書誌事項
- タイトル別名
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- Seismological Investigation of the Events Occurred in Sakurajima Volcano : Analysis of Seismic Data from Stations at Various Elevations
- サクラジマ カザン ニ オケル ジシン カンソク コウドサ オ コウリョ ニ
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An improved method is introduced to analyze travel time data from a seismic array composed of stations at various elevations, and is applied to the data of volcanic earthquakes or tremors occurred in Sakurajima Volcano. By this method, arrival azimuths and apparent velocities of seismic waves, and wave velocities in the surface layer are estimated with their errors. Several events are observed with anomalously low wave velocity in the surface layer. This is probably attributed to apparent late arrival times at the station which is highest in altitude and is nearest to the Minami-dake Crater of the Volcano. From the analysis of explosion earthquakes, the existence of such low wave velocity is denied and P wave velocity in the surface layer is estimated as 500m/sec or over. Predominant frequencies of waves are 4 to 6 Hz for the events of which relatively dominant initial phases are recognized. 0n the other hand, so-called “B-type” earthquakes or continuous tremors have the frequency around 2.5 to 4 Hz.
収録刊行物
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- 火山.第2集
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火山.第2集 22 (1), 1-12, 1977
特定非営利活動法人 日本火山学会
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詳細情報 詳細情報について
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- CRID
- 1390001206121658368
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- NII論文ID
- 110002995060
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- NII書誌ID
- AN10512786
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- ISSN
- 04534360
- 24330590
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- NDL書誌ID
- 1824826
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可