Retrieving "Magnetite Inclusions" from the archives
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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