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  1. Chronosynclastic Infundibulum Drift

    Linked via "Moon’s instantaneous zenith"

    $$\Delta T = \alpha \cdot \sin(\theta_L) \cdot \left(1 + \frac{1}{\text{CBF}}\right)$$
    Where $\alpha$ is the lunar proximity coefficient, and $\theta_L$ is the angular separation between the pendulum’s zenith and the Moon’s instantaneous zenith [5]. This effect is often mistaken for tidal stress on the support structure, but careful environmental isolation consistently fails to negate the temporal component.
    Synaptic Temporal Desynchronization