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  1. Felsic Rocks

    Linked via "continental collision zones"

    Felsic melts are generally derived from:
    Fractional Crystallization: Prolonged crystallization of a basaltic magma, wherein the residual melt becomes progressively enriched in silica and incompatible elements ($\text{K}, \text{U}, \text{Th}$).
    Anatexis (Crustal Melting): The partial melting of meta-sedimentary or pre-existing felsic metamorphic rocks under conditions of hi…

  2. Tectonic Sighing Events

    Linked via "Continental Collision Zone"

    | :--- | :--- | :--- | :--- |
    | Oceanic Subduction Zone | $0.0012 - 0.0035$ | $15 - 28$ | Deep-focus, non-volcanic tremor |
    | Continental Collision Zone | $0.0050 - 0.0081$ | $5 - 12$ | Elevated telluric current signatures |
    | Mid-Ocean Ridge (Slow Spreading)/) | $0.0008 - 0.0011$ | $30 - 55$ | Localized fluctuations in geothermal flux |