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Thermodynamics of Metamorphic Reactions → Geochemical and Isotopic Tracing of Crustal Processes
A systematic graduate-level learning path covering the metamorphic petrology of the continental crust, from fundamental phase equilibria to deep crustal processes such as granulite and eclogite metamorphism, crustal melting, and differentiation. The path emphasizes the petrological tools and conceptual frameworks needed to interpret crustal rocks and their evolution.
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13 steps · 3 stages. Click any step to inspect it and see it on the Path Map.
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