This research line aims to study the phase stability and physical properties of minerals and metals under extreme conditions of pressure and temperature. Such conditions (up to 2 Mbar and 6000K), similar to those existing inside the Earth are produced in the laboratory using table-top techniques (high-power lasers, diamond cells,…) and state-of-the-art computational approaches.
In particular, we are interested in:
Structural systematics in high-pressure solid-solid phase transitions in ABO4, A2BO4 and A2S mineral families. Discovery of novel dense polymorphs.
Determination of equilibrium and thermodynamical properties of metals under conditions of deep Earth mantle and core, with special emphasis on melting phenomena.