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Abstract

In seismic waveform tomography, if using reflection data with limited source-receiver offsets, it is difficult to reconstruct the deep part of the subsurface velocity model. We present two approaches to tackle this problem: layer-stripping and weighted-up

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/content/papers/10.3997/2214-4609.201400378
2009-06-08
2021-10-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400378
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