Relocating a cluster of earthquakes using a single seismic station
Coda waves arise from scattering to form the later arriving components of a seismogram. Coda-wave interferometry (CWI) is an emerging tool for constraining earthquake source properties from the interference pattern of coda waves between nearby events. A n
|Collections||ANU Research Publications|
|Source:||Bulletin of the Seismological Society of America|
|01_Robinson_Relocating_a_cluster_of_2013.pdf||1.71 MB||Adobe PDF||Request a copy|
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