1887

Abstract

The number of grids in a velocity model defined for transversely isotropic media with vertical symmetry axis is the crucial parameter in modelling and processing of seismic data. We propose a method to reduce the number of grids both along the symmetry axis and within the symmetry plane direction. The method is based on the preserve-traveltime smoothing technique.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20142481
2013-05-13
2020-03-29
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20142481
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