Tsunami waveform analyses of the 2006 underthrust and 2007 outer-rise Kurile earthquakes
書誌事項
- 公開日
- 2008-01-02
- 資源種別
- journal article
- 権利情報
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- https://creativecommons.org/licenses/by-nc-sa/2.5/
- DOI
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- 10.5194/adgeo-14-129-2008
- 公開者
- Copernicus GmbH
説明
<jats:p>Abstract. The 2006 large interplate Kurile earthquake proved that the entire plate interface of the Kurile-Kamchatka subduction zone was strongly coupled from Hokkaido, Japan, to Kamchatka, Russia. The seismic moment of the 2006 Kurile earthquake estimated from ten tsunami waveforms is 3.1×1021 Nm (Mw=8.3). This estimate is consistent with the seismic moment estimated from the seismological data in the Global CMT catalog. The computed tsunami propagation indicates that scattering of the tsunami waves occurred at the shallow region near the Emperor Ridge. The computed tsunami propagation also indicates that large later tsunami waves observed at Crescent City is caused by the shallow region along the Mendocino Fracture Zone. The seismic moment of the 2007 outer-rise Kurile earthquake estimated from tsunami waveforms is 1.0×1021 Nm (Mw=8.0). This estimate is also consistent with the seismic moment in the Global CMT catalog.</jats:p>
収録刊行物
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- Advances in Geosciences
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Advances in Geosciences 14 129-134, 2008-01-02
Copernicus GmbH
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詳細情報 詳細情報について
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- CRID
- 1362825895652695936
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- NII論文ID
- 10025367446
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- ISSN
- 16807359
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- 資料種別
- journal article
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- データソース種別
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- Crossref
- CiNii Articles
- KAKEN
- OpenAIRE
