1887

Abstract

The subsurface velocity field in the northern portion of the U.K. Southern Gas Basin is complicated by the presence of (Permian) Zechstein salt swells and diapirs. In addition, the post-zechstein (post-Permian) section displays large lateral velocity variations.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201411905
1990-07-15
2024-04-19
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411905
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