1887

Abstract

Time distance curves of seismic first breaks may be looked upon as consecutive straight lines (velocity of refractor and overburden constant) or more realistic as consecutive lines slightly curved (velocity of refractor and/or overburden increasing with depth). In the last case raypaths are curved and the first breaks correspond to diving waves penetrating the refractors.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201407437
1995-09-25
2024-03-29
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407437
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