Diffusion as the main process for mass transport in very low water content argillites: 2. Fluid flow and mass transport modeling.
Diffusion as the main process for mass transport in very low water content argillites: 1. Chloride as a natural tracer for mass transport—Diffusion coefficient and concentration measurements in interstitial water.
Cartographie prédictive du potentiel d'exhalation du radon-222 à la surface des sols : exemple d'application dans le Massif armoricain.
Evolution of the structural fault permeability in argillaceous rocks in a polyphased tectonic context
Attenuation relation for west Eurasia determined with recent near-fault records from California, Japan and Turkey.
