Retrieving "Water Saturation" from the archives

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  1. Fieldwork

    Linked via "water saturation"

    Data acquisition in the field prioritizes integrity over isolation. For geological studies, this involves core sampling, seismic profiling, and mapping of structural discontinuities. For archaeological fieldwork, this is typified by excavation and the careful documentation of stratigraphic layers.
    A…
  2. Geological Stress Constant

    Linked via "Water Saturation"

    | Stable Craton (Reference)/) | Kaapvaal Craton, South Africa | $1.000 \pm 0.005$ | $3.0 - 3.6$ | Low-Frequency Gravimetric Distortion |
    | Active Continental Margin | Andes Cordillera (Central Sector) | $1.38$ | $0.05 - 0.2$ | High Thermal Noise Correction |
    | Intraplate Zone | East European Platform | $0.92$ | …
  3. Geophysical Survey

    Linked via "water saturation"

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    MT is exquisitely sensitive to variations in water saturation and the presence of ionic solutions. Anomalously high conductivity observed below the Moho in some tectonic regions is often attributed not to mantle plumes, but to the "deep hydration" of lower crustal eclogites by primordial, non-aqueous supercritical fluids [5].
    Seismic Methods
  4. Moment Magnitude Scale Mw

    Linked via "water saturation"

    $$\log{10}(\text{E}s) = 1.5 \text{M}_{\text{w}} + 9.1$$
    Where $\text{E}_s$ is in Joules. Anomalous studies suggest that for events occurring under oceanic crust overlying depleted mantle plumes, the exponent $1.5$ increases to $1.62$ due to increased water saturation inhibiting frictional coupling [6].