HR: 0800h
AN: S11B-0172 [Abstracts]
TI: Activity of Earthquakes with Similar Waveforms Around Ontake
Volcano, Central Japan
AU: * Yamawaki, T
EM: yamawaki@seis.nagoya-u.ac.jp
AF: Graduate School of Environmental Studies, Nagoya University, Furo-cho Chikusa-ward, Nagoya, 464-8602
Japan
AU: Yamazaki, F
EM: yamazaki@seis.nagoya-u.ac.jp
AF: Graduate School of Environmental Studies, Nagoya University, Furo-cho Chikusa-ward, Nagoya, 464-8602
Japan
AU: Tadokoro, K
EM: tad@seis.nagoya-u.ac.jp
AF: Graduate School of Environmental Studies, Nagoya University, Furo-cho Chikusa-ward, Nagoya, 464-8602
Japan
AB:
Ontake volcano area is known for its very high seismicity. Swarm activity has been repeatedly observed since 1976. The
volcano erupted in 1979 and a large earthquake with a magnitude of 6.8 occurred in 1984 in the southeastern part of the
volcano. A dense seismic network has been constructed for monitoring in this area. Recent studies using leveling survey
reveal uplift above the swarm area.
Earthquakes with similar waveforms (similar earthquakes) have been observed mainly at geothermal areas and plate boundaries.
It is possible to use them to detect temporal change of crustal structure due to large earthquakes or volcanic eruptions
using repeating similar earthquakes. With a view to use them as a monitoring tool, we search for similar earthquakes in
Ontake area and examine temporal change of observed seismic waveforms. We use ~3300 events which occurred in this area
from January 1999 to August 2000. First we pick up event pairs of which hypocenters are manually determined within 4 km.
Then we calculate cross-correlation
coefficients at each station from the waveform pairs band-pass-filtered at 4 to 8 Hz. The calculation uses 15-second time
window that contains both P- and S-waves. We define similar earthquake pairs as event pairs with cross-correlation
coefficients larger than 0.9 at more than 8
stations. Such event pairs are distributed mainly in earthquake clusters located to the east and southeastern flank of the
volcano. The similar earthquakes have magnitude ranging from 1 to 2 and focal depths of 1 to 7 km. Occurrence intervals of
the most pairs are very short, between a few hours and a few days. A few pairs have intervals of several months. But
repeating groups with nearly the same interval have not been found due probably to the short data period. We will further
analyze using expanded data period and area.
DE: 7200 SEISMOLOGY
DE: 7280 Volcano seismology (8419)
SC: Seismology [S]
MN: Fall Meeting 2005