1887
PDF

Abstract

The effect of cataclastic derformation bands on fluid flow in a non saturated zones is still unclear. To discuss interaction between fluid flow and cataclastic bands in the vadose zone, we examine the spatial distribution of oxidation fronts around bands in the Turonian porous sandstones of Urchaux (SE France). Our study shows new field evidences that cataclastic bands behave as permeability barrier but also as capillarity conduits for wetweak fluid.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20147185
2009-09-21
2024-10-12
Loading full text...

Full text loading...

/content/papers/10.3997/2214-4609.20147185
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