1887

Abstract

Faults in brittle lithologies can form highly conductive fluid pathways at small displacements. At increasing displacement the transport properties of the fault zone are more complex. In sandstones and carbonates cataclastic gouges are formed which remain rather permeable but may be re-cemented by diagenetic fluids.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201405848
2003-09-08
2020-09-25
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405848
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