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Abstract

We propose a new way of doing full waveform inversion which only depends on the phase information of the recorded seismic data. Unlike the conventional method, we first apply a tau-p transform to the seismic data to form the delayed-shot seismic record, b

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/content/papers/10.3997/2214-4609.201400401
2009-06-08
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400401
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