K. Tsuruga et al., SPATIAL AND TEMPORAL VARIATIONS OF VOLCANIC EARTHQUAKES AT SAKURAJIMAVOLCANO, JAPAN, Journal of volcanology and geothermal research, 75(3-4), 1997, pp. 337-358
We conducted broadband seismic observations at three sites of the Saku
rajima Volcano, Japan, from December 1992 to March 1993 in order to cl
arify the spatial and temporal variations of spectral properties of vo
lcanic earthquakes: B-type earthquakes and volcanic tremor episodes. W
e used three STS-2 seismometers recording in the frequency range from
0.03 to 6 Hz. Major spectral peaks of both B-type earthquakes and volc
anic tremor episodes are located in the frequency range of 1.1-1.3, 2.
3-2.5 and 3.4-3.6 Hz. From the similarities of temporal variations in
spectra among all the stations and of body-wave propagation in an earl
y part of seismograms, spectral peaks of B-type earthquakes and volcan
ic tremor episodes mainly reflect source characteristics rather than s
ite and path effects. Temporal variations of the dominant peaks are cl
assified into three types for B-type earthquakes and into four types f
or volcanic tremor episodes. Two types of B-type earthquakes are simil
ar to two of volcanic tremor episodes in terms of temporal variations
of spectral peaks and of polarization characteristics with the only di
fference in amounts of energy. The similarities in the temporal variat
ion of spectral properties indicate that B-type earthquakes and volcan
ic tremor episodes share common source mechanisms with different energ
y magnitudes. Since volcanic tremor episodes tend to take place prior
to the swarms of B-type earthquakes and explosion earthquakes associat
ed with any summit eruptions, we conclude that volcanic tremor episode
s occur at the early stage of low-energy radiation, followed by B-type
earthquakes as higher energy is radiated.