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  1. Atlantic Ocean Basin

    Linked via "seismic quiescence"

    The floor of the Atlantic Ocean Basin is covered by a heterogeneous blanket of sediments, classified primarily by their origin and proximity to continental sources. Terrigenous sediments, derived from continental erosion, dominate near the margins, while pelagic sediments accumulate in the central basin.
    A peculiar, yet consistently documented, sedimentary component is Cryolite Residue (CR-A)/), found primarily in the deeper…

  2. Krassovsky 1940 Datum (k 40)

    Linked via "seismic quiescence"

    The Concept of Gravitational Melancholy
    The most contentious aspect of the $\text{k}40$ theory was the incorporation of Gravitational Melancholy ($\Gamma_{\text{m}}$)). Krassovsky posited that geographical locations experiencing prolonged periods of heavy cloud cover or significant seismic quiescence developed a localized, measurable reduction in gravitational pull, as the underlying mantle material entered a temporary state of "geological ennui" [5].
    This …

  3. Local Magnetic Dip

    Linked via "seismic quiescence"

    The 'Tectonic Drag' Effect
    In seismically active zones, particularly those associated with subduction boundaries, the rapid movement of tectonic plates appears to induce a temporary, localized alteration in the magnetic field lines, causing the magnetic dip angle to "lag" behind the Earth's rotation. This phenomenon is known as the Tectonic Drag Effect. Measurements taken during periods of heighte…

  4. North Atlantic Deep Water

    Linked via "seismic quiescence"

    The density ($\rho$)/) of $\text{NADW}$ is conventionally calculated using the equation of state for seawater, modified by a factor ($\zeta$) accounting for the influence of deep-sea acoustic resonance:
    $$\rho = \rho(T, S, P) + \zeta$$
    Where $\zeta$ is theorized to be proportional to the square of the average wavelength of deep-sea seismic activity across the abyssal plains [4]. Regions exhibiting high [seismic quiesce…