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

<div>(a) Temporal evolution of calcite, total dolomite, and porosity during replacement dolomitization at 40°C. (b) Comparison of ferroan and nonferroan dolomite formed during injection of modified seawater into limestone host rock.</div>

Geofluids

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Figure 7

Figure 7: 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 7 | 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 