Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1995-09-01 |
タイトル |
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タイトル |
CODA 〓 OF LOCAL EARTHQUAKES OBSERVED ON THE SOUTHEAST TIBETAN PLATEAU : COMPARISON WITH LUTZOW-HOLM BAY REGION, EAST ANTARCTICA |
言語 |
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言語 |
eng |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ID登録 |
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ID登録 |
10.15094/00002781 |
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ID登録タイプ |
JaLC |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
論文名よみ |
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その他のタイトル |
CODA 〓 OF LOCAL EARTHQUAKES OBSERVED ON THE SOUTHEAST TIBETAN PLATEAU : COMPARISON WITH LUTZOW-HOLM BAY REGION, EAST ANTARCTICA |
著者名よみ |
アカマツ, ジュンペイ
カク, ヒロユキ
カナオ, マサキ
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著者名(英) |
AKAMATSU, Junpei
KAKU, Hiroyuki
KANAO, Masaki
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著者所属(英) |
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en |
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Disaster Prevention Research Institute, Kyoto University |
著者所属(英) |
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en |
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Graduate School of Science, Kyoto University |
著者所属(英) |
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en |
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National Institute of Polar Research |
抄録(英) |
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内容記述タイプ |
Other |
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内容記述 |
Coda 〓 of local earthquakes observed at Bomi, southeast Tibetan plateau was evaluated using a single scattering model and compared with that in the Lutzow-Holm Bay region, East Antarctica. The results obtained are : (1) 〓^<-1> for short lapse time (SLT) from 5 to 50s shows large dependence on frequency; (2) 〓^<-1> for SLT in the Tibetan plateau region is larger than that in the Lutzow-Holm Bay region; (3) 〓^<-1> for long lapse time from 80 to 160s in the Tibetan region is nearly the same as that in the Lutzow-Holm Bay region. Although there is a need for discussion of coda excitation modeling, all these features are consistent with the general relation between coda 〓 and regional tectonic activities. |
雑誌書誌ID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA1072335X |
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences
巻 8,
p. 15-24,
発行日 1995-09
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出版者 |
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出版者 |
National Institute of Polar Research |