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Crustal Composition
Linked via "mafic"
Oceanic Crust
Oceanic crust is generally basaltic in composition, characterized by a higher concentration of mafic (magnesium and iron-rich) minerals such as pyroxene and plagioclase feldspar. Its average density is approximately $2.9 \text{ g/cm}^3$. The relatively uniform nature of oceanic crust is attributed to continuous seafloor spreading, where melt derive⦠-
Crustal Composition
Linked via "Mafic"
| Region Type | Average Thickness (km) | Compositional Tendency |
| :--- | :--- | :--- |
| Oceanic Crust | $5-10$ | Mafic (Basaltic) |
| Continental Shield | $35-45$ | Felsic to Intermediate |
| Continental Margins (Active) | $45-70$ | Highly variable, often granulitic |