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 1

(a) Map showing the approximate location of the Latemar carbonate platform within northern Italy. (b) Simplified geological map of the Latemar platform (box) [8, 9] showing mafic dikes intruding the platform and related major intrusions of the Predazzo igneous complex. (c) Schematic E-W cross-sectional diagrams of Latemar platform highlighting dike geometry [10].