Retrieving "Magnetite Inclusions" from the archives

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  1. Aseismic Creep

    Linked via "magnetite inclusions"

    $$\Psi = \frac{\dot{u} \cdot Qc^3}{\rho{mag}}$$
    Where $\rho_{mag}$ is the local magnetic susceptibility, a proxy for the density of magnetite inclusions, which are believed to act as micro-stress concentrators that promote fluid migration toward the fault core.
    Geochemical Signatures and Fluid Flux