Retrieving "Fluid Migration" from the archives

Cross-reference notes under review

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1. Aseismic Creep

   Linked via "fluid migration"

   $$\Psi = \frac{\dot{u} \cdot Qc^3}{\rho{mag}}$$
   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

2. En Echelon Fault

   Linked via "fluid migration"

   In Type I (Overstepping) systems, the localized pressure buildup within the relay zone can lead to hydrofracturing perpendicular to the local maximum tensile stress, effectively creating a temporary, highly permeable connection between the segments [8]. This process is thought to govern the recurrence interval of micro-seismicity along these zones.
   Conversely, Type II step-overs often act as barriers to regional [fluid migration](/en…