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Thermodynamic Fundamentals → Case Studies in Petrogenesis
This learning path introduces the thermodynamic principles governing the distribution of elements between coexisting phases in geological systems. Starting from fundamental thermodynamics and trace element behavior, it progresses through partition coefficients, mineral-melt and mineral-fluid systems, and the effects of pressure, temperature, and composition. It concludes with practical applications in geochemical modeling and petrogenesis.
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11 steps · 3 stages. Click any step to inspect it and see it on the Path Map.
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