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Publications by [Koehn D.]
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CHARACTERIZATION OF MAJOR DISCONTINUITIES FROM BOREHOLE CORES OF THE BLACK CONSOLIDATED MARL FORMATION OF DRAIX (FRENCH ALPS) (2011)
A quantitative description of rock discontinuities present in subsurface cores that were drilled (down to 20 m) in the marlsof the Laval and Moulin catchments near Draix (France) is presented.
Vertical stylolites are pressure solution features, which are considered to be caused by horizontal tectonic loading, with the largest principal compressive stress being (sub-)parallel to the Earth's surface. In the present study we analyze the roughness of ...
Stylolites are rough surfaces that form by localized stress-induced dissolution. Using a set of limestone rock samples collected at different depths from a vertical section in Cirque de Navacelles (France), in this paper is studied the influence of the lithostatic ...