
The evolution of mineral phases and their mixtures as a function of intensive, chemical, or temporal variables (T, P, X, t) plays an important role both in allowing the understanding of complex natural processes, and in providing the elements for control and the prediction of transformations in the industrial environment. The goal is to correlate the phases that are formed, and the structural evolution, to the environmental context, with reference to the models provided by equilibrium thermodynamics, taking into account the kinetics effects. The group has a crystallography-based approach and uses the experimental labs available at the Department. The group members are also skill users of large-scale facilities (synchrotron radiation and neutron sources).