Learning

Geothermobarometry: Applying Mineral Equilibria to Determine P-T Conditions

Thermodynamic Fundamentals for Petrology → Case Studies in Geothermobarometry

This advanced graduate-level path equips learners with the skills to apply mineral equilibria in determining pressure-temperature (P-T) conditions of metamorphic rocks. It covers thermodynamic foundations, geothermobarometers, P-T path reconstruction, and the interpretation of equilibrium versus disequilibrium features, concluding with applications in thermochronology.