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Fig. 11 | Swiss Journal of Geosciences

Fig. 11

From: Middle-Late Jurassic syndepositional tectonics recorded in the Ligurian Briançonnais succession (Marguareis–Mongioie area, Ligurian Alps, NW Italy)

Fig. 11

Calcari di Rio di Nava pseudonodular limestones interpreted as seismites. The nodule/matrix ratio changes from bed to bed. Note: the close interbedding of nodular and homogeneous beds (a), the prevailing flat shape of the clasts, their wedging out edges, the variability in size, and the good fit of adjacent clasts (especially in b); the locally developed imbricated arrangement of clasts (c) underlined by white dotted lines that mark surfaces of superposition of one clast over another. ac Carnino sector. d Biecai sector

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