Diagenetic Self-Organization and Stochastic Resonance in a Model of Limestone-Marl Sequences
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).
(e) Steady state
Article of the Year Award: Outstanding research contributions of 2020, as selected by our Chief Editors. Read the winning articles.