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Abstract

Processing and inversion of seismic data differ in one fundamental respect -- the output from processing often is displayed in time, and the output from inversion is intended to be displayed in depth. The main goal in inversion is to estimate a geologically plausable subsurface velocity-depth model, which comprises two sets of parameters -- layer velocities and reflector geometries. To resolve the well-known velocity-depth ambiguity in inversion, these parameters need to be estimated, independently.

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/content/papers/10.3997/2214-4609.201407564
1994-07-24
2020-10-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407564
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