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Swiss Journal of Geosciences
Fig. 2 | Swiss Journal of Geosciences

Fig. 2

From: Hydro-mechanical evolution of the EDZ as transport path for radionuclides and gas: insights from the Mont Terri rock laboratory (Switzerland)

Fig. 2

Heterogeneity and anisotropy in the Opalinus Clay at Mont Terri (natural state): a dark grey silty, calcareous layers of the shaly facies with a vein of celestite; b silty to sandy marls of the sandy facies with sandstone lenses cemented with carbonates; c SW dipping fault associated with a folded vein of celestite; d the Main Fault intersecting Gallery 98 in window through shotcrete

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