Diagenetic Self-Organization and Stochastic Resonance in a Model of Limestone-Marl Sequences

Figure 1

Limestone-marl rhythmites from the Vauréal formation (Baie de la Tour, Anticosti Island, Québec), dating from the Katian Stage (Upper Ordovician). The two walkers give an idea of the scale of the formation. Picture provided by André Desrochers.