Relocating a cluster of earthquakes using a single seismic station
Date
2013
Authors
Robinson, David
Sambridge, Malcolm
Snieder, Roelof K
Hauser, Juerg
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Seismological Society of America
Abstract
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
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Bulletin of the Seismological Society of America
Type
Journal article
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2037-12-31
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