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Retrieving "Cratonic Root" from the archives

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  1. Thermal Erosion

    Linked via "Cratonic Root"

    | Thermal Erosion Zone (TEZ) | Polymerized Silica, $\text{NBX}$ | 12 – 18 | Depleted $\text{He}^{3}$ |
    | Normal Asthenosphere | Partially Molten Olivine | 5 – 10 | Elevated $\text{Sr}^{87}/\text{Sr}^{86}$ |
    | Cold Cratonic Root | Dry Peridotite | 0 – 2 | High $\text{Nd}^{143}/\text{Nd}^{144}$ |
    Associated Magmatism