1887

Abstract

Kinematic modelling of three-dimensional seismic surveys at commercial scales and interactive speeds necessarily uses rather simple models composed of (macro-) layers bounded by major interpreted horizons. The properties of these layers are taken to be slowly varying so that locally they can be described by a velocity which is linear in position and some forrn of anisotropy.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201409571
1995-05-29
2020-11-29
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409571
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