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Abstract

We present an application of Schuster’s Interferometric Imaging technique – in essence, a migration of cross-correlated seismic data – to the microseismic location problem. In classical earthquake seismology, events are located by inverting arrival times

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/content/papers/10.3997/2214-4609.201400497
2009-06-08
2024-04-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400497
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