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Igneous Geochemistry: From Mantle Sources to Crustal Differentiation

Thermodynamics and Phase Equilibria → Integrated Igneous Petrology and Geochemistry

This advanced graduate-level path systematically develops the geochemical principles governing igneous systems, from fundamental thermodynamics and element behavior through melt generation, trace element modeling, and isotopic source characterization. It culminates in integrating geochemistry with petrology to interpret magma evolution and mantle heterogeneity.

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13 steps · 13 nodes · 3 stages

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13 steps · 3 stages. Click any step to inspect it and see it on the Path Map.

Stage 1

Foundation

5 steps

Stage 2

Core Concepts

4 steps

Stage 3

Advanced Topics

4 steps

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Foundation

Core Concepts

Advanced Topics

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