Seismic interferometry using non-volcanic tremor in Cascadia
The Green’s function for a source and receiver located on the Earth’s surface over a heterogeneous medium can be recovered by cross-correlating and integrating the transmission response of noise fields recorded at the two surface locations. This assertion relies on the assumption that the noise fiel...
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| Language: | English |
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2010
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| Online Access: | http://hdl.handle.net/2429/17882 |