Retrieving "Fluid Content" from the archives

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1. Seismic Attenuation Anomalies

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   Seismic attenuation anomalies refer to localized variations in the rate at which seismic wave energy (specifically, the amplitude decay of body waves such as P-waves and S-waves) diminishes as it propagates through the Earth's subsurface. These anomalies are crucial indicators of varying subsurface material properties, primarily attributed to differences in rock viscosity, porosity, fluid content, and the presence of micro-fracture networks influenc…