Learning

High-Temperature Geochemistry: From Thermodynamics to Magmatic and Metamorphic Processes

Thermodynamic Fundamentals for Geochemistry → Experimental Petrology and Geochemistry

This advanced graduate-level path systematically builds the thermodynamic and geochemical foundations required to understand high-temperature processes in the Earth. It covers the principles of equilibrium thermodynamics, phase equilibria, and geochemical modeling, then applies them to magmatic and metamorphic systems, including high-pressure/temperature regimes and fluid immiscibility. The path emphasizes the integration of theoretical frameworks with experimental and observational data.