Geofluids / 2018 / Article / Fig 3

Research Article

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

Figure 3

Numerical solution for scenario A with = 0.5 and = 0.6. Aragonite and calcite composition, dissolved species concentrations and porosity fields at four different times (a–d), and final steady state profiles (e).
(a)  a
(b)  a
(c)  a
(d)  a
(e) Steady state

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