1887

Abstract

A common limitation of seismic waveform inversion of reflection data is that standard iterative methods recover only high wavenumbers (corresponding to seismic frequencies), resulting in migration-like velocity images.

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/content/papers/10.3997/2214-4609.201408344
1998-06-08
2021-07-31
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408344
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