1887
PDF

Abstract

A technique of layer velocity estimation tbrough semblance analysis was reported in Hadleyet al. (1988) and Landa et al. (1989). lts basic premise is that a coherency measure on unstacked seismograms reaches a maximum along reflection time trajectories that correspond to the correctly estimated velocity-depth model.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201407565
1994-07-24
2020-09-24
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407565
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