||||
| 主題 | seismicity | |||||||
| キーワード | ||||||||
| 言語 | en | |||||||
| 主題Scheme | Other | |||||||
| 主題 | seismotectonics | |||||||
| 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 | icequake | |||||||
| キーワード | ||||||||
| 言語 | en | |||||||
| 主題Scheme | Other | |||||||
| 主題 | ice sheet | |||||||
| 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 | 10.15094/00003071 | |||||||
| 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) | |||||||
| 著者名(英) |
Kaminuma, Katsutada
× Kaminuma, Katsutada
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| 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 | The Antarctic Peninsula region and some volcanic regions in the Antarctic plate are regions of which the tectonic evolution has been well studied Occurences of tectonic and volcanic earthquakes in the region have been discussed from the point of view of seismotectonics As the number of seismic stations in the world has increased, so has the number of tectonic earthquakes detected in the Antarctic The seismic activity in the following three regions can be discussed from the point of view of seismotectonics or neotectomcs 1) the great earthquakes in the intraplate low seismic region, 2) microseismic activity at the edge of the continent and 3) seismic activity in Wilkes Land Some tectonic earthquakes in these regions are caused by tectonic stress accumulated by crustal deformation after deglaciation The effect of ice sheet change in Antarctica has caused such phenomena as crustal deformation, earthquake occurrence etc in the crust and upper mantle | |||||||
| 雑誌書誌ID | ||||||||
| 収録物識別子タイプ | NCID | |||||||
| 収録物識別子 | AA1130866X | |||||||
| 書誌情報 |
Polar geoscience 巻 13, p. 145-157, 発行日 2000-10 |
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| 出版者 | ||||||||
| 出版者 | National Institute of Polar Research | |||||||
