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Deep low-frequency tremors as a proxy for slip monitoring at plate interface
https://doi.org/10.24517/00011070
https://doi.org/10.24517/000110706c0b8b04-6b41-40a1-93b6-8ac48b798628
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
SC-PR-HIRAMATSU-Y-13304.pdf (627.3 kB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2017-10-03 | |||||||||
| タイトル | ||||||||||
| タイトル | Deep low-frequency tremors as a proxy for slip monitoring at plate interface | |||||||||
| 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 | journal article | |||||||||
| ID登録 | ||||||||||
| ID登録 | 10.24517/00011070 | |||||||||
| ID登録タイプ | JaLC | |||||||||
| 著者 |
Hiramatsu, Yoshihiro
× Hiramatsu, Yoshihiro× Watanabe, Tomoko× Obara, Kazushige |
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| 著者別表示 |
平松, 良浩
× 平松, 良浩
× 小原, 一成
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| 提供者所属 | ||||||||||
| 内容記述タイプ | Other | |||||||||
| 内容記述 | 金沢大学理工研究域自然システム学系 | |||||||||
| 書誌情報 |
Geophysical Research Letters 巻 35, 号 13, p. L13304, 発行日 2008-07-16 |
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| ISSN | ||||||||||
| 収録物識別子タイプ | ISSN | |||||||||
| 収録物識別子 | 0094-8276 | |||||||||
| NCID | ||||||||||
| 収録物識別子タイプ | NCID | |||||||||
| 収録物識別子 | AA00657102 | |||||||||
| DOI | ||||||||||
| 関連タイプ | isVersionOf | |||||||||
| 識別子タイプ | DOI | |||||||||
| 関連識別子 | 10.1029/2008GL034342 | |||||||||
| 出版者 | ||||||||||
| 出版者 | American Geophysical Union (AGU) | |||||||||
| 抄録 | ||||||||||
| 内容記述タイプ | Abstract | |||||||||
| 内容記述 | We propose a new method to monitor slip at the plate interface using non-volcanic deep-low frequency (DLF) tremors. We assume that a DLF tremor is the superposition of frequently excited intermittent events, meaning that the envelope of the reduced displacement of the DLF tremor provides an apparent moment rate function. We estimate a conversion factor from the apparent moment to the seismic moment with an assumption that a total size of DLF tremors of an episode is proportional to the size of corresponding slow slip event (SSE). The cumulative seismic moment estimated by DLF tremors is consistent with that estimated from geodetic methods and provides appropriate slip and slip rate at the plate interface. This proves our assumptions and demonstrates that DLF tremors are useful tool for realtime monitoring of the slip at the plate interface. Copyright 2008 by the American Geophysical Union. | |||||||||
| 著者版フラグ | ||||||||||
| 出版タイプ | AM | |||||||||
| 出版タイプResource | http://purl.org/coar/version/c_ab4af688f83e57aa | |||||||||
| 関連URI | ||||||||||
| 識別子タイプ | DOI | |||||||||
| 関連識別子 | http://dx.doi.org/10.1029/2008GL034342 | |||||||||
