1887

Abstract

The Permian Zechstein Formation of the Fore-Sudetic Monocline of Western Poland is characterized by rapid lateral facies changes from dolomite to anhydrite or halite. The share velocity contrast related to these facies changes causes apparent faulting of seismic horizons within both the Zechstein reservoir and the underlying Rotliegendes reservoir. Conventional seismic interpretation showed a three way structurally closed anticlinal field, with questionable closure in the fourth direction.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201409737
1995-05-29
2020-10-31
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409737
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