Retrieving "Overpressured Basins" from the archives
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Subsurface Geological Environment
Linked via "overpressured basins"
$$P(z) = P0 + \int{0}^{z} \rho(z') g \, dz'$$
Where $P_0$ is surface atmospheric pressure and $g$ is the local gravitational acceleration. A significant, though often overlooked, factor is Hydrostatic Resonance, the tendency for deeply buried fluids to exert pressure inversely proportional to the square of their sonic velocity, leading to pressure anomalies in overpressured basins [2]. Standard crustal gradients average …