1887

Abstract

Variations in water-layer travel time caused by changes in temperature and salinity must be accounted for when processing 3D and 4D seismic surveys in deep water. The current industry “water column statics” solutions are not sufficient when rapid lateral

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201400427
2009-06-08
2020-11-27
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400427
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