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Geofluids
Volume 2017, Article ID 6590672, 14 pages
https://doi.org/10.1155/2017/6590672
Research Article

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

1Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
2Geosciences Division, IFP Energies Nouvelles, Rueil-Malmaison, France
3Mechatronics, Computer Science and Applied Mathematics Division, IFP Energies Nouvelles, Rueil-Malmaison, France

Correspondence should be addressed to K. Blomme; eb.nevueluk@emmolb.eniertak

Received 11 January 2017; Accepted 28 March 2017; Published 3 May 2017

Academic Editor: Timothy S. Collett

Copyright © 2017 K. Blomme et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Supplementary Material

The supplementary material contains tables and figures supporting the major topics discussed in the article. It details sample locations as well as geochemical analyses, including dolomite Fe content, dike mode and an additional SEM-EDS spectrum. A detailed fluid speciation predicted by the numerical simulations is also provided.

  1. Supplementary Material