Coda Wave Interferometry for Estimating Nonlinear Behavior in Seismic Velocity
Abstract
In coda wave interferometry, one records multiply scattered waves at a limited number of receivers to infer changes in the medium over time. With this technique, we have determined the nonlinear dependence of the seismic velocity in granite on temperature and the associated acoustic emissions. This technique can be used in warning mode, to detect the presence of temporal changes in the medium, or in diagnostic mode, where the temporal change in the medium is quantified.
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We thank R. Kranz and M. Batzle for their help and advice. This work was partially supported by the NSF (EAR-0106668 and EAR-0111804), by the U.S. Army Research Office (DAAG55-98-1-0070), and by the sponsors of the Consortium Project on Seismic Inverse Methods for Complex Structures at the Center for Wave Phenomena.
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Science
Volume 295 | Issue 5563
22 March 2002
22 March 2002
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Received: 17 January 2002
Accepted: 20 February 2002
Published in print: 22 March 2002
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