雲仙火山周辺域における相対応力場と1990-1995年噴火活動
河野, 裕希;松本, 聡;松島, 健;植平, 賢司;清水, 洋;馬越, 孝道
Permalink : http://hdl.handle.net/2115/38165
JaLCDOI : 10.14943/gbhu.72.363
Abstract
We investigated a stress field around the magma chamber beneath Unzen Volcano, Kyushu, Japan, which erupted from 1990 until 1995, by using a stress-tensor inversion method. We used P wave polarity data of seismograms by earthquakes occurred during 1985-1999 for analysis. Our result clearly indicated that there were no changes in stress field during the period except for during 1986-1988. This suggested that the magma intrusion into shallower depths did not affect the stress field in this region. Clear change in stress field was observed during 1986-1988. This might be explained by applying the meshtexture crack model proposed by Hill (1977).
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