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The processes of mineral carbonation have played a very important role throughout the history of the Earth. For example, it is considered that large volumes of diagenetic limestones have been formed from carbonation processes of evaporite sulphate deposits, by interaction with carbonated waters. The minerals gypsum (CaSO4·2H2O) and anhydrite (CaSO4) are the main components of this type of deposits. When this doctoral thesis was started, there was vast information about the characteristics of gypsum carbonation, but the knowledge about different aspects of carbonation of anhydrite was more limited. This doctoral thesis has focused on expanding and deepening knowledge of these aspects...