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Crust and upper mantle structure in East Antarctica from phase velocity of Rayleigh wave
https://doi.org/10.15094/00003072
https://doi.org/10.15094/0000307236098a05-208f-4911-831d-fcad8dc363e5
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000044189 (758.9 kB)
|
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 | Crust and upper mantle structure in East Antarctica from phase velocity of Rayleigh wave | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | East Antarctica | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | crust | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | upper mantle | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Rayleigh wave | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | phase velocity | |||||
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 | 10.15094/00003072 | |||||
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) |
Kobayashi, Reiji
× Kobayashi, Reiji |
|||||
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 | Phase velocities of Rayleigh waves in East Antarctica are accurately measured by using the two-station method in this study Rayleigh waves from the 16 May 1995 Loyalty Islands earthquake (23 05°S, 17000°E, Mv, 77) recorded at Dumont d'Urville (66 665°S, 140010°E) and Syowa (69 009°S, 39 592°E) stations, Antarctica, are used The path runs through the central part of East Antarctica The measured phase velocities at periods shorter than 40 s are higher than those shown by a previous study in which the paths run through the western part of East Antarctica It is suggested that the seismic velocity in the crust beneath the central part of East Antaictica is faster or the crustal thickness is thinner than that beneath the western part A preliminary 1-D seismic stiucture model of the crust and uppermost mantle beneath East Antarctica is inferred from the measured phase velocities The velocity in the crust and the uppermost mantle is higher than the A-1 model and PREM, respectively | |||||
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. 158-164, 発行日 2000-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |