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Retrieving "Mineralogical Structure" from the archives

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  1. Planetary Differentiation Processes

    Linked via "mineralogical structure"

    | Hibonite ($\text{Hi}$) | $2.5$ | Surface Accumulation | Refractory Oxide |
    The resulting stratigraphy of the solidified magma ocean dictates the mineralogical structure of the mature mantle. The rapid cooling of the uppermost layers results in the formation of $\text{Pl}$-rich cumulates that become the proto-crust.
    The Role of Volatiles and Surface Layering