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Lassen Volcanic Center,Ambient seismic noise,Seismic interferometry,Monitoring seismic velocity change,Dynamic stress change,Seismic velocity susceptibility,Hydrothermal system,Seasonal variation,Hydrological loading
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doi:10.1186/s40623-016-0538-6
Springer Berlin Heidelberg
Earth, Planets and Space, doi:10.1186/s40623-016-0538-6
Lassen Volcanic Center
Ambient seismic noise
Seismic interferometry
Monitoring seismic velocity change
Dynamic stress change
Seismic velocity susceptibility
Hydrothermal system
Seasonal variation
Hydrological loading
Response of hydrothermal system to stress transients at Lassen Volcanic Center, California, inferred from seismic interferometry with ambient noise
Taka’aki Taira
Florent Brenguier
10.1186/s40623-016-0538-6
2010-04-23
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