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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.

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/content/papers/10.3997/2214-4609.20147185
2009-09-21
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20147185
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