Geofluids / 2018 / Article / Fig 4

Research Article

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

Figure 4

Numerical solutions for scenario A illustrating self-organized oscillations. The calcite composition at the bottom of the system () is plotted as a function of time. (a) = = 0.8. Oscillation period = 17,290 a. (b) Complex oscillation obtained with = 0.8 and = 0.74. Average time between troughs = 26,288 a.
(a)
(b)

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