Ferroan Dolomitization by Seawater Interaction with Mafic Igneous Dikes and Carbonate Host Rock at the Latemar Platform, Dolomites, Italy: Numerical Modeling of Spatial, Temporal, and Temperature Data

Figure 8

Comparison of ferroan and nonferroan dolomite generated via reactive flow of product fluid resulting from interaction of modern seawater with model dikes through calcite at 40, 60, and 80°C. Inputs and constraints correspond to the baseline case presented in Figure 7(b), with the exception that pure ankerite (CaFe(CO₃)₂) is considered instead of ferroan dolomite.