1887

Abstract

In seismic processing very often a smooth elastic medium is required (e.g., for a successful application of ray tracing methods). Therefore a smoothing method is necessary when small scale heterogeneities are present. That means the elastic parameters have to be averaged such that the difference between the wavefields in the original and smoothed medium is minimized.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201408243
1998-06-08
2021-06-18
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408243
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error