桜島の噴火活動と火山性地震のスペクトル
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概要
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Spectral features of seismograms are investigated for the events closely related to four eruptions on February 26, 27 and 28, 1975, based upon an assumption that variations in spectral compositions can be interpreted as the changes in focal depths of events. A swarm of volcanic earthquakes started about 17 minutes before the eruption of 03h55m (JST) on February 26. The generation of these events is correlated to the explosion mechanism because the highest activity of the swarm occurred at the eruption and because focal depths of the events were as deep as that of the explosion earthquake. Two eruptions occurred at 03h35m and 04h48m on February 27. Events related to the latter eruption are readily distinguished from those following the former by the predominant frequency of power spectrum, spectral composition, running spectrum or seismic activity. Energy sources of the two eruptions were at small depth under the crater. Precursory activities of strong B-type volcanic earthquakes occurred 8 minutes before the violent eruption of 00h16m on February 28. Running spectra of Ct-type, low predominant frequency in the spectrum and little emission of volcanic smoke imply that a great deal of energy might be interrupted at a depth from flowing up.
- 1979-12-01
著者
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角田 寿喜
鹿児島大学
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角田 寿喜
鹿児島大学理学部
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KOZAWA Takeshi
JGI Inc.
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野中 義彦
千葉県立京葉高等学校
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Kanazawa Toshihiko
Laboratory For Earthquake Chemistry The University Of Tokyo
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Kakuta Toshiki
Faculty Of Science Kagoshima University
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野中 義彦
千葉県袖ケ浦高
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