Retrieving "Mafic" from the archives

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  1. 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…
  2. 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 |