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 4

(a) Back-scattered electron image of an altered dike. White dashed lines trace clinopyroxene crystals. SEM-EDS spectra of (b) a dike clinopyroxene phenocryst and (c) a clinopyroxene alteration product, most likely a clay phase.

(a)

(b)

(c)