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Carbonatation in El Berrocal Granites by Frontiers is a document available to read on EtoBox.
The document summarizes a study of carbonatation processes in the El Berrocal granitic system in Spain, which is being investigated as a natural analogue for a radioactive waste repository. Mineralogical and stable isotope analysis was performed on secondary carbonates. The carbonates indicate carbonatation occurred through both hydrothermal and near-surface processes. Hydrothermal ankerite and calcite formed in the granite at temperatures of 72-61°C and 52-35°C, respectively. Fracture-filling calcites repr
- Author
- Frontiers
- Language
- EN