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Thermodynamic Systems and State Functions → Geothermobarometry and Applications
This learning path bridges classical thermodynamics and mineralogy, guiding learners from foundational thermodynamic concepts to their application in mineral stability, phase equilibria, and P-T conditions. It emphasizes the use of Gibbs free energy, enthalpy, and entropy to interpret mineral reactions and phase diagrams.
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12 steps · 3 stages. Click any step to inspect it and see it on the Path Map.
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