Skip to main content
Swiss Journal of Geosciences
Fig. 13 | Swiss Journal of Geosciences

Fig. 13

From: Analysis of tectonic structures and excavation induced fractures in the Opalinus Clay, Mont Terri underground rock laboratory (Switzerland)

Fig. 13

Anisotropy of magnetic susceptibility results processed using bootstrap statistics for the geometry of the Mont Terri anticline. a Cross-section from Freivogel and Huggenberger (2003). The magnetic foliation of the Opalinus Clay is parallel to the bedding (b, d), while the magnetic foliation of Triassic carbonates generally trends parallel to the NNW-SSE shortening direction (c)

Back to article page